H0002	Version 	3															
H0003	Date_generated	22/8/2008															
H0004	Reporting_period_end_date	22/8/2008															
H0005	State	TAS															
H0100	Tenement	EL21/2005															
H0101	Tenement_holder	Venture Minerals Ltd															
H0102	Project_name	Mt Lindsay															
H0106	Tenement_operator	Venture Minerals Ltd															
H0150	250K_map_sheet	SK5503 Burnie															
H0151	100K_map_sheet	7914 Pieman															
H0152	50K_map_sheet	na															
H0153	25K_map_sheet	"3437 Stringer, 3438 Livingstone, 3637 Rosebury, 3638 Parsons, 3639 Ramsay"															
H0200	Start_date_of_data_acquisition	22/8/2007															
H0201	End_date_of_data_acquisition	22/8/2008															
H0202	Data_format	SG3 															
H0203	Number_of_data_records	982															
H0204	Date_of_metadata_update	22/8/2008															
H0500	Feature_Located	Rock Unit Interval															
H0501	Geodetic_datum	not applicable															
H0502	Vertical_datum	not applicable															
H0503	Projection	not applicable															
H0531	Projection_zone	not applicable															
H0900	Remarks: 																
D	Hole	From	To	Recovery	Colour	Weathering	Lith1	Lith2	Lith3	Vein	Vein	Alteration	Magnetite	Sulfide	Texture	Description	Comments
D		metres 	metres 	%							%		%	%			
D	LV001	0	4.8	na	dgn gy bn	mox	SAND			qz	2		0	0		"20cm plant roots at top of hole passing into qtz rich fine sandston, float?"	
D	LV001	4.8	43.6	na	dgy wt bk	mox	FG				0		0	0		"small 5cm piece of FGRA core rich in tu, possibly part of a VQT. Recovered core consists of a coarse qtz rich (granite) sand. Bk flecks of tu throughout. At 22.9m a 5cm block of tu sits in dgy/wt granite sand. "	
D	LV001	43.6	52.9	na	dgn wt gy	mox	FG				0	cl	0	0		blocky/rubbly weathered qtz rich granite. Granite is a dgn colour where alteration to cl is taking place. 3m loss between 46.9 to 49.9m before intercepting FGRA again ~15cm between 49.9 - 52.9m	
D	LV001	52.9	73.9	na	na	mox	NREC				0		0	0		lost - no recovery	
D	LV001	73.9	92.7	na	gy wt bk 	mox	FG				1		0	0		"10cm of tu-qtz rock possibly from a VQT in the FGRA, before passing into semi-cohesive granite regolith. Lost between 75.8 - 91.9m, back into granite regolith from 91.9 - ~92.7m. "	
D	LV001	92.7	190.7	na	dbn yw	mox	RGOS				0	he mt lm	15	0		"dbn/yw ferruginsed/oxidised rock. Yw limonitic staining pervasive. Core is vuggy and contains oxidised straited rossestte faces which look like replaced actinolite? Hematite common throughout, present as tabular flecks on surface which look micaceous and "	
D	LV001	190.7	202.7	na	dgy gn wt	wox	FG			qz cl	5	cl he	0	0		"dkgy/gn/wt rubbly qtz rich rock with VQ and vugs in some veins, horizons of small qtz phenocrysts in soft wt feldspar matrix suggesting granitic origin?. Mostly core consists of qtz dominant rock with large amounts of cl, 30cm horizon of dkgn cl-qtz-mica "	
D	LV001	202.7	216.6	na	cm gn	wox	qSS				0	cl he	0	0		"Rubbly core, largely comprised of siliceous material. Intact blocks contain irregular cavities, some after veins. Variable hematite staining. Chlorite rich incohesive material occurs."	
D	LV001	216.6	230.5	na	wt	fr	qSS			ca	30		0	0		Altered calcareous SSDT? (carbonate cemented qz-arenite?). Alteration controlled by pervasive network of carbonate veins. Unidentified gy coloured mineral disseminated about veins. 	
D	LV001	230.5	232.15	na	wt	fr	FG				0	tu cc	0	0		"Altered FGRA. Tu? disseminated and occasional irregular clusters up to 1cm long. Irregular patches of unidentified viterous hard green mineral, patches appear ""stretched"", possible growth habit? Secondary cc.  "	
D	LV001	232.15	233.4	na	gn	fr	FG			tu	1	ep tu po mt	2	1		Altered FGRA by pervasive epidotization. Tu? disseminated and as veinlets. Anhedral porphyroblasts of qz+cc. Original mineralogy no longer observable.   	
D	LV001	233.4	243.7	na	bk	fr	FG			tu	1	tu po ep mt	5	1		"Bk altered FGRA?, colour imparted by fine grained tu? prevasively disseminated throughout matrix. Dark  material moderately magnetic, some magnetite present. Po and ep also occur disseminated in matrix. Distinctive large, very irregularly shaped patches o"	
D	LV001	243.7	244.7	na	wt	fr	FG				0	tu	0	0		Ifg FGRA with tu alteration. 	EOH 244.7
D	ML065	0	11	90	dgy og	wox	SS	ST			0		0	0		SGWK with minor beds of SSLT - weathered surface rock	
D	ML065	11	61.9	90	dgy	fr	SS	ST		qz cl	1	cl si sx 	5	1		"Ms SGWK interbedded SSLT. Minor graded beds. Alteration in rare veins and blebs mainly in coarser beds (blebs mostly cl), fractured near fault zone"	
D	ML065	61.9	66.4	80	lgy bk gn	fr	XFBC	ST		qz cl	1	cl	2	2		cohesive fault breccia with bk gn cl matrix and silicified SSLT clasts. Minor cc filling fractures. Zones (<0.5m) of fractured SSLT between breccia. From 66.2 - 66.4m breccia zone becomes more silicified.	
D	ML065	66.4	74.5	80	bn lgy dgy	fr	STUF			qz cl	2	si cl po	0	1		"silicified SSLT and SGWK with VQL, po commonly occurs in VQL. Gradational change into ZSKCS containing minor mt. "	
D	ML065	74.5	106.4	95	dgy lgy gn	fr	ZSKCS	STUF		sx	2	si cl mt am vs po	20	5		"ZSKCS with STUF near top of unit, grades into ZSKCS. ZSKCS contains ds mt and appears considerably silicified. Thin veinlets of po and cc. Varying concentrations of mt, in places >40% zones <0.5m."	
D	ML065	106.4	117.8	90	gn bk dgy	fr	ZSKM			cl ca sx	2	mt cl am po	50	2		ZSKM with ds po and thin cl and cc veins. Mt occurs as patches and zones in carbonate rock. ZSKM is moderately fractured.	
D	ML065	117.8	118.6	100	bn gn gy	fr	ZSKCS			qz sx ca	10	am po mt	2	5		ZSKCS with a large 4cm wide VQCX running near parallel to core axis. Ds po throughout.	
D	ML065	118.6	119	100	wt gy	fr	XFBC			qz ca	60	si cl cc py po mt	2	5		"cohesive breccia with angular ZSKCS clasts in a qz rich matrix, containing also cc and X (of which py is dominant with some po)"	
D	ML065	119	120	100	gy bn	fr	ZSKCS			qz ca	1	mt am vs po	30	5		ZSKCS with high% of mt and vs with ds po 	
D	ML065	120	120.1	100	wt gy	fr	XFBC			qz	50	vs am mt cc	10	0		"10cm brecciated zone, ZSKCS clasts rich in vs and mt in a qz cc rich matrix."	
D	ML065	120.1	127.8	100	dgy bn gn	fr	ZSKCS	ZSKM		qz cl ca	10	cl am mt vs po cpy	10	5		0.8m of ZSKCS followed by 0.8m of ZSKM which then grades into a mt vs rich ZSKCS	
D	ML065	127.8	130.4	90	gy bn gn	fr	STUF			cl qz sx	5	si cl po bt 	0	5		"silicified SGWK and SSLT with VL, VQL and thin veins of VX (mostly po) and ds po. Bn pl colouration possibly due to bt in the system"	
D	ML065	130.4	131.5	80	gn bk 	fr	XFBI	XFBC	ST		0	cl	0	0		small (~10cm) cohesive brecciated zone passing into 0.5m of incohesive breccia with soft cl matrix and cl altered SSLT clasts. Highly fractured core persists around fault breccia from 131.5 - ~134.7m	
D	ML065	131.5	136.4	50	gy gn	fr	ST	SS		ca cl	10	cl cc	0	0		highly fractured silicified SSLT with minor cc veins and weathered cl veins 	
D	ML065	136.4	136.5	100	wt gy	fr	XFBC				0	cl si	0	0		cohesive silicified fault breccia with bk gn cl matrix and STUF angular to subrounded clasts.	
D	ML065	136.5	136.8	100	wt bk gn	fr	FG	ST		qz cl	5	cl	0	0		"small, fine qz, feld, bt rich granite dyke contacting SSLT and XBC uphole."	
D	ML065	136.8	145.1	100	dgy dgn	fr	ST	SS		qz cl	2	cl si	0	0		dominantly SSLT with SGWK beds and minor STUF alteration. Small thin qz veinlets with pk possibly stilbite or FGRA dyke with a similar compostion to above FGRA	
D	ML065	145.1	145.3	100	pk gy	fr	FG			qz tu	2		0	0		"fine pk qz and feldspar rich FGRA also rich in bt and/or tourmaline, appears slightly brecciated at downhole margin with SSLT."	
D	ML065	145.3	148.4	90	dgy gn	fr	ST	SS		qz cl	1	cl po	0	0		"dominantly SSLT with minor VQ and VQL, fractured core near granite contact downhole."	
D	ML065	148.4	150.6	100	pk wt gy	fr	FG			qz tu	10		0	0		"pk qz and k-spar rich granite, rich in bt and tourmaline. Veins of qz tourm common."	
D	ML065	150.6	152.4	100	dgy	fr	ST			qz cl	1	cl	0	0		SSLT with minor veinlets of qz and VQL. Qz filling small discontinous fractures.	
D	ML065	152.4	159.5	100	pk gy 	fr	FG	ST	lSS	qz tu	2		0	0		dominantly pk qz and k-feldspar rich granite with <1m intervals of SSLT/SGWK. FGRA contains patches of bt/tourm. Some feldspars appear to be altered to sericite? (minor alteration)	
D	ML065	159.5	166.8	100	dgy	fr	ST	SS		qz cl	2	cl	0	0		"interbedded SSLT and SGWK with VL and minor VQ, small 1cm wide pk FGRA dyke at 163.1m "	EOH 166.8m
D	ML066	0	11.9	70	lgy dgy	wox	ST	SS		qz cl	5	si mt	2	0		"broken and kaolanised weakly weathered siltstone and greywacke, bn/og limonitic staining throughout qtz veins up to 1.5cm wide"	
D	ML066	11.9	38.7	100	dgy gn bk	fr	SS	ST		qz cl sx	1	cl mt po cpy py	2	1		"fine grained SGWK to very fine sanstone with beds of SSLT. Alteration zones and veins of chlorite and qz with sulphides (po, cpy and py) disseminated in them. At 29m there is a small 25cm highy qz veined zone appearing brecciated by networking qz veins. f"	
D	ML066	38.7	50.2	70	dgy bk gn	fr	XFBI	SS	ST	qz cl	1		0	0	fz	"fracture zone, rubbly broken core with chlorite on fracture faces with very minor sulphides"	
D	ML066	50.2	54	50	bn dgy gn	fr	XFBI	ST	lSS	qz cl sx	1		0	1	fz	"brecciated and fractured siltstone and greywacke, fault breccia is not silicified so later stage fault, some disseminated sulphides (<1%) of mainly po"	
D	ML066	54	57.9	80	dgy bk gn	fr	XFBI	SS	ST		2	si cl	0	1	fz	"fractured and rubbly core, 56.9m undulating bedding contact between SGWK and SSLT"	
D	ML066	57.9	61.9	90	dgy bn gn	fr	XFBI	ST			1	cl ka	0	0	fz	"angular to subrounded brecciated clasts of siltstone country rock in fine SSLT altered in zones to soft clay, small amounts of discontinuous qz veins"	
D	ML066	61.9	98.5	100	lbn lgn	fr	SM	SS	ST	qz ca	15	cl py po	0	5		"fine gn ltgy mudstone intensely veined in parts with chlorite alteration veins and beds. Sulphide (mainly py) disseminated through cl veins and in beds of mudstone. Interbedded greywacke, beds vary in size from 2cm +. At 77.7m there is a 1.5cm wt gn carbo"	SMDT from 61.9 - 69m then becomes coarser with bedded SSLT and SGWK.
D	ML066	98.5	100.5	100	wt lgy yw	fr	FG			qz tu	2	ep	0	1		"acidic granite, made up of >80% qtz and feldspar. Small felcks of bt and veins of tourmaline. Gn ep alteration throughout granite ?sill?"	
D	ML066	100.5	103.7	100	dgy bk gn	fr	ST	SS		qz cl sx	1		0	1		siltstone beds underlain by greywacke ~30cm from granite contact	
D	ML066	103.7	104.5	100	pk wt gy b	fr	FG			qz tu	1	ep	0	0		"wt pk gy acidic granite with black flecks of bt and tourmaline, gn ep alteration"	
D	ML066	104.5	136.7	95	dgy gn bn	fr	SS	ST		qz ca cl sx	5		0	0		"greywacke beds and interbedded siltstone, greywacke beds have often got a bn colour and visible qtz grains. Extensive VLQC between 109.2 - 109.5m depth in siltstone. Between 131.0 and 132.3m there is disseminated sulphide occupying ~50% of a carbonate vei"	
D	ML066	136.7	141	70	dgy bk gn	fr	ST				0		0	0		fracture zone in siltstone mostly cohesive rock	
D	ML066	141	141.8	70	na	na	XFBI	ST		FG	0		0	0		"Weak brecciated siltstone 141.7 - 141.8, rubbly and broken fragments, pk fragments of k-spar and qtz rich granite dyke at ~141m depth with flecks of bk bt and very minor specs of py"	
D	ML066	141.8	145.6	70	na	na	ST				0		0	0		fracture zone in siltstone mostly cohesive rock	
D	ML066	145.6	155.2	95	dgy gn wt	fr	SS	ST		ca cl	20	ep sb	0	0		greywacke to medium sandstone beds and finer siltstone beds with pk veins of stilbite and wt veins of carbonate. Lt gn veins of ep nearer end of hole	EOH 155.2
D	ML067	0	23.5	70	dgy	wox	SS	ST		qz cl	5	qz cl py	0	0		"sfg-smg dkgy SGWK beds, interbedded with SSLT. Poorly differentiated bedding, og fe-oxide weathering, rocks very fractured and rubbly, ka alteration minor, network cl + qtz veins mm-scale and individual veins up to 10mm width, v.minor ds X (py), bedding ~"	Start of NQ -23.5m
D	ML067	23.5	96.7	95	dgy	fr	SS	ST		qz cl	5	cl qz bt sb cpy py ab	0	1		interbedded sfg-smg dkgy SGWK and SSLT. Patchy weak to non magnetic. Patches of network cl + qtz veining throughout (mm-scale). Feldspar (albite?) occurs in some veins with chlorite instead of qtz. Weak silicification around qtz-cl network veins. Wt to tr	
D	ML067	96.7	97.3	95	dgy	fr	XFBI	SS		qz cl	20		0	0		"semi-consolidated sfg SGWK XBRC, cl and qtz veins, possible minor ifg arsenopyrite/stannite/cassiterite?"	
D	ML067	97.3	132	98	dgy	fr	SS	ST			1	cl qz cpy po py bt cc ab	0	1		"fractured wall rock below XBRC down to ~102.6m. Common fg secondary cl in SGWK and SSLT beds from 103-107.3m. 111.5m S0 - grading downhole. 131-132m - cl + qtz altered zone with minor cpy, py + po. 131.7m vein of cc, po, cpy, minor tour and a black lustre"	
D	ML067	132	236.6	95	dgy	fr	ST	SS			1	qz cl cpy sb ep	1	0		"more dominantly SSLT beds, weakly to moderately magnetic. 167m S0 up hole apex is truncated by VQL. 180m - smg SGWK bedding grading downhole. Minor patches of bt + si alteration starting at 229m depth,  zones of minor STUF"	
D	ML067	236.6	248.8	100	lgy dgy	fr	STUF	ST			1	cl cc po py am cpy	0	1		"236.1-245.1 very fractured regions where bt-si alteration is more banded (along bedding planes?). Silicified SSLT, SGWK and SMDT with VL/VC & minor X. Non-magnetic , minor gn am (?actinolite). Increasing amount cc + po downhole with VC up to 5cm thick."	
D	ML067	248.8	261.1	100	dgy gn bk 	fr	ZSKM	ZSKCS	SM		3	mt am cc cl	60	1		"mt-am skarn ~1.2m thick. Cc veins numerous. Ds po, minor cpy. Predominantly ZSKM with patchy fg mt and interspersed ZSKCS up to 50cm thick. 250.3-250.5 silicified SMDT bed. Increasing patches of cc downhole to thick (max 10cm) predominantly cc horizons wi"	
D	ML067	261.1	263	100	dgn bk	fr	ZSKCS				0	mt cl cc ep am	15	0		ZSKCS with some mg mt and gn acicular am	
D	ML067	263	279	100	bk dgn gn 	fr	ZSKM			ca sx	1	mt cc cl am ep cpy po py do	65	1		"ZSKM with minor VCX, VC increasing downhole. Mt fg-mg in thick bands (<5cm) and also ds. Minor X ds with most in veins with cl & cc. 266.8m - VCL (3cm thick) with unusual overgrowth texture of acicular to patchy cc in cl ""matrix"". Pale yw mineral in patch"	
D	ML067	279	282	100	bk gn	fr	ZSKCS			ca sx	1	ep cl cc mt po	20	1		"dominant mineral is med-hardness, vitreous lustre and appears to streak white - vs?, mt found in bands through ZSKCS. "	
D	ML067	282	290	100	bk gn	fr	ZSKM	ZSKCS		ca sx	1	ep cl am qz cc ak do cpy py	40	1		Small STUF layer at 284m. Interlayered ZSKM and ZSKCS	
D	ML067	290	297	100	bn gn	fr	ZSKCS				0	ep am cl mt qz vs py cpy	20	2		"at 290m - small area of STUF. Distinct lack of po, 292-293m high mt zone (40%). 294.5m - drop in mt %. Mt mostly in bands but some ds."	
D	ML067	297	320	100	lgy lbn	fr	STUF				0	qz bt py po cl mt	5	1		"X + cl in blebs and veins, po has alteration halos around blebs. Mt disseminated + fine grained. 306.8m - mt in beds with sulphides to 309.4m. Beds younging downhole. 309.5m - less silicified zone to 311.1m. Magnetism generated by po in core, weakly patch"	
D	ML067	320	329.1	100	dgy	fr	SS	ST			0	qz bt cl cc po py	0	1		"po and py present in small quanities, 328.3m granite dyke"	329.1m EOH
D	ML068	0	14.7	40	dgy bn og	wox	ST			qz cl	1	lm	0	0		"broken up, rubbly og bn weathered zone, little core recovery, limonitic staining throughout but more common on fracture faces, core feels like clay in parts."	
D	ML068	14.7	39.9	85	dgy gn bk	fr	ST			qz cl mt sx	3	mt	1	1		siltstone with qtz-cl vein alteration at 24.6m there is a 25cm qtz-cl vein with minor (5-7%) mt concentrated at the margins and v.minor amounts of sulphide (po cpy and ?py?). Pk/rd small veins of qtz and stilbite. Siltstone beds are weakly magnetic.	
D	ML068	39.9	47.3	75	dgy bk gn	fr	XFBI	ST	lSS	qz	15		1	1	fz	"fracture zone, fractured broken siltstone and greywacke with a apparent brecciation zone at between 41.5 and 41.85m of networking stilbite and qtz veins with v.minor vx (py)"	
D	ML068	47.3	59.3	100	lgn gn d	fr	ST	SS		qz cl sx	1	cl	1	1		"weakly bedded siltstone and greywacke with cl alteration and veined qtz, cl veins with disseminated sulphides (py, cpy and po)"	
D	ML068	59.3	87.4	100	dgy lgn	fr	STUF	SM	ST	qz cl ca	25	bt cl sx	0	1		"altered interbedded siliceous mudstone, siltstone and grey wackes. Beds of greywacke contain small mud rip up clasts that lie parallel to bedding in some zones. Bn colouration due to altered bt in the beds. Sulphides in veins and alteration bands (po and "	
D	ML068	87.4	95.3	100	dgy dgn	fr	ZSKCS			ca cl sx	3	am mt cc sx	20	10		"gn bn dkgy amphibole and carbonate rich zone, wt veins and zones 'fizz' with HCL. Disseminated sulphide throughout (typically po and cpy ± py), patchy concentrations of mt thoughout. Bn yw silicate mineral in the first metre of the ZSKCS, possibly ?vesuvi"	
D	ML068	95.3	133.6	100	dgy dgn	fr	ZSKM				5	mt cl am cc sx vs	50	5		"high percentage of mt making up most of the rock, very magnetic, wt carbonate alteration and green ampibole possibly actinolite (visible when next to carbonate veins). Significant sulphide disseminated in patches througout skarn, mostly po next to cpy and"	
D	ML068	133.6	138.5	60	bk dgy gn	fr	XFBI	XFBI	ST	qz cl ca	2		0	0	fz	"fractured rubbly core with brecciation zone and cataclasite at 134.6 - 136m, qtz and calcite vein clasts in breccia."	
D	ML068	138.5	178.5	85	dgy bk gn	fr 	SS	ST		qz cl ca	1		0	0		beds of mostly greywacke with thin veins of pk stilbite. Veins of qtz and cl	
D	ML068	178.5	185.3	100	wt lgy bk	fr	FG			qz tu sx	5	cl ep	0	1		"contact with granite is sharp, there appears to be no baked/chilled margins. At 180.1 - 180.2m the granite contains more tourmaline, possibly a vein, with two 0.5 - 1cm thick bands of pyrite. A coarse grained qtz and plagioclase rich granite with ~10% bt "	185.3m EOH
D	ML069	0	19.1	90	dgy	wox	ST	SS		qz cl sx	2	py	0	1		"med-thick bedded (poorly bedded) gy greywacke and siltstone; minor thin beds of gn gy greywacke. Bedding ~400, minor mm scale network veins of qtz and cl scattered f.g qtz-cl veins up to 10mm. Og fe-oxide weathering"	
D	ML069	19.1	33.2	100	gn gy wt b	fr	STUF			qz ca cl sx	2	si cl po	0	1		thin-med bedded ltgn gy bn cm greywacke and bn SSLT with minor laminations in thin beds of ltgn cm SMDT. Brecciated zones that have undergone later stage silicification and qtz/C/cl veining. 21.5m FT filled with cl and siliceous SDMT. Common cl veining th	
D	ML069	33.2	35.4	100	lgy dgy	fr	ZSKCS			ca cl sx	2	si cl do	0	1		laminated to thinly bedded SMDT and SGWK (well bedded). 32.9m to 34m mudstone beds are fracture (cleavage?) perpendicular to bedding. Minor secondary cl crystal flecks. Dolomite present in SGWK beds. SMDT beds heavily silicified 	
D	ML069	35.4	36.9	100	bk dgy	fr	ZSKM				0	mt cc px	60	1		"magnetite (px rich skarn package), from 35.6-36m the core has been dissolved leaving a honeycombing pattern with a secondary black needle shaped crystal growth. "	
D	ML069	36.9	44.2	100	lgy bngn	fr	STUF	ZSKCS		ca cl sx	3	do cc po py cpy si mt gn	5	5		"laminated to thinly bedded silicified SMDT and f.g-img SGWK, interlayered with sulphide (po rich), do/cc/px skarn. Bn bt alteration of silicified SMDT in some areas. Little magnetite-no visible crystals, gn am cl alteration."	
D	ML069	44.2	48.5	100	dgy bn bk	fr	ZSKCS	ZSKM		ca cl sx	2	px/am mt do/cc po	15	10		silicified beds of SMDT and minor SGWK interbedded with mt-px-do patches. 	
D	ML069	48.5	63	100	dgy bk	fr	ZSKM	ZSKCS			1	mt px po py cc cpy	60	10		"main mt-px skarn. Cc and X veining minor. 51-54m cm yw mineral disseminated throughout ?albite? Small zones of calc-silicate, X rich zone from54.4-62.4m (end of ZSKM). As/stanite flecks? From 55.3m zone becomes 50/50 mt and cal-silicate skarn; am and cl a"	
D	ML069	63	67.3	100	gn gy wt c	fr	ZSKCS				2	po py am cl cc mt	10	7		"ZSKCS, disseminated X throughout, including mostly po with py and cpy. Undulating zones of cl alteration. Veins of wt cc and veined X. Some infrequent patchy mt zones (<10%). Hard gn mineral occurs throughout. Texture is sometimes laminated but mostly alt"	
D	ML069	67.3	97.5	100	gn gy bk w	fr	STUF			qz cl ca sx	2	si cl bt po py mt 	2	10		"silicified laminations/thin beds of mudstone and greywacke with cl alteration in beds and in veins. From 68.5-69m there a ZSKM, mt >50%. Sulphide veins contain bk/gn alteration halo around some of them, veins cut across beds. Po main sulphide-causing weak"	
D	ML069	97.5	129.6	100	dgy gn bk	fr	SS	ST		qz cl ca	2	si cc cl po py cpy am tu sb ep bt	0	1		"thin-med interbedded dkgy SGWK and SSLT. Sfg-smg SGWK beds. Non magnetic. Cl, qtz, cc, am veins scattered throughout. V.minor cpy, po and py veins. SGWK beds grade down hole into SSLT where visible. Poorly differentiated bedding, v.small amounts of bt in "	
D	ML069	129.6	130.3	80	dgy bk gn	fr	XFBI				0	ka	0	0	fz	small fault breccia zone. 	
D	ML069	130.3	131.2	80	dgy gn	fr	SS	ST			0		0	0		Fractured wall rock to EOH	EOH 131.2
D	ML070	0	17.4	50	dgy yw og	wox	ST	SS		ca cl qz	1	lm ka	2	0		"yw/bn/og weathered SSLT and SGWK, broken and rubbly core, weakly magnetic"	
D	ML070	17.4	65.2	95	dgy bk gn	fr	ST	SS		qz cl	1	cl py po sb	2	0		"predominantly siltstone beds with thin-med beds of SGWK. Weakly magnetic. Thin qtz-cl veins with minor sulphides (<2-5% in veins). Pk bk granite dykelet 10cm tk kspar & qz with ~40% bk tm + bt, at 63.8-65.2m there is considerable calcite veining with incr"	20.4m - Start of NQ core
D	ML070	65.2	86.3	100	dgn dgy	fr	STUF			qz cl sx	15	si cl am	0	3		"interbedded SMDT/SSLT/SGWK variably altered by cl and si. Anastomosing cl veinlets in fine SMDT beds. High % of qtz veins appearing gn due to cl, small 3cm long X vein (po and cpy). Bn/dkgy beds of SGWK containing minor ds X (py). Alteration bands of cl a"	
D	ML070	86.3	93.8	100	dgn wt cm	fr	ZSKCS				2	am si cc mt cl po py cpy	15	15		"dark gn am and cl alteration and wt carbonate making up dominant lithology. Zones of si skarn at 87.2-88m. ds X throughout and patchy in concentrated veins (po, py and cpy)."	
D	ML070	93.8	96.5	100	dgn dgy	fr	STUF	ZSKCS		qz ca cl sx	15	si cl am sx ca	0	5		interbedded SMDT/SSLT/SGWK variably altered by cl and si.	
D	ML070	96.5	103.7	100	dgn wt cm	fr	ZSKCS	ZSKM		ca	2	am cc mt cl si vs	15	7		"ds X throughout and patchy in concentrated veins (po, py and cpy). ?Phlogopite? (or vesuvinite) present at 87.8m. Mt rich zones, patchy magnetism clusters of bladed gn crystals of am (?actinolite?) at 97.1m, in broken core end. Patches of higher concentra"	
D	ML070	103.7	115.4	100	dgy dgn	fr	ZSKM	ZSKCS			1	mt am px cl po py cpy cc	60	10		"dkgy/bn mt concentrated into bands with dkgn am. Mt becomes more massive, overall high % of mt. >10% ds and veined X (po py cpy). Carbonate veins and patches of carbonate in more ZSKCS zones. Patchy mt zones, broken by <1m zones of ZSKCS."	
D	ML070	115.4	118.3	100	dgy dgn	fr	ZSKCS	ZSKM			5	am cc po py mt cpy	5	20		calc-silicate skarn with noticably less mt and higher concentrations of am and cc.	
D	ML070	118.3	144.35	100	dgy dgn	fr	ZSKM	ZSKCS		qz	5	mt am cc po py cpy cl si ep	50	20		"fine-med mt making up >50% of the rock. V.fine am crystals. X abundant throughout, from 20-40% of the core in places. Veined and ds X (po, py, cpy). Between 127.7 and 128.3, more ZSKCS than ZSKM. ZSKM more concentrated in bands with ZSKCS which appear to "	
D	ML070	144.35	161.2	100	dgn dgy	fr	STUF			qz ca cl sx	15	si cl am po py	0	1		"little to no mt present, sharp contact with ZSKM. Silicified SMDT and SGWK beds with cross cutting VL. Am present in dkgn bands a with ds X, no cc in bands. Qtz veins often have a silicified cl halo around them. Patches of more concentrated X occurning in"	
D	ML070	161.2	162.6	100	bk dgy gn	fr	ZSKM	STUF			2	mt am po py ep si cpy	65	10		"ZSKM with >60% mt, ds X throughout, patches of silicified units (STUF)."	
D	ML070	162.6	172.5	100	lgn gy d	fr	STUF			qz sx cl	20	si cl qz	0	5		"silicified beds of mostly SMDT and SSLT with a high density of cross cutting VQL. Various alteration bands and colours some of the cross cutting VQLX offset each other, suggesting fracturing. 167-170m silicified SMDT and SSLT, looks less ""cherty"" than oth"	
D	ML070	172.5	174.9	60	dgn gy bn	fr 	ZSKCS			ca	2	am sx mt cc	10	10		"173.6m - broken, fractured core with a cc vein running parallel to core axis for ~10cm. Core fractured due to XFLT? Or due to cc vein, more easily broken. Dkgn ZSKCS zone, abundant bn mineral, bt?"	
D	ML070	174.9	177.45	100	bk dgn gy	fr	ZSKM				2	mt cl am sx cc	60	15		"ZSKM with dkgn minerals present throughout- am/cl?/ep?, high % mt and X, cc veining"	
D	ML070	177.45	190.2	100	lgy gn pk	fr	STUF			qz cl sx	10	si cl sx	0	10		"interbedded silicified SMDT and SGWK beds, SMDT beds altered with ltgn and ltpk alteration bands. Anastomosing and cross cutting veins of XL and Q often with L halo. 182.7m - silicified XBRC ~10-20cm long. (cl, ep alteration)"	
D	ML070	190.2	192.8	50	dgy gn	fr	XFBI	SS	ST	ca	2	ka cc	0	0	fz	"fault breccia at 190.2m, broken and rubbly core to EOH, unsilicified, fault zone, cataclasite and cc veining. "	EOH 192.8m
D	ML071	0	8.65	50	dgy og dbn	wox	SS	ST			0		0	0		"SSLt and SGWK beds which are moderately fractured and broken up. Dkbn, dkrd and yw weathering on fracture faces appearing hematitic, v.minor sulphide (po) in vuggy veins, non magnetic"	
D	ML071	8.65	83.8	95	dgy dgn	fr	ST	SS		qz cl sx ca	2	sx si cl 	0	1		interbedded SSLT and SGWK with small (<2mm wide) cross cutting VQL and VL. Minor ds X in SSLT/SGWK beds at 13.4m. Sulphide veins at 14.1m of po and a VQ with mostly py associated and minor am. Rock in core has uundergone minor silicification. 24.6m depth 	
D	ML071	83.8	92.85	100	lgy dgy dg	fr	STUF			qz cl ca	5	si cl	0	0		"gradational change into STUF, patchy STUF/SSLT and SGWK. Interbedded SMDT, SSLT and SGWK beds pervasively altered by si. Thin veinlets of cl and qtz common. At 86.5m - on fracture face bn elongate patches (fine, no fizz with HCL) ?hematitic mud beds?"	
D	ML071	92.85	96	100	dgn dgy wt	fr	ZSKCS			ca qz	2	am cc po py cpy	0	15		"high % of am and cc, dkgn am in places has the appearence of actinolite. High sulphide content, mostly po and cpy. Also py and 'silvery' coloured sulphide (most likely po, but looks like asp or stanite?) see 93.9m depth."	
D	ML071	96	97.7	100	dgn lgn db	fr	STUF			qz cl	5	vs po py	0	5		"STUF with thin sulphide (po, py) veinlets through SSLT."	
D	ML071	97.7	111.3	100	dgn dgy wt	fr	ZSKCS			ca qz	1	am cc po cpy ep mt	2	25		ZSKCS at 97.7m contains an increased % of sulphide (mostly po). Minor magnetite. 'silver' coloured sulphide in low concentrations in ZSKCS with large amounts of po and cpy	
D	ML071	111.3	114.9	100	dgy yw wt 	fr	ZSKM	ZSKCS			0	mt am cc po cpy	50	25		increased amounts of mt in ZSKCS. Am and cc dominant with po as the major sulphide	
D	ML071	114.9	116.4	100	dgn dgy	fr	ZSKCS	STUF			1	am po cc cpy	10	20		"ZSKCS with interbedded STUF, high % am and cc and X (po, cpy)"	
D	ML071	116.4	126.1	100	dgy dbn cm	fr	STUF			qz cl sx	2	si cl po cpy ep	1	5		"silicious sediments with ms, ds and veinlets of X. Bn/bk mineral - hardness >6, cassiterite? Garnet? Bn/yw mineral, looks like vesuvintie moderatelty common"	
D	ML071	126.1	126.9	95	gn gy wt b	fr	V			qz sx cc	na	qz po cc cpy cl ep	0	50		"transparent, gn qtz with cl and ep alteration, contains high % po and minor cpy. Large amount of cc associated."	
D	ML071	126.9	131.8	80	dgy dbn dg	fr	STUF			qz cl ca	2	si cl sx po py	0	5		ltbn/cm siliceous beds with minor sulphides on broken core faces and in veinlets	
D	ML071	131.8	154.35	95	dgy dgn db	fr	ST	SS		qz cl sx	2	cl si cpy po py	0	2		"near STUF there are mostly SSLT beds, with interbedded SGWK, minor thin beds containing bt. Bt skarn occurs in zones throughout"	
D	ML071	154.35	155.4	90	lgy wt bk	fr	FG				0	ep cl	0	0		"sharp contact with SGWK/SSLT unit, wt plag + qtz rich granite, also rich in bk bt flecks ~15% and tourmaline, ± muscovite. High ep alteration content"	EOH 155.4m
D	ML072	0	28	80	dgy lgy og	wox	SS	ST		cl sx	15	cl mt cpy	1	0		"interbedded SSLT and fine to med grained SGWK (beds poorly defined). Non-weakly magnetic (fine mt crystals visible in some veins with cl and ds in some beds causing modertate magnetism. V.minor sulphides. Silicification in last~1m, very fractured and rubb"	
D	ML072	28	33	99	dbn lgy lg	fr	SS	ST		qz cl sx	5	bt cl qz si cpy po cc px	0	0		interbedded fine-med grained SGWK + SSLT. Weak bt alteration + minor si alteration. Minor sulphide in veins; weak to no magnetism	
D	ML072	33	44	98	wt cm lgy 	fr	STUF				0	 po cpy	0	0		"interbedded fine to med SGWK + SSLT with minor SMDT beds that have strong patchy silicified and bt altered. 37.9m alteration becomes banded  (~1mm-3cm). 40.2m - 60cm core lost, ?fault zone?, og weathered rubble. Minor patches of calc-silicate, towards end"	
D	ML072	44	45.63	30	og	mox	XFBI				0		0	0		"fault zone, og weathered rubble"	
D	ML072	45.63	49.85	100	bk dgn wt	fr	ZSKCS	ZSKM			0	cl cc mt si am px po cpy asp cs vs	30	1		banded calc-silicate skarn with patchy magnetite skarn. Cl has been silicified (v.hard) 	
D	ML072	49.85	61.85	100	bk dgn wt	fr	ZSKM			sx	0	mt po am cc cl cpy asp bt	50	20		ZSKM with bk am (hornblende?). Pervasive ds po + in veins. Cc + cl ds in areas throughout unit. 58.8m calc silicate (cc + cl) component increasing	
D	ML072	61.85	73	100	dgn wt bk 	fr	ZSKCS	ZSKM			0	cc cl mt am po si do si vs cpy	30	10		"dominantly ZSKCS (cl, cc, si) with layers of mt throughout. Minor do patches, minor X + veins. At 64.8m ~30cm thick massive mt zone. Cm bands, scratch with scribe, not soluble in HCL (vs/garnet?). Zones of more silicified skarn. Dkgn am and ltgn carbonate"	
D	ML072	73	92.2	100	dgy dgn lg	fr	STUF			qz sx cl	2	si cl am cc mt ep po cpy	1	1		"Gradational change into STUF with ZSKCS horizons ~10-25cm near ZSKCS zone, STUF - gn/bn/gy beds of silicified SMDT/SSLT/SGWK with cl + ep alteration. VX at 77m looks like X has permeated along minor falut related fractures in core. 80.1m - higher % po acc"	
D	ML072	92.2	124.2	100	dgy dgn db	fr	SS	ST		qz sx cl	1	cl bt py po cpy si am	0	3		"mod-poorly sorted qtz-?feld? (possibly volcaniclastic) grains of SGWK and beds of SSLT. Bn bt in SGWK, still part of the subdivision of bt skarn. Ds X in varying concentrations and in small veinlets. At 100.1m depth - patch of dkgn am and ds X, looks like"	124.2m EOH
D	ML073	0	32.2	75	dgy bn og 	WOX	SS	ST		qz cl	5	cl	0	0		Weakly weathered og/bn/yw SGWK and SSLT. Non magnetic. Yw limonitic staining throughout and dkrd hematitic staining in places. Wt/cm soft altered qtz veins to ka. Some (<1%) patches of dkbn/bk hematitic weathered core are magnetic.	
D	ML073	32.2	96	80	dgy dgn bk	fr	SS	ST		qz	5	cl qz sb	5	0		"Weakly to moderately magnetic, core is broken and moderately / heavily fractured. Qtz-cl, cl and qtz-stilbite veins are abundant throughout. At 42.4 m in qz-stilbite vein there is a minor amount of py/po."	
D	ML073	96	122	99	dgy	fr	ST	SS		mt tu	5	cl sb qz	1	0		Weakly magnetic SSLT. MT occurs in chlorite as blebs and veins. Stilbite only occurs in veins and fractures. Non-magnetic below 120m.	
D	ML073	122	125	99	gn lgy dgy	fr	ST	SS	STUF	qz cl ca	1		0	0		"From 122-123.8m stockwork veining occurs comprised of qtz, cl and minor cc. From 123.8 - 124.6m cl is the dominant mineral."	
D	ML073	125	136	99	gn lgy dgy	fr	ST	SS			5	cl	1	0		Chlorite is dominant mineral. Unit is weakly magnetic to 131.4 m.	
D	ML073	136	138.8	100	dgy	fr	STUF				1	qz cl bt sb sx	1	0.1		Silica skarn	
D	ML073	138.8	144	100	na	fr	SS	ST			1	qz cl bt sb sx	1	0.1		Greywacke and siltstone.	
D	ML073	144	154	100	dgy	fr	ST	SS			1	cl qz sb cc	1	0		Bedding at 145.7 m has ripup clasts and scouring suggesting younging downhole. Mt occurs disseminated in the sediment.	
D	ML073	154	170	99	dgy	fr	SS	ST			0.1	cl qz sb cc py	1	0		Greywacke and siltstone with a minor band of silica skarn occuring at 157.8 m (10 cm thick). Mt occurs at the top of the band.	
D	ML073	170	171.5	99	lgy	fr	STUF	ST	lSS		0.1	qz cl bt py sb	0	0.1		Interbedded silica skarn and greywacke.	
D	ML073	171.5	174.9	99	lgy	fr	STUF				0.1	qz cl bt py sb	0	0.1		Silica skarn.	
D	ML073	174.9	175.4	95	lgy	fr	XFBI	ST	lSS		40	qz	0	0		Breccia.	
D	ML073	175.4	195.4	100	gy bn	fr	STUF			sx	0.1	qz bt cl po cpy cc	0	0.1		Silica skarn with minor sulphides occurning in veins. Weakly magnetic in veins due to po content. Sulphide content increases below 185.0 m where biotite content is increased.	
D	ML073	195.4	198.4	100	gn bn	fr	ZSKCS				1	cl fl am ba mt po py cpy cc	10	10		Calcsilicate skarn with high amounts of fluorite and barite and small amounts of cc. Mt occurs in bands.	
D	ML073	198.4	200.9	100	bn	fr	ZSKM				0.1	mt bt fl po py cpy cc	50	5		"Magnetite skarn with mt occuring disseminated and in bands throughout the interval. A soft pink mineral occurs within the interval, possibly sphalerite."	
D	ML073	200.9	210.5	100	bn	fr	ZSKCS				0.1	cl bt do po fl tu am py cpy cc asp	30	15		"Calcsilicate skarn with mt occuring in bands. Fl, cl, x veins are common. Mt is found with po in bands. STUF occurs interbedded with ZSKCS from 207.8 to 208.1 and from 209 to 210 m."	
D	ML073	210.5	214.9	100	bl bn	fr	ZSKM				0.1	mt am cl bt po cpy py fl	50	15		Magnetite skarn with fluorite and quartz occuring in veins.	
D	ML073	214.9	220.7	100	gn bk	fr	ZSKCS	ZSKM			0.1	cl bt mt fl qz po py cpy	20	10		Calcsilicate skarn with magnetite skarn occuring in bands. Minor silica skarn occurs from 218.0 to 218.6 m.	
D	ML073	220.7	222.8	100	bk gy	fr	ZSKM	ZSKCS		sx	0.1	mt po cpy py sh	50	20		Magnetite skarn with calcsilicate skarn. Rare clots of red / pink sphalerite. Bedding parallel bands of semi-massive magnetite. Sulphides occurs as blebs and rare veinlets.	
D	ML073	222.8	230.2	100	na	fr	STUF	ZSKCS		qz sx	0.1	po mt cpy py cl fl	2	10		Minor magnetite skarn occurs from 224.4 to 225.0 m. Sulphides occur dominantly in bands of calcsilicate skarn bands that are 20 to 50 cm thick. Fracture and vein controlled chlorite alteration occurs with silica skarn sections. Sulphide content decreases 	
D	ML073	230.2	231.3	100	gy gn	fr	STUF			sx	1	po cpy py cl fl	0	3		Chlorite alteration halos po py veinlets. Local bleaching halos of hairline healed fractures and sulphide veinlets.	
D	ML073	231.3	236.1	100	bn	fr	STUF				0.1	po fl ca	1	5		"Folding, boudinage and truncation of narrow laminar beds is common. Carbonate healed breccia with angular clasts occurs from 234 to 234.1 m and at 234.7 m (5 cm thick). Carbonate healed fracture stockwork is common below 234.0 m. A narrow ( 3 cm) sediment"	
D	ML073	236.1	241.2	100	gy gn	fr	STUF	ZSKCS		cl sx	1	cl po cpy mt py	1	8		Silica skarn with calcsilicate skarn comprising 30% of the interval. The majority of the sulphide content occurs in the calcsilicate bands which are generally chlorite altered. Chlorite veinlets are common. Sulphides occur as blebs and narrow veins. Local	
D	ML073	241.2	244.5	100	gy bl	fr	STUF			cl sx	5	po cpy cl	0	5		Fine grained banded (1-5cm) unit with several 2-5 cm thick po veins +/- cpy. Chlorite veins and hairline fracture chlorite stockworks are common. Possible gold occurs on a fracture at 243.3 m.	
D	ML073	244.5	244.9	100	wt	fr	FG				0		0	0		Medium grained leuco granitoid with a very weakly developed foliation. Irregular contacts.	
D	ML073	244.9	250.8	100	bn	fr	STUF			qz sx	0.1	py po	0	1		Silicified poorly sorted sfg/smg greywacke with laminated siltstone. Folding and boudinage is present. Local white bleaching affects truncated coarse poorly sorted (smg / scg) sandstone beds. Rare blebs of po and local py veinlets.	
D	ML073	250.8	251.7	100	wt	fr	FG				0		0	0		Medium grained leuco granitoid with sharp contacts.	
D	ML073	251.7	254.4	100	bn	fr	STUF			qz sx	0.1	am po py	0	0.1		Very fine grained silicified siltstone with greywacke. Local quartz amphibole veins.	EOH 254.4 m
D	ML074	0	14.1	100	dgy bn og 	wox	SS	ST		qz	1	lm cl si	0	0		Weakly weathered lm SGWK and SSLT. At 8.3 m silicified dkgn SGWK and wt mudrock. Core broken and rubbly in trays. Non magnetic. Soft wt veins altered to ka.	
D	ML074	14.1	62.7	100	dgy bk dgn	fr	ST	SS		qz cl ca sx	1	cl si mt py cpy po	2	0		Interbedded SSLT and thinner beds of SGWK which have moderate to high silica content with some broken faces having the fracture of chert (conchoidal). Core appears dkgn as it contains cl pervasively throughout. <1% finely disseminated sulphide. Thin (<5 c	
D	ML074	62.7	72	100	dgy dgn bk	fr	STUF			qz ca cl sx	1	cl si cc am po cpy py	0	1		"63.2 m VQLC, recrystallized breccia zone ~ 10 cm across (silicified XFLT). STUF - silicified bed of SSLT/SGWK and SMDT with various alteration zone picking out different lithologies. Sulphides (mostly po and cpy) have found their way along many of the thi"	
D	ML074	72	75.6	100	dgn dgy wt	fr	ZSKCS				1	am cc po vs cl cpy py	0	5		"Mottled coloured ZSKCS made up of mostly am, cc and po and cpy, wt cc veins dkbn / mottle coloured mineral of relatively high abundance - vs. Py in fine granined euhedral form in bands on a broken core face at 74.55 m."	
D	ML074	75.6	77.6	100	dgy cm lgn	fr	STUF				1	si cl po py	0	2		"STUF - various bands of colours denoting different alteration in fine beds, disseminated po and py throughout but mainly on fracture faces."	
D	ML074	77.6	86	100	dgn wt dgy	fr	ZSKCS	STUF			1	cc am vs mg sr po py cpy mt fl tu	0	5		ZSKCS with increased amounts of carbonates including cc and magnesite. Serpentine associated with magnesite on fracture faces. Fine tetragonal faces of a bk translucent mineral at 80 m (am?). Dkgy / bk mineral at 81.35 m - tourmaline and associated flouri	
D	ML074	86	89	100	dgn wt dgy	fr	STUF	ZSKCS			1	si cl cc cpy po	0	2		Thin fracture in STUF with cpy common and cc in veinlets.	
D	ML074	89	94.6	100	dgn wt dgy	fr	ZSKCS			ca	1	am cc po py mt cpy cl ep	1	5		Coarse am and cc typical of ZSKCS seen in other holes. Similar % of am and cc. From 93 - 94.5 m mostly am and po+py with some cc. Ms po at 94 m. Rare narrow bands of magnetite.	
D	ML074	94.6	109.5	100	dgy bn gn	fr	STUF			qz sx cl ca	5	si cl bt po	0	1		"Thin gouge / fractures in STUF some infilled with po + py, core broken and rubbly, possible XBRC at 95m  with cc infilling fractures. Partially recrystallised fault zone from 94.6 - 95.3 m, broken fractured core surounding zone up to 98.2 m. At 99.2 there"	
D	ML074	109.5	110.5	100	na	fr	ST	SS			na		0	0			
D	ML074	110.5	111	100	na	fr	XFBI	XFBI		cl qz ca	5	cl	0	0		Broken fractured core with minor brecciation and cl veins. Some cl rich fracture faces have a clay (ka) weathering.	
D	ML074	111	123.4	100	na	fr	ST	SS		qz cl sx ca	3	cl po cpy bt	1	1		Largely SSLT with VLX at 112.1 m and small beds of SGWK. Dkgn colored cl around VQ commonly seen with sulphides (po+cpy) at 116.2 m. Weakly magnetic.	
D	ML075	0	45.4	50	dgy og yw 	wox	ST	SS			0	cl	0	0		Weakly weathered mostly SSLT with beds of SQWK common. Largely broken and rubbly core. Og/bn oxidation on exposed faces. Soft wt veins.	
D	ML075	45.4	82.1	100	dgy	fr	ST	SS		qz cl	1	cl	0	0		"SSLT with thin beds of SGWK, vein of qtz and cl throughout. At 50 to 50.7 m anastamosing VQL and fractures gives the core a brecciated appearance. VQXL occurs locally at 52 and 64.9m. Pk/rd stilbite occurs locally on fractures. Moderately magnetic below 6"	
D	ML075	82.1	82.6	100	na	fr	XFBI	STUF			na		0	0		Recrystallised breccia zone.	
D	ML075	82.6	161	100	dgy bk dgn	fr	SS	ST		qz cl sx	1	cl am po cpy	0	1		SGWK with SSLT with broken sections. Weak to moderately magnetic below 119 m.	
D	ML075	161	176.6	90	dgn dgy lg	fr	STUF			qz cl ca	2	si cl bt am cpy po py	0	1		"Gradational phase into STUF with minor STUF in SGWK/SSLT beds, typical STUF alteration patterns become more abundant. More common conchoidal fractures. Dkgn am, cpy in or around veins."	
D	ML075	176.6	190.7	100	dgn bn dgy	fr	ZSKCS	STUF		ca sx	1	am cc si mt po cpy py	2	5		lt/dkbn and dkgn ZSKCS with abundant cc. Bands of dkgy / bk mt. Abundant sulphide (mostly po) disseminated throughout. Dk/ltbn/yw VS common in ZSKCS. Often minor (<1m) STUF interbedded with ZSKCS. Patches of dkgn skarn with increased am content. At 182 m 	
D	ML075	190.7	200.8	100	dgy dgn wt	fr	ZSKM	ZSKCS		ca sx	2	mt am cc po cpy py fl	40	10		"ZSKM with appreciable ZSKCS, mt often coarser with euhedral crystals commonly associated with sulphides (po, cpy + py). ZSKCS in equal proportions made up of mostly fine grained am and cc. At 193.85 m euhedral mt crystals with po, cpy and fl. At 197.3 m -"	
D	ML075	200.8	225.2	100	dgn dgy wt	fr	ZSKCS			sx	1	am cc po cpy po cl	10	20		"Gradation into ZSKCS with mt bands fading out dramatically over ~0.3 m. Po most dominant sulphide occupying 20-30% of rock. At 202 m tarnished dkbn / bronze mineral, possibly bornite or tarnished po. High concentration of po in veins from 201 to 203.3 m a"	
D	ML075	225.2	233	100	lgn dgn dg	fr	STUF	ZSKCS		cl qz ca sx	1	si cl po	0	2		Gradual change from ZSKCS to more dominantly STUF. Unit begins where vs becomes less abundant to nonexistent. Distinct colour change from mottled ZSKCS to lt/dkgn's of the STUF zone. Bands of alteration often accompanied by grainsize variations. Minor ds 	
D	ML075	233	235.9	100	dgn dgy wt	fr	ZSKCS			ca sx	na	am cc mt fl po py cpy	20	10		"ZSKCS with mt in patches but concentrated at 234.2 -235 m associated with po,py and fl, there is plenty of cc in the system as most of it fizzes with HCL, plus magnesite at 235.3 m."	
D	ML075	235.9	241.2	100	dgn dgy wt	fr	STUF	ZSKCS		qz cl sx	5	si cl po cc	0	2		"Silicified bedded sediments with varying alteration states, minor sulphides (po) ds throughout. Bedding at 236 m appears to be younging downhole. Thin veinlets of VQL +/- po. Rounded non sperical X filled shapes in core with an undulating alteration front"	
D	ML075	241.2	254.3	100	dgy bn dgn	fr	ST	SS		qz cl sx	1	cl bt po si	0	2		"SSLT and SGWK beds with an overall lower si content, dkbn bt zones common near STUF boundary at ~243 m. Thin (~5 cm) zones of STUF infrequently occur, eg at 242.8 m. Fine flaky transparent mineral, no fizz when HCL added, qtz? on fracture at 243.15 m."	EOH = 254.3m
D	ML076	0	9.7	50	dgy bk dgn	wox	ST	SS		qz	1		0	0		"weakly weathered mostly SSLT beds, infrequent vuggy veins and minor VQ. Lm, ka and some go on weathered fractured/rubbly core"	
D	ML076	9.7	104	90	dgy bk dgn	fr	ST	SS		qz cl sx am	1	qz cl po si am cpy mt	2	1		"mostly SSLT beds with thin SGWK beds occurring. VQL with po and sometimes associated am. Where these veins are of a higher concentration there is a minor STUF developed, eg at 21.6m. SSLT becomes weakly to moderately magnetic at ~22.5m. Increasing proport"	
D	ML076	104	124.8	100	dgn dbn wt	fr	STUF			qz cl ca sx	1	si qz cl bt po py	0	2		"gradational change into STUF, the boundary is subjective, in this case a boundary has been drawn where there is a more obvious colour and alteration change. At 108.65m - smg poorly sorted SSDT/SGWK loading SMDT bed, youning direction is downhole. Minor po"	
D	ML076	124.8	125	100	na	fr	XFBI	STUF	ZSKCS		0		0	0		minor recrystallised (silicified) XBRC	
D	ML076	125	126.6	100	dgn dgy lb	fr	ZSKCS			ca sx cl	2	am cc cl po vs cpy	0	5		"start of ZSKCS, mostly am and cc with  X (po)"	
D	ML076	126.6	127.1	80	na	fr	XFBI				0		0	0		Recrystallised breccia zone	
D	ML076	127.1	145.5	100	dgn dgy lb	fr	ZSKCS	ZSKM		ca sx	2	am cc vs cl mt po cpy	2	5		"ZSKCS is made up of mostly dkgn fine grained am and cc with varying amounts of vs, po and mt. At 128.5m - dominantly wt insoluble qtz with cc in veins through it. Minor mt skarn from 131.3-132m. Increased mt content after 132m ~20-30%, mostly dkgn am and "	
D	ML076	145.5	158.3	100	dgy dbn gn	fr	STUF			qz cl sx	3	si cl bt po py ep	0	5		"Lt/dk bn and gy fine grained STUF with high concentrations of VQL veinlets with minor po and py. Dkbn patches at 147.4m (Bn bt in bedding?) Several small (0.5-1.5cm) subrounded darker clasts in fine grained STUF beds, clasts often filled with po - 'volcan"	
D	ML076	158.3	184.8	100	dgy	fr	ST	SS		qz cl ca	3	qz cl si	0	0		Boundary with STUF is again subjective as there are minor STUF in SSLT/SSWK beds. At 170.8m there is a 5cm wide FGRA dyke. The dyke is composed of mostly qtz (>80%) with around 15-20% assimilated wall rock. At 174.55m there is a 5-7cm wide granite dyke. T	
D	ML077	0	31.2	50	bn gy og y	wox	ST	SS			0		0	0		"Mox broken core, predominantly SSLT, vox and altered to clay in places, minor wt veins (not effervesant) >50% vox, weak and friable. Short sections of fr intact si SSLT and SGWK increasing down hole. HQ."	
D	ML077	31.2	34.8	90	dgy	wox	ST	SS		cl	0.1	cl	0	0		"Fr Si SSLT with minor SGWK, decreasing rubbly, broken core. M cl on fracture surfaces and minor wt veins - cl?"	
D	ML077	34.8	68.7	100	gy	fr	SS	ST		ca cl	0.1	cl sb	0	0		"Core size changes from HQ to NQ at 34.9m. Rock type changes tp predominantly ltgy Si SGWK. With minor Si SSLT, minor oxidation on fracture surfaces. Minor pink veins increasing in abundance and thickness down hole. Weakly magnetic sections are common."	
D	ML077	68.7	72.2	100	gy	fr	XFBI			ca	1	ca cl sb	0	0		"Healed, silicified brecciated and broken core sections. Weak bedding and controlled green chlorite alteration parallel to bedding. Carbonate and stilbite veins are common."	
D	ML077	72.2	74.9	100	dgy	fr	SS	ST		ca cl	0.1	cl	0	0		SGWK with minor beds of SSLT. Local bands (<5cm) of light green cl alteration halo veins	
D	ML077	74.9	81.8	100	dgy	fr	ST			ca sb	4	ca si 	0	0		Laminated to thinly bedded siltstone with minor SGWK. VC with stilbite veins are common. Minor bands of wk chloritic alteration. Local wk bleaching of SWGK bed. Sections of weak silicification. Weakly magnetic in unaltered sections.	
D	ML077	81.8	109.1	100	dgy	fr	ST			ca	1	si	0	0		"As above, with only rare carbonate-stilbite veinlets. Variably weakly magnetic. Healed fracture/crackle breccia from 85.8 - 86.7m."	
D	ML077	109.1	114.5	100	gn dgy	fr	ST			ca sx cl	5	cl ca	0	0.1		Carbonate - stilbite vein stockwork within SSLT. Numerous healed fractures. Bands of green cl alteration are common local py-cpy-cl veins. 	
D	ML077	114.5	122.8	100	dgy gn	fr	ST	SS		ca cl	1	cl	0	0		Dark grey siltstone with sections that are chlorite altered to green associated with local carbonate-stilbite veins. Minor black cl vein stockworks. Variably weakly magnetic with patchy silicification. Non-magnetic in cl altered zones.	
D	ML077	122.8	133.9	100	dgy gn	fr	ST	STUF		ca	1	si cl	0	0		Pervasively silicified SSLT with minor bands of silica skarn. Gradational transition to silica skarn down hole. Narrow bands of green chlorite alternation. Local ca veins and narrow  (2-5cm) ca healed breccia at 132.4m	
D	ML077	133.9	139.6	100	lgn dgy	fr	STUF	ST		ca cl	1	cl si po py	0	2		Intermixed silica skarn and silicified siltstone. Po is disseminated and occurs as blebs. Green chlorite veinlets are common. Local ca veins. 135-135.5m is XBRC weakly developed due to stockwork veining	
D	ML077	139.6	141.7	100	dgn lbn	fr	ZSKCS	STUF		ca cl	1	am ca po py mt	3	7		Calcsilicate skarn with bands of silica skarn. Variable mt and po content. Fizzes with HCL	
D	ML077	141.7	143	100	bk gn	fr	ZSKM			ca	0.1	mt po cpy	30	10		Mt rich ZSKCS with po blebs throughout. 	
D	ML077	143	144	100	gn lgn	fr	ZSKCS	STUF		cl	1	po mt py cl	5	15		Po rich ZSKCS grading to STUF	
D	ML077	144	146.8	100	lgn bn	fr	STUF			cl sx	2	cl si po 	0	2		Silica skarn with hairline po veinlets. Green cl veinlets are common. Banded sections maybe representative of thin bedding (0.5-1cm)	
D	ML077	146.8	149.1	100	dgy lgn 	fr	ST	STUF		ca	0.1	cl si po	0	1		SSLT and SGWK is locally overprinted by irregular lt gn patches of silification with anastomising patterns of gn cl rimming light coloured silification and bleaching (EOH)	
D	ML078	0	33.3	50	dgy bk og 	wox	ST	SS		qz cl	3	im cl	0	0		"Dkgy/bk fine SSLT and SGWK beds, mostly weakly weathered to rubbly broken og/wt FeO core. Some minor po on fracyure face at around 23.5m depth, where there is a zone of minor silicified dkgn beds - these are non-magnetic. At around 30m the core increases "	
D	ML078	33.3	112.3	60	dgy bk dgn	fr	SS	ST		qz cl ca	0.1	qz cl si po cpy	0	0		"Similar proportions of SSLT and SGWK beds, cl alteration is common espoecially on fractured faces of core and in veins, often with qz. Variably non-magnetic to weakly even moderately magnetic in places. Minor silicification at 52 - 53m around VQCL. Core i"	
D	ML078	112.3	115	70	na	na	XFBI				na					At 112.3 - 110.1m broken rubbly core with zones of fault breccia throughout. Fractured zone 112.3 - 120.4m	
D	ML078	115	166	100	dgy bk dgn	fr	SS	ST		qz cl sx	na						
D	ML078	166	171.8	100	dgy	fr	ST	SS		qz cl ca sx	na	cl qz cc	0	0.1		"Fine grained SSLT and SGWK with blebs and veins of cl. Cl also found in fractures. There is stockwork veining of cl, qz and cc at 166 - 166.2m. The core turns to rubble at 167.3 - 167.6. Zat 168.4m the veins include very minor x (py and cpy)"	
D	ML078	171.8	200.3	100	dgy	fr	SS	ST		cl qz	0.1	cl qz cc sb mt cpy py	0.1	0.1		"SGWK and SSLT with blebs and veins of cl, minor sb and mt but veins are only weakly magnetic. Magnetisim increases at 179.7 but is still weak. At 187.5 the cl veins show bleaching around them and minor silicification. Magnetism decreases again at 196m. Sb"	
D	ML078	200.3	209.8	100	dgy	fr	ST	STUF		qz cl	0.1	si cl sx bt	1	0.1		SSLT is strongly silicified and interlayered with STUF. At 200.8 - 201m there is stockwork veining of qz and cl. The cl and bt follow bedding planes. The sulphides forund in this unit are cpy and py. The exact boundaries of this unit are hard to locate as	
D	ML078	209.8	224.9	100	bn gn gy	fr	STUF			cl qz sx	0.1	si bt cl cpy py po	0	0.1		"211.5 beds coarsen up hole and there are, either possible rip up clasts or a shattered bed at 214.1. VLQX is around 8cm thick. Cl and x are found mostly in veins and veinlets. The whole unit has been washed in Si and qz can be found in veins and veinlets."	
D	ML078	224.9	233.7	100	bk bn gr	fr	ZSKCS				0	cl am mt do cc qz cpy py tu vs gt mg	30	0.1		ZSKCS with high mt and do percentage. Mt is occuring mainly in veins and blebs.	
D	ML078	233.7	251.3	100	bk bn gr	fr	ZSKM			ca	0.1	mt am cc do po cpy py	60	5		"Po is disseminated. At 244.5m there is a red m ineral occuring in a vein with cc. It is soft, vitreous and may have a tetragonal system. Petrology has been requested. "	
D	ML078	251.3	259	100	bk gy	fr	ZSKCS	ZSKM		ca	0.1	am mt do cc po cpy py	40	5		At 256m there is a vein of cc and do. Mt is mainly found in layers but is also disseminated. 	
D	ML078	259	263.7	100	gy gn	fr	ZSKCS			ca	1	am cl do cc po cpy py qz	30	5		Sulphides are found in layers but also disseminated	
D	ML078	263.7	264.7	100	bn gn	fr	STUF	ZSKCS			0.1	cl qz bt cc am	0	0.1		Interlayered STUF and ZSKCS	
D	ML078	264.7	270.1	100	bn gy	fr	STUF			cl qz	2	qz bt cl cc po cpy py	0	0.1		STUF is bt rich and has disseminated x maily po	
D	ML078	270.1	275.3	100	dgy	fr	SS	ST		qz cl	1	qz bt cc cl	0.1	0			
D	ML079	0	21.4	100	og dgy	mox	ST	SS			0	si	0	0		Variably clay altered limonitic wethered siltstone. Fresh sections are silicified. Numerous clay altered broken/rubbly sections. White clay healed fracture stockworks are common. Clay seams are common.	
D	ML079	21.4	39.4	100	dgy og	wox	ST	SS			0	si	0	0		Locally weathered and limonitic siltstone. Local SGWK beds up to 10 cm thick. Weathering and broken sections are less intense than the above interval.	
D	ML079	39.4	56.2	100	dgy	fr	SS	ST			0		0	0		Fine grained poorly sorted SGWK with siltsone. Limonite and clay fracture coatings.	
D	ML079	56.2	72	100	dgy	fr	SS	ST		ca cl	0.1	cl am	0	0		Fine grained poorly sorted SGWK with beds of laminated SSLT. Local minor green chlorite alteration and chlorite veins. Carbonate and chlorite veins are also present though rare. Local patches with recrystallized green amphibole (?).	
D	ML079	72	123.2	100	dgy	fr	SS	ST		ca cl	0.1		0	0		As abvove but without chlorite alteration. Rare VLX (veinlets) with narrow (<1 cm) bleaching halos. Rip up clasts at 111.8 m indicate younging downhole.	
D	ML079	123.2	140.5	100	dgy	fr	ST	SS		ca	0.1		0	0		Thinly bedded to laminated siltsone with SGWK interbeds. Local carbonate-stilbite veinlets and minor black chlorite veinlets.	
D	ML079	140.5	156.5	100	dgy	fr	SS	ST		qz cl	0.1	cl	0	0		Fine grained poorly sorted SGWK with siltstone interbeds. Local quartz-chlorite veins. Minor local green chlorite alteration.	
D	ML079	156.5	161.5	100	dgy	fr	ST	SS			0	am cl	0	0		Laminated  to thinly bedded siltstone with interbeds of SGWK. Several areas have hairline healed fractures that offset bedding up to 2 cm. Minor clots of green amphibole / chlorite.	
D	ML079	161.5	176.5	100	dgy	fr	SS	ST		qz cl	0.1	cl	0	0		SGWK with siltstone interbeds. Local quartz-chlorite veins with narrow bleaching halos up to 1 cm thick.	
D	ML079	176.5	183	100	dgy gn	fr	SS	STUF		qz cl	0.1	si	0	0		SGWK with interbedded siltstone with bands of silicfication and minor silica skarn. Narrow bleaching halo's around qtz-cl veinlets which occur locally.	
D	ML079	183	188	100	dbn	fr	STUF	SS			0	si he	0	0		"Strongly silicified SGWK and SSLT unit is dark brown colored, likely due to hematite alteration."	
D	ML079	188	199.4	100	dgy	fr	SS	ST			0	cl	0	0		SGWK with interbedded siltstone. Local bands of weak chlorite alteration.	
D	ML079	199.4	211.6	100	lgn dgy	fr	STUF	SS		qz cl	1	cl si po	0	0.5		Silica skarn bands overprint dark grey SGWK. Green chlorite veins are common throughout. Local quartz veining. Bleaching related the veining is common. Rare blebs of po.	
D	ML079	211.6	215.5	100	lgn gn	fr	ZSKCS				0	cl po mt asp st ca	4	5		Magnetite bearing calcsilicate is overprinted by chlorite alteration. Sulphides (dominantly po) are common. Silver grey sulphides (asp / st) are also present. Magnetite occurs in bands.	
D	ML079	215.5	222.3	100	gn bk	fr	ZSKCS				0	cl mt po asp st ca	10	7		As above with increased magnetite and sulfide content.	
D	ML079	222.3	246.4	100	bk	fr	ZSKM				0	mt po asp st cpy	60	20		High grade magnetite skarn with a high sulphide content. Sulphides occur as blebs and stringers often >1 cm. Silver-grey sulphides possibly arsenopyrite or stannite are common. Locally preserved green amphibole gives the unit a mottled appearance.	
D	ML079	246.4	248.1	100	dgy gn	fr	STUF			sx	0.1	si cl po	0	4		Silicified SGWK with fine disseminated po. Po also occurs as stringers and blebs locally. Local patches of fracture related bleaching.	
D	ML079	248.1	250.6	100	bk gn	fr	ZSKM	ZSKCS			0	mt po py	15	10		Magnetite bearing calcsilicate with common stringers and blebs of po.	
D	ML079	250.6	262.7	100	gn	fr	ZSKCS			ca cl	1	cl po mt cpy	3	8		Green massive mottled to locally banded sulphide rich calcsilicate skarn. Po is the most common sulphide and occurs as blebs. Local bands and clots of disseminated magnetite. Local light green chlorite alteration. Magnetite content is variable throughout 	
D	ML079	262.7	268.2	100	lgn dgn	fr	STUF	XFBI		sx qz cl ca	3	cl po	0	2		Strongly silicified skarn is commonly banded. Chloirte veining and alteration related to a healed fracture stockwork is common throughout.	
D	ML079	268.2	277.5	100	bn	fr	ST	SS		qz sx cl	1	cl po si he	0	1		Siltstone with interbedded SGWK is locally silicified. Brown coloration throughout maybe indicative of hematite alteration. Local patches of bleaching haloing green chlorite rimmed po blebs. Sulphides and chlorite alteration end by 276.1 m.	
D	ML080	0	43.6	30	og bn	vox	ST	SS			0		0	0		"very weathered clay with iron staining. There are small patches of white clay and minor lithics, this unit is moist"	
D	ML080	43.6	47.1	50	gy	vox	ST	SS			0		0	0		"weathered SSLT and SGWK (ka and lm weathering). Rock types are no longer cohesive, but do not have iron staining. This unit is grading to rubble. "	
D	ML080	47.1	54.5	90	wt lgy	mox	STUF	ST			0	si 	0	0		light coloured highly silicified sediments. Bedding still visible in places where core is not rubble	
D	ML080	54.5	72.2	100	dgy lgy bn	fr	STUF	ZSKCS			0	si cc po py cpy cl bt	0	0		weak patchy magnetism possibly due to po. Lighter fine grained areas of this unit show higher amounts of cc and darker si. Some grains appear to be stretched and welded. Large replacement po circles ringed in light colour qtz. X mostly seem to be replacin	HQ starts at 61.4m
D	ML080	72.2	189.5	100	dgy gn bk	fr	SS	ST		qz cl sx	2	cl bt si cpy po	0	0		"beds of dominantly SGWK with increasing SSLT beds from ~90m depth. From 72.2-73m, near boundary with STUF there is a gradual change into SGWK beds with common bn mineral (bt?) and minor silicification. Cpy and minor po in qtz-cl vein at 80m depth. network"	
D	ML080	189.5	191	100	lgn dgy	fr	STUF			qz cl	20	si cl	0	0		"minor STUF, with high VL and VQL content"	
D	ML080	191	195.1	100	dgy	fr	ST	SS			0	cl	0	0		beds of SSLT and SGWK with minor STUF zones	
D	ML080	195.1	197.1	100	dgy cm lgn	fr	STUF			qz cl	20	si cl 	0	0		"STUF with a high % of VQL and VL, some equigranular cl crystals at 196.9m"	
D	ML080	197.1	245.5	100	dgy dgn	fr	SS	ST		qz cl mt sx	5	cl bt am mt po	0	0		"beds of SSLT and SGWK in similar proportions, VQL abundant with minor intermittent STUF style alteration. Altered SSLT/SGWK contain minor networking VL and VQL, zone which appears moderately brecciated and gouge. Possibly minor tourmaline on fracture face"	
D	ML080	245.5	259.5	100	dgy dgn bn	fr	STUF			qz cl	1	si cl bt po cpy	0	0		STUF with zones of bt skarn near contact with SGWK/SSLT. Mudstone beds show up silica alteration more clearly. Minor amounts of po and cpy S0 apparent with varying alteration bands picked out by colour changes.	
D	ML080	259.5	260.6	100	gy	fr	ZSKM				na	ac cc po	80	10		"ZSKM with irregular ""patches"" of am-cc-po alteration "	
D	ML080	260.6	264	100	gy gn	fr	ZSKCS	STUF	ZSKM		na	si ac vs mt po 	5	5		Ac-bearing ZSKCS with up to 10cm-thick mt-am-po ZSKM bands. Zones of STUF appear to overprint.	
D	ML080	264	268.4	100	gy	fr	ZSKM				0	ac cc po 	80	10		"ZSKM with irregular ""patches"" of am-cc-po alteration. 30cm thick qz-ac-vs ZSKCS band at 264.3. Po-rich zones occur sporadically i.e. at 266.2m."	
D	ML080	268.4	276.3	100	gn	fr	ZSKCS	ZSKM			na	cc po 	20	5		Coarsely mineralogically banded green (am +/- ep?) and pink (vs +/- gn?) ZSKCS with ZSKM bands. 	
D	ML080	276.3	281	100	gy 	fr 	ZSKM				na	cc ac po cpy	80	5		ZSKM with irregular ac-cc-po +/- cpy alteration. Alteration patches ranges from <1cm up to 20cm along core axis. 	
D	ML080	281	291.6	100	gy gn 	fr 	ZSKCS	ZSKM	STUF		na	si cc po 	10	10		"Coarsely banded ZSKCS and ZSKM with mottled STUF. Desseminated sulphide, chiefly po but also cpy is conspicuous and often, though not exclusively associated with mt. Secondary ac-cc alteration occurs."	
D	ML080	291.6	295.7	100	gy	fr	STUF	ZSKM			na	si po cl cc	5	10		Transition from ZSKCS to STUF. ZSKM persists as patchy cm-scale bands. Desseminated po conspicuous.	
D	ML080	295.7	306.5	100	gy	fr	STUF				na	si po cl cc	0	5		Chloritic STUF.	
D	ML080	308.4	325.6	100	gy	fr	ST	SS			na	si	0	1		Si SSLT and SGWK.	EOH - 324.6m
D	ML081	0	0.9	0	na	na	NREC				0		0	0		no recovery	
D	ML081	0.9	1.8	100	cm	fr	FG				0	ep tu	0	0		img hypidomorphic bt-FGRA tu and ep alteration 	
D	ML081	1.8	3.7	100	gy	fr	ST			bt	2	si cl bt	0	0		chloritic si SSLT with bt-veinlets	
D	ML081	3.7	5.3	100	cm	fr	FG				0	ep tu	0	0		bt porphyritic FGRA with tu and ep alteration 	
D	ML081	5.3	6.1	100	gy	fr	ST				0	si cl	0	0		chloritic si SSLT	
D	ML081	6.1	11.2	100	cm	fr	FG			tu	1	ep tu	0	0		img hypidomorphic FGRA with tu-veinlets 	
D	ML081	11.2	11.8	100	gy	fr	ST				0	si cl	0	0		chloritic si SSLT	
D	ML081	11.8	13.3	100	cm	fr	FG				0	ep tu	0	0		img FGRA 	
D	ML081	13.3	25	100	bn	fr	STUF			qz cl sx	5	si cl bt po	0	2		cl-bt-STUF with fine VQLX veinlets	
D	ML081	25	26	100	gn	fr	ZSKCS			qz	1	mt po cpy	50	5		gn-coloured mt-ZSKCS with conspicuous po-cpy associated with mt minor qz veinlets 	
D	ML081	26	30	100	cm	fr 	STUF			qz cl sx	5	cl	0	5		STUF with VQLX	
D	ML081	30	44.1	100	gn	fr	ZSKCS			qz cl sx	1	si cl mt po	30	5		silicified vs/ep?-bearing mt-ZSKCS po associated with mt minor VQLX veinlets 	
D	ML081	44.1	49.5	100	gy	fr	FG			qz	2	ep tu	0	0		porphyritic FGRA where contacts with skarn are assimilated tu alteration is conspicuous forming clots 	
D	ML081	49.5	52.1	100	gn	fr	ZSKCS			qz cl sx	3	si cl mt po cc	10	2		ZSKCS with minor mt 2ndry si-cl-cc throughout gradational to STUF	
D	ML081	52.1	61.3	100	bn	fr	STUF			cc qz vs	2	cl vs cc si	0	2		chloritic STUF fractures hosting 2ndry vs-cc-qz alteration	
D	ML081	61.3	86.2	100	cm	fr 	FG			qz tu	2	ep tu	0	0		img-icg bt-porphyritic FGRA and qz-porphyry ep and possibly cl record deuteric alteration tu alteration is intense forming melanocratic patches 	EOH
D	ML082	0	39	na	bn og	vox	ST	SS			0		0	0		VOX SSLT and SGWK	
D	ML082	39	56.15	na	gy	fr	ST	SS		qz ca sx	1	si cl po	0	2		Variably fractured and oxidised chloritic SSLT and SGWK with VQCX (po) and quartz-chlorite veins infilling fractures	
D	ML082	56.15	81.5	na	cm	fr	STUF			qz ca sx	1	si cl po	0	2		"Cl-STUF and cl-bt-STUF with VX, VQX and VQL. Cm to gn coloured cl-STUF is predominant between 56.2 - 64.8m and between 64.8 - 81.6m gn-bn coloured cl-bt STUF is predominant. The cl-bt STUF has distinctive whispy texture produced by extensive cl veining. T"	
D	ML082	81.5	98	100	bn gy	fr	SS	ST		qz cl	2	si cl bt	0	0		"sfg SGWK and SSLT. The SSLT is a resinous bn colour, possibly froas VQL from 1mm to 4cmm secondary bt. This unit also has a soft powdery mineral, that appears to disolve in HCL and coats fracture surfaces - stilbite?"	
D	ML082	98	102.1	100	gy	fr	STUF			qz sx	2	si cl bt po	0	0		"Cl-bt STUF with VQ, VX, VQX, VQL. This is a resinous brown coloured skarn with dark green cl associated with veining."	
D	ML082	102.1	129	100	gy	fr	ST			qz cl sx	5	si	0	2		"Dark grey SSLT with VQX and VQX (po, stilbite and epidote group minerals). The vein textures are network transitional to breccia."	
D	ML082	129	156.3	100	gn gy	fr	ST			qz cl sx	2	si cl cc st cpy	0	5		"Dark grey SSLT with quartz +/- stilbite +/- epidote +/- pyrrhotite. The network veins of quartz and chlorite become dominant down hole.  At 134m beds show grading down hole and at 141.7m there is a minor fault breccia with a matrix of stilbite, calcite an"	
D	ML082	156.3	157	100	dgy	fr	SS	ST			0.1	si cl cc po	0	0.1		SGWK groundmass with SSLT clasts. The clasts are sub-angular and vary in size from 2mm-1cm. Clasts maybe rip-up clasts.	
D	ML082	157	187.6	100	dgy	fr	ST	SS		sx qz cl ca	2	si cl cc x	0	5		"Silicified dark grey SSLT and SGWK with minor alteration mineralisation. At 159.3m there is possible loading indication younging down hole but, these could also be minor fracture disturbances. At 161.8m there are two beds that are fining up hole. "	
D	ML082	187.6	201	100	gn	fr	STUF			qz sx	10	si cl po 	0	2		Green chloritic STUF with quartz + phyrrotite +/- epidote. There are veins up to 15cm thick with some brecciation.	
D	ML082	201	214	100	gy	fr	STUF			qz cl sx	5	si cl po cc	0	10		This unit consists of a dark grey STUF with VQLX and VX that transitions to a very fine grained silicious meta-sediment. The pyrrhotite occurs as veins but also replaces the primary lithology with cauliform textures developed	
D	ML082	214	216.6	80	dgy gn bn	fr	XFBI	STUF	ST	sx	20	si cl qz cc po cpy	0.1	5		"Brecciated and re-cemented STUF and SSLT. The matrix consists of quartz, chlorite and clacite. There are veins and blebs of sulphides and some micro-folding."	
D	ML082	216.6	291.9	90	bn gn	fr	STUF			sx qz cl ca	2	qz bt cl cc po cpy	0	5		"This unit is STUF with bands of chlorite, biotite and pyrrhotite possibably following former bedding planes. There are thick (5cm), but rare VLQCX. Biotite decreases down hole and chlorite increases down hole to 220.9m. At 220.9m biotite becomes the domin"	
D	ML082	291.9	300.8	100	dgy	fr	SS	ST			0.1	cl qz ac po	0.1	0.1		"Patchy, weakly magnetic SGWK with minor beds of SSLT. This unit has limited alteration"	
D	ML082	300.8	303.5	100	bn gy	fr	STUF			qz ca	1	si bt qz po	0	1		Highly silicfied sediments with biotite and pyrrhotite forming along old bedding planes ans quartz and chlorite forming in veins.	
D	ML082	303.5	308.4	100	dgy	fr	ST	SS		qz cl	0.1	si cl po qz	0	5		"Silicified SSLT and SGWK with pyrrhotite disseminated, in blebs and in fractures. There are also infrequent quartz and chlorite filled fractures and veins"	
D	ML082	308.4	311	100	bn gy	fr	STUF			qz sx cl ca	1	si bt po cl qz cc	0	6		Pyrrhotite rich banded STUF with a cherty appearance. This unit also has thick minor VQXLC's	
D	ML082	311	330.1	100	dgy	fr	ST	SS		qz cl sx	1	bt qz po cl ep	0	1		dark gery SSLT and SGWK with pronounced bedding. Both silicification and and sulphide content decrease down hole as does veining. At 319.8 and 316.1m there are small bands of highly silicified SSLT ans SGWK containing epidote	
D	ML082	330.1	331	40	l gy wt pk	fr	XFBI	ST			0	cc qz cl	0	0		Brecciated SSLT that has been partially re-cemented with calcite and pink quartz and minor chlorite. The clasts of SSLT are angular and do not include SGWK.	
D	ML082	331	344.8	90	dgy	fr	SS	ST			0.1	cl qz sb cc ep	0	0		interbedded SGWK and SSLT with fractures filled with stilbite and calcite or chlorite	
D	ML082	344.8	347.5	100	l gy l gn	fr	SS	ST		ep qz cl ca	20	ep qz cl cc	1	0		"Light grey coarse grained SGWK with minor SSLT. This unit has a network of veins of epidote, quartz, chlorite and calcite"	
D	ML082	347.5	354.3	100	dgy	fr	SS	ST		ca ep qz	0.1	cc qz ep sb	0	0		Coarse grained SGWK and medium grained SSLT with minor veins of calcite and epidote or quartz. Fractures filled with stilbite.	EOH 354.3m
D	ML083	0	8.6	100	cm	fr	FG			tu	1	tu ep	0	0		bt-porphyritic FGRA with minor saussuritization and tu alteration. Lower contact sharp.	
D	ML083	8.6	10.3	100	gy	fr	ST			qz	1	si bt 	0	0		si-bt-altered SSLT.	
D	ML083	10.3	11.5	100	cm	fr	FG			qz tu	1	tu ep si	0	0		Porphyritic FGRA with tu-ep-si alteration and qz veinlets. A pegmatitic vein occurs at the upper contact. Upper and lower contacts sharp. 	
D	ML083	11.5	15.1	100	gy	fr	ST			qz	1	si bt po	0	1		si-bt-altered SSLT transitional to STUF. Minor qz veinlets and disseminated flecks of po.	
D	ML083	15.1	15.9	100	cm	fr	FG				0	tu ep 	0	0		Porphyritic FGRA with sharp upper and lower contacts.	
D	ML083	15.9	29.6	100	bn cm	fr	STUF			qz cl sx	2	si bt cl po	0	2		bt-STUF with bleached silicified bands. VQLX occurs with conspicuous cl/qz selvages. Minor disseminated po.	
D	ML083	29.6	37.5	100	cm	fr	FG				0	tu ep	0	0		Porphyritic FGRA with icg equigranular to pegmatitic patches. Pegmatitic parch between 131.0 - 131.4 is strongly ep altered. Tu alteration moderated throughout. Poor core recovery conceals upper contact but the lower is sharp. 	
D	ML083	37.5	40.4	100	gn	fr	ZSKCS			cl sx	2	si cl po sd	0	5		Strongly silicified and bleached ZSKCS. Possible siderite occurs with disseminated po.	
D	ML083	40.4	52.4	100	cm	fr 	FG				0	tu	0	0		Upper contact is sharp. Within 10cm of upper contact tu alteration is strong and associated with minor disseminated po. Body is icg equigranular bt-FGRA.	
D	ML083	52.4	53.8	100	gn	fr	ZSKCS				0	si	0	0		Extremely silicified ZSKCS partially assimilated with surrounding FGRA. 	
D	ML083	53.8	61.3	100	cm	fr	FG				0	tu	0	0		Away from assimilated margin FGRA is icg equigranular with minor tu alteration. 	
D	ML083	61.3	62.5	100	cm	fr	ZSKCS				0	si	0	0		Broad zone of wall rock assimilation characterized by extreme silicification. 	
D	ML083	62.5	73.5	100	gn gy	fr	ZSKCS			cl sx	1	si cl mt po	30	5		Silicified mt-rich ZSKCS. Disseminated po. Calc-silicate mineralogy appears to be almost exclusively dominated by dk gn amphibole. Lt gn si-cl patches give a mottled appearance. 	
D	ML083	73.5	96.4	100	cm gn	fr	STUF	ZSKCS		cl sx	1	si cl mt po cpy asp	10	5		Chloritic STUF possibly replacing ZSKCS. ZSKCS present as irregular patches and bands of mt+/-amhibole+/-po. Disseminated sulphide in STUF dominated bt po but minor cpy and arsenopyrite occur.	
D	ML083	96.4	106.7	100	cm bn 	fr 	STUF			qz cl	1	si bt	0	2		"Transition from above marked by loss of mt-bands, decrease in abundance of cl and increase in abundance of bt. Relict sandy beds preserved. Very fine VQL veinlets occur. Disseminated sulphide is minor. "	
D	ML083	106.7	109.1	100	bn	fr	STUF			sx	2	bt po cpy cl tp	0	30		Conspicuous po-cpy-bt-rich and cl-po-cpy-rich bands with possible topaz. 	
D	ML083	109.1	123	100	cm bn 	fr 	STUF			qz tu	5	si bt cl	0	5		bt-STUF with si-cl bleached bands. Distinctive veins dominated by qz+tu+po+/-cpy+/-topaz?+/-Fe-carbonate. 111.1m qz-tu vein approx 35%po 5%cpy. 113.6m qz-tu vein has produced an associated VQ stockwork with brecciated textures. 123.4m qz-tu vein contains 	
D	ML083	123	152.6	100	gy	fr	FG			tu	1	tu ep	0	0		"qz-tu vein marks contact. Top 1m of FGRA is gy and strongly tu-altered with distinctive tu spots with minor disseminated po associated. Body of FGRA is distinctly spotted qz- fl- porphyritic. Phenocrysts are subhedral, qz up to 1cm d, fl up to 2cm d. Tu a"	
D	ML084	0	43.7	70	rdog yw	mox	RCLY				0	ka lm he	0	0		"Very weathered orange clay, mostly cohesive with moderate recovery in places. Original textures and grains are very hard to see, but are weakly present. Red hematite staining."	
D	ML084	43.7	52	50	dgy wt lgy	wox	SS	ST			0	ka	0	0		Weakly to moderately weathered dk/ltgy to wit fine grained sediment altered to clay in places. Minor relict VQL.	
D	ML084	52	151.9	85	dgy dgn bn	fr	ST	SS		qz cl sx	1	cl bt po	0	0		dkgy/gn fine to medium grained sediments of predominantly SSLT and SGWK bed. Chlorite alteration in veins and occasionally patchy in bedding. Minor VQ that occasionally contain po/cpy. Weakly to moderately magnetic. Clear bedding planes present. Minor si 	
D	ML084	151.9	156.5	80	dgy lgy	fr	XFBI	XFBI			1	cl si ca	0	0		Brecciated SSLT / SGWK fault zone. Breccia clasts range in size from 0.5 to 5 cm. Two small areas of gouge at 152.8 and 156 m. Chlorite vein networking in more cohesive rock. Orange/red hematite-quartz-cl veining from 155.2 to 155.9 m.	
D	ML084	156.5	181.4	98	dgy lygy b	fr	SS	ST		cl qz ep	3	cl ep sb qz si ca	0	0		"Fine to medium grained SGWK interbedded with SSLT.  156.5-157.8m after fault zone, contains cl vein networking.  Minor cl, ep, stil, and qtz veining throughout rest of cohesive rock.  Unit is moderately fractured with some areas becoming rubbly.  Very wea"	
D	ML084	181.4	190	70	dgy	fr	XFBI	XFBI			0	cl ca	0	0		Brecciated fault zone with two small sections of gouge at186.5m and 189.5m.  Cl alteration coats surface of fractured and rubbly rocks.	
D	ML084	190	193.45	100	lygy wt dg	fr	STUF	ZSKCS		sx cl ca	2	si cl po py cpy ca do asp	0	2		"Minor calc-silicate patches amongst si altered sediment.  Disseminated po, cpy and py in ZSKCS zones, along with cl alteration.  Po, cpy, py, ca veining.  Non-magnetic."	
D	ML084	193.45	203.35	100	gn bn cm w	fr	ZSKCS	ZSKM	STUF	sx ca	2	ca do cl po bt cpy py si mt	1	15		Non-magnetic  apart from minor magnetite and pyrrhotite zones.  Large po mineralisation between 194.5-196m (disseminated and in veins).  Minor ca veins.  Magnetite mineralisation starts ~200.9m; occurs as disseminated and as large individual cubic crystal	
D	ML084	203.35	218.15	100	dgy bk dgy	fr	ZSKM	ZSKCS		qz bt	1	mt do cl po py cpy bt asp	50	20		"Magnetite is mainly disseminated and gives a mottled affect with do, po, py, bt and cl.  Occasional mt bands.  Sulphide veins contain po, py, cpy and asp.  Minor qtz-bt veins.  Green mica (clinochlore?) appears in veins with qtz and fsp."	
D	ML084	218.15	236.4	100	bn dgy lgy	fr	STUF	ZSKM	ZSKCS	sx qz cl ca	2	bt si do po mt cl fp ca	20	5		No magnetism from 218.15-219.7m- highly biotite altered zone.  Patchy magnetite zones from 219.7m onwards.  Magnetite occurs mostly in calc-silicate and po-rich regions.  Highly silicified zones mostly magnetite free.  Banding (bedding?) is present in sed	
D	ML084	236.4	240.25	90	lgy	fr	XFBI	XFBI		cl ca	10	cl ca	0	0		Fault gouge between 236.55-236.85m.  Brecciated zone between 237-240.25m- mostly cemented by cl alteration on fracture surfaces and veining. Non-magnetic.  Minor ca veins.	
D	ML084	240.25	256.1	98	lgy dgy bn	fr	ST	SS		ca fl bt	2	cl si bt fp qz ca	0	0		ltgy-dkgy SSLT interbedded with fine-medium grained SGWK.  240.25-245.6m  is fractured wallrock from fault zone.  Non-magnetic. 15cm fp-ca vein at 247.5m. 8cm fp-tu-bt vein (possibly dyke/sill from granite).  Mod-high bt alteration from 254-256m just befo	
D	ML084	256.1	260	100	wt cm bk y	fr	FG			tu	2	ep tu	0	0		fp-qtz-bt-ep-rich granite intrusion into SSLT/SGWK.  Tourmaline is present mainly in veins.  Zones of equigranular medium grained crystals and coarse-grained crystals.	
D	ML084	260	266.37	100	dgy	fr	SS	ST		ca qz bt	1	bt ca qz	0	0		Medium-grained dkgy SGWK with minor beds of SSLT.  Bt-qtz and ca veins.  Small white elongate crystal flecks from 264.5-265.8m.	
D	ML084	266.37	313.9	100	wt cm bk y	fr	FG			tu bt	1	ep tu asp	0	0		"Porphyritic granite; fp-Kspar-qtz-ep phenocrysts up to ~2cm; groundmass consists of qtz, fp, k-spar, bt and ep.  Minor tu-bt veins.  Minor asp sprinkled throughout.  ~10cm bt-tu-py vein at 279.7m.  ~40cm tu-bt-fp-qtz vein at 293.5m."	EOH 313.9m
D	ML085	0	23.7	50	gy	fr	ST			qz cl sx	2	cl bt	0	1		chloritic gy SSLT with minor 2ndry bt (especially in sandier fractions) minor VQLX Fe-hydroxides coat J 	
D	ML085	23.7	30.2	100	gy 	fr 	ST			qz cl sx	4	cl bt 	0	1		gradational increase in amount of bt and veining towards STUF transition	
D	ML085	30.2	47.4	100	gy gn 	fr	ST			cl sx	2	cl po 	0	2		variably developed bt-bearing STUF	
D	ML085	47.4	49.5	100	gn	fr 	XFBI	ST		cl	50	cl	0	0		"extensive chloritization of STUF by prevasive VL network producing some brecciation, weakly faulted zone"	
D	ML085	49.5	62.4	100	gy gn 	fr 	ST			cl sx	2	cl po 	0	2		resumption of bt-bearing STUF	
D	ML085	62.4	90	100	gy 	fr 	ST	SS		qz cl	2	si cl 	0	0		"si gy SSLT with some beds normally grading to SGWK, gradation appearance of cm & gn STUF"	
D	ML085	90	118	100	gy bn 	fr 	STUF			cl sx	4	si cl po 	0	2		bt-bearing STUF with conspicuous cm-gn-coloured cl-rich zones relatively minor VLX stilbite coats J	
D	ML085	118	127.1	100	bn gy 	fr 	STUF			qz cl sx	10	si cl po 	0	2		veining as VQLX becomes more intense towards FGRA contact 	
D	ML085	127.1	147.5	100	cm 	fr 	FG			tu qz	2	ep tu 	0	0		very sharp contact between STUF and ifg to img qz-fl-bt- porphyritic FGRA ep-alteration is strong at upper contact fine qz-veinlets cross-cut contact	
D	ML085	147.5	159	100	gn 	fr 	ZSKCS 			tu sx	5	py cc cl po 	0	5		direct FGRA lower contact not observed but adjacent 50cm of ZSKCS is strongly chloritized with up to 10% 2ndry py as well as carbonated veinlets away from contact ZSKCS is mottled bt-po-bearing with up to 1cm thick qz-tu-po veins	
D	ML085	159	162.5	100	gn 	fr 	XFBI	ZSKCS		ca	10	cc py 	0	0		between 159 and upper FGRA contact ZSKCS core is rubbly with abundant cc veinlets and 2ndry py	
D	ML085	162.5	233.1	100	cm	fr	FG			qz tu	2	ep tu 	0	0		"5cm thick FGRA vein at 162m FGRA alternating as diffuse meter to decimeter scale bands between strongly porphyritic and coarse-grained equigranular; porphyritic variety is gy-coloured with euhedral qz up to 1cm, strongly saussuritized subhedral to anhedra"	
D	ML085	233.1	407.9	100	cm	fr	FG			qz tu	2	ep tu	0	0		From 233.1 FGRA has icg equigranular texture. Tu-ep alteration is moderate to strong with tu forming  irregular patches up to 10cm thick.	
D	ML086	0	3.8	60	dgy	fr	ST				0	si po	0	0		Moderately silicified SSLT with minor po	
D	ML086	3.8	6.7	80	lgy og	fr	FG				0	qz fp bt am ep	0	0		Iron stained equigranular  FGRA with occasional FP and QZ phenocrysts. This unit becomes more felsic close to contacts and hirnblende is also concentrated in this area	
D	ML086	6.7	16.9	98	dbn	fr	STUF			qz sx	0.1	si bt qz py cpy po	0	5		Bt rich STUF with disseminated sulphides and sulphides found in veinlets with qz. At 8.5 - 9m there is a large qz vein with a bt vein running parallel to it from 8.8 - 9m. At 16.8m there is a minor FGRA dyke with a xenolith and minor ep.	
D	ML086	16.9	18.8	95	lgy	fr	FG				0	qz fp am bt tu ep	0	0		Equigranular qz fp am bt FGRA with minor tu and ep. At 18.8m there is a either a xenolith or and onclave that is 5cm in diameter	
D	ML086	18.8	40.1	100	lgy bn	fr	STUF			qz ca	0.1	si bt cl py cpy cc qz po	0	5		"BT rich STUF with disseminated sulphides and sulphides also found growing along remenant bedding planes. BT content decreases down hole and the unit becomes pale greay due to intense silicification. CC, qz and po are very minor and only found near the up "	
D	ML086	40.1	43.9	100	bn	fr	ZSKCS				0	am do cc mt cl si py cpy	20	5		"ZSKCS with mt found in blebs and bands. This unit contains moderate amounts of silica, a possible over wash?"	
D	ML086	43.9	47.9	100	bk bn	fr	ZSKM 	STUF			0	am mt cc do si cpy py po	50	2		ZSKM with bands of STUF	
D	ML086	47.9	51.1	100	bn cm	fr	ZSKCS				0	am cc do mt po py cpy	20	2		ZSKCS with actionolite being the dominant amphibol rather than hornblende	
D	ML086	51.1	52.9	100	gy	fr	ZSKM				0	mt am si po cpy cc py asp	60	2		ZSKM with mt increasing close to contact. Minor asp or stanite found in this unit	
D	ML086	52.9	55.7	100	gy	fr	FG			qz ca	0.1	qz fp bt tu cl	0	0		Medium grained FGRA with veins of tu at 53m. These veins are 10 and 58cm thick. There are also thick cl veins at 54.7m	
D	ML086	55.7	69.5	100	gy wt	fr	FG				0	qz fp bt tu	0	0		Coarse grained FGRA with concentrations of tu.	
D	ML086	69.5	71.9	100	gy	fr	FG				0	qz fp bt tu ep	0	0		Fine grained FGRA with phenocrysts of fp (possibably orthoclase). This unit has mionr ep at 168.6 and veinlets of tu	
D	ML086	71.9	78.5	100	bn gy	fr	ZSKCS	STUF			0	cl vs am bt do cc py po qz	15	5		"Vs and do rich ZSKCS with mt and occasional bands of STUF. The am in this ubnit are mostly hornblende and actiolite. At 47.4m there is a 30 cm thick, very felsic granite dyke with chlorite alteration"	
D	ML086	78.5	96.8	100	gy bn 	fr	STUF			qz ca sx	2	si bt cl am po py cpy qz	0.1	5		"Weakly magnetic banded dk gy, lt gy and bn STUF with sulphides found in veinlets and the occasional bleb. AM (hornblende) found in the first 5m of this unit, as individual crystals or in aggregate bands. From 94 - 96.8m the unit is almost exclusively bt a"	
D	ML086	96.8	97.6	100	lgy	fr	FG				0	qz fp bt ep	0	0		Medium grained qz fp bt FGRA with minor ep and phenocrysts of both qz and fp.	
D	ML086	97.6	106.5	100	bn	fr	STUF			sx	0.1	si bt cl po cpy cc py	0	5		Extremely bt rich STUF with sulphides found in bands and blebs. Bt and si comprise around 90% of this unit.	
D	ML086	106.5	124.5	na	dgy	fr	SS	ST		qz sx	0.1	cl qz cpy	0	0.1		Dark grey SGWK with minor beds of SSLT. Alteration in this unit is limited to small patches of cl with bleached haloes and very minor VQX	EOH=124.5m
D	ML087	0	11.1	50	bn gy 	wox	R				0	clay	0	0		Rubbly bn gy sslt weathered to clay. 	
D	ML087	11.1	23.3	50	og bn 	vox	RCLY				0	clay	0	0		Fe-rich clay after either SSLT or possibly ZSKCS.	
D	ML087	23.3	26.3	70	og 	mox	XFBI	ST			0	clay	1	0		Fe-rich brecciated SSLT which has maintained some of its original structure. Unit becomes less Fe-rich and more clay rich down hole.	
D	ML087	26.3	29.5	90	gn bn	mox	ZSKCS	ST			0	cl mt cc clay 	10	0		Weathered chloritic SSLT/ZSKCS with blebs of mt. Some disseminated cassiterite. 	
D	ML087	29.5	51.3	60	og	mox	RCLY				0	clay mt 	2	0		This unit ranges from cohesive bleached Fe-stained SSLT to incohesive vox Fe-stained clay. Magnetism is only patchy. 	
D	ML087	51.3	58.9	80	bk gn bn 	fr	ZSKCS	STUF			0	si cl bt py cpy cs st po cc	1	10		Sulphide rich with visable patches of cassiterite (10%) and stanite (2%). This unit has small bands of STUF. The unit is wox for 2m then fr.	
D	ML087	58.9	144.6	100	gy 	fr 	ST	SS		qz cl	2	si cl	0	0		Si chloritic SSLT with minor SGWK beds 	
D	ML087	144.6	145.3	100	cm	fr 	FG				0	tu	0	0		ifg FGRA dyke with very sharp irregular orientated contacts	
D	ML087	145.3	146.5	100	gy 	fr	ST			qz ca	2	si cl 	0	0		si chloritic SSLt with VQC infilling late stage fractures	
D	ML087	146.5	164	100	cm	fr	FG				0	tu ep	0	0		"Very sharp upper contact of FGRA, diffuse banding on m-scale between ifg hypidomorphic and qz-fl-bt porphyritic. Phenocrysts afe subhedral, fl saussaritized, minor tu alteration as clots and diffuse veins. "	
D	ML087	164	165.3	100	gn	fr 	XFBI	FG			0	cl	0	0		Silicified and cohesive brecciated FGRA with c. 10% chloritic matrix. Og-coloured fl. 	
D	ML087	165.3	167	70	gn	fr	ST			qz ca	5	cl	0	0		Rubbly gn chloritic SSLT with abundant VQC veinlets and tension gashes. 	
D	ML087	167	174.4	100	gy 	fr 	ST	SS		qz	2	si cl	0	0		si chloritic SSLT with minor SGWK beds. VQ infilling fractures.	
D	ML087	174.4	176.3	70	gn	fr	ST				0	cl	0	0		Rubbly chloritic SSLT .	
D	ML087	176.3	176.5	100	gn	fr 	XFBI	FG			0	cl	0	0		Upper contact brecciated and mechanically mixed with above chloritic rock. 	
D	ML087	176.5	192	100	cm	fr 	FG				0	tu ep	0	0		"FGRA ranges from ifg hypidomorphic to ifg bt-porphyritic to img qz-fl-bt porphyritic. 20cm thick pegmatic body at 180m. Tu  alteration is moderate, ep alteration very minor. Lower contact poorly preserved but appears sharp without evidence of brecciation."	
D	ML087	192	194.9	100	gn	fr 	ST			qz	1	si cl	0	0		Rubbly chloritic SSLT .	
D	ML087	194.9	207.9	100	cm	fr 	FG				0	ep tu 	0	0		"Upper contact fractured and infilled by VL for upper 10cm. FGRA is qz-fl-bt-porphyritic. Contains dark gy qz-rich irregular to sphericle patches - assimilated wall rock? Tu alteration moderate, ep alteration minor. "	
D	ML087	207.9	208.2	100	gn	fr 	ST			qz	10	si	0	0		30cm band of intensely qz-veined si SSLT with sharp upper and lower contacts. 	
D	ML087	208.2	233.8	100	cm	fr 	FG				0	tu ep	0	0		qz-fl-bt- ifg to icg porphyritic FGRA with m-scale bands with icg hypidiomorphic texture. 	
D	ML087	233.8	234.5	100	bn gy 	fr	STUF	XFBI		qz	30	si bt 	0	0		Cohesive bt-STUF breccia. Small xenoliths of bt-STUF contained in immediately adjacent upper and lower FGRA contacts.	
D	ML087	234.5	236.8	100	cm	fr	FG				0	tu	0	0		ifg FGRA dyke 	
D	ML087	236.8	237.8	100	bn gy 	fr	STUF			qz cl	30	bt si cc cl py cpy	0	0		"si-bt altered SGWK and SSLT, sharp contact with avove FGRA, VQL intense "	
D	ML087	237.8	245.6	70	gn	fr	STUF				0	cl	0	0		Rubbly chloritic STUF at transiton to ZSKM.	
D	ML087	245.6	252.4	100	dgy	fr 	ZSKM 			ca	1	mt cl ac po cpy cc py sb	70	5		Fractured and rubbly ZSKM from 245.6 to 248.3. Mt banded and massively disseminated. Minor bands of ZSKCS. Minor VC. 	
D	ML087	252.4	252.8	100	cm	fr 	FG	ZSKCS 			0	si 	0	0		Sheared si-rich FGRA dyke. 	
D	ML087	252.8	265	100	dgy	fr 	ZSKM 	ZSKCS		ca	1	mt cl ac po cpy cc py sb	70	5		Mt banded and massively disseminated. Minor bands of ZSKCS. Minor VC.	
D	ML087	265	287.8	100	dgy gn	fr 	ZSKM 	ZSKCS 		ca sx	3	cc ac mt cl do cpy stb py po	50	5		Banded ZSKM and ZSKCS with VC. Proportion of ZSKCS increases down hole. 	
D	ML087	287.8	299.2	100	dgy gn	fr 	ZSKCS 	STUF	ZSKM 	ca sx	2	cc cl ac si mt po cpy py gn do bt	10	3		Banded ZSKCS and STUF (STUF overprinting?) with minor ZSKM bands	
D	ML087	299.2	299.3	100	cm	fr 	FG				na	tu cl	0	0		qz-tu rich FGRA with cl alteration	
D	ML087	299.3	306.7	100	dgy gn	fr 	ZSKCS 	STUF	ZSKM 	ca sx	2	cc cl ac si mt po cpy py gn do bt	10	3		Banded ZSKCS and STUF (STUF overprinting?) with minor ZSKM bands	
D	ML087	306.7	313.2	100	gy 	fr 	STUF	ZSKCS		cl sx	1	si bt cl cc po py mt 	2	2		bt-rich ZKSQ with minor zones of mt-ZSKCS. Some bt-rich zones contain disseminated sulphide. 	
D	ML087	313.2	334.5	100	cm	fr 	FG			tu	1	ep tu 	0	0		"Equigranular bt-FGRA, ep alteration throughout, tu as patches and veins. Very minor sulphides as rare alteration. "	EOH 334.5m
D	ML088	0	9.9	100	cm	fr 	FG				0	tu ep	0	0		Porphyritic bt-FGRA with moderate tu alteration. Band of bt-rich STUF occurs between 1.5-2m with sharp contacts with enclosing FGRA.	
D	ML088	9.9	16.5	100	bn	fr	STUF			qz	1	si bt cl po	0	1		Bt-rich STUF with gn cl-rich alteration associated with dissemenated po. 4cm FGRA vein at 10.5m with sharp contacts.	
D	ML088	16.5	17.6	100	cm	fr	FG				0	tu ep	0	0		FGRA dyke with strong tu and ep alteration.	
D	ML088	17.6	19.8	100	bn	fr 	STUF			qz	1	si bt cl po 	0	1		Bt-rich STUF with variable cl and minor po.	
D	ML088	19.8	20.4	100	cm	fr 	FG				0	tu ep	0	0		FGRA dyke with strong tu and ep alteration.	
D	ML088	20.4	25.5	100	bn	fr 	STUF			qz	1	si bt cl po	0	1		Bt-rich STUF with variable cl and minor po.	
D	ML088	25.5	77	100	cm gy 	fr 	FG			tu	1	tu ep	0	0		Porphyritic and icg equigranular FGRA coarsely banded at a m-scale. Tu alteration as diffuse veins associated with ep alteration. Plag strongly saussaritized. Large white fl phenocrysts in gy porphyritic FGRA produces a distinctive spotted rock. 	
D	ML088	77	80	100	na	fr 	STUF	FG			0	si tu ep 	0	0		Contact zone between upper FGRA body and STUF with several closely spaced tu-altered FGRA dykes. Suggestive of a sill-like body emplaced as a series of concordant dykes? STUF has strong green-pink coloured alteration.	
D	ML088	80	87.9	100	bn	fr 	STUF			qz	5	si bt cl po	0	1		Bt-rich STUF preserving original clastic textures. Cm-coloured bleached zones. Irregular VQ networks.	
D	ML088	87.9	88.5	100	cm	fr	FG				0	tu ep	0	0		Strongly tu-altered FGRA dyke.	
D	ML088	88.5	99.3	100	bn	fr	STUF			qz	5	si bt cl po	0	0		Bt-rich STUF preserving original clastic textures. Cm-coloured bleached zones. Irregular VQ networks.	
D	ML088	99.3	103.8	100	gn	fr 	ZSKCS			qz cl	1	mt si cl po	15	1		Mt-ZSKCS with bleached si-cl zones. Mt occurs as irregular bands.	
D	ML088	103.8	147.8	100	cm	fr	FG				0	tu ep	0	0		"Contact with above ZSKCS partially obscured by intense silicification. Gy-porphyritic ""spotted"" FGRA with large (up tp 2cm) phenocrysts of fl (K-spar?). Tu alteration is weak and disseminated throughout. Minor saussaritization of plag. Texturally homogeno"	
D	ML089	0	38	30	og yw	vox	RCLY				0	ka il he	0	0		"Iron stained, deeply weathered regolith clay"	
D	ML089	38	42	50	lgy	mox	STUF				0	si ka mt	0.1	0.1		Weathered ka rich STUF with minor dedretic magnetite veinlets	
D	ML089	42	62.1	90	lgy	fr	STUF			qz sx	1	si bt cl py qz po cpy	0.1	2		Biotite rich STUF with sulphides and quartz found in veins or along remnant bedding plane. This unit also has pyrite shaped vugs.	HQ finishes at 50m
D	ML089	62.1	65.9	30	dgy	fr	XFBI	ST	lSS		0	si ka il cl 	0	0		Intensely fractured and silicified SSLT and SGWK. This unit has not been re-cemented.	
D	ML089	65.9	120.4	98	dgy	fr	ST	SS	STUF	cl sx	5	si cl st py	0.1	1		Moderately silicified SSLT and SGWK with chlorite found in veins and blebs. This unit has stilbite and pyrite found in veins.. There is a pronounced STUF unit found at 104.2 - 104.9m. At 85.4m there are two ovals of greywacke within a siltstone unit. Poss	
D	ML089	120.4	120.7	100	pk	fr	FG				0	qz fp bt cl	0	0		Fine to medium grained pink quartz and feldspar rich granite dyke with chlorite alteration and blaeching at contacts. Both contacts are 45 degrees from core axis.	
D	ML089	120.7	127	98	dgy	fr	ST	SS		qz cl ca	0.1	si cl qz cc	0.1	0		"Patchy weak magnetic SSLT and SGWK with qz, cl and cc in veins"	
D	ML089	127	127.6	100	pk	fr	FG				0	qz fp bt ep cl	0	0		Fine grained qz and fp rich granite with bt. This unit also has epidote and chlorite	
D	ML089	127.6	128	100	dgy	fr	ST	SS		qz cl ca	0.1	si cl qz cc	0.1	0		"Patchy weak magnetic SSLT and SGWK with qz, cl and cc in veins"	
D	ML089	128	128.5	100	pk	fr	FG				0	qz fp bt ep cl	0	0		Fine grained qz and fp rich granite with bt. This unit also has epidote and chlorite	
D	ML089	128.5	135.3	70	dgy	fr	ST	SS		qz	0.1	si cl qz	0	0		Weak patchy magnetic SSLT and SGWK that is highly fractured	
D	ML089	135.3	138.1	80	pk lgy	fr	FG				0	qz fp bt cl cc st ep	0	0		Medium grained FGRA with the occasional phenocryst of k-feldspar (possibably orthoclase). Both these contacts are undulating	
D	ML089	138.1	196.9	95	dgy	fr	ST	SS		qz	0.1	si cl cc st py	0.1	0.1		"Silicified SSLT and SGWK with blebs of chlorite increasing down hole. Pink, green and white xeolites found in fractures. At 141.4m there is a bed of rip up clasts and bed fining that suggestsbeds are younging up hole. At 180.5 there is possible loading su"	
D	ML089	196.9	200.2	100	dgy gn	fr	ST	SS		cl qz ca	50	cl si cc	0	0		Intensely cl veined SSLT and  SGWK with minor VQC	
D	ML089	200.2	202.5	60	gy	fr	XFBI	ST	lSS		0	ka cl si	0	0		Fault brecciated SSLT and SGWK with 50% of the unit re-cemented	
D	ML089	202.5	206.1	95	lgy bn	fr	STUF			cl ca qz	5	si bt qz	0	0		Carbonate and chlorite veined STUF that is bt rich. The veins of quatrz in this unit show a brecciated texture.	
D	ML089	206.1	213.8	80	bn	na	XFBI	STUF		qz sx	5	si bt qz py	0	0.1		Brecciated STUF. Around 20% of this unit holds it cohesion and about 20% has been re-cemented.	
D	ML089	213.8	217.5	100	lgn bk	fr	ZSKCS			qz ca	1	ep cl mt cc cpy py vs po	20	1		Magnetic ZSKCS with the mt content increasing down hole from 5 to 20%. The sulphides and mt in this unit is disseminated and there is network veining of VQC	
D	ML089	217.5	221.3	90	lgn bk	fr	ZSKM			ca	1	mt ep cl cc	60	1		ZSKM with minor cc veins	
D	ML089	221.3	230.2	90	lgy	fr	FG			qz	0.1	qz fp bt tu ep py	0	0.1		icg FGRA with pheoncrysts of k-feldspar. This unit is highly fractured	
D	ML089	230.2	239	98	gy	fr	ST	SS	STUF	qz	0.1	si bt cl po cpy	1	0.1		Silicified SSLT and SGWK with minor STUF	
D	ML089	239	239.5	100	lgy wt	fr	FG				0	qz fp ep bt tu cl	0	0		icg FGRA with blebs of cl and ep	
D	ML089	239.5	251.3	100	dgy	fr	ST	SS		qz	0.1	si cl bt	0.1	0		Silicified SSLT and SGWK with bt content increasing close to the granite content	
D	ML089	251.3	296.1	100	lgy	fr	FG			bt tu	0.1	qz fp bt cl ep	0	0		icg equigranular very felsic FGRA with veins and concentrations of tourmaline +/- bt.	EOH is 296.1m
D	ML090	0	12.1	40	bk dgy og	wox	ST	SS		qz cl	2	cl	0	0		weakly weathered SSLT-SGWK; moderately fractured/rubbly core with original textures and grains preserved; dkbn possibly hematitic staining; non-magnetic.	
D	ML090	12.1	61.1	50	og yw bn	mox	RCLY			qz cl	5		0	0		"moderately to very weathered rock.  Most of the rock has been altered to clay, however veining textures still apparent.  Bk striated veins, possibly weathered VQL.   At 38.3m there is vuggy core, possibly representing the once present sulphides."	
D	ML090	61.1	69.5	95	dgn dgy	fr	ZSKCS	STUF		ca sx	5	po am si cpy mt	2	30		ZSKCS with po making up >30% of the rock unit. Po is concentrated in bands and ds throughout.  Minor 2-3cm band of mt at 62m and between 67 to 67.5m where it is more patchy.  Possibly minor arsenopyrite ds throughout unit.  This unit also contains a moder	
D	ML090	69.5	71.6	80	dbn dgy gn	fr	STUF			qz cl	10	si bt po cl  	0	5		minor bt STUF with po replacing an original 'whispy' texture on a mm-scale.	
D	ML090	71.6	97.15	90	dgy dgn bk	fr	ST	SS		qz cl ca	2	cl bt	0	0		SSLT-SGWK with VQL and minor VC. Very minor bt bands at 85.9m.	
D	ML090	97.15	98.2	90	wt cm bk	fr	FG			qz tu	2	ep tu	0	0		ifg qtz-feldspar-bt and tourmaline dominant granite dyke; ~10cm VQT at 97.4m.	
D	ML090	98.2	164.3	98	dgy bk	fr	SS	ST		qz cl tu	2	cpy po	5	0		"SGWK-SSLT sharp contact with granite dyke, qtz veins increasing to near granite dykes. younging DH. 15cm granite dyke at 100.85m of similar composition to previous dyke.  At 104.4m-cpy filling thin <1cm wide VQL. FGRA dyke from 107.6-108.25m, ifg granite "	
D	ML090	164.3	167.3	90	wt bk cm	fr	FG			qz tu	1	ep fl cl	0	0		"img granite with small <1cm fsp phenocyrsts. Qtz-fsp-tu-rich granite.  Mostly plag, with minor k-spar."	
D	ML090	167.3	185.3	70	dgy dgn bk	fr	SS	ST		qz cl ca	2	cl	2	0		"SGWK-SSLT rock units fractured with poor recovery in places.  At ~179-184m rock contains high proportions of VC; veins appear moderately dissolved, leaving vugs."	
D	ML090	185.3	187	80	dgy dgn bk	fr	XFBI	SS	ST	ca	2	cl	0	0		brecciated/rubbly SGWK-SSLT with cc veins	
D	ML090	187	223	70	wt cm bk d	fr	FG				2		0	0		"ifg-img qtz-fsp-tu-bt-rich granite, highly fractured.  Overall recovery is poor, granite is moderately fractured.  At 203.7-204.8m fractured SSLT with 1-2cm granite dyke running parallel to core axis through it."	
D	ML090	223	255	50	dgy dgn bk	fr	SS	ST		qz cl ca	1	cl si sb	0	0		"poor core recovery, blocky rubbly core.  Beds of SSLT-SGWK. Hard to piece together for structural readings. SSLT-SGWK often contains cl and qtz veins.  Very minor po in core qtz-cl veins.  At 243.7m- small 15cm brecciated/networking vein zone containing c"	
D	ML090	255	262.4	80	dgy dbn gn	fr	STUF			qz cl	2	si bt cl cc	0	0		gradadtional change into more altered rock containing more si.  STUF contains appreciable amounts of bt; common qtz-cl veins.	
D	ML090	262.4	264.2	60	dgn dgy	fr	XFBI				2	cl mt po	2	5		"fractured STUF which becomes altered to a soft cohesive rock that exhibits brecciation. Matrix contains cl, si, mt; clasts appear to be STUF developing into mt and ZSKCS clasts.  Fault gouge ~15cm at 263.5m."	
D	ML090	264.2	276.2	100	dgn dgy	fr	ZSKM			ca sx	1	mt am cl cc si po cpy	50	2		high content of patchy and apparently banded mt with VC and minor VX (mostly cpy) and ds po and cpy interbedded bands and zones of ZSKCS	
D	ML090	276.2	283	100	dgy dgn	fr	ZSKCS			qz cl sx	1	si mt cc am cl cpy po asp	35	5		ZSKCS with high values of mt. ZSKCS here contains high amounts of si.	
D	ML090	283	285.1	100	wt dgn	fr	FG			qz ca cl	1	cl ep	0	2		ifg- img FGRA with small phenocrysts of qtz and fsp.  Small amounts of py in VQL. ~15% bt and or tu flecks throughout granite.	
D	ML090	285.1	289	100	dgy dgn bk	fr	ZSKCS				2	si cl mt vs po py	10	5		silicified ZSKCS with a small cl veined granite dyke from 285.6 to 285.9m.  Another dyke from 286.7-286.8m. ZSKCS contains patchy ds mt.	
D	ML090	289	289.6	100	wt bk cm	fr	FG			qz tu	50		0	0		ifg granite dyke with large amounts of tu and VQT from 289.5-289.8m 	
D	ML090	289.6	291.1	100	dgn dgy	fr	ZSKCS			qz ca cl	2	si mt po am	30	10		ZSKCS with ds mt and patchy po around VQCL at 290.3m	
D	ML090	291.1	292.4	100	wt gn bk	fr	FG			qz tu	50	ep bt	0	0		"ifg-img FGRA with fsp and qtz phenocrysts; ds tu and VQT.  Considerable ep alteration.  Near margin with ZSKCS, granite appears blue and contains bands of bt."	
D	ML090	292.4	301.9	100	dgn dgy	fr	ZSKCS			qz cl	1	si mt vs cl po	20	5		silicified ZSKCS with abundant vs and cl veining. FGRA dyke with qtz-fsp phenocrysts.  FGRA dyke from 296.6-296.7m.  FGRA dyke from 298.3-298.55m.	
D	ML090	301.9	326.6	100	wt gn cm	fr	FG			qz tu	2	ep	0	0		img FGRA with qtz and fsp phenocrysts and flecks of bt and tu.  Bt abundant ~5-10%.  Significant alteration throughout.veins of qtz-tu common ranfing from a few cm's thick to 0.5m. Rectangular euhedral phenocrysts of fsp present; different from dykes in Z	EOH=326.6m
D	ML091	0	11	na	gy	fr	ST	SS		qz sx	1	cl py sb	0	1		"Rubbly, fractured core with limonite coating fractures on upper 8ms. Gy si cl SSLT with minor SGWK beds. Zeolites occur on fracture surfaces along with qz and minor py."	
D	ML091	11	28	na	gy	fr	ST	SS		qz sx	1	cl py sb mt	1	1		Gy moderately magnetic si chloritic SSLT and SGWK.	
D	ML091	28	32	na	gy 	fr 	ST	SS		qz cl sx	1	si cl bt py	0	1		"Transition to STUF marked by significant drop in magnetism, apperance of secondry bt and silicification controlled by irregular fractures."	
D	ML091	32	82.8	na	bn	fr	ST	STUF		qz cl ca sx	4	si bt cl po py sb	0	1		Bn-coloured  bt-altered ST and STUF  with cm-gn-coloured bleached bands and irregular silicified fractures. Minor py and zeolite persists coating late? Fractures. Po occurs as thin bands and blebs parallel to colour banding in STUF (also as VQLX in silici	
D	ML091	82.8	83.3	na	na	fr	XFBI				na		0	1		broken zone in bt-altered ST	
D	ML091	83.3	108	na	na	fr	ST	STUF			na		0	1		Bn-coloured bt-altered ST and STUF with cm-gn-coloured bleached bands and irregular silicified fractures. Minor py and zeolite persists coating late? Fractures. Po occurs as thin bands and blebs parallel to colour banding in STUF (also as VQLX in silicifi	
D	ML091	108	128	na	gy	fr	ST	SS		qz ca sx	1	si cl bt po	0	1		Gy si SSLT and SGWK. Transition from STUF marked predominantly by reduction in bt. Silicified fractures still occur but less frequently.	
D	ML091	128	129	na	bn	fr	STUF			qz	1	si bt 	0	0		Band of bt-STUF with pk-coloured porphyroblasts.	
D	ML091	129	136	na	gy	fr	ST	SS		qz ca sx	1	si cl bt po	0	1		Gy si SSLT and SGWK.	
D	ML091	136	157.4	na	gy	fr	ST	SS		qz ca cl sx	2	si cl bt po py cc sb	0	1	fr	Fracturing in SSLT and SGWK becomes notably more intense. 	
D	ML091	157.4	157.6	na	gn	fr	XFBI				0		0	0	ft	20cms of gn-coloured gouge.	
D	ML091	157.6	162	na	bn	fr	STUF			qz ca cl sx	5	si bt cl po py cc sb	0	2	fr	Intensely fractured bt-STUF.	
D	ML091	162	163.5	na	gn	fr	ZSKCS			qz ca cl sx	2	si po py	0	5		Band of ZSKCS with disseminated po approaching 5%. Same style of fracturing as encloing STUF but intensity has deceased.	
D	ML091	163.5	168	na	bn 	fr 	STUF			qz ca cl sx	1	si bt cl po py cc sb	0	2		Bt-STUF.	
D	ML091	168	169.9	na	bn	fr	STUF	FG			10	si bt po	0	1		Bt-STUF close to FGRA contact intruded by a series of thin fine-grained granitic veins with qz-fl-tu-ep-po mineralogy.	
D	ML091	169.9	170.6	na	cm	fr 	FG				0	ep tu 	0	0		Upper 70cm of FGRA has fine-grained chilled? Texture with strong ep-tu alteration. Sharp contact with skarn.	
D	ML091	170.6	187.5	na	cm	fr	FG			tu	1	tu ep	0	0		Icg equigranular FGRA with variable tu-ep alteration and diffuse tu veins and patches. Lower contact sharp.	
D	ML091	187.5	190.5	na	bn	fr	STUF			qz sx	1	si po	0	1		Strongly silicified STUF with disseminated po and VQX-po.	
D	ML091	190.5	191.6	na	bl	fr	V			qz sx bt fl	100	fl po asp	0	5		"Iridescent-translucent blue vein of flourite-qz-po-ap. Po approaches 5%, arsenopyrite very minor phase."	
D	ML091	191.6	197.4	na	bn	fr	STUF			qz sx	1	si po	0	1		Strongly silicified STUF.	
D	ML091	197.4	198.2	na	cm	fr	FG				0	ep tu	0	0		Fine-grained chilled? FGRA in sharp contact with above STUF. Strong fine-grained ep-tu alteration.	
D	ML091	198.2	221.6	na	cm	fr	FG			tu	1	tu ep	0	0		Icg equigranular FGRA with variable tu-ep alteration along with diffuse tu veins and patches. 	
D	ML092	0	73.3	20	og yw bk	mox	RCLY				1	il ka	0	0		og yw clay with vein textures in the top 30m of the hole	
D	ML092	73.3	136.5	80	dgy cm	fr	STUF			qz cl ca sx	1	si cl cc po bt vs 	0	0		"dgy & cm laminated STUF, bleaching around VQLs. Dgy bl marble band 77.9-78.9m. Wt gy silicified zone with patches of carbonate with po, vs, cc and minor cp at 83-84m. Thin (<1cm) wide veins of po often associated with VC, po veins more common 92-101m.  VC"	NQ starts at 79.1m
D	ML092	136.5	257.3	100	dgy	fr	SS	ST		sx qz cl	2	cl bt qz cc po sb cpy	0	0.1		"Dgy SGWK with some SSLT, becomes weakly magnetic from 239.6m. Minor sulphides, dominantly cp in veins. Cp increases and po decreases downhole from 162.8m. Cl, qz & minor sx in fractures. Beds at 145.5m grade down hole. Network of cl, qz & cp veins 158.9-1"	
D	ML092	257.3	260.6	90	dgy	fr	ST	SS		cl	0.1	si cl	0.1	0.1		Fractured SSLT and SGWK with cl in veins & fractures	
D	ML092	260.6	264.6	100	dgy	fr	SS	ST		cl qz sx	0.1	si cl qz cpy	0.1	0.1		SGWK and SSLT with cl following remnant bedding. Minor veinlets of VLQX (cp) with bleaching selvedges.	
D	ML092	264.6	266.2	90	dgy	fr	SS	ST			0	si cl	0.1	0.1		Fractured SGWK and SSLT with cl in fractures.	
D	ML092	266.2	354.6	100	gy	fr	SS	ST		cl qz sx	0.1	si cl bt cpy	1	0.1		"Weak, patchy magnetic SGWK and SSLT with minor veins of VQLX. The only visible sulphide in this unit is cpy and it is only found in veins. At 336-338 the unit is extensively veined with cl, qz, cc and cpy veinlets. At 349.6-353m the unit is also extensive"	
D	ML092	354.6	367.5	100	gy	fr	SS	ST		cl	10	si cl bt	0	0		Intensely chloritised veined and mildly silicified SGWK and SSLT. This unit is not magnetic and does not contain any sulphides. 	
D	ML092	367.5	375	70	gy bn 	fr	XFBI	ST	STUF	cl qz	60	si cl bt cc cpy	0	0.1		"Intensely veined and brecciated SSLT, SGWK and minor STUF, very minor sx. 75% of this breccia has been cemented with cl, bt and si."	
D	ML092	375	375.5	70	gy bn 	fr	XFBI				60	si cl bt cc cpy	0	0.1		Fault gouge at 375-375.5m.	
D	ML092	375.5	376.8	70	gy bn 	fr	XFBI	ST	STUF		60	si cl bt cc cpy	0	0.1		"Intensely veined and brecciated SSLT, SGWK and minor STUF, very minor sx. 75% of this breccia has been cemented with cl, bt and si."	
D	ML092	376.8	381	90	wt lgy	fr	FG			tu	0.1	qz fp bt ep tu cpy	0	0.1		"Fractured medium grained equigranular FG with occasional tu veins, minor ep, & minor sx associated with cl. "	
D	ML092	381	425.5	100	wt lgy	fr	FG			tu	1	qz fp bt ep tu	0	0		Cohesive equigranular course grained weakly porphyritic FGRA with tu veins and minor epidote. 	EOH - 425.5m
D	ML093	0	36.5	30	og bn dgy	wox	SS	ST	RCLY	qz	1	ka fe cl	0	0		"Very fractured, rubbly, weakly weathered sfg-smg SGWK, interbedded with thin SSLT beds.  Moderate ka and VQ in cohesive rock units.  From 34.1m to 36m rock unit is altered to og clay.  Non-magnetic."	
D	ML093	36.5	216.3	85	dgy og lgn	fr	SS	ST		cl qz sx	3	ke fe po cl ca cpy py bt st	1	1		Dominantly SGWK unit with minor SSLT beds.  Fractured and rubbly with intermittant zones of more cohesive rock. From 36.5m to 57m fractures have fe-oxide and ka weathering; after 57m alteration in fractures converts to mainly cl-zeolite.  From 60.2m to 65	"HQ cased off at 77.3m, needs to broken down into several intervals in logging"
D	ML093	216.3	315.9	na	na	fr	ST	SS			0	si bt mt	0	0		"Dominant lithology now SSLT, interbedded with sfg-smg SGWK beds.  Minor bands of si-alteration throughout unit.  Patchy weak to moderate magnetism in most of unit- mainly attributed to po veins and dissemination.  some areas are not magnetic.  Some SGWK b"	needs to broken down into several intervals in logging
D	ML093	315.9	379.6	na	na	fr	SS	ST			0	bt cl si mt	0	0		"sfg-smg with minor scg SGWK, interbedded with SSLT.  Patchy weak to moderate magnetism. Moderate bt-cl-si alteration from 311.2m to 318m, with minor cl and si alteration bnads throughout rest of unit.  ~2cm thick VQLmt at 366.6m.  pk-og stilbite in fractu"	needs to broken down into several intervals in logging
D	ML093	379.6	386.9	na	na	fr	SS	ST		fl	10	fl bt cl si mt	0	0		"sfg-smg with minor scg SGWK, interbedded with SSLT.  Patchy weak to moderate magnetism.  379.6m to 386.9m contains bluish-greenish veins (do not fizz from HCl or flouresce--barite?)"	needs to broken down into several intervals in logging
D	ML093	386.9	407.5	na	na	fr	SS	ST			0	bt cl si mt	0	0		"sfg-smg with minor scg SGWK, interbedded with SSLT.  Patchy weak to moderate magnetism. Moderate bt-cl-si alteration from 311.2m to 318m, with minor cl and si alteration bnads throughout rest of unit.  ~2cm thick VQLmt at 366.6m.  pk-og stilbite in fractu"	needs to broken down into several intervals in logging
D	ML094	0	18	na	na	fr	ST				0		0	0			
D	ML094	18	38.8	na	dgy	fr 	STUF			qz	0.1	si	0	0		Dk gy coloured STUF with irregular cm-gn coloured bands. Minor disseminated po near transition to ZSKCS.	
D	ML094	38.8	48.3	na	gy	fr 	ZSKCS	STUF		qz	0.1		0	0		Carbonate-rich ZSKCS (impure marble?). Variably silicified with bands of cm-gn STUF.	
D	ML094	48.3	50.6	na	dgy 	fr 	STUF			qz sx	0.1	si po	0	0.1		Dk gy coloured STUF with veinlets of po.	
D	ML094	50.6	51.4	na	gn	fr 	ZSKCS				0	po asp cpy sh	0	1		Band of qz-actinolite?-ep?-po-arsenopyrite-chalcopyrite-schleelite ZSKCS. 	
D	ML094	51.4	52.6	na	dy gy 	fr 	STUF				0		0	0		Dk gy coloured STUF with irregular cm-gn coloured bands.	
D	ML094	52.6	53	na	gn	fr 	ZSKCS				0	po asp cpy sh	0	1		Band of qz-actinolite?-ep?-po-arsenopyrite-chalcopyrite-schleelite ZSKCS. 	
D	ML094	53	65.8	na	dgy 	fr 	STUF				0	cpy asp	0	1		Dk gy-coloured STUF with cm-gn-colored bands. Minor sulphide as veinlets and disseminations. Sulphide may be quite coarse (up to 1cm long patches).	
D	ML094	65.8	86	na	bn dgy	fr 	ZSKCS				0	po cpy asp sh mt	2	30		Dk gy-bronze coloured sulphide-rich skarn (sulphide ~ 30% total unit). Po predominant with chalcopyrite and arsenopyrite conspicuous. Sulphides as coarse disseminations and semi-massive patches. Matrix of fine-grained dark minerals including amphibole-gar	
D	ML094	86	87.3	na	dgy	fr 	STUF			qz cl sx	5	si po cpy	2	2		"Dk gy-coloured STUF with cm-gn-coloured bands, minor po+/-cpy occurs as veinlets (+/-qz) and as disseminations."	
D	ML094	87.3	87.5	na	gy	fr 	FG				0	si tu ep	0	0		"Porphyritic FGRA dyke with si-tu-ep alteration, alteration strongest about margins."	
D	ML094	87.5	89.5	na	dgy	fr 	STUF			qz cl sx	5	si po cpy	2	2		"Dk gy-coloured STUF with cm-gn-coloured bands, minor po+/-cpy occurs as veinlets (+/-qz) and as disseminations."	
D	ML094	89.5	89.6	na	gy	fr 	FG				0	si tu ep	0	0		"Ifg FGRA dyke with si-tu-ep alteration, alteration strongest about margins."	
D	ML094	89.6	95.5	na	dgy	fr 	STUF			qz cl sx	5	si po cpy	2	2		"Dk gy-coloured STUF with cm-gn-coloured bands, minor po+/-cpy occurs as veinlets (+/-qz) and as disseminations."	
D	ML094	95.5	97.3	na	bn dgy	fr 	ZSKCS				0	po cpy asp sh mt	2	40		Sulphide-rich ZSKCS.	
D	ML094	97.3	99.8	na	cm gn	fr 	STUF			qz cl sx	5	si cl po cpy asp mt	2	2		Cm-gn-coloured STUF with extensive whispy veins of qz+/-cl+/-sulphide. Mt as irregular patches.	
D	ML094	99.8	100.7	na	bn dgy	fr 	ZSKCS				0	po cpy asp sh mt	2	20		Sulphide-rich ZSKCS.	
D	ML094	100.7	111.8	na	cm gn	fr 	STUF			qz cl sx	5	si cl po cpy asp mt	5	1		Cm-gn-coloured STUF with extensive whispy veins of qz+/-cl+/-sulphide. Mt as irregular patches (after originally thicker bands?) and thin bands.	
D	ML094	111.8	112.9	na	gy	fr 	ST			qz sx	5	po cpy sh	0	5		Weakly altered SSLT hosting qz-po-cpy-scheelite stockwork (producing some minor brecciation). Stockwork assoc with FGRA vein.	
D	ML094	112.9	113.1	na	gy	fr 	FG				0	tu po	0	0		Tu-po altered ifg FGRA vein	
D	ML094	113.1	113.4	na	gy	fr 	ST			qz sx	5	po cpy sh	0	5		Weakly altered SSLT hosting qz-po-cpy-scheelite stockwork (producing some minor brecciation). Stockwork assoc with FGRA vein.	
D	ML094	113.4	117.6	na	gy	fr 	ST	STUF		qz cl sx	2	bt am po mt	2	2		SSLT with irregular bands of amphibole-sulphide STUF developed. Thin bands (beds?) of mt.	
D	ML094	117.6	118	na	gn	fr 	ZSKCS				0	am po	0	5		Amphibole-po ZSKCS band developed about hydrothermal breccia. 	
D	ML094	118	129.6	na	gy	fr 	ST	STUF		qz cl sx	2	bt am po mt	2	2		SSLT with irregular bands of amphibole-sulphide STUF developed. Thin bands (beds?) of mt.	
D	ML094	129.6	134.4	na	gy	fr	FG				0	si tu ep py	0	0		Rubbly core of fractured FGRA. Fracturing of FGRA assoc with pervasive anatomizing qz veinlets. Strong si-tu-ep-py alteration.	
D	ML094	134.4	135.4	na	bn	fr	XFBI	ST			0		0	0		Brecciated bn SSLT. Upper margin with FGRA brecciated.	
D	ML094	135.4	136.2	na	bn	fr	ST				0		0	0		Bn-coloured SSLT with qz-cc tension gashes. Lower margin with FGRA marked by 1cm wide bk-coloured breccia.	
D	ML094	136.2	137.6	na	gy	fr	FG				0	si tu ep py	0	0		Si-tu-ep-py altered FGRA with anatomizing qz-veinlets.	
D	ML094	137.6	137.8	na	gn	fr	XFBI				0		0	0		Gn-coloured fault gouge and cataclasite.	
D	ML094	137.8	139.5	na	gy	fr	FG				0	si tu ep py	0	0		Si-tu-ep-py altered FGRA with anatomizing qz-veinlets.	
D	ML094	139.5	139.6	na	gn	fr	XFBI				0		0	0		fault zone with approx 4cm of gn-coloured fault gouge and cataclasite	
D	ML094	139.6	139.8	na	bk	fr	FG				0	tu cpy asp sh	0	1		Strongly tu-altered FGRA with disseminated cpy-arsenopyrite-scheelite.	
D	ML094	139.8	144.3	na	gy	fr	FG				0	si tu	0	0		Si-tu altered img equigranular FGRA	 EOH = 144.3m
D	ML095	0	32	na	gy	fr	ST			qz cl sx	1	si cl	0	0		"Chloritic gy SSLT. Rubbly core down to 18.5m. J surfaces Fe coated. Branching VQL(X), minor po assoc with chlorite-rich veins. "	HQ to 20.3
D	ML095	32	74.3	na	gy 	fr	ST	SS		qz cl sx	2	si cl bt po	0	0		"Gy-coloured, weakly altered SSLT and SGWK. Small scale faulting locally disrupts bedding. Alteration as variable secondary bt and as gn si-cl? bands. Branching, sometimes whispy, VQLX with cl selvages (locally strong). Zeolite coats J. "	
D	ML095	74.3	83.6	na	gy	fr	ST			qz cl sx	5	si cl po	0	0		Zone of strong VQLX veining. Larger veins are irregular and whispy. Two generations of tension gashes.	
D	ML095	83.6	114	na	gy	fr	ST	SS		qz cl sx	2	si cl bt po	0	0		"Gy-coloured, weakly altered SSLT and SGWK. Alteration as variable secondary bt and as gn si-cl? bands. Branching, sometimes whispy, VQLX with cl selvages (locally strong). Zeolite coats J. "	
D	ML095	114	209	na	gy	fr	ST	SS		qz cl sx	1	si cl mt po	2	0		"Gy SSLT and SGWK. Gradual loss of secondary bt and development of patchy, weak to moderate magnetism, mark change. Veins of pink zeolite-cc-cl fill late fractures. "	
D	ML095	209	224.6	na	gn	fr	ST	SS		qz sx	1	si cl po	0	0		Gn coloured chloritic SSLT and fine-grained SGWK.	
D	ML095	224.6	234.7	na	dgy	fr	ST	SS			0		1	0		Dk gy si altered SSLT + SGWK with cm-gn bands. Weakly magnetic throughout.	
D	ML095	234.7	235.3	na	bn	fr	STUF			qz cl sx	1	si bt 	0	0		Resinous bn finely banded STUF. Banding wavers. VQLX (po) with cl selvage cuts banding at high angle.	
D	ML095	235.3	267.4	na	dgy	fr	ST	SS		qz sx	1		1	1		Dy gy si altered SSLT + SGWK with cm-gn bands. Weakly magnetic in patches. Trace po developed as thin mm-scale bands and blebs.	
D	ML095	267.4	269.1	na	bn	fr	STUF			qz sx	1		0	1		Resinous bn finely banded STUF with po as thin bands and porphyroblastic blebs. Minor VQX veins cut skarn at high angle to banding.	
D	ML095	269.1	270	na	dgy	fr	ST	SS		qz	1		1	0		Dk gy si weakly altered SSLT + SGWK with cm-gn altered bands. Patchy weak magnetism. Minor VQ veinlets. 	log unfinished
D	ML096	0	14.5	10	gy	fr	ST				0		0	0		"Rubbly, poorly recovered, grey, weakly weathered SSLT with Fe coating joints"	
D	ML096	14.5	69.6	90	bn og	vox	RCLY				0.1		0	0		Og-bn clay with relic veins pseudomorphed by Fe and transition with SSLT. There is also a bright green mineral. This could be weathered number 2 zone	
D	ML096	69.6	74.6	80	gy	fr	ST	SS	SCGL	qz	2	si cl py po	0	1		SSLT and SGWK with SCGL beds. The SCGL is a SGWK matrix supporting a sub-rounded SSLT clasts. The clasts range in size from 2mm - 5cm. SI is found in veins and as a wash. Cl and X are found coating fractures. 	
D	ML096	74.6	75	30	gn	fr	XFBI	ST	lSS		0	cl py	0	1		Pulverised and not re-cemented SSLT and SGWK. This unit has 90% cl which shows a fiberous/platy texture	
D	ML096	75	88.8	100	lgy gy bn	fr	STUF			qz cl sx	5	si bt cl cpy py po	0	1		"STUF with si being the dominant mineral up hole and bt the dominant mineral down hole. The light grey si rich STUF also has a dendric black mineral through out it that is too fine grained to identify. Petrology requested. Si, cl and x are found in veins a"	
D	ML096	88.8	90.5	70	dgy	fr	XFBI	ST	lSS		0	si	0	0		Fractured SSLT and SGWK with Fe coating fractures	
D	ML096	90.5	123.2	90	dgy	fr	ST	SS		qz cl ca sx	0	bt cl si py po cpy cc	0	1		"SSLT with some SGWK. Cpy and py found in veins with cl, si and cc or along bedding planes with bt. Po is also found along bedding plane contacts, or as vugy blebs through out beds. Fractures in this unit are coated with cl or Fe."	
D	ML096	123.2	149.6	60	dgy	fr	ST	SS		qz	0.1	si cl cc bt	0	0		"Fractured rubbly SSLT with minor SGWK. Cl, cc and si found coating fractures."	
D	ML096	149.6	161.6	100	lgy 	fr	STUF			qz cl sx	0.1	si bt cl po py	0	2		Cohesive STUF with thick (2-5cm) veins of VQLX. Dominant x is po. Cl is in blebs and along fractures	
D	ML096	161.6	166.7	60	dgy gn	fr	XFBI	ST	lSS		0	cl tu cc si	0	0		Brecciated SSLT and SGWK with black cl re-cementing around 70% of this unit. The rest of the unit is rubbly with cl in fractures and coating rubble. No direction of fault movement possible	
D	ML096	166.7	196.8	90	gy	fr	ST	SS		tu qz	2	cl tu si	0	0		SSLT with some minor SGWK. The begining of this unit has cl and tu veins (2cm thick). There are also some minor beds that have been silicified (5cm thick). Cl found in blebs and along fractures.	
D	ML096	196.8	210.1	100	dgy bn	fr	ST	SS		cl	1	si bt cl	0	0		Si and bt rich SSLT and SGWK with veinlets of cl.	
D	ML096	210.1	251.2	100	lgy bn gn	fr	STUF			qz sx	0.1	si bt cl po py	0	0.1		"Bt and cl rich STUF showing remnant matrix supported SCGL with small (1-2mm) clasts. X is found in veins with qz. At 224.5m there is an open vein of a soft black, vitreous mineral with a white streak and sugary texture. The bedding at 222.8m and 223.1 are"	
D	ML096	251.2	253.8	100	lgy cm	fr	FG			tu	0.1	po py	0	0.1		"Fine grained equigranular FGRA consisting of qz, fp and very minor bt with some minor x"	
D	ML096	253.8	308.5	100	gy wt 	fr	FG			tu	0.1	tu ep	0	0		Coarse grained fp and qz porporitic FGRA with minor ep alteration and minor tu veins	
D	ML097	0	32	90	dgy og	fr	SS	ST		qz cl	1	fe ka cl	0.5	0		sfg to smg SGWK interbedded with SSLT. Patchy weak to moderate magnetism.  Very fractured and rubbly from top of hole down to 18.8m. Fractures have fe-oxidation and some also have ka alteration.  Unit fractured from 29m to 32m where the next lithology beg	NQ from top of hole.
D	ML097	32	35.9	100	lgy cm gn 	fr	STUF	ZSKCS		cl	1	si cl py ca gt vs cpy do	0	1		"Weakly banded STUF with units of weathered, holey ZSKCS.  Disseminated py occurs in patches throughout STUF. STUF also has pk fine-grained veins.  Minor cpy. MOX fe weathered zone at 35.5m, associated with 2.7m core loss."	
D	ML097	35.9	38.6	0	na	na	NREC				na					"MOX fe weathered zone at 35.5m, associated with c. 2.7m core loss."	
D	ML097	38.6	44.65	100	lgy cm gn 	fr	STUF	ZSKCS		cl	1	si cl py ca gt vs cpy do	0	1		"Weakly banded STUF with units of weathered, holey ZSKCS.  Disseminated py occurs in patches throughout STUF. STUF also has pk fine-grained veins.  Minor cpy. MOX fe weathered zone at 35.5m, associated with 2.7m core loss."	
D	ML097	44.65	49.6	100	bk wt cm d	fr	ZSKCS	XFBI			0	ca am mt cl fp	2	0		"ca-am-fp-cl rich ZSKCS.  Weakly developed scheelite zone from 46.5m to 47.7m.  3 semi-consolidated becciated zone ~10cm thick each at 48.7m, 49m, and 49.15m- possibly fault zones but no gougy matrix! Patchy moderate to strong magnetism."	
D	ML097	49.6	55.3	100	dgy bk cm 	fr	ZSKCS				0	py cpy po mt am sd cl bt si cs	1	20		"py-cpy-po-mt rich sulphide ZSKCS. Py is weathering out leaving honeycomb texture. Sd is assocciated with py- infilling holes? Dkbn matrix (bt?), possibly some cs.  49.6m to 53.5m is dominated by py.  Last 70cm has po banding interbedded with si alteration"	
D	ML097	55.3	61.7	100	bz dbn lgy	fr	ZSKCS				0	po cpy am bt cl si cs	0.5	50		Banded and disseminated po-cpy rich ZSKCS with dkbn matrix (bt? Som cs?). Minor bands of si alteration in unit. Weak magnetism from po.	
D	ML097	61.7	70.25	100	bz dbn lgy	fr	ZSKCS	STUF		qz ca sx	2	po cpy si bt ca cl am asp	1	15		Banded po-ZSKCS interbedded with si-bt altered SSLT-SGWK. Minor VCX and VQX. Weak magnetism from po. ~1cm thick Vasp at 63.1m.	
D	ML097	70.25	83.2	100	lgy wt bn 	fr	STUF	ZSKCS		sx qz cl	1	si bt cl po py gt vs	0.2	1		"si-bt altered STUF with minor ZSKCS at 73.3m to 73.8m and 74.6m to 74.9m.  Patchy weak magnetism from po. Po occurs as round blotches, veins and flecking along bedding plains.  Disseminated py throughout. In areas with intense si alteration there is abund"	
D	ML097	83.2	95.6	100	dgy lgy gn	fr	SS	ST		fl sx cl	2	ca ba qz si po cpy	0	0		Predominantly sfg SGWK interbedded with SSLT. Minor areas of si and cl alteration. Cl flecking occurs throughout unit. From 83.45m to 84m there is Vba? causing minor brecciation of rock. Minor Vxtu and VC. Non magnetic.	NQ from top of hole. EOH 95.6m
D	ML098	0	18.3	80	dgy og bn	wox	SS	ST		cl sx mt	1	fe ka cl qz py po mt 	1	0.5	fc	"Fractured and rubbly sfg to smg SGWK, interbedded with SSLT. Fe-oxide weathering in fractures. Two 2-3cm thick VL with si halos at 2m and 4.2m. Minor VQ and VLXmt. ~10cm thick bn-clay cones at 15m and 16m.  Rock less fractured from 16.5m to end of unit. P"	
D	ML098	18.3	18.35	na	gy	fr	XFBI				0		0	0		~5cm thick gy fault gouge.	
D	ML098	18.35	22.8	100	dgy og	fr	SS	ST		qz	1	fe cl ka qz py	1	0	fc	"Less fractured sfg to smg SGWK, interbedded with SSLT. Fe-oxide weathering +- ka and cl in fractures. Very minor VQ."	
D	ML098	22.8	25.05	100	dgy	fr	SS	ST		qz sx mt tu cl	2	cl qz cpy py ze mt sb si	2	1		"sfg to smg SGWK interbedded with SSLT. Fe weathering no longer present in fractures; cl now dominant. Minor VQmtX+- L scattered throughout unit. Weak silicification towards end of unit, with mm scale VQ +- X (py). Moderately magnetic."	HQ ends at 23m
D	ML098	25.05	25.08	na	dgy	fr	XFBI				0		0	0		~3cm thick fault gouge.	
D	ML098	25.08	53.15	100	dgy	fr	SS	ST		qz sx mt tu cl	2	cl qz cpy py ze mt sb si	2	1		"sfg to smg SGWK interbedded with SSLT. Fe weathering no longer present in fractures; cl now dominant. Minor VQmtX+- L scattered throughout unit. Weak silicification towards end of unit, with mm scale VQ +- X (py). Moderately magnetic."	
D	ML098	53.15	58.3	100	dgy wt	fr	SS	ST		cl qz	1	cl qz py po sb mt	2	0.5		smg to scg SGWK interbedded with SSLT. Majority of cg particles are fp. Moderatley magnetic. Minor VQL+- po and mt.	
D	ML098	58.3	71.54	100	dgy	fr	ST	SS		qz sx bt	1	qz bt po cl py ca	0.5	1		"Predominantly SSLT beds interbedded with sfg-smg SGWK. Not magnetic down to 64m then weakly magnetic to end of unit. SGWK beds increase DH. VQXbt dispersed through unit, some displaying whispy mottled texture. Minor po veins."	
D	ML098	71.54	71.56	na	gy	fr	XFBI				0		0	0		~2cm thick fault gouge.	
D	ML098	71.56	72.5	100	dgy	fr	ST	SS		qz sx bt	1	qz bt po cl py ca	0.5	1		As above description of last SGWK/SSLT unit.	
D	ML098	72.5	89.8	100	dgy	fr	SS	ST		qz cl sx	1	qz cl py po cpy si ze mt	0.5	0.5		Dominant lithology now smg (with minor sfg) SGWK interbedded with minor beds of SSLT. Patchy weak magnetism. VQLX+- mt spread sparsely throughout unit. VCLX have lbn si halo around them.	
D	ML098	89.8	110	100	dgy	fr	SS	ST		qz cl sx ca	2	si cl ca po py cpy bt sb ka	1	1		sfg to smg SGWK with minor beds of SSLT. Patchy weak magnetism. Thin VQ throughout. Minor zone of mottled si-bt alteration at 105.15m to 105.4m. 	
D	ML098	110	122.2	100	dgy	fr	SS	ST		qz cl ca sb	2	qz cl cpy py sb ze ca	1	1		"Dominantly sfg SGWK with minor smg beds, interbedded with minor SSLT beds. Patchy moderate magnetism. Poor bedding differentiation. VQ, VL and Vzeolite present throughout."	EOH 122.2m
D	ML099	0	19	na	gy	fr	ST	SS		qz	0	si	0	0		Dk gy-gn coloured si SSLT with lesser sfg SGWK. Minor VQ.	
D	ML099	19	22.9	na	bn gy	fr	ST	SS		qz	0	si bt ac cl	0	0		Bn-gn coloured altered si SSLT with lesser sfg SGWK. Minor VQ.	
D	ML099	22.9	30	na	cm bn	fr	STUF	ST		qz cl	1	si ac cl po	0	0		Banded cm-coloured ZSKQ and gn-bn coloured act? altered SSLT. Irregular networks of dendretic VQL produces light coloured selvages. Very minor disseminated po.	
D	ML099	30	31.8	na	gn	fr	ZSKCS				0	ac cl cc si po vs	0	0		Silicified act-rich ZSKCS with cc and possible vs?/ep?	
D	ML099	31.8	33	na	dgy	fr	ZSKM				0	mt ac cl po	50	1		Massive ZSKM with lesser act-cl	
D	ML099	33	34.9	na	wt	fr	ZSKM				0	cc cl mt	20	1		"Unusual cc-rich breccia, clasts of coarse-grained cc in cl matrix. Breccia disrupts mt-rich skarn. Margins of enclosing skarn brecciated."	
D	ML099	34.9	37.4	na	gn	fr	ZSKCS				0	mt ac cl po cc vs	20	2		"Mt-rich banded ZSKCS, mt as diffuse ""poikolitic"" bands. "	
D	ML099	37.4	41	na	gn	fr	ZSKCS				0	ac cl cc si po	5	2		Variably silicified act-rich ZSKCS gradational to upper mt-bearing ZSKCS. Coase disseminations of po occur.	
D	ML099	41	57	na	gy	fr	STUF			qz cl sx	1	si ac cl po	0	0		"Gy-banded ZSKQ with minor act-po-rich bands with ""poikolitic"" overprinted? textures. Irregular networks of dendretic VQLX producing some selvage."	
D	ML099	57	57.2	na	gn	fr	XFBI				0	cl py	0	0		Chloritic XBRC with minor py.	
D	ML099	57.2	59	na	gy	fr	STUF			qz cl sx	1	si ac cl po	0	0		Gy-banded ZSKQ.	
D	ML099	59	62	na	gy	fr	ST			qz	0	si	0	0		Rubbly core of gy si SSLT. Fracturing of core along cl-Fe coated J.	
D	ML099	62	62.3	na	gn	fr	XFBI				0	cl py	0	0		Poorly recovered fracured chloritic XBRC with minor py.	
D	ML099	62.3	62.8	na	gy	fr	ST			qz	0	si	0	0		Rubbly core of gy si SSLT. Fracturing of core along cl-Fe coated J.	
D	ML099	62.8	62.9	na	gn	fr	XFBI				0	cl py	0	0		Poorly recovered fracured chloritic XBRC with minor py.	
D	ML099	62.9	66.6	na	gy	fr	ST			qz	0	si	0	0		Rubbly core of gy si SSLT. Fracturing of core along cl-Fe coated J.	
D	ML099	66.6	77.5	na	gy	fr	ST			qz	0	si	0	0		Largely intact gy si SSLT. Where fractured cl-Fe coat J. EOH 77.5m.	
D	ML100	0	24	50	dgy og 	wox	SST			qz cl	2	cl po si	0	0		weakly weathered SGWK and SSLT beds with qz cl veining. Rd/og hematitic staining on fracture faces	
D	ML100	24	43	90	dgy gn	fr	SST	STUF		qz cl sx	5	bt po py cl	0	5		"Thinly bedded sandstone and siltstone beds. Sandstone beds are fg and often poorly sorted with dominantly lithic clasts. Po and py mineralisation in altered sediments where considerable VQL occurs. Laminated tuffite horizons containing po and py, often se"	
D	ML100	43	45.6	100	lgn lgy	fr	STUF	SST		qz cl sx	5	po mt bt cl	1	5		laminated tuffite with VQL and po replacement in beds and in veins. Thin conglomerate horizon in tuffite at 45.4m	
D	ML100	45.6	69	70	dgy lgn 	fr	SST			qz cl sx	2	bt cl py po	0	1	fr between 64-71m	Sandstone/siltstone beds with appreciable quantities of fine grained bt throughout. Py often concentrated in VQL. 	
D	ML100	69	71	30	dgn	fr	XFBI	SST			0	cl py	0	0		"incohesive fault breccia with SST clasts and a cl matrix, with minor py"	
D	ML100	71	82	80	dgy lgn bn	fr	SST	STUF	XHB	qz cl ca	50	bt cl py po	0	1	networking VQ infilling f	severly fractured sandstone/siltstone and tuffite horizons. Fractures infilled with mostly qtz plus cl and cc. Minor hydrothermal(?) cohesive breccia developed between 72.4 - 72.5m. Minor py infilling fractures.	
D	ML100	82	85.2	90	lgn bn	fr	STUF	SST		qz cl ca	10	bt cl cc py	0	0		"fractured STUF rich in bn fine bt, highly fractured between 82.3 - 83m, vuggy fractures and cavaties partially infilled with cc and minor py."	
D	ML100	85.2	90.3	100	dgn gy yw	fr	ZSKCS	ZSKM		ca qz sx	2	mt py po cc	15	20		ZSKCS with high % of mt in patchy concentrations. Py and po ds and in veins throughout.	
D	ML100	90.3	93.9	100	dgy bn	fr	ZSKM			qz sx	2	mt py cl am	50	10		"massive mt with ~10-15% sulphide, dominatly py in bands and veins."	
D	ML100	93.9	113.2	100	dgy	fr	ZSKCS	STUF	ZSKM 	qz sx	2	mt py bt po cpy	5	10		"fine grained ZSKCS with thin (~2-4cm) bands of STUF. Py concentrated in veins and often ds in bands. Mt is found commonly replacing bands 2-5cm thick, and often up to 20cm thickness. Mt in these bands commonly has a patchy habit. Dgn am abundant. "	
D	ML100	113.2	121.9	100	bk gn dgy	fr	ZSKM	ZSKCS		ca qz sx	5	mt py po am cl cpy	50	10		dominantly ZSKM with py and increasing po content from ~120m nearing sulphide skarn. Mt occurring in bands ranging in thickness up to ~15cm thick. 	
D	ML100	121.9	128.1	95	yw dgn bn	fr	ZSKX			ca sx	1	po mt am bt cl py cpy	2	50		"massive po skarn, >50% sulphide throughout. Py + cpy also common. Dgn am in bands and in patches. Bn colouration most likely due to bt. Infrequent mt bands."	
D	ML100	128.1	145.4	100	dgn dgy yw	fr	ZSKCS	STUF		ca qz sx cl	2	po py cpy bt mt asp cl	1	10		"am and sulphide rich ZSKCS, po concentrated into bands 1-5cm thick. Po more common near ZSKX, silver ap and/or stanite present. ZSKCS often thinnly banded with STUF, pk/rd mineral at 133m depth resembles garnet or vs."	
D	ML100	145.4	155.5	90	bn dgy gn	fr	ZSKCS	STUF	FG	qz sx	5	bt po py asp mt	2	10		"similar lithology to above ZSKCS, however there is a noteable increase in bt content nearing the FGRA. Sulphide rich ZSKCS, mostly po, py and ap. Thin <5-10cm across veins/dykes of granite composition qz-feldspar plus silver coloured stanite or ap."	
D	ML100	155.5	155.8	100	gy wt	fr	FG				0	cl	0	1		"qz tormaline rich FGRA dyke with minor py and/or po, gn cl alteration"	
D	ML100	155.8	158.5	100	bn dgy	fr	ZSKCS			qz sx	2	bt po asp st py	0	2		bt rich ZSKCS with minor py and po	
D	ML100	158.5	172.2	100	wt lgn cm	fr	FG			qz tu	5	cl ep se	0	0		"sharp steeply dipping contact with ZSKCS, fine grained equigranular and porphyritic granite, qz and plagioclase phenocrysts dominant plus tourmaline. Lgn ep alteration of k-spars. Concentrations of tu in veins commonly associated with qz. FGRA is finer gr"	EOH - 172.2m
D	ML101	0	18.8	na	bn	fr	SST			qz am sx	1	bt	0	0		Medium to fine bedded bt altered sfg lithic arenites and siltstones.	
D	ML101	18.8	18.9	na	cm gn	fr	FG				0	si ep	0	0		"Ifg silica-rich FGRA vein with unidentified gn alteration, possibly ep."	
D	ML101	18.9	20.3	na	bn	fr	SST			qz am sx	1	bt	0	0		Biotite altered medium to fine bedded sfg lithic arenites and siltstones.	
D	ML101	20.3	20.4	na	cm gn	fr	FG				0	si ep	0	0		"Ifg silica-rich FGRA vein with unidentified gn alteration, possibly ep."	
D	ML101	20.4	26	na	bn	fr	SST			qz am sx	1	bt	0	0		Biotite altered medium to fine bedded sfg lithic arenites and siltstones.	
D	ML101	26	34.5	na	bn gn cm	fr	STUF	ST		am sx	5	px gt bt po	0	1		Finely bedded svfg STUF and lesser ST. STUF extensively altered to probable calc-silicate assemblage. ZBT after ST with resinous bt alteration and po following relict bedding planes.	
D	ML101	34.5	43	na	gn	fr	ZSKCS	STUF		ca am sx	2	px gt bt am mt po	5	1		Gn cpx-dominated ZSKCS with mt-rich bands. Lighter gy-pk coloured bands of persistant STUF.	
D	ML101	43	56.5	na	gn	fr	ZSKCS			ca	1	am mt po cpy aspy ca	20	2		Amph-mt-sulphide skarn interbanded with gy-gn very fine grained layers of altered ST.	
D	ML101	56.5	66	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	66	66.3	na	gn	fr	ZSKCS			ca	1	am po aspy	0	2		Amph-sulphide skarn band.	
D	ML101	66.3	74.6	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	74.6	75.7	na	gn	fr	ZSKCS			ca	1	am mt po cpy aspy px	5	5		Amph-mt-sulphide skarn with lesser cpx.	
D	ML101	75.7	77.7	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	77.7	77.8	na	cm gn	fr	FG				0	si ep	0	0		Altered porphyritic FGRA dyke.	
D	ML101	77.8	78.2	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	78.2	78.8	na	cm gn	fr	FG				0	si ep	0	0		Altered porphyritic FGRA dyke.	
D	ML101	78.8	92.5	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	92.5	93.4	na	cm	fr	FG				0	tu	0	0		Tu altered img equigranular FGRA dyke.	
D	ML101	93.4	94.2	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	94.2	94.6	na	cm	fr	FG				0	tu	0	0		Tu altered img equigranular FGRA dyke.	
D	ML101	94.6	95.9	na	bn gn cm	fr	STUF			am sx	5	px gt bt po	0	1		"Finely bedded svfg STUF, strongly altered to calc-silicate assemblage."	
D	ML101	95.9	97.3	na	bn	fr	SST			qz	1	bt	0	0		Fine to medium bedded sfg protolith now dominated by bt with minor po.	
D	ML101	97.3	97.5	na	cm	fr	FG				0	tu se	0	0		Tu-se altered img FGRA.	
D	ML101	97.5	98.7	na	bn	fr	SST			qz	1	bt	0	0		Fine to medium bedded sfg protolith now dominated by bt with minor po.	
D	ML101	98.7	98.9	na	cm	fr	FG				0	tu	0	0		Tu altered ifg FGRA.	
D	ML101	98.9	99.1	na	bn	fr	SST			qz	1	bt	0	0		Fine to medium bedded sfg protolith now dominated by bt with minor po.	
D	ML101	99.1	99.2	na	cm	fr	FG				0		0	0		Ifg FGRA.	
D	ML101	99.2	99.5	na	bn	fr	SST			qz	1	bt	0	0		Fine to medium bedded sfg protolith now dominated by bt with minor po.	
D	ML101	99.5	100	na	cm	fr	FG				0	tu	0	0		Tu-altered FGRA.	
D	ML101	100	102.3	na	gy	wox	SST			qz	1	bt	0	0		WOX bt altered SST with clay minerals.	
D	ML101	102.3	109.2	na	yw	vox	FG				0	ka 	0	0		VOX FGRA with relict qz and feldspar phenocrysts preserved sporadically in clay-rich matrix. Rotted qz-tu veins preserved with he staining. 	
D	ML101	109.2	109.4	na	cm	wox	FG				0	he 	0	0		WOX intact porphyritic FGRA with variable he staining. Motar texture developed in groundmass.	
D	ML101	109.4	110.8	na	cm	fr	FG			qz	5	se tu py 	0	0		Fresh porphyritic FGRA with se-tu alteration and simple VQ. Minor py fills fractures. 	
D	ML101	110.8	125.1	na	cm	fr	FG				0	se	0	0		Se altered porphyritic FGRA.	
D	ML102	0	5.3	40	gy og	fr	ST				0	lm ka	0	0		Broken and rubbly SS and ST with minor lm and clay alteration.	
D	ML102	5.3	17.4	90	gy	fr	SST				0	si cl se py	0	1		Lithic sandstone and siltstone with cl and X in fractures and minor VL. Minor fe staining.	
D	ML102	17.4	20.6	95	gy	fr	SS				0	cl bt si	0	0		"Lithic sandstone with minor siltstone and minor VL. Cl and bt alteration follow SS beds, with minor iron staining."	
D	ML102	20.6	27	80	dgy	fr	SST	SCGL		qz cl sx	2	cl si ka bt py cpy	0	0.5		"Highly fractured SST with 5% of core rubbly and cl coating fractures. Network VQLX. X only in veins. Extremely minor SCGL at 23.2m approx 2cm thick, with SS matrix and SSLT clasts."	
D	ML102	27	34.7	100	dgy	fr	SST			cl sx	0.5	cl bt se py	0	0.5		SST with cl and X coating fractures. Occasional VLX that appear to follow bedding planes. Core extremely fractured between 31.1m and 31.9m. From 17.8m to 19.6m bt alteration occurs in medium grained SS beds.	
D	ML102	34.7	144.6	100	dgy	fr	SS			sx	2	bt cl qz po cpy py cc	0	1		Dgy medium to fine grained SS with 30% medium grained dgy ST. Bt-cl alteraion more prominant in SS beds and cl coating fractures throughout the unit. X only in veins. Non magnetic unit. XHB from 38.1m to 38.6m with qz cl and po matrix and sedimentary clas	
D	ML102	144.6	146.1	100	dgy pk og	fr	SST			sb	20	sb	0	0		"sfg SS and ST with zones of intense sb veining, causing rock to fracture."	
D	ML102	146.1	157.7	100	dgy dbn	fr	SS			qz bt sx	2	cl qz bt ba ze	0	0		"sfg-smg SS with minor beds of ST. Minor cl alteration bands. Minor VQX. From 151.9m to 152.6m has been fractured by veining of ba?-wt zeolite?, causing XHB of host rock. Bt alteration has also occurred around the area."	
D	ML102	157.7	158.3	100	dgy cm 	fr	ST			cl	40	cl	0	0		Felsic lithic ST package. Lithics up to 1mm. Intense cl? Veinlets throughout.	
D	ML102	158.3	160.3	100	dgy	fr	ST			cl qz	1	cl po qz	0	0		Predominantly ST with minor sfg SS beds. Cl flecking throughout. Minor VLQ.	
D	ML102	160.3	168.9	100	dgy dgn	fr	SST			cl sx	0.5	cl si po bt	0	0		Interbedded SS and ST. Weakly altered by cl banding. Possible cross-lamination at 163.5m. Two 10-15cm thick conglomerate beds at 163.8m and 164.4m. They contain lithic clasts and quartz clasts. Minor bt alteration.	
D	ML102	168.9	179.5	100	dgy dbn lb	fr	STUF			qz cl ca sx	2	bt po py si px cl am	0	1		"Banded fine to medium grained polylithic tuffite from 168.9 to 173.85m. Most beds are well sorted but some are poorly sorted, containing very fine grained ~1mm felsic clasts in a fine to medium grained matrix. From 173.9 to 179.5m tuffite has mottled text"	not completed yet
D	ML102	179.5	195.7	100	dgy bk gn 	fr	ZSKCS			qz ca	1	ca am po do sd qz mt py cpy gt sh cl	5	5		cc-am-X ZSKCS. Banded and disseminated mt scattered throughout which increases DH. From 187.75m to 190m is ca-rich zone. Minor thin (cm) tuffite bands in upper unit. Very minor scheelite. X mostly disseminated.	
D	ML102	195.7	203.5	100	dgy bk yw	fr	ZSKM	ZSKX	ZSKCS	ca sx	2	mt py po ap cpy am ca sd bt sh gt	40	15		mt-X rich skarn. Banded and disseminated mt. X in veins and disseminated. Ca disseminated with mt and in veins. Ap rich zones at 198.9m to 199m and 201.8m to 202.2m. A crenulated/zebra stripe texture appears in several beds from 197.9m to 199.7m. Minor sc	
D	ML102	203.5	205.9	100	yw bz ov	fr	ZSKX	ZSKCS	STUF	ca sx gt sh	2	po py cpy ap am mt gt ca bt sh sd	10	30		"po-py-cpy rich sulphide skarn. Ov coloured mineral (sd?) interbedded with X. VCX+-gt, sh common. Minor STUF bands."	
D	ML102	205.9	208.1	100	dgy lgy	fr	ZSKCS	STUF		ca sx gt	1	po ca am mt gt bt ap	2	5		ZSKCS with interbedded STUF. ZSKCS contains minor mt bands. STUF is in thin banded beds and also in less well defined thicker beds. Minor bt alteration of tuffite beds.	
D	ML102	208.1	216.15	100	lgy bn	fr	STUF	SST	ZSKCS	ca sx	1	si po bt ca cl	0	2		lgy fine grained tuffite interbedded with bn bt altered siltstones-sandstones. ~50cm ZSKCS from 212.6m to 213.1m. 10cm thick VXQC at 214.9m. STUF has light and dark bands.	
D	ML102	216.15	221.55	100	dgy bk lgy	fr	ZSKCS			ca sx	3	ca am mt po py cl	5	3		216.15m to 218m are dark coloured calc-silicate minerals. 218m to 221.55m is light coloured ca-rich. Mt bands in dark ZSKCS with VX. VC in ca-rich ZSKCS. At 220.4m is a 4cm thick VC.	
D	ML102	221.55	226.3	100	lgy bn	fr	STUF	SST	ZSKCS	qz sx	1	si bt po cl	0	0		weakly banded tuffite with possible interbeds of bt-altered SS and ST. Thin po veins in SST. 224.3m to 224.85m have ignimbrite textured or volcaniclastic beds.	
D	ML102	226.3	228.1	100	pl gy	fr	ZSKCS	STUF			0	si am ca cl po	0	1		small interval of ZSKCS with minor STUF beds.	
D	ML102	228.1	233.1	100	bn	fr	SST	STUF		qz sx	3	bt po qz	0	2		"bt-altered siltstone and very fine grained sandstone, with thin po veining throughout. Minor STUF beds. Very weakly magnetic (from presence of po)."	
D	ML102	233.1	237.7	100	gy lgn bk 	fr	ZSKCS	STUF		sx	0.5	am mt po cpy si gt	2	3		calc-silicate skarn with minor STUF beds. Minor VX veins.	
D	ML102	237.7	246.6	100	bn wt gy	fr	SST	STUF		sx qz	1	bt po qz px mt py	1	2		"bt-altered fine-to-medium grained sandstone and siltstones interbedded with tuffite. From 243.5m to 245.5m is sa zone of well defined, coarse grained tuffite. At 245.5m the tuffite bed is truncated by the overlying sandstone bed (STUF S0= 32 alpha; SS S0="	
D	ML102	246.6	248.6	100	wt bk	fr	FG			tu	1	tu se	0	0		"quartz-feldspar-bt rich granite with minor tu and weak se alteration. Minor Vtu. Equigranular, minus the odd qz and fp phenocrysts. Granite contact with overlying unit at 35 degrees to the core axis."	EOH 248.6m
D	ML103	0	5.5	20	dgy og	wox	SST				0		0	0		"rubbly core, poor recovery of siltstone and sandstone with yw/og lm staining"	
D	ML103	5.5	25.3	100	dgy gn bn	fr	SST			qz cl	0	tu am cl bt mt po	2	0		"Sandstone/siltstone beds , weakly magnetic. Minor mt in very thin horizons between 7-8m depth, appears to be parallel to bedding. Bt and cl alteration textures throughout tu or am as bk radating acicular crystals"	NQ starts 20.3m
D	ML103	25.3	26.2	100	wt bk	fr	FG			qz tu	5	cl se	0	0		"fine-med grained porphyritic granite dyke, qz and feldspar phenocrysts. Some feldspars are altered to dgn se. VQT common, tu occurs throughout."	
D	ML103	26.2	39.3	100	dgy bn lgn	fr	SST	STUF		qz cl tu	2	bt po py cl tu	0	1		sandstone/siltstone beds with tuffaceous horizons often containing po. Sediments often contain thin VQT	
D	ML103	39.3	51.7	100	dgn lgn bn	fr	STUF	SST	ZSKCS	qz cl tu	2	si bt cl py po mt	0	2		laminated tuffaceous beds and SST horizons often containing high amounts of bt. Tuffite beds contain thin cl bands parallel to laminations and VL crossing laminations. ZSKCS bands <15cm thick contain concentrated po up to ~20% plus am. Minor mt in ZSKCS b	
D	ML103	51.7	55.8	100	dgn dgy	fr	ZSKCS	STUF		qz	5	bt mt po cl	5	2		"intervals of ZSKCS and STUF, mt distributed in thin bands. Bt common throughout. Dgn amphibole (actinolite?) crystals visible but mostly too fine. Po found in patchy concentrations. "	
D	ML103	55.8	56.1	100	wt gy	fr	FG			qz tu	1	cl	0	0		"FGRA dyke with an undulating contact, fine grained qz-feld-bt/tu? rich granite "	
D	ML103	56.1	61	100	lgn cm bn	fr	ZSKCS	STUF		qz cl	1	si bt mt py po	5	2		"fine grained calc-silicate minerals in ZSKCS mostly dgn am, intervals of laminated STUF with po replacement along S0. mt ds and in bands throughout unit."	
D	ML103	61	62.5	100	dgy dgn	fr	ZSKM	ZSKCS		qz	1	mt py po bt	50	2		mt occurs in ms bands of varying thickness (~<2cm-10cm). Dgn fine am associated with the mt	
D	ML103	62.5	69.6	100	dgn gy	fr	ZSKCS 	ZSKM		qz cl sx	1	mt py po cl	10	15		"dgn am rich ZSKCS with patchy mt and ds sulphide mostly py and po, minor thin fractures or veins infilled with py and po."	
D	ML103	69.6	72.1	100	dgy bk gn	fr	ZSKM			qz cl sx	2	mt cl po py	50	10		"banded patchy mt and am, ds po and py throughout. VQL with po."	
D	ML103	72.1	76.8	100	dgy gn	fr	ZSKCS	STUF			0	po mt cl bt vs	10	10		"ZSKCS contains predominantly dgn am more concentrated in bands. Po ds throughout, thin intervals of mt and minor laminated STUF containing bt."	
D	ML103	76.8	77.2	100	wt gn gy	fr	FG				0	cl	0	0		"fine/med grained equigranular granite predominantly composed of qz-plag-kspar and bk bt/tu?, irregular contact with ZSKCS."	
D	ML103	77.2	81.1	100	dgn dgy cm	fr	ZSKCS	STUF		qz sx	1	po py mt cl	10	10		dgn am ZSKCS with thin horizons of STUF. Ds po and py mostly in the ZSKCS.	
D	ML103	81.1	83.7	100	dgn gy	fr	ZSKM	ZSKCS			0	mt po py cc	50	10		"ZSKM containing mt in bands and patches throughout, py often associated with more dominant po"	
D	ML103	83.7	92.5	100	dgn lgn	fr	ZSKCS			qz ca cl sx	5	po py mt cc cpy	5	5		"dgn am rich ZSKCS with minor banding that could represent bedding planes. Mt in patchy concentrations, py and po throughout, minor cpy. "	
D	ML103	92.5	99.6	100	lgn dgn cm	fr	ZSKCS	STUF		qz cl	5	po cl bt mt	2	5		"similar amounts of ZSKCS and STUF, STUF occurs in thin intervals between ZSKCS. STUF is lgn/cm with bn bands containing bt. This (<2cm) veins of qz-bt/tu? Fine grained purple mineral common in ZSKCS in this hole (dolomite?garnet?)"	"At 98.6m depth - 10cm zone which appears like a XBC, has a very high SG and contains mt and he. Outer edge of core is more porous with small rhombohedral or tetrahedral crystals often filling vesicles"
D	ML103	99.6	141	95	wt gy og r	fr	FG			qz tu	2	cl he se	0	0		"variably altered granitiod, equigranular and porphyritic. Large phenocrysts of qz and plagioclase, gn se replacement of some feldspars. Fe oxide dusting common throughout, becomes more concentrated in bands. Patches of granite altered to clay. Hematite pr"	EOH -141.0m
D	ML104	0	23.4	60	dgy og yw	wox	SST				0	he 	0	0		"beds of sandstone and siltstone which have been weakly oxidised, coarser beds seem subject to more intense weathering. Og/yw he and lm staining in many exposed fracture faces"	
D	ML104	23.4	27.7	90	lgn bn gy	wox	STUF			cl sx	2	po bt he py	0	10		"weakly oxidised STUF, some exposed fractures contain he staining. Ds po throughout and in VX. Fine grained bt present. Po is oxidised to a rusty bn colour."	
D	ML104	27.7	61	70	dgy og bn	wox	SST			qz cl	1	se	0	0		"beds of siltstone and fine-med grained sandstone, some poorly sorted beds containing coarser grains. Rd/og he staining throughout. Soft wt clay mineral on some fracture faces. "	
D	ML104	61	63.9	75	dgy gn	fr	SST			qz	1	cl	0	0		"mostly siltstone with thin sandstone beds, core is severly fractured"	
D	ML104	63.9	66.4	65	dgy dgn	fr	XFBI	XFBC		qz cl	1	cl	0	0		incohesive fault breccia mostly between 65.3-65.5m and 66-66.3m with vuggy/fractured SST with minor cohesive brecciation associated.	
D	ML104	66.4	68.4	95	wt lgn 	fr	SCB			ca	5	cc cl po	0	0		"fine grained carbonate rock, relatively unmineralised, minor po. Bedding is hard to distinguish, weak to moderate alteration."	
D	ML104	68.4	86.9	100	dgy lgn	fr	ZSKCS	SST		ca cl	5	mt po py cl	10	20		"ZSKCS with high % of cc and VC, high concentration of py often with po and less abundant cpy. Mt occurs in bands throughout and occurs in more concentrated intervals"	
D	ML104	86.9	97.1	100	dgy dgn lg	fr	ZSKM	ZSKCS		ca sx	2	mt po py cpy	50	15		"similar proportions of ZSKM and ZSKCS, bands of ms mt and ds po and py throughout. Cc in veins with po and py often associated. Dgn fine grained am and cl present throughout. Speckled texture of calc-silicate minerals and mt"	
D	ML104	97.1	99.1	100	lgn dgn pl	fr	STUF	ZSKCS			0	mt po py cl	10	10		laminated STUF with thick (~20cm) intervals of ZSKCS containing mostly po plus py and mt. STUF intervals contain minor flattened/elongate fragments along laminations.	
D	ML104	99.1	103.7	100	dgn yw bn	fr	ZSKX	ZSKCS		ca sx	1	po py cpy	0	50		"predominantly po skarn with py and cpy visible. Fine grained am making up most of the rest of the rock. Sulphides are weakly banded and ds, wispy texture where sulphides have migrated along bedding and in fractures."	
D	ML104	103.7	110.3	100	dgn bn	fr	ZSKCS	STUF		ca sx	5	po py cpy bt mt ap	5	15		"mostly ZSKCS with significant po, minor ap seen at ~106.7m, thin intervals of STUF containing bt in some beds. Mt in ZSKCS nearer the ZSKX at 104.6m depth."	
D	ML105	0	1	na	gy	fr	SST				0		0	0			
D	ML105	1	6.6	na	gn cm	fr	STUF	ZSKCS		qz cl	15	am po py bt	2	5		Weak laminations cut by VQL+/-am. Disseminated po-py throughout. Veins parralel to sub-parralel to S0. 	
D	ML105	6.6	9.5	na	gn	fr	ZSKCS			cl	2	mt py po 	30	5		mt-rich ZSKCS. Mt as bands and patches.	
D	ML105	9.5	26.5	na	gn	fr	ZSKCS				0	mt po py	10	5		am-po-mt ZSKCS.	
D	ML105	26.5	26.8	na	cm	fr	FG				0		0	0		Porphyritic FG.	
D	ML105	26.8	27.2	na	gn	fr	ZSKCS				0	am gt po cpy	0	5		am-ZSKCS with gt. Disseminated sulphide.	
D	ML105	27.2	54.2	na	cm og	wox	FG				0	se ka Fe	0	0		Porphyritic FG with seriticized fd. Other fds stained og by he? Wox zones with variable Fe-ka alteration.	
D	ML106	0	15.9	100	cm bn	fr	STUF			qz sx	5	bt po cpx	0	1		Thin bedded altered STUF with sedimentary structure preserved. Dendretic veinlets of qz+/-am+/-po. Po along bedding planes.	
D	ML106	15.9	22.7	100	gy	fr	STUF	ZSKCS			0	mt cpx am ep po gt	5	1		Altered gy laminated STUF with bands of mt+cpx+/-am+/-ep ZSKCS.	
D	ML106	22.7	23.5	100	gn	fr	ZSKCS				0	ac cc 	0	0		ac-cc ZSKCS	
D	ML106	23.5	25.9	100	gy	fr	STUF	ZSKCS			0	mt cpx am ep po gt	5	1		Altered gy laminated STUF with bands of mt+cpx+/-am+/-ep ZSKCS.	
D	ML106	25.9	34.4	100	gn	fr	ZSKCS				0	mt ac po cpy 	20	2		mt-ac-rich ZSKCS with mt concentrated into patchy cm-scale bands. Po with lesser cpy occurs as coarse dessiminations.	
D	ML106	34.4	37.4	100	gy	fr	ZSKCS				0	ac mt po sd asp cpy	20	20		Sulphide-rich amphibole skarn. Sulphide dominantly po+/-apy+/-cpy associated with sd. Mt-rich bands occur.	
D	ML106	37.4	48	100	gn	fr	ZSKCS			sx	1	cpx mt po ac cpy sd	20	10		Banded ZSKCS: bands are gy v fine grained cpx?-rich and mt+po+am+/cpy+/-sd.	
D	ML106	48	53.7	100	gy	fr	ZSKX			ca sx	1	po ac gt cpy asp 	0	40		Po-rich skarn with ac-gt-cpy-apy. 	
D	ML106	53.7	57.5	100	gn	fr	ZSKCS			ca sx	1	cpx ac gt po cpy	0	5		V fine grained cpx? ZSKCS with locally coarse disseminations of sulphide.	
D	ML106	57.5	59.3	100	gy	fr	ZSKX			ca sx	1	po ac gt cpy asp 	0	40		Po-rich skarn with ac-gt-cpy-apy. 	
D	ML106	59.3	62.1	100	gn	fr	ZSKCS			ca sx	1	cpx ac gt po cpy mt	2	5		cpx ZSKCS with dessimenated sulphide and minor mt.	
D	ML106	62.1	64	100	cm	fr	FG				0	tu se po cpy asp sd	0	5		Altered porphyritic FG dyke with sulphide-sd-tu-se.	
D	ML106	64	65	100	gy 	fr	ZSKCS				0	am cpx po mt	5	5		am-rich ZSKCS with coarsely dissemenated sulphide po.	
D	ML106	65	65.3	100	cm	fr	FG				0	tu se	0	0		tu-se altered porphyritic FG dyke.	
D	ML106	65.3	66.5	100	gy 	fr	ZSKCS				0	am cpx po mt	5	5		am-rich ZSKCS with coarsely dissemenated sulphide po.	
D	ML106	66.5	67.3	100	cm	fr	FG				0	tu se	0	0		tu-se altered porphyritic FG dyke.	
D	ML106	67.3	68.3	100	gy 	fr	ZSKCS				0	am cpx po mt	5	5		am-rich ZSKCS with coarsely dissemenated sulphide po.	
D	ML106	68.3	72.4	100	gy	fr	ZSKCS				0	mt po am	20	5		mt-rich amphibole skarn.	
D	ML106	72.4	89.7	100	gn	fr	ZSKCS				0	mt am cpx gt	10	0		Thinly banded ZSKCS (after sfg material with a tuffaceous component) with some sedimentary features preserved. Mineralogy varies with bed; am+mt; am; cpx+gt.	
D	ML106	89.7	95.7	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML106	95.7	98.6	100	og	wox	FG				0	ka fe se tu	0	0		Band of wox og-coloured FG with strong ka-Fe-se alteration.	
D	ML106	98.6	100.2	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML106	100.2	101.7	100	og	wox	FG				0	ka fe se tu	0	0		Band of wox og-coloured FG with strong ka-Fe-se alteration.	
D	ML106	101.7	102.9	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML106	102.9	103.8	100	og	wox	FG				0	ka fe se tu	0	0		Band of wox og-coloured FG with strong ka-Fe-se alteration.	
D	ML106	103.8	104.3	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML106	104.3	104.7	100	og	wox	FG				0	ka fe se tu	0	0		Band of wox og-coloured FG with strong ka-Fe-se alteration.	
D	ML106	104.7	106.8	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML106	106.8	107.5	100	og	wox	FG				0	ka fe se tu	0	0		Band of wox og-coloured FG with strong ka-Fe-se alteration.	
D	ML106	107.5	116.7	100	cm	fr	FG				0	tu se	0	0		Strongly porphyritic FG with minor se-tu alteration.	
D	ML107	0	17.5	na	gy	fr	SST				0		0	0		Gy SST	
D	ML107	17.5	81	100	gy	fr	SST				0	bt cpx	0	0		Gy SST with patchy gn-bn bt+/-cpx alteration. Non-magnetic.	
D	ML107	81	93.5	100	gy	fr	SST				0	bt cpx	0	0		Weakly bt+/-cpx altered SSL. Core broken along Fe+/-cl coated J.	
D	ML107	93.5	95.6	0	na	na	NREC				na					Zone of core loss	
D	ML107	95.6	95.8	100	kk	vox	RCLY				0		0	0		kk-coloured clay	
D	ML107	95.8	101.1	0	na	na	NREC				na					Zone of core loss	
D	ML107	101.1	102.7	50	kk	vox	RCLY				0		0	0		kk-coloured clay	
D	ML107	102.7	104.6	90	gy	fr	STUF				0	cpx	0	0		Finely bedded gy cm altered STUF	
D	ML107	104.6	119.6	22	yw og	vox	RCLY				0		0	0		yw og clay with rare relict fine scale bedding and veining	
D	ML107	119.6	122.6	0	na	na	NREC				na					Zone of core loss	
D	ML107	122.6	125.6	90	kk	vox	RCLY				0		0	0		kk-coloured clay with rare relict fine scale bedding and veining	
D	ML107	125.6	134.6	0	na	na	NREC				na					Zone of core loss	
D	ML107	134.6	137.6	66	rd og	vox	RCLY				0		0	0		rd og coloured clay	
D	ML107	137.6	150.6	100	gy	fr	STUF				0	cpx	0	0		Fine bedded gy coloured altered STUFF.	
D	ML107	150.6	161.4	100	gy	fr	ST				0		0	0		Gy svfg ST.	
D	ML108	0	54.8	na	gy	fr	SST				0		0	0		Gy SST	
D	ML108	54.8	62.6	100	gn	fr	STUF				2		0	5		sfg gn-bn altered lam tnb STUF. Ds po. Fine branching veinlets of am?	
D	ML108	62.6	72	100	gy	fr	SST				0		0	0		Gy SST	
D	ML108	72	72.4	100	gy	fr	SST	XHB		qz	5		0	0		Network VQ zone producing some brecciation.	
D	ML108	72.4	116	100	gy	fr	SST			qz	1		0	0		Gy SST.	
D	ML108	116	124.4	na	gy	fr	SST			ca cl	2		0	0		"Rubbly SST core, broken along cl+/-cc coated fractures."	
D	ML108	124.4	124.55	na	gn	fr	XFBI				na	cl	0	0		Chloritic fault breccia.	
D	ML108	124.55	125.4	na	gy	fr	SST			qz	2		0	0		Fractured core of SST with network VQ producing brecciation.	
D	ML108	125.4	128.4	0	na	na	NREC				na					"No core recovery, except for mushy cuttings of chloritic XBI."	
D	ML108	128.4	128.7	na	gn	fr	XFBI				na	cl	0	0		Chloritic fault breccia.	
D	ML108	128.7	133	100	gy	fr	SST			qz	2	bt cpx	0	0		Dark SST with patchy bn-gn bt-cpx? alteration. Extensive VQ network with brecciation.	
D	ML108	133	146.9	100	gy	fr	SST	STUF		qz	1	bt cpx	0	0		Dark SST with conspicuous bn bt alteration + patchy gn cpx?. Thin interbeds of gy-gn tuffaceous material.	
D	ML108	146.9	151.25	100	gy	fr	ZSKM			qz	1	mt ac cpy po	50	2		Relatively impure fine grained mt- ac-skarn +/- cpx. Minor porphyroblastic po. Minor qz veinlets. Marly protolith?	
D	ML108	151.25	153.9	100	gn	fr	ZSKCS	V		qz tu	5	ac cpx po asp cc	0	2		"Gy-gn am- cpx- skarn with patchy to whispy texture, after strongly altered tuffaceous protolith? Minor porphyoblastic cc. Patches of coarse sulphide. Rare diffuse qz+tu+/-po+/-asp veins."	
D	ML108	153.9	154.4	100	gy	fr	ZSKM			qz	1	mt ac	70	0		Pure coarse grained mt-ac skarn. Minor qz veinlets.	
D	ML108	154.4	157.2	100	gy	fr	ST	STUF		qz ca	2	cpx po mt	1	1		Dark sfg ST with gy lam tuffaceous interbeds. Minor coarse po patches locally. Mt very minor.	
D	ML108	157.2	162.9	100	gy	fr	ZSKM			qz	1	mt ac po 	60	5		Mt- ac- skarn with abundant coarse po.	
D	ML108	162.9	171.4	100	bk	fr	ZSKCS			qz sx	1	am po mt	5	20		"Black-bronze coloured am- po- rich skarn. Am fine grained and black, hb member? Po strongly magnetic: as coarse diffuse bands. Mt is relatively minor."	
D	ML108	171.4	180.5	100	gn	fr	STUF			sx	5	cpx po asp cpy am	0	5		Gn-gy very fine grained finely banded skarn after altered tuffaceous material. Conspicuouc sulphide as patches and more notably veins parralel to sub-parralel with layering.	
D	ML108	180.5	181.6	100	bk	fr	ZSKCS			sx	10	am po asp cpy	0	10		Fine-grained bk (am?) skarn with conspicuous sulphide as layer parralel veins or replacement. Textures suggest some shearing with minor brecciated clasts of skarn in sulphide matrix.	
D	ML108	181.6	202.2	100	gy	fr	STUF	SST		sx qz tu	5	cpx po asp cpy am	0	5		Gy-gn fine grained finely to medium bedded altered STUF with minor gy-bn altered SST interbedded. Sub-parallel to parallel VX. Minor qz+tu+fp+po+/-cpy granitic veins.	
D	ML108	202.2	203.5	100	bk	fr	ZSKCS				0	am po asp cpy	0	20		"Bk am- po- skarn with significant asp, approaching 5%."	
D	ML108	203.5	215.3	100	gy	fr	SST	STUF		am VQT	2	cpy am po	0	1		Gy-gn altered SST and STUF. STUF cut by fine dendretic am veinlets. Granitic qz-tu-fp with whispy textures occur.	
D	ML108	215.3	216.3	100	bn	fr	ZSKCS				0	am fp po cpu	0	5		Bn medium grained am-fp-po- skarn with trace cpy.	
D	ML108	216.3	220	100	gy	fr	STUF			am	2	cpy am po	0	1		Gy-gn altered finely bedded STUF with small scale faulting disprupting beds.	
D	ML108	220	233.9	100	bn	fr	SST			qz tu	2	bt am 	0	0		Bn medium bedded altered SST cut by whipsy qz-fp-tu veins containing trace sulphide.	
D	ML108	233.9	237	100	cm	fr	FG				0	se tu	0	0		img equigranular FG with minor se alteration and tu-rich patches.	
D	ML108	237	239.3	100	bn	fr	SST			qz tu	2	bt am 	0	0		Bn medium bedded altered SST cut by whipsy qz-fp-tu veins containing trace sulphide.	EOH
D	ML109	0	49.1	100	gy	fr	SST			cl sx	1		0	0		Gy mdb SST. Fe coated J throughout. Minor fractures developed with fine gn selvages with associated po.	
D	ML109	49.1	49.5	100	cm	fr	STUF				0	po	0	1		Cm weakly altered lam tnb tuff bed. Po replaced lapilli occur.	
D	ML109	49.5	73.6	100	gy	fr	SST			cl sx	1		0	0		Gy mdb SST. Fe coated J throughout. Minor fractures developed with fine gn selvages with associated po.	
D	ML109	73.6	91.1	na	bn	vox	RCLY				0		0	0		Bn waterlogged RCLY.	
D	ML109	91.1	115.4	na	gy 	fr	SST 	RCLY			0	cs	0	0		Tnb mdb gy SST with strongly clay altered and oxidized beds. Possible cs-rich replacements occur.	
D	ML109	115.4	117.4	na	gn	wox	ZSKCS				0	ac cc mt py	15	2		Wox ac-cc-mt ZSKCS	
D	ML109	117.4	127.2	na	gy gn 	fr	STUF	ZSKCS			0		5	1		"Meter-scale bands of STUF and ZSKCS. STUF packages tnb gy-pk with dendretic veinlets of am, minor po ds throughpout. ZSKCS packages pale gn verfy fine grained cpx-skarn with patchy bands of mt. Very minor po+py+/-cpy+/-asp ds. "	
D	ML109	127.2	142.8	na	gy	fr	STUF	ST			0		0	1		Tnb to mdb tuff and tuffaceous ST. Tuff as tnb packages of gy-pk-bn altered material with dendretic am veinlets. ST as ms bn beds of sfg altered material.	
D	ML109	142.8	144.9	na	gy	fr	ST				0		0	1		Ms bn sfg ST.	EOH
D	ML110	0	6.2	na	gy	fr	SST				0		0	0		Rubbly core of Fe stained gy SST.	
D	ML110	6.2	34.3	100	bn	fr	SST	SBRC			0	bt cpx po	0	0		Mdb sfg gn bn altered SST. Minor up to 10cm thick beds of intraformational mud chip SBRC with po replacing some (bk SMH?) clasts.	
D	ML110	34.3	35.4	100	gn pk 	fr	STUF			am	1	cpx gt po	0	1		Tnb gn pk altered STUF with veinlets of am. Minor po ds.	
D	ML110	35.4	38.1	100	bn	fr	ZMARB				0	gt 	0	0		Impure carbonate with mottled texture from development of glomeroporphyroblastc clusters.	
D	ML110	38.1	40.2	100	gy	fr	STUF				0	cpx po	0	1		Tnb gy gn STUF with ds po.	
D	ML110	40.2	46.9	100	gn	fr	ZSKCS				0	mt am sd po asp cpy cpx	10	5		Mottled gn ZSKCS with appreciable mt +am+sd+cpx+po+asp+cpy.	
D	ML110	46.9	53.55	100	gy	fr	STUF				0	cpx gt po	0	1		Pk gy altered tnb STUF.	
D	ML110	53.55	56.3	100	gn	fr	ZSKCS			sx	1	ac po mt 	10	1		Dk gn fine grained am- rich skarn with bands of mt occuring.	
D	ML110	56.3	60.7	100	bk	fr	ZSKM			sx	1	mt ac po 	75	1		Bk medium grained ZSKM of good purity. Minor po-veinlets. Minor thin interbeds of gn altered ST.	
D	ML110	60.7	75.75	100	gn	fr	ZSKCS			sx	10	am po mt asp cpy	15	30		Fine grained dk gn banded am- rich skarn with abundant po+/-asp+/-cpy as bands and veins. Mt rich bands relatively minor.	
D	ML110	75.75	84.6	100	gn	fr	SST				0	am	5	0		Strongly altered dk gn am altered SST transitional to ZSKCS.	
D	ML110	84.6	99	100	gy	fr	SST	V		qz tu	2	bt	0	0		Gy bn altered SST cut by qz+fp+tu+/-po veins.	
D	ML110	99	101.5	100	gy	fr	STUF	V		qz tu	5		0	1		weakly broken and veined STUF	
D	ML110	101.5	108	na	na	fr	XFBI	STUF	V	qz tu	na		0	1		Crush zone of fractured and veined STUF with minor clasts of qz+/-tu. Fractures either barren or infilled with VQC and po+/-cpy veins.	
D	ML110	108	108.1	100	gy	fr	XFBI				0		0	0		Gy fault breccia <10 cm tk with clasts of qz-cc-veined STUF in clayey matrix.	
D	ML110	108.1	110.5	100	gy	fr	FG				0	se tu	0	0		"Chilled gy porphyritic FR, chilling noticable through smaller phenocrysts and greater proportion of ivfg groundmass. Minor se alteration. Tu as conspicuous flecks throughout."	
D	ML110	110.5	125	100	cm	fr	FG				0	se tu sh	0	0		Strongly porphyritic cm FG with incipent se alteration. Tu as diffuse patches with very fine flecks of scheelite.	EOH
D	ML111	0	36.8	na	gy	wox	SST				0		0	0		Strongly fractured wox gy SST. Fe and clay alteration associated with fractures.	
D	ML111	36.8	39.9	na	gn	fr	SST				0	cl	0	0		Fracture or crush zone of patchly altered gn bn SST strongly overprinted by cl altereation. 	
D	ML111	39.9	40	na	gn	fr	XFBI				0	cl	0	0		Chloritic fault breccia.	
D	ML111	40	42.1	na	gn	fr	SST				0	cl	0	0		Fracture or crush zone of patchly altered gn bn SST strongly overprinted by cl altereation. 	
D	ML111	42.1	42.2	na	gn	fr	XFBI				0	cl	0	0		Chloritic fault breccia.	
D	ML111	42.2	52.1	na	gn	fr	SST			qz	2	cpx bt	0	0		Intact core of SST with patchy gn bn alteration.	
D	ML111	52.1	64.1	na	gn	wox	SST			qz	1	cpx bt	0	0		Rubbly core of weakly clay altered SST.	
D	ML111	64.1	76.1	na	og	vox	RCLY				na					Og RCLY with relict banding and bk veins.	
D	ML111	76.1	102.2	na	gy	fr	ZSKX			qz sx	1	po asp sd am	0	40		Metalic gy tn to md banded po-skarn. Po as replacement style alteration. Sd and am are conspicuous phases. Minor cm-scale beds of svfg altered sediment occur rarely.	
D	ML111	102.2	112.2	na	gy gn 	fr	ZSKCS	STUF		am sx	2	cpx po am	0	10		Decimeter-scale packages of gy altered tuff and am-po-rich skarn. Am-po-rich skarn has relict brecciated texture and is strongly veined by VX. 	
D	ML111	112.2	148.5	na	gy	fr	STUF			am	1	cpx po	0	2		lm tnb svfg gy altered STUF cut bu networks of fine whispy am-po veins. 	
D	ML111	148.5	151.3	na	bn	fr	SST			qz sx	1	bt po 	0	1		Bt-altered SST with minor VQX.	EOH
D	ML112	0	36.2	na	bn	fr	SST			qz sx	1	bt	0	0		Bt-altered SST with minor VQX.	
D	ML112	36.2	37.8	na	cm	fr	FG				0	si tu	0	0		Silicified FG dyke.	
D	ML112	37.8	75.5	na	bn	fr	SST			qz sx	1	bt	0	0		Bt-altered SST with minor VQX.	
D	ML112	75.5	78.5	na	gy	fr	STUF			cl sx	1		0	1		Altered lm STUF.	
D	ML112	78.5	82	na	bn	fr	SST			qz sx	1	bt	0	0		Bt-altered SST with minor VQX.	
D	ML112	82	83.3	na	gy	fr	STUF			cl sx	1		0	1		Altered lm STUF.	
D	ML112	83.3	144.5	na	bn	fr	SST			qz sx	1	bt	0	0		Bt-altered SST with minor VQX.	
D	ML112	144.5	165.5	na	bn gy	fr	SST	STUF		am	1	bt am gt po	0	1		bt-altered mdb SST with decimeter to meter scale beds of pk gn gt am altered STUF cut by am-po veins.	
D	ML112	165.5	167	na	gn	fr	ZSKCS				0	ac vs mt cc po	5	2		Coarse grained band of ac-vs-cc-mt-po skarn.	
D	ML112	167	185.3	na	gy	fr	STUF			qz am	1	cpx gt bt am po	0	2		lm tnb STUF with disrupted bedding preserved. Minor VQ and Vam.	
D	ML112	185.3	189.4	na	gn	fr	ZSKCS	STUF			0	am vs gt mt cpx	2	0		Medium grained am-vs-mt skarn interbedded with gy gn lm packages of STUF.	
D	ML112	189.4	198	na	gn gy 	fr	ZSKCS				0	mt am cpx 	30	0		"Thinly banded dk gn gy skarn; dk gn bands rich in mt+am; gy bands non-magnetic, rich in cpx."	
D	ML112	198	198.1	na	cm	fr	FG				0	si tu ep	0	0		Silicified tu ep altered img FG vein.	
D	ML112	198.1	209.1	na	gn	fr	ZSKCS				0	mt am cpx po	30	2		Mt-bearing tnb ZSKCS as above with some bands containing appreciable po.	
D	ML112	209.1	210.5	na	cm	fr	FG				0	si 	0	0		Tu altered ifg FG dyke.	
D	ML112	210.5	214.7	na	gy	fr	ST			sx	1	am vs mt po	5	1		Am-vs-mt altered ms sfg ST. 	
D	ML112	214.7	216.5	na	bn	fr	ZSKCS				0	vs cpx mt	10	0		Distinctive medium grained yellow-brown vs-rich skarn with appreciable mt.	
D	ML112	216.5	218.9	na	gy	fr	ST			sx	1	am po mt	5	1		Gy ms sfg magnetic ST.	
D	ML112	218.9	242.2	na	cm	fr	FG				0	tu	0	0		Porphyritic FG with flecks of tu. 	EOH
D	ML113	0	24.8	na	gy	wox	SST				0	lm clay	0	0		Strongly fractured weak to moderately weathered SST. Limonite Fe staining is common on fractures. Fracture controlled clay alteration. Rubbly core at the top of hole to 8.5 m depth.	
D	ML113	24.8	33	na	dgy	fr	SST				0	cl	0	0	fr	Strongly fractured SST with clean open fracture surfaces.	
D	ML113	33	41	na	dgy	fr	SST				0	cl clay	0	0	fr	Rubble zone of SST with local clay alteration.	
D	ML113	41	48.4	na	dgy bk	fr	XFBI				0	cl	0	0	fz	Chloritic fault breccia zone with rubble sections. Local clay alteration. The core is unconsolidated between 42 and 45 m.	
D	ML113	48.4	71.2	na	gn	fr	SST				0	cl bt	0	0		Intact core with bands of green and brown alteration.	
D	ML113	71.2	74.3	na	bn gn	fr	SST			qz ca	10	cl bt	0	0	stwk	As above overprinted by a qz ca veining forming a weakly developed stockwork.Weak bleaching overprint.	
D	ML113	74.3	83.8	na	bn gn	fr	SST			qz ca	1	cl bt cp	0	0.1		SST with minor beds of STUFF. Local disseminated chalcopyrite.	
D	ML113	83.8	86.4	na	gn	fr	SST	SCHT			0	cl cp	0	0.1	fr	SST with laminated light colored cherty bands. Fractured sections are common. Possible hydrothermal breccia.	
D	ML113	86.4	97.5	25	og	vox	RCLY				0	clay lm	0	0	fz	Orange colored clay altered rubble with significant core loss.	
D	ML113	97.5	103.9	na	gn	fr	ZSKCS			ca	3	cl clay py cp	0	5		Locally clay altered and vuggy calc-silicate skarn. Pyritic with minor chalcopyrite. Local folded carbonate veins.	
D	ML113	103.9	107.1	na	gn	fr	ZSKM			po	5	am mt po cp	30	30		Magnetite skarn with sections of semi-massive pyrrhotite.	
D	ML113	107.1	164.2	na	gn	fr	ZSKX			cp	5	am po cp mt	5	40		Banded pyrrhotite skarn. Po occurs as replacement. Veins of chalcopyrite up to 1 cm thick occur locally. Rare bands of magnetite.	
D	ML113	164.2	168.9	na	gn	fr	ZSKCS	ZSKX		py cp po t	8	am to po py mt cp	15	30		Magnetite bearing sulphide rich calc-silicate skarn. Bands of medium grained tourmaline are common. Vuggy pyrite veins up to 5 cm thick are common. Bands of semi-massive pyrrhotite.	
D	ML113	168.9	176.1	na	gn bn	fr	ZSKX			po py qz t	15	am to po py cp	1	25		Sulphide rich po veined calc-silicate skarn. Local vuggy pyrite veins up to 5 cm thick. Quartz veins +/- tourmaline are common throughout the interval.	
D	ML113	176.1	180.7	na	na	na	ZSKCS	ZSKX		po	10	am po mt cp	15	20		Sulphide rich calc-silicate skarn with intervals of magnetite skarn. Po veinlets and blebs are common throughout the interval. Local blebs of chalcopyrite.	
D	ML113	180.7	185.9	na	gn	fr	ZSKCS	STUF		cl qz	5	am cl po mt	2	4		Intermixed transitional unit of calc-silicate skarn and STUFF. Chlorite veinlet stockworks are commonn and local quartz veins are present. Minor patchy magnetite bearing sections.	
D	ML113	185.9	196.6	na	gy gn	fr	STUF	ZSKCS		cl	3	am cl po	0	1		Grey tuff with bands of calc-silicate skarn. Veinlets of chlorite are common. Local veinlets and blebs of po.	
D	ML113	196.6	200.6	na	bn	fr	SST			cl py	1	bt	0	1		Brown bt altered SST with minor chlorite and sulphide (po py) veinlets.	
D	ML113	200.6	206.4	na	wt gy	fr	FG				na		0	0	ms img	Fresh medium grained granite.	EOH 206.4m
D	ML114	0	11	na	gy	fr	SST				0	bt	0	0		Rubbly core of gy sfg non-magnetic SST with minor Fe coating broken surfaces at top of hole.	
D	ML114	11	24.5	na	gy	fr	SST			qz	1	bt	0	0		Intact core of gy non-magnetic ST with patchy bt alteration in sandier fractions.	
D	ML114	24.5	35.3	na	gy	fr	SST	STUF		am	1	bt cpx gt po	0	1		Sfg gy non-magnetic SST interbedded with thin beds of svfg lt gn and pk altered STUF with minor ds po and Vam.	
D	ML114	35.3	36.5	na	cm	fr	SBRC			ca	1	cc gt	0	0		Ms poorly sorted matrix supported breccia with altered sedimentary clasts in a fine grained carbonate bearing matrix: uncertain origin.	
D	ML114	36.5	50.5	na	gn gy 	fr	ZSKM	STUF		ca	1	mt am cpx po 	50	2		Mdb fine grained mt-am-po skarn with lt gn cpx-po altered STUF.	
D	ML114	50.5	57.8	na	gn	fr	ZSKCS				0	am cpx mt 	5	5		"Fine grained am-cpx- rich skarn with varying ds po and minor thin, diffuse mt-bands."	
D	ML114	57.8	59.8	na	gy gn 	fr	STUF			am	1	cpx gt	0	2		Lm tnb gy gn altered sfg STUF.	
D	ML114	59.8	62	na	gn	fr	ZSKCS				0	am cpx po mt	2	2		Fine grained am-cpx-po skarn with minor po.	
D	ML114	62	88.7	na	gy gn 	fr 	STUF			am	2	cpx am po	0	2		"Tnb sfg altered STUF, some beds with strong am alteration."	
D	ML114	88.7	100	na	bn 	fr	SST	V		qz tu	1	bt	0	1		Tnb bt altered non-magnetic SST with minor qz-po and qz-tu veins.	
D	ML114	100	101.4	na	gy	fr	SSIC			am	1	am	0	1		Gy tnb intraformational mud chip grit with convoluted bedding.	
D	ML114	101.4	109.8	na	bn	fr	SST	V		qz tu sx	1	bt	0	1		Tnb bt altered SST with minor thin beds of more tuffaceous material. Qz-po and qz-tu veins occur.	
D	ML114	109.8	115.6	na	gn	fr	XFBC	SST			0	cl	0	0		Cl altered fractured crush zone overprinting SST. Core is rubbly but no distinct fault rock occurs.	
D	ML114	115.6	116	na	cm 	fr	FG				0	si	0	0		Ifg si FG dyke.	
D	ML114	116	119.4	na	gn	fr	XFBC	SST			0	cl	0	0		Cl altered fractured crush zone overprinting SST. Core is rubbly but no distinct fault rock occurs.	EOH
D	ML115	0	31.7	na	gy	fr	SST			qz fp	1		0	0		Gy tnb mdb SST with minor qz+/-fp? veins.	
D	ML115	31.7	36.8	na	gy	fr	SST			qz fp cl p	5		0	1		Gy tnb mdb SST cut by qz+/-fp+/-cl+/-py vein network producing minor hydrothermal brecciation.	
D	ML115	36.8	51	na	gy	fr	SST	STUF	SBRC	qz fp cl p	1	po py	0	2		"Irregularly tnb SST, STUF & intraformational SBRC (disrupted bedding or broken formation). Blebs of po and py conspicuous in tuffaceous material."	
D	ML115	51	55.9	na	bk	fr	ST				0	po	0	2		lm svfg ST with conspicuous po blebs parralel to S0.	
D	ML115	55.9	83	na	gy	fr	SST			qz fp	1	bt	0	0		Gy mdb monotonous sfg SST with weak patchy bt alteration.	
D	ML115	83	84.7	na	gn	fr	STUF				0	po cpx	0	2		Svfg gn altered STUF with porphyroblastic po.	
D	ML115	84.7	115.6	na	gy	fr	SST			qz fp	1	bt cpx	0	0		Weakly bt+/-cpx altered mdb SST.	
D	ML115	115.6	116.5	na	gn	fr	XFBI				na	cl cc	0	0		Zone of intensly broken core with cl-cc coated surfaces.	
D	ML115	116.5	140.5	na	gy	fr	SST			qz fp	1	bt cpx	0	0	fr	Broken core of weakly bt+/-cpx altered mdb SST.	
D	ML115	140.5	143.5	na	na	na	XFBI				0		0	0		"Zone of core loss within broken zone, most likely fault zone"	
D	ML115	143.5	159.4	na	bn	fr	SST			qz fp	1	bt cpx	0	0	fr	Alteration of SST increases in intensity. Core remains broken throughout.	
D	ML115	159.4	177	na	bn	fr	SST	STUF		qz fp	3	bt cpx	0	0		bt-cpx altered SST with gn altered tuffaceous interbeds. Veining becomes more intense throughout as fine networks. 	
D	ML115	177	179.2	na	gn	fr	XFBI				0	cl	0	0			
D	ML115	179.2	196.1	na	gy	fr	SST				0		0	0		Intact core of dk gy sfg mdb SST.	EOH
D	ML116	0	33	na	gy	wox	SST				0	lm cy	0	0		Interbedded sandstone and siltstone. Weak weathering with lm coated fractures. Moderate to strongly fractured.	
D	ML116	33	45.4	na	gy	fr	SST				0	lm cy	0	0		Interbedded sandstone and siltstone.  Limonite coatings are common on fractures. Local blocky sections.	
D	ML116	45.4	72.1	na	gy	fr	SST				0		0	0		Interbedded sandstone and siltstone. Local lm fracture coatings.	
D	ML116	72.1	74.8	na	gy gn	fr	STUF	ZSKCS			0	am	0	0		Grey tuff with bands of calc-silicate skarn.	
D	ML116	74.8	79.1	na	gy	fr	SST				0		0	0		Interbedded sandstone and siltstone. Local lm fracture coatings.	
D	ML116	79.1	81	na	gy gn	fr	STUF	ZSKCS			0	am	0	0		Grey tuff with bands of calc-silicate skarn.	
D	ML116	81	85.7	na	bn	mox	ST	STUF			0	cy	0	0	fr	Brown altered siltstone with local bands of laminated chlorite altered STUF(?). Core loss occurs within a clay altered rubbly interval from 82 to 85.2 m.	
D	ML116	85.7	96.1	na	og	vox	RCLY	ZSKCS			0	cy lm	0	0	fr fz	Rubbly limonitic oxidized clay interval. Textures locally preserved look like the calc-silicate skarn below this interval. Rubble and core loss is common throughout the interval.	
D	ML116	96.1	100.5	na	gn	wox	ZSKCS				0	cy lm he	0	0	vs	Weakly clay altered and locally limonitic calc-silicate skarn. Local vesicular sections.	
D	ML116	100.5	108.3	na	gy	fr	STUF	ZSKCS		ca	1	cl ca py	0	0.1		Grey banded tuff with local bands of calc-silicate skarn. Limonitic clay altered rubble occurs from 102.5 to 104.7 m.	
D	ML116	108.3	124.1	na	gy	fr	ST	STUF	ZSKCS	ca	1	cl ca py	0	0.1	tnb	Dominantly silstone with interbeds of STUF. Local bands of sulphide bearing calc-silicate skarn. Local vuggy dissolution within skarn bands. Thin to medium bedding with with 1-3 cm thick beds being dominant.	
D	ML116	124.1	129.3	na	gn	fr	ZSKCS			ca	1	am cl ca po py	1	3		Calc-silicate skarn altered SST. Transitional unit to the skarn below. Blebs of pyrite and pyrhotite are common. Vein carbonate up to 15 cm thick occurs in places.	
D	ML116	129.3	141.6	na	gn	fr	ZSKM				na	am mt py po	10	5		Magnetite bearing calc-silicate skarn.	
D	ML116	141.6	143.2	na	gy	fr	STUF				0	mt po	3	1		Banded tuff with minor narrow bands of magnetite.	
D	ML116	143.2	144.6	na	gn	fr	ZSKM				0	am mt py po	8	3		Magnetite skarn with interbeds of tuff.	
D	ML116	144.6	146.9	na	gy gn	fr	STUF	ZSKCS			0	am mt po	3	3		Banded calc-silicate altered tuff with local cm scale bands of magnetite.	
D	ML116	146.9	147.6	na	wt gy	fr	FG				0		0	0		Granitic dyke.	
D	ML116	147.6	154.9	na	gn	fr	ZSKM	ZSKX			0	am mt py po	25	10		Dominantly magnetite skarn with narrow sections of sulphide skarn.	
D	ML116	154.9	163.5	na	gy gn	fr	STUF			po py	1	am mt py po	3	4		Interbedded tuff and siltstone with bands of calc-silicate alteration that are magnetite and sulphide bearing.	
D	ML116	163.5	165	na	wt gn	fr	FG			py	0.1	py	0	0.1		Granitic dyke.	
D	ML116	165	166.8	na	gn	fr	STUF				0	am py po	0.5	3		Tuff with local sulphide skarn. Minor magnetite content.	
D	ML116	166.8	175	na	wt gn	fr	FG				0	lm cy	0	0		Medium to coarse grained granite. Local fracture controlled limonite and weak clay alteration occurs between 173 and 173.7 m.	EOH 175.0m
D	ML117	0	10.9	80	gy og	mox	SST				0	lm clay	0	0	fr	Strongly fractured to rubbly interbedded siltstone and sandstone. Fracture controlled weak clay alteration. Limonite oxide staining occurs throughout the interval.	
D	ML117	10.9	17.5	na	gy	wox	SST				0	lm clay	0	0		Interbedded siltstone and sandstone. Limonite oxide coatings on fractures occur throughout the interval.	
D	ML117	17.5	24.8	na	gy gn	fr	ST	ZSKCS		po	21	am po	0	1		Siltstone with sections of calc-silicate skarn. Minor amounts of pyrhotite are present as veinlets and small blebs with the skarn intervals. Chlorite healed fracture stockwork occurs between 23.7 and 24.0 m.	
D	ML117	24.8	55.8	na	gy	fr	SST	ZSKCS			0	am bt	0	0		Interbedded sandstone and siltstone with minor bands of calc-silicate skarn alteration. Rare tuffaceous light green colored interbeds up to 5 cm thick.	
D	ML117	55.8	73.9	na	gy	fr	SST			ca cl	0.1		0	0.1		Interbedded sandstone and siltstone. Rare ca and cl veinlets.	
D	ML117	73.9	77	na	wt gy	fr	FG				0	lm	0	0		Granite dyke with minor fracture controlled limonite stain.	
D	ML117	77	96.1	na	gy	fr	SST				0	cl	0	0		Interbedded sandstone and siltstone. Minor chlorite on fractures.	
D	ML117	96.1	96.8	85	gy og	wox	XFBI				0	lm clay	0	0	fr	Strongly fractured broken incohesive interval with remnant clay gouge material. Possible fault.	
D	ML117	96.8	102.8	na	gy	fr	SST			qz ca	0.5	cl	0	0		Intermixed siltstone and sandstone. Minor quartz carbonate veinlets. Local chlorite on fractures.	
D	ML117	102.8	103.6	na	wt lgn	fr	FG				0	se	0	0		Granite dyke.	
D	ML117	103.6	111.5	na	gy	fr	SST			qz ca	0.5	lm	0	0		Intermixed sandstone and siltstone. Local fracture related limonite staining.	
D	ML117	111.5	113	85	gy og	wox	XFBI				0	lm cl clay	0	0	fr	Limonitic strongly fractured to broken interval with remnant clay gouge material. Chlorite alteration.	
D	ML117	113	122	na	gy	fr	SST				0	lm cl	0	0		Intermixed siltstone and sandstone with local chloritic and limonitic broken intervals.	
D	ML117	122	134.5	na	gy bn	fr	SST			qz tu	0.5	bt gt	0	0		Brown biotite altered siltstone and sandstone with garnet rich sections.	
D	ML117	134.5	141.4	na	gy bn	fr	SST				0	bt	0	0	stwk	Interbedded sandstone and siltstone unit has been overprinted by a healled fracture stockwork. The fracture openings have been filled with light green fine sand material. Brown biotite altered patches.	
D	ML117	141.4	142.4	na	gn	fr	ZSKCS				0	am	0	0		Narrow band of calc-silicate skarn.	
D	ML117	142.4	144.4	na	bn gy	fr	SST			ca	0.5	bt	0	0		Brown biotite altered interbedded siltstone and sandstone. Local chloritic broken core from 143.6 to 143.8 m.	
D	ML117	144.4	145.4	na	wt lgn	fr	FG				0	se	0	0		Granite dyke.	
D	ML117	145.4	158.2	na	gy bn	fr	SST			ca	1	bt	0	0	stwk	Interbedded siltstone and sandstone is locally overprinted by fine sand filled healed fracture stockworks. Brown biotite altered patches.	
D	ML117	158.2	173	na	gy gn	fr	FG				0	cl py	0	2		Coarse grained granite has been altered to a greyish green color. Pyrite blebs occur locally throughout the interval. Weak clay alteration. Local druzy quartz lined vugs.	
D	ML117	173	200.1	na	wt gy	fr	FG				0	se lm	0	0		Coarse grained granite with minor fracture related limonite stain.	
D	ML118	0	16.3	80	gy og	wox	SST			qz cl	2	he cl	0	0		weakly weathered siltstone/sandstone beds with weak he staining. Ka alteration common	
D	ML118	16.3	51.7	100	gy gn	fr	SST	STUF		qz cl	2	cl po py bt	0	1		"beds of predominantly siltstone and fine sandstone, wekly oxidised fractures. Minor ds po and py in patchy concentrations associated with minor STUF."	Start of NQ - 34.8m
D	ML118	51.7	52.9	100	lgn bn 	fr	STUF			qz	1	cl po py bt	0	5		banded tuff with ds po ± py. Bn bt horizons present. Sulphide occurs often as isolated rectangular blebs of unequal size.	
D	ML118	52.9	59.9	100	gy gn	fr	SST			qz cl	5	cl si bt po	0	1		"beds of siltstone and sandstone with varying alteration of cl veins and siliceous horizons, minor bt nearing fault."	
D	ML118	59.9	59.95	50	gn gy	fr	XFBC				0	cl	0	0		"5cm cohesive fault zone, consisting of SST clasts in a cl matrix. (clast supported)"	
D	ML118	59.95	86.3	90	gy gn	fr	SST			qz cl	2	cl po bt	0	1		beds of sandstone and siltstone with VL and VQL and fine blebs of po often in concentrated bands parallel with bedding	
D	ML118	86.3	90.1	100	dgy bn	fr	SST			qz cl	1	cl bt py po	0	2		"sandstone/siltstone beds with increased amounts of bt, fine py/po dusting common. Weakly magnetic"	
D	ML118	90.1	93.5	100	lgn bn 	fr	STUF	SST		cl	5	bt po py	0	2		banded STUF with significant bt alteration and VL often containing po and py. Po and/or py dusting common	
D	ML118	93.5	109	60	og bn lgn	fr	RCLY				0	lm mt 	5	0		"lgn/og/bn clay, relict banding present, mt present close to upper contact."	
D	ML118	109	119.7	100	lgy gn bn	fr	SCB			qz cl	1	bt cl cc po py gt	0	1		"thin-med bedded carbonate bed that fizzes with HCL, significant bt alteration throughout, cl weathered zones"	
D	ML118	119.7	134.7	95	dgn dgy	fr	ZSKCS	SCB		ca sx	1	mt cl cc po py	10	5		Am and carbonate rich ZSKCS with patchy concentrations of do and mt. increasing sulphide content nearing fault zone downhole.	
D	ML118	134.7	134.8	50	gy bn	fr	XFBC				0	py cl	0	20		clast supported cohesive breccia with cl matrix and high amounts of py	
D	ML118	134.8	149.3	100	gy bn	fr	ZSKM	STUF		qz cl	1	mt bt cl py po	50	15		bands of mt and non-magnetic bt rich zones near fz becoming more mt rich with bands of STUF	
D	ML118	149.3	163.1	90	lgn bn gy	fr	STUF	ZSKM		qz cl	5	bt mt cl si po py	10	10		"laminated bands of STUF with high bt proportions throughout. Patchy mt common, po ds throughout and in localised banded concentrations"	
D	ML118	163.1	187.1	100	lgn bn	fr	STUF			sx cl qz	10	bt si cl po py asp	0	5		"banded STUF, rich in bt, po occuring in small veinlets and ds throughout. Thin (2-5cm) VQT + bt often containing asp? And/or py. "	
D	ML118	187.1	205	100	cm bk	fr	FG			qz tu	20		0	0		med-coarse grained qtz-feld-tourm rich granite. Mostly equigranular with finer bt/tourmaline crystals. Concentrated veins of qz-tu common. Early alteration of some feldspars to gn ka. V.minor gy sulphide in VQT (asp/stannite?)	EOH 205.0m
D	ML119	0	1.6	85	dk gn	fr	ZSKM				0	ac mt po	50	10		Coarse grained ac-mt-po skarn.	
D	ML119	1.6	4.5	100	gy gn	fr	cSS	STUF			0	cc gt vs cpx po	0	1		Tnb altered calcareous sandstone and tuffaceous siltstone.	
D	ML119	4.5	6.2	100	bz bk	fr	ZSKX				0	po am mt cpy	5	40		Banded po-rich skarn with minor mt and cpy.	
D	ML119	6.2	9.9	100	gy gn	fr	cSS	STUF			0	cc gt vs cpx po	0	1		Tnb altered calcareous sandstone and tuffaceous siltstone.	
D	ML119	9.9	11.3	100	dk gn	fr	ZSKCS				0	po hb cpx mt	2	20		Heterogeneous fine-grained po-hb-cpx skarn.	
D	ML119	11.3	14.3	100	gy	fr	STUF			am	1	cpx am bt po	0	1		Stongly altered tuffaceous siltstone.	
D	ML119	14.3	16.1	100	gy gn	fr	ZSKCS			cc po cpy	5	ac cpx po mt cpy	5	10		Heterogeneous fine-grained ac-cpx-po skarn cut by cc-po-cpy veins.	
D	ML119	16.1	20.1	100	gy gn	fr	cSS	STUF			0	cc gt vs cpx po	0	1		Tnb altered calcareous sandstone and tuffaceous siltstone.	
D	ML119	20.1	20.4	100	bl	fr	VF			fl po qz asp	100	fl po qz asp	0	50		Fluorite-pyrrhotite vein with minor qz and trace asp + cpy.	
D	ML119	20.4	32.2	100	gy	fr	STUF	ZSKCS		am	1	cpx bt gt po am	0	1		Tnb cpx- gt- altered tuffaceous siltstone with minor am+po+/-cpx calc-silcate altered beds.	
D	ML119	32.2	32.3	100	bl	fr	VF			fl asp tu	100	fl asp tu	0	50		Fl- asp- tu- vein.	
D	ML119	32.3	33.4	100	bl gn	fr	VF				100	fl asp tu	0	50		fl+asp+tu vein	
D	ML119	33.4	51.75	100	dgy gy	fr	SST	STUF			1	po qz bt am	0	1		sfg to smg sandstone and siltstone beds interbedded with very minor tuffaceous beds. weak bt+am alteration through some beds.  Non magnetic unit.  Minor beds of lithic sandstone beds.  Sulphide(x)+quartz(Q)veins	
D	ML119	51.75	55.8	95	dgy	fr	SST				5	cl py qz	0	0.1		As above without the alteration bands and tuff beds.  Non magnetic.  Moderate cl veining.  Moderately fractured rock.  Very minor sulphide in some fractures	
D	ML119	55.8	55.9	na	na	fr	XFBI	SST			5		0	0		~10cm gauge zone with breccia and fractured rock several ms either side.	
D	ML119	55.9	76.55	95	dgy	fr	SST				na	cl qz 	0	0.1		As SST above	
D	ML119	76.55	76.65	na	na	fr	XF81				na		0	0		10cm incohesive breccia before XFBI	
D	ML119	76.65	78.25	90	gy	fr	XFBC	SST			50	cl qz ca	0	0		"~2m of mostly cohesive SST breccia,with cl matrix"	
D	ML119	78.25	78.35	na	na	fr	XFBI				na		0	0		7-10cm incohesive breccia after XFBC	
D	ML119	78.35	80.2	95	gy	fr	SST	XHB			30	cl ca	0	0		sandstone + siltstone mod to intensely veined by cl with some hydrothermal brecciation	
D	ML119	80.2	98.5	95	dgy	fr	SST				2	cl ca vs?	0	0		sfg sandstone-siltstone beds with cl veining + flecks. Ca veining also. Mod-intensely fractured. Patchy mod magnetism. ~5cm pk k-spar rich granite dyke at 94.3m	
D	ML119	98.5	99	na	lgy	fr	SST	SILT			0		0	0		unconsolidated silt with sfg sandstone and siltstone fractured rock	
D	ML119	99	118.8	95	dgy	fr	SST				0	cl ca	0	0		"unconsolidated silt with sfg sandstone and siltstone fractured rock, patchy weak to mod magnetism."	
D	ML119	118.8	118.9	na	na	fr	XFBI				na		0	0		"~5cm unconsolidated granule to pebble sized sediment, along with minor gougey material"	
D	ML119	118.9	129.85	100	cm gy	fr	FG			tu	1	tu se	0	0		"granitoid in possible fault contact with SST as there is ~5cm unconsolidated granule to pebble sized sediment, along with minor gougey material. Equigranular and porphyritc texture"	
D	ML119	129.85	142.5	100	dgy	fr	SST			cl ca qz	1	cl	0	0		sfg sandstone and siltstone beds. Mod magnetism decreasing to no magnetism DH	
D	ML119	142.5	164.2	100	gy bn gn	fr	SST			qz cl ca	1	bt am si 	0	0		"bt and am altered sfg to smg sandstone and siltstone beds. Non magnetic. Qz, cl, cc and clinochlore veins common. Some beds are silicified."	
D	ML119	164.2	175.8	100	bn lgy	fr	SST			qz po am ca	2	bt am si po cl	0	1		"blotchy bt and si altered sfg to smg sandstone and siltstone, with minor whispy, mottled tuffaceous mudstone, po ds as well as veined"	
D	ML119	175.8	180	100	bn gy lgn	fr	STUF	SST	ZSKCS	qz po bt	na	bt si am po py	0	2		"banded tuffaceous mudstone and siltstones, with some bt alteration. Po in veins and ds"	
D	ML119	180	184	100	dgy lgy lg	fr	ZSKCS			po gt cc	2	am po px si cc mt gt vs	2	5		"mottled calc-silicate skarn and tk gy beds, with po veins and dissemination. Minor cc and gt veins"	
D	ML119	184	188.4	100	gy gn pk 	fr	ZSKCS	ZSKM		po cc	1	am po mt cc sd px cpy py	25	2		calc-silicate and mt rich skarn. Mt banded and ds. Minor banding but mostly mottled	
D	ML119	188.4	192.4	100	dgy bk	fr	ZSKM	ZSKCS		po fp fl cl	1	mt am po	50	10		mt-am-rich ZSKM with minor sulphides disseminated and in veins.	
D	ML119	192.4	196	100	gn gy pk y	fr	ZSKCS	ZSKM		po cpy py cc	1	am mt po py sd gt vs?	20	5		mottled and weakly banded am-mt rich ZSKCS. Po+- cpy +-py veins present.	
D	ML119	196	198.8	100	bk gn	fr	ZSKM	ZSKCS		po	1	mt am vs po py gt	50	3		mt-am rich weakly banded ZSKM. Mt banded and disseminated. Minor po veins.	
D	ML119	198.8	201.8	100	gy gn pk 	fr	ZSKCS	ZSKM		ca	1	am mt po py sd gt vs?	20	2		as ZSKCS above.	
D	ML119	201.8	204.4	100	dgy bk bn	fr	ZSKM	ZSKCS		py	1	mt am vs po py gt	60	2		as ZSKM above. Plus minor thin tuff beds.	
D	ML119	204.4	213.3	100	dgy lgy pk	fr	ZSKCS	ZSKM	STUF	po qz	2	am mt vs gt bt si po	10	5		am-mt-gt rich ZSKCS with bands of mt skarn and tuff. Po is disseminated and in veins.	
D	ML119	213.3	218.1	100	lgy gbn gn	fr	STUF	ZSKCS	ZSKM	po	2	bt am mt	3	2		bt altered tuffaceous mudstone/siltstones. Po disseminated more in bt altered weakly banded sediments. Weak magnetism due to po.	
D	ML119	218.1	222.75	100	bn gy	fr	SST			po py	2	bt	1	2		bt altered sfg to smg sandstone and siltstone unit. Minor tuff beds. Non magnetic.	
D	ML119	222.75	223.7	100	yw wt bk	fr	FG			tu	10	se tu	0	0		ifg quartz-tu rich granitoid. Tu veins common and minor sericite alteration present.	
D	ML119	223.7	232.5	100	bn dgy lgy	fr	SST			cl fl am	1	bt si po cpy	0	1		weakly bt and si altered sfg to smg sandstone and siltstones. Non magnetic. 231.3m-232m has subrounded/subangular mudstone conglomerate bed (matrix supported). ~80cm thick am-qz-po-cpy-cl rich calc-silicate vein?lense?	
D	ML119	232.5	236.8	100	dgy	fr	SST			cl fl	1	cl	0	1		sfg sandstone and siltstone unit. Non magnetic.	
D	ML119	236.8	237	100	gy	fr	SILT						0	0		unconsolidated silt-fine sand at the end of hole. EOH 237m.	EOH 237m
EOF