H0002	Version	4																	
H0003	Date_generated	7/11/2014																	
H0004	Reporting_period_end_date	29/09/2014																	
H0005	State	NT																	
H0100	Tenement_no	EL26831	EL26835	EL28656	EL30156														
H0101	Tenement_holder	Sandfire Resources NL																	
H0102	Project_name	North Batten JV																	
H0106	Tenement_Operator	MMG Exploration Pty Ltd																	
H0200	Start_date_of_data_acquisition	1/01/1985																	
H0201	End_date_of_data_acquisition	11/09/2014																	
H0202	Template_format	DL_4																	
H0203	Number_of_data_records	490																	
H0204	Date_of_metadata_update	10/11/2014																	
H0300	Downhole_lithology_data_file	GR321_2014_GA_08_Appendix4_DownholeLithologicalLogs																	
H0301	Location_data_file	GR321_2014_GA_06_Appendix2_DrillCollars																		
H0302	Downhole_lithology_data_file	GR321_2014_GA_08_Appendix4_DownholeLithologicalLogs																	
H0307	Lithology_code_file	GR321_2014_GA_10_Appendix6_LithCodes																																		
H0400	Drill_code	DD																	
H0402	Description	Diamond Drilling																	
H1000	Hole_id	DEPTH_FROM	DEPTH_TO	Relogged	Lith_Qualifier	Lith_Qualifier2	Lith_Qualifier3	Lithology	Acidtest	Weathering	Regolith_Type	Hardness	ColourShade	Colour1	Colour2	Grainsize_Crystal	Comments	Stratigraphy	LoggedBy
H1001	Units	metres	metres																
H1004	Accuracy	0.1	0.1																
D	11BLDD0015	0	95.8	P				NL											
D	11BLDD0015	95.8	100.82	P	bnd	lam	fra	SSL		5			MD	BRN	BRN	fg	Completely weathered laminated siltstones; 6mm thick cherty horizons	Pmnc	
D	11BLDD0015	100.82	110.8	P	bnd	lam		SSL		4			MD	BRN	BRN	fg	Highly weathered siltstones with minor sedimentary breccias; SBX are slightly haematite stained by waterflow; Lith1RegolithOverprint : Bleached Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : BR Lith2Colour2 : RD   ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmnc	
D	11BLDD0015	110.8	118.57	P	bnd	lam		SSL		5			MD	BRN	BRN	fg	Completely weathered siltstones with minor sedimentary breccias; SBX are slightly haematite stained by waterflow; Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : BR Lith2Colour2 : RD   ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmnc	
D	11BLDD0015	118.57	122.08	P	bnd	lam		SSL		4			MD	BRN	BRN	fg	Completely weathered laminated and banded siltstones (no sedimentary breccias) partly silicified and haematised; no dolomite reaction to HCl; Lith1RegolithOverprint : Silicified       	Pmnc	
D	11BLDD0015	122.08	131.53	P	bnd	lam		SSL		4			MD	BRN	BRN	fg	Highly weathered siltstones with minor sedimentary breccias; no dolomite reaction to HCl possibly due to weathering; Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : BR    ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmnc	
D	11BLDD0015	131.53	136	P	mas			SBX		4			LT	GRY	GRY		Silicified sedimentary breccia appears to be composed of dolomitic siltstone fragments some with possible domal stromatolites; Lith1RegolithOverprint : Silicified       	Pmx	
D	11BLDD0015	136	140.08	P	mas			SBX		4			MD	BRN	BRN	cg	Massive sedimentary breccia includes some fragments containing possible domal stromatolites; no dolomite reaction with HCl; Lith1RegolithOverprint : Silicified       	Pmx	
D	11BLDD0015	140.08	156.64	P	mas			SBX		4			MD	BRN	BRN	cg	Highly weathered sedimentary breccia composed of angular dolomitic siltstone clasts; weakly silicified and bleached zones.  Minor dolomitic siltstone; no dolomite reaction to HCl.; Lith1RegolithOverprint : Bleached Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : BR    ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmx	
D	11BLDD0015	156.64	161.7	P	bnd	fra		STD		3			LT	GRY	GRY	fg	Pale blue grey dolomitic siltstones (dolomite leached out); partly silicified with extensive bleaching emanating into mass from fractures; Lith1RegolithOverprint : Bleached Lith2pc : 20 Lith2ColourTone : P Lith2Colour1 : GY Lith2Colour2 : WH   ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmx	
D	11BLDD0015	161.7	165.87	P	mas			SBX		3			DK	BRN	BRN	cg	Sedimentary breccia with many jigsaw fit fragments of dolomitic siltstone; some fragments angular are more than 10cm long.  Sharp irregular transition to unit below.; Lith1RegolithOverprint : Silicified       	Pmx	
D	11BLDD0015	165.87	223	P	mas	bnd		SBX		3			MD	GRN	GRN	cg	Coarse sedimentary breccia consisting of silicified stromatolitic dolomite fragments with minor dolomitic siltstone horizons.  Fragments are strongly silicified. Includes white silica-clay nodules within breccia.; Lith2pc : 5 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : BL   ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmx	
D	11BLDD0015	223	243.8	P	bnd			SBX		4			LT	GRY	GRY	cg	Grey blue sedimentary breccias becoming more bleached downwards.; Lith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : P Lith2Colour1 : WH    ; Grainsize_Crystal2; fg  Lith2_Qualifier; slt  Lith2_Qualifie2; alg	Pmx	
D	11BLDD0015	243.8	262.17	P	lam	bnd	fra	SSL		1			MD	RED	RED	fg	Laminated red siltstones interbedded with  sedimentary breccias; SBX are partly jigsaw fit and do not appear to have moved far.; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BL   ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmq	
D	11BLDD0015	262.17	276.15	P	mas			SBX		3			MD	GRY	GRY	cg	Sedimentary breccias dominate; and include polymictic fragments indicating much greater transport than highr up. Siltstone has many rip up clasts.; LithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : PK   ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	276.15	284.72	P	mas			SSH		4			MD	BLU	BLU	cg	Both sedimentary breccias and siltstones are partially bleached with porous zones.; Lith2pc : 50 Lith2ColourTone : M Lith2Colour1 : BL Lith2Colour2 : WH   ; Grainsize_Crystal2; fg  Lith2_Qualifier; bnd	Pmq	
D	11BLDD0015	284.72	299.25	P	mas	bed		SBX		5			MD	BRN	BRN	cg	Extensive haematite staining and deposits in fractures and along bedding; some thin zones completely weathered.; Lith1RegolithOverprint : Bleached Lith2pc : 50 Lith2ColourTone : P Lith2Colour1 : CR Lith2Colour2 : RD   ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	299.25	313.13	P	bnd	lam	fra	SDM		3			MD	GRY	GRY	fg	Moderately silicified sequence of stromatolitic dolomites and dolomitic siltstones with minor sedimentary breccias. PY in some fracture filling; with sparse carbonate.; Lith1RegolithOverprint : Silicified Lith2pc : 45 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : BK   ; Lithology3; SBX	Pmq	
D	11BLDD0015	313.13	318.8	P	bnd	lam		STD		1			MD	GRY	GRY	fg	Slightly silicified  sequence of dolomitic silstones; dolomites with thin coarser unit of dolomitic arenite. Thin carbonate veins oriented both along bedding planes and steeply inclined along the core axis.; LithStructure :  Vein (undifferentiated); LithStructure :  Vein (undifferentiated); Lith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : P Lith2Colour1 : GY    ; Lith2_Qualifier; mas  Lithology3; SSD	Pmq	
D	11BLDD0015	318.8	324.32	P	lam			STD		0			MD	GRN	GRN	fg	Sequence of dolomitic siltstones and dolomite with dolomitic arenite units increasing downhole.  Sequence is pale green and red.; LithStructure :  Vein (undifferentiated); LithStructure :  Vein (undifferentiated); Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : GY    ; Lith2_Qualifier; bnd  Lithology3; SSD	Pmq	
D	11BLDD0015	324.32	331.17	P	slt	lam	alg	SDM		0			MD	GRY	GRY	fg	Slightly silicified sequence of dolomitic silstones with domal stromatolites with dolomites.  Some dolomitic arenites form 12cm deep channel structures with bands of rip up clasts.; LithStructure :  Vein (undifferentiated); LithStructure :  Vein (undifferentiated); Lith1RegolithOverprint : Silicified Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : GY    ; Lith2_Qualifier; mas  Lithology3; SSD	Pmq	
D	11BLDD0015	331.17	336.74	P	ool	bnd		SSD		1			MD	GRY	GRY	mg	Arenite composed of black ooliths to 2mm diameter; thicker units composed of subangular dark grey to black oolith fragments; Lith2pc : 10 Lith2ColourTone : D Lith2Colour1 : GY Lith2Colour2 : BK   ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	336.74	349.25	P	mas	bnd		SSD		1			LT	PNK	PNK	mg	Arenite is recrystalised and silicified with numerous stylolites in places indicating dolomitic content.  Black oolites in darker medium grained units.; texture:scour marks; Lith1RegolithOverprint : Silicified Lith2pc : 30 Lith2ColourTone : D Lith2Colour1 : GY    ; Grainsize_Crystal2; fg	Pmq	
D	11BLDD0015	349.25	354.4	P	slt	bnd	alg	SDM		0			MD	GRY	GRY	fg	Finer unit of dolomitic siltstones with thin dolomites and some stromatolites.  Numerous rip up clasts in thin units.; Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GY    ; Lith2_Qualifier; mas	Pmq	
D	11BLDD0015	354.4	359.97	P	mas	bed		SSD		0			LT	PNK	PNK	mg	Fresh dolomitic sandstone; dolomitic siltstone. ; Lith1RegolithOverprint : Silicified Lith2pc : 20 Lith2ColourTone : D Lith2Colour1 : BR Lith2Colour2 : BK   ; Grainsize_Crystal2; fg  Lith2_Qualifier; bnd	Pmq	
D	11BLDD0015	359.97	371.02	P	lam	bnd		STD		0			MD	CRM	CRM	fg	Fr dolomitic siltstone interbedded with dolomitic arenite.  SDOL massive. ; LithStructure :  Deformed; Lith1RegolithOverprint : Silicified Lith2pc : 30 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : PK   ; Grainsize_Crystal2; cg   Lithology3; SDO	Pmq	
D	11BLDD0015	371.02	397.9	P	lam	bnd	<F	STD		0			DK	RED	RED	fg	Fr Dolomitic siltstone interbedded with dolomite.  Microfracturing offsetting lamination planes. ; Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : RD    	Pmq	
D	11BLDD0015	397.9	417.67	P	mas	fra	itb	STD		0			MD	GRY	GRY	fg	Fr silty dolomite; fractured and slumped interbedded with course grained dolomitic arenite. ; LithStructure :  Slumped; Lith1RegolithOverprint : Silicified Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; cg	Pmq	
D	11BLDD0015	417.67	432.9	P	bnd	lam		STD		0			DK	GRY	GRY	fg	Fr dolomitic siltstone interbedded with strom. dolomite.  microfractured. Pyrite blebs. ; LithStructure :  Slumped; LithStructure :  Slumped; Lith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : D Lith2Colour1 : GY    ; Lith2_Qualifier; mas	Pmq	
D	11BLDD0015	432.9	439.4	P	mas	bnd	itb	SSH		0			DK	BLK	BLK	fg	Pyritic black shale interbedded with minor beds of silicified dolomite.  ; Lith2pc : 10 Lith2ColourTone : L Lith2Colour1 : CR    	Pmq	
D	11BLDD0015	439.4	452.78	P	lam	bnd	<F	STD		0			MD	RED	RED	fg	Red Green laminated siltstone.  Dolostone with intermittent stylolites. ; Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : CR    	Pmq	
D	11BLDD0015	452.78	463.7	P	mas	fri	fra	SDO		0			LT	GRY	GRY	fg	fine grained dolomite with carbonacous veins;chert nodules;  stylolites and well silicified. Silty dolomite; Lith1RegolithOverprint : Silicified Lith2pc : 10 Lith2ColourTone : L Lith2Colour1 : GY    ; Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	463.7	467.84	P	mas	<F	itb	SDO		0			LT	GRY	GRY	fg	dolomite with stylolite compression bands.  At 466.6m vuggy with py vein.  ; Lith1RegolithOverprint : Silicified Lith2pc : 50 Lith2ColourTone : M Lith2Colour1 : GY    ; Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	467.84	469.9	P	mas	vug		SSD		0			LT	GRY	GRY	mg	SDAR sub-ang poorly sorted; matrix supported - vuggy sections.  ; Lith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	469.9	474.78	P	lam	bnd	itb	STD		0			DK	GRY	GRY	fg	SDAR interbedded with SDOL. Pyrite @ 476.82m blebby.; Lith1RegolithOverprint : Silicified Lith2pc : 60 Lith2ColourTone : M Lith2Colour1 : GY    ; Lith2_Qualifier; mas  Lithology3; SSD	Pmq	
D	11BLDD0015	474.78	477.64	P	lam	itb		STD		0			DK	GRY	GRY	fg	Interbedded lithologies ; Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : GY    ; Grainsize_Crystal2; cg  Lith2_Qualifier; mas	Pmq	
D	11BLDD0015	477.64	486.25	P	mas	lam		STD		0			MD	GRY	GRY	fg	 Silty dolomite; Stylolite compression bands throughout sequence. Blebby py at 481.7m.  ; Lith1RegolithOverprint : Silicified       	Pmq	
D	11BLDD0015	486.25	489.6	P	mas	lam		STD		0			LT	GRY	GRY	fg	Domal stromatolites.  Compressioni stylolites in silty dolomite. ; Lith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    	Pmq	
D	11BLDD0015	489.6	496.43	P	mas			SDO		0			MD	GRY	GRY	fg	Silty dolomite and dolomite.  Compression bands - stylolites. ; Lith1RegolithOverprint : Silicified Lith2pc : 40      ; Lith2_Qualifier; lam	Pmq	
D	11BLDD0015	496.43	502.45	P	mas	alg		SDM		0			DK	GRY	GRY	fg	Stromatolites - domal in structure.  Pyrite at 500.38m.; Lith1RegolithOverprint : Silicified       	Pmq	
D	11BLDD0015	502.45	511.1	P	lam	mas	<F	STD		0			MD	GRY	GRY	fg	Silty dolomite with small intervals of domal stromatolite.  ; Lith1RegolithOverprint : Silicified Lith2pc : 20 Lith2ColourTone : D Lith2Colour1 : GY Lith2Colour2 : WH   	Pmq	
D	11BLDD0015	511.1	517	P	lam	mas	fra	SMD		0			DK	RED	RED	fg	Diagenetically altered red mudstones.  Carbonacous fracturing. ; Lith2pc : 30   Lith2Colour2 : CR   	Pmq	
D	11BLDD0015	517	549.04	P	lam	mas	fra	STD		0			MD	RED	RED	fg	Fractured mudstone with carbonacous infill.  Vuggy sections.  Very minor beds of sandstone.  ; Lith2pc : 5 Lith2ColourTone : L Lith2Colour1 : CR Lith2Colour2 : RD   ; Grainsize_Crystal2; mg	Pmq	
D	11BLDD0015	549.04	567.3	P	mas			SDO		0			LT	CRM	CRM	fg	Interbedded lithologies with minor intervals of SDAR.  Fractured with carbonacous infill.  ; Lith1RegolithOverprint : Silicified Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : RD    ; Lithology3; SSD	Pmq	
D	11BLDD0015	567.3	570.03	P	mas	fra		SDO		0			LT	PNK	PNK	fg	SDAR poorly sorted; med. grained. rounded grains.  sequence fractured.  CH on fracture surfaces.; Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : OR    ; Lith2_Qualifier; lam  Lithology3; SSD	Pmq	
D	11BLDD0015	570.03	581.15	P	mas	fra		SST		0			MD	CRM	CRM	mg	Poorly sorted; rounded to sub rounded grains.  Fractures with qtz infill.  Brecciated with SSD matrix ; Lith1RegolithOverprint : Silicified Lith2pc : 20 Lith2ColourTone : L Lith2Colour1 : OR Lith2Colour2 : WH   ; Grainsize_Crystal2; cg	Pmi	
D	11BLDD0015	581.15	601.4	P	lam	fra	itb	SST		0			LT	RED	RED	mg	Recrystalised SSD interbedded with siltstone laminae.  Fractured with qtz infill.  ; Lith1RegolithOverprint : Silicified Lith2pc : 5 Lith2ColourTone : D Lith2Colour1 : GY    ; Grainsize_Crystal2; fg	Pmi	
D	11BLDD0015	601.4	631	P	mas	lam	fra	SST		0			MD	RED	RED	mg	sub-round  poorly sort grains.  FRA with silty infill.  Siltstone laminated.  Some coarse intervals.  Fractured with 1 cm off set at 642.3m  Minor acid reaction. ; Lith2pc : 15 Lith2ColourTone : D Lith2Colour1 : GY    ; Grainsize_Crystal2; fg	Pmi	
D	11BLDD0015	631	647.5	P	bnd			SST		0			MD	RED	RED	mg	Medium reddy sandstones with thin finer sandstone beds.  Thin laminae of green mudstone.; Lith2pc : 9.5 Lith2ColourTone : M Lith2Colour1 : RD    ; Grainsize_Crystal2; fg  Lith2_Qualifier; lam	Pmi	
D	11BLDD0015	647.5	651.9	P	bnd	lam		SST		1			DK	RED	RED	mg	Medium and fine grained dark reddy sandstone with green clay laminae and 2cm thick slightly weathered clay unit.  Thin PY on clay lamina; Lith2pc : 95 Lith2ColourTone : M Lith2Colour1 : RD    ; Grainsize_Crystal2; fg	Pmi	
D	12BLDD0016	0	2	P	pi			LCV		5	Alluvial		MO	RED	RED	mg		T	
D	12BLDD0016	2	38	P				LCV		5	Alluvial		MD	YEL	YEL	mg		K	
D	12BLDD0016	38	64	P				SST		3	Residual		MD	GRY	GRY	fg		Pmq	
D	12BLDD0016	64	80	P				SPH		3	Residual		MD	RED	RED	fg		Pmq	
D	12BLDD0016	80	86.6	P	pyr	grd		SPH		3	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	86.6	90.4	P	pyr	grd		SPH		3	Residual		MO	YEL	YEL	fg	Graded normallyLith2pc : 20      	Pmq	
D	12BLDD0016	90.4	94.78	P	pyr	alg		SPH		3	Residual		MO	YEL	YEL	fg	Minor stromatilitic portions. Could be soft sed deformation.stromatolitic; Lith2pc : 20      	Pmq	
D	12BLDD0016	94.78	99.55	P	pyr	grd		SPH		3	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	99.55	100.16	P	alg			SDM		3	Residual		MO	GRY	GRY	fg	Stromatolitic; Lith2pc : 30      ; Lith2_Qualifier; bed	Pmq	
D	12BLDD0016	100.16	103.6	P	pyr	grd		SPH		3	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	103.6	104.23	P	pyr	alg		SPH		3	Residual		MO	YEL	YEL	fg	Minor stromatilitic portions. Could be soft sed deformation.stromatolitic; Lith2pc : 20      	Pmq	
D	12BLDD0016	104.23	120.15	P	pyr	grd		SPH		3	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	120.15	122.15	P	pyr	bxd		SPH		4	Residual		MO	YEL	YEL	fg	Texturally very similar to the last interval. Some brecciation. Bedding crosses oxidation boundries suggesting the colour changes are due to weathering. Inverted weathering profile due to sulphides.Lith2pc : 40      	Pmq	
D	12BLDD0016	122.15	125.6	P	mas			SPH		3	Residual		MO	BRN	BRN	fg	Some scour channels filled with sulphide.Lith2pc : 10      ; Lith2_Qualifier; bed	Pmq	
D	12BLDD0016	125.6	127.48	P				SPH		3	Residual		LT	BLU	BLU	fg		Pmq	
D	12BLDD0016	127.48	129.4	P	bed			SPH		1	Residual		MO	BRN	BRN	fg	SSS is gossan-likeLith2pc : 10      	Pmq	
D	12BLDD0016	129.4	129.71	P	pyr	grd		SPH		1	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	129.71	133.44	P	bed			SPH		1	Residual		MO	BRN	BRN	fg	SSS is gossan-likeLith2pc : 10      	Pmq	
D	12BLDD0016	133.44	135.15	P	pyr	grd		SPH		1	Residual		MO	YEL	YEL	fg	Lith2pc : 20      	Pmq	
D	12BLDD0016	135.15	151.24	P	bed			SPH		1	Residual		MO	BRN	BRN	fg	SSS is gossan-like. Some brecciation; could be collapse breccia or sedimentary.Lith2pc : 10      	Pmq	
D	12BLDD0016	151.24	162.6	P	bxd			SST		1			MD	GRY	GRY	fg	Slightly bedded at times. Chaotic breccias. Dolomite has been silicified.RegolithProfille :  Fresh rock; Lith2pc : 40      	Pmei	
D	12BLDD0016	162.6	179.73	P				SBX		0			MO	BLU	BLU	mg	Sub-angular conglomerate.RegolithProfille :  Fresh rock; Lith2pc : 20      ; Lith2_Qualifier; mas	Pmei	
D	12BLDD0016	179.73	185.34	P	bxd			STD		0			LT	BLU	BLU	mg	Brecciated areas are polymictic; but predominantly dolomite.RegolithProfille :  Fresh rock; Lith2pc : 30      ; Grainsize_Crystal2; fg	Pmei	
D	12BLDD0016	185.34	189.38	P	bxd			SDO		0			LT	PNK	PNK	fg	Mostly massive; but some areas are brecciated then welded again.RegolithProfille :  Fresh rock	Pmei	
D	12BLDD0016	189.38	210.77	P	bxd			STD		0			LT	BLU	BLU	mg	RegolithProfille :  Fresh rock; Lith2pc : 20      ; Grainsize_Crystal2; fg  Lith2_Qualifier; bed	Pmei	
D	12BLDD0016	210.77	211.07	P				SSL		4	Residual		MD	BRN	BRN	mg		Pmei	
D	12BLDD0016	211.07	212.54	P				SBX		4	Residual		MD	BRN	BRN	mg		Pmei	
D	12BLDD0016	212.54	214.14	P				SSL		4	Residual		MD	BRN	BRN	mg		Pmei	
D	12BLDD0016	214.14	216.5	P				SBX		3	Residual		MO	RED	RED	mg		Pmei	
D	12BLDD0016	216.5	217.64	P				SBX		4	Residual		DK	GRY	GRY	mg	Sulphide rich matrix.	Pmei	
D	12BLDD0016	217.64	219.96	P				SBX		3	Residual		LT	PNK	PNK	mg		Pmei	
D	12BLDD0016	219.96	221.8	P				SBX		3	Residual		MD	BLU	BLU	fg		Pmei	
D	12BLDD0016	221.8	223.07	P				SDO		0			LT	PNK	PNK	fg	RegolithProfille :  Fresh rock	Pmei	
D	12BLDD0016	223.07	225.84	P				SBX		3	Residual		MD	BLU	BLU	fg		Pmei	
D	12BLDD0016	225.84	226.57	P				SBX		3	Residual		MD	BLU	BLU	fg	Lith2pc : 40      ; Lith2_Qualifier; bed	Pmei	
D	12BLDD0016	226.57	230	P				SBX		3	Residual		MD	BLU	BLU	fg		Pmei	
D	12BLDD0016	230	231.2	P				SSL		4	Residual		MD	BRN	BRN	cg		Pmei	
D	12BLDD0016	231.2	232.6	P				CLS										Pmei	
D	12BLDD0016	232.6	233.2	P				SDO		3	Residual		LT	GRY	GRY	fg	Large dolomitic clasts.	Pmei	
D	12BLDD0016	233.2	238.31	P				SBX		3	Residual		MD	YEL	YEL	cg		Pmei	
D	12BLDD0016	238.31	256.03	P	alg	bxd		SDM		0	Residual		MD	GRY	GRY	fg	Stromatolitic	Pmei	
D	12BLDD0016	256.03	273.89	P				SBX		3	Residual		MO	GRY	GRY	mg	Large dolomitic clasts in the SBXStromatolitic; Lith2pc : 20      ; Grainsize_Crystal2; fg  Lith2_Qualifier; alg	Pmei	
D	12BLDD0016	273.89	278.75	P	bnd			SDO		0			LT	GRY	GRY	fg	Banded dolomite with bands of sedimentary breccia with dolomite clasts.LithStructure :  Deformed; Lith2pc : 10 Lith2ColourTone : L Lith2Colour1 : GY    ; Lith2_Qualifier; ang	Pmei	
D	12BLDD0016	278.75	278.97	P	rnd	bed		SBX		0			LT	GRY	GRY	fg	Sedimentary breccia with rounded to sub-angular dolomite clasts. Matrix of fine silty dolomite	Pmei	
D	12BLDD0016	278.97	280.67	P	bnd	<F	shr	SDO		0			LT	GRY	GRY	fg	stylolites in dolomite. Wavey banding is microfaulted. Banding is at a steep angle to core axis.Lith2pc : 20 Lith2ColourTone : L Lith2Colour1 : BL Lith2Colour2 : GY   ; Lith2_Qualifier; mas	Pmei	
D	12BLDD0016	280.67	294.5	P	ang	bnd	<F	SBX		0			LT	GRY	GRY	fg	Silicified fracture. Dolomite breccia. Banding perpendicular to core axis.	Pmei	
D	12BLDD0016	294.5	295.42	P	rnd	bc		SBX		0			LT	BLU	BLU	fg	Clast supported dolomite breccia with fine matrix of silty sand	Pmei	
D	12BLDD0016	295.42	296.9	P	bnd	frl		SDO		0			LT	GRY	GRY	fg	Banded dolomite with stylolites.	Pmei	
D	12BLDD0016	296.9	313.5	P	bnd	alg	fra	SDM					MD	GRY	GRY	fg	Some recrystalising of the dolomite.Fragmented stromatolitic dolomite; interbedded with masive silty dolomite and minor fault breccia.Lith1RegolithOverprint : ADVISE DBA Lith2pc : 35 Lith2ColourTone : L Lith2Colour1 : CR Lith2Colour2 : GY   ; Lith2_Qualifier; mas  Lithology3; BRE	Pmei	
D	12BLDD0016	313.5	317.5	P	grv			BFL					MD	BRN	BRN		Fault breccia with clasts of stromatolitic dolomite and banded dolomite in a fine silty matrix	Pmei	
D	12BLDD0016	317.5	320.12	P	fra			SBX					MD	BLU	BLU	fg	Silty matrix supported breccia with rare dolomite clasts and silicified fractured dolomiteLith1RegolithOverprint : Silicified Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : BL   	Pmei	
D	12BLDD0016	320.12	320.8	P	grd			SBX		0			MD	BRN	BRN	fg	Fine silty matrix rich breccia with dolomite clasts fining up hole	Pmei	
D	12BLDD0016	320.8	324.33	P	bed	frl		SDO		0			LT	GRY	GRY	fg	Dolomite unit with recrystallised breccia and banded dolomiteLith2pc : 30 Lith2ColourTone : L Lith2Colour1 : GY    ; Lith2_Qualifier; bnd  Lithology3; SDO	Pmei	
D	12BLDD0016	324.33	325	P	mas	grd		SMD		0			MD	BRN	BRN	fg	Mudstone matrix with fine sandy bands. Angular clasts of dolomite up to 4cm.texture:matrix; Lith2pc : 5 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : WH   ; Lith2_Qualifier; ang	Pmei	
D	12BLDD0016	325	330.81	P	ang	frl	itb	SBX		0			MD	BRN	BRN	fg	Sedimentary breccia with mudstone matrix; banded dolomite and massive siltstone clasts. Interedded banded siltstoneLith2pc : 10 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : GN   ; Lith2_Qualifier; bnd	Pmei	
D	12BLDD0016	330.81	332.5	P	bnd	<F	frl	SDO		0			LT	GRY	GRY	fg	Breccia with silicified sandstone clasts in a dolomitic matrix interbedded with banded dolomite. Stylolites frequent. Possible boulder?texture:wavy bedding; LithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : PK   ; Lith2_Qualifier; rxt	Pmei	
D	12BLDD0016	332.5	333.9	P	ang	fra		SBX					MD	BRN	BRN	fg	Siltstone matrix with clasts of	Pmei	
D	12BLDD0016	333.9	334.7	P	frl			SBX		0			LT	GRY	GRY	fg	Silicified dolomite breccia. Possible boulder?	Pmei	
D	12BLDD0016	334.7	338.4	P	frl			SBX		0			LT	BRN	BRN	fg	Muddy matrix with massive dolomite clasts interbedded with masive dolomiteLith2pc : 50 Lith2ColourTone : L Lith2Colour1 : CR Lith2Colour2 : GY   ; Lith2_Qualifier; mas	Pmei	
D	12BLDD0016	338.4	339.25	P	mas	frl	itb	STD		0			LT	GRY	GRY	fg	Lith2pc : 30 Lith2ColourTone : L Lith2Colour1 : CR Lith2Colour2 : GY   	Pmei	
D	12BLDD0016	339.25	344.1	P				SDO					LT	GRY	GRY	fg	Fault breccia with competant weakly silicified dolomite and mudsone bands.	Pmei	
D	12BLDD0016	344.1	346.9	P	mas	fra		STD					LT	BLU	BLU	fg	Highly fractured. Silica nodules	Pmei	
D	12BLDD0016	346.9	351.85	P	itb			STD					LT	BLU	BLU	fg	Lith2pc : 30 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : BL   ; Lith2_Qualifier; slt  Lith2_Qualifie2; alg   Lithology3; SDM	Pmei	
D	12BLDD0016	351.85	353.3	P	mas	bed	<F	SSD					LT	GRY	GRY	fg		Pmei	
D	12BLDD0016	353.3	355.1	P				CVT										Pmei	
D	12BLDD0016	355.1	385.9	P	bnd	alg	shr	SDM		0			MD	GRY	GRY	fg	Massive. Minor pyrite associated with stromatolites. Stromatolites are matted  and broken into clasts. High energy environmentRegolithProfille :  Fresh rock; LithStructure :  Deformed; Lith2pc : 10 Lith2ColourTone : D Lith2Colour1 : BK    ; Lith2_Qualifier; mas	Pmea	
D	12BLDD0016	385.9	391.51	P	bnd	alg		SDM		0			DK	GRY	GRY	fg	Undeformed bands. Calmer environment. Stromatolites are domal.stromatolitic	Pmea	
D	12BLDD0016	391.51	394	P	bnd			STD		0			MD	GRY	GRY	fg	transitional lower boundary to a higher energy environmentLithStructure :  Deformed	Pmea	
D	12BLDD0016	394	416.5	P	bnd			STD		0			MD	GRY	GRY	fg	StylolitesLithStructure :  Deformed; Lith2pc : 15 Lith2ColourTone : L Lith2Colour1 : GY    ; Lithology3; SAD	Pmea	
D	12BLDD0016	416.5	425	P	bnd			STD		0			MD	GRY	GRY	fg	Stylolites. Slickensiden fractures on dolomitic mudstone. SDMD preferentially fracturesLith2pc : 20 Lith2ColourTone : D Lith2Colour1 : GY    	Pmea	
D	12BLDD0016	425	430.07	P	bnd	mas		STD		0			MD	GRY	GRY	fg	StylollitesLithStructure :  Deformed	Pmea	
D	12BLDD0016	430.07	435.25	P	slt	bnd	alg	SDM		0			MD	GRY	GRY	fg	LithStructure :  Deformed	Pmea	
D	12BLDD0016	435.25	436.5	P	ang	itb		SBX		0			MD	GRY	GRY	fg	Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Lith2_Qualifier; bnd	Pmea	
D	12BLDD0016	436.5	447.3	P	bnd	<F		STD		0			MD	GRY	GRY	fg		Pmea	
D	12BLDD0016	447.3	456.85	P	bnd			STD		0			MD	GRY	GRY	fg	Stylolites. mm scale banding	Pmea	
D	12BLDD0016	456.85	466.5	P	bnd			STD		0			MD	GRY	GRY	fg	Calm marine environment	Pmea	
D	12BLDD0016	466.5	468.8	P	bnd			STD		0			MD	GRY	GRY	fg	cm scale sandy beds; more energetic environment than higher in hole.Lith2pc : 10 Lith2ColourTone : D Lith2Colour1 : GY    ; Lithology3; SST	Pmea	
D	12BLDD0016	468.8	472.1	P	bnd	itb		STD		0			MD	GRY	GRY	fg	stylolites; rip up clastsLithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Lith2_Qualifier; srd	Pmea	
D	12BLDD0016	472.1	477.5	P	mas			STD		0			MD	GRY	GRY	fg	Stylolites and rip up clasts.Lith2pc : 20      ; Lith2_Qualifier; bnd	Pmea	
D	12BLDD0016	477.5	487.8	P	bnd	itb		STD		0			MD	GRY	GRY	fg	LithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; cg   Lithology3; SAD	Pmea	
D	12BLDD0016	487.8	489.4	P	bnd	itb		STD		0			MD	GRY	GRY	fg	Transition into red bedsLithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD    	Pmea	
D	12BLDD0016	489.4	492.4	P	itb			SBX		0			MD	RED	RED	cg	Red bedLithStructure :  Deformed; Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD    ; Grainsize_Crystal2; fg  Lith2_Qualifier; bnd  Lithology3; SSL	Pmea	
D	12BLDD0016	492.4	502.2	P	bed	itb		SSD		0			MD	GRY	GRY	fg	transitional zoneLith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    	Pmt	
D	12BLDD0016	502.2	507.8	P	bed	itb	<F	SSD		0			MD	RED	RED	fg	Fractured and deformed with stylolites.Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD    ; Lithology3; SST	Pmt	
D	12BLDD0016	507.8	509	P	bnd	itb		SSD		0			MD	GRY	GRY	fg	Red bedsLithStructure :  Deformed; Lith2pc : 35 Lith2ColourTone : M Lith2Colour1 : RD    ; Lithology3; SBX	Pmt	
D	12BLDD0016	509	512	P	mas	bed	itb	SSL		0			MD	RED	RED	fg	Red bedsLith2pc : 50 Lith2ColourTone : M Lith2Colour1 : RD    ; Lith2_Qualifier; grn	Pmt	
D	12BLDD0016	512	523	P	ang	itb		SBX		0			MD	RED	RED	cg	Red bedsLith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : GY   ; Grainsize_Crystal2; fg  Lith2_Qualifier; bnd  Lithology3; SSL	Pmt	
D	12BLDD0016	523	536.87	P	bed	<F	itb	STD		0			MD	RED	RED	fg	Red beds with mm scale banding interbedded with mm scale sandy beds; massive silts beds up to 20cm and cm-scale SBX bedsLith2pc : 10 Lith2ColourTone : M Lith2Colour1 : RD    ; Grainsize_Crystal2; cg   Lithology3; SSD	Pmt	
D	12BLDD0016	536.87	539.28	P	mas			STD		0			MD	RED	RED	fg		Pmt	
D	12BLDD0016	539.28	550	P	bed	itb		STD		0			MD	RED	RED	fg	Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : RD    ; Lith2_Qualifier; mas	Pmt	
D	12BLDD0016	550	558.68	P	bed	<F	itb	STD		0			MD	RED	RED	fg	Lith2pc : 5 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : GY   ; Lithology3; SBX	Pmt	
D	12BLDD0016	558.68	560.7	P	bnd	itb	<F	SSD		0			MD	GRY	GRY	mg	Grey interval- no iron stainingLith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; fg  Lith2_Qualifier; bed  Lithology3; SBX	Pmt	
D	12BLDD0016	560.7	569.3	P	bed	<F	itb	STD		0			MD	RED	RED	fg	Base of red beds; MG sandy beds up to 2cm.Lith2ColourTone : M Lith2Colour1 : RD    ; Grainsize_Crystal2; cg   Lithology3; SSD	Pmt	
D	12BLDD0016	569.3	571.07	P	bc	<F		SBX		0			MD	GRY	GRY	cg	Broken zone with slickensided fractures with chlorite directly beneath red beds- fault?Lith2pc : 40 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; fg  Lith2_Qualifier; bed	Pmt	
D	12BLDD0016	571.07	585.3	P	ang	pol		SBX		0			MD	GRY	GRY	cg	Poorly sorted with angular clasts of dolomite and silty dolomite mm-cm scale	Pmt	
D	12BLDD0016	585.3	586.3	P	bed	itb		STD		0			MD	GRY	GRY	fg	Lith2pc : 35 Lith2ColourTone : M Lith2Colour1 : GY    ; Lith2_Qualifier; mas	Pmt	
D	12BLDD0016	586.3	593.1	P	ang	bc		SBX		0			MD	GRY	GRY	mg		Pmt	
D	12BLDD0016	593.1	597.65	P	slt	bed	alg	SDM		0			MD	GRY	GRY	fg	Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; mg	Pmt	
D	12BLDD0016	597.65	600.77	P	bed	<F	itb	STD		0			MD	GRY	GRY	fg	Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; mg  Lith2_Qualifier; rnd	Pmt	
D	12BLDD0016	600.77	602.88	P	rnd	pol		SBX		0			MD	GRY	GRY	fg	Fine silty matrix with coarse clasts 2-10mm	Pmt	
D	12BLDD0016	602.88	608.8	P	slt	bed	alg	SDM		0			MD	GRY	GRY	fg	Lith_Qualifier5; itb	Pmt	
D	12BLDD0016	608.8	610.5	P	rxt			SBX		0			MD	GRY	GRY	fg		Pmt	
D	12BLDD0016	610.5	628.94	P	bed	<F	itb	STD		0			MD	GRY	GRY	fg	Lith2pc : 30 Lith2ColourTone : L Lith2Colour1 : GY    ; Lith2_Qualifier; mas  Lithology3; SBX	Pmt	
D	12BLDD0016	628.94	631.88	P	rnd			SBX		0			DK	GRY	GRY	fg	Fine silty matrix with clasts 1-5mm	Pmt	
D	12BLDD0016	631.88	636	P	bed	<F	itb	STD		0			LT	GRY	GRY	fg	Pebble breccia?Lith2pc : 30 Lith2ColourTone : L Lith2Colour1 : GY    ; Grainsize_Crystal2; cg  Lith2_Qualifier; rnd	Pmt	
D	12BLDD0016	636	657	P	bed	<F	itb	STD		0			MD	GRY	GRY	fg	Matted stromatolitesLith2pc : 30 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; cg  Lith2_Qualifier; ang  Lithology3; STD	Pmt	
D	12BLDD0016	657	663.09	P	slt	alg	<F	SDM		0			MD	GRY	GRY	fg	Massive dolomite beds 10cm. Casts from evaporitesLith2pc : 30 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : GY   ; Lith2_Qualifier; bed  Lithology3; SDO	Pmt	
D	12BLDD0016	663.09	668.28	P	bed	<F	itb	STD		0			MD	GRY	GRY	fg	Lith2pc : 40 Lith2ColourTone : L Lith2Colour1 : WH Lith2Colour2 : GY   ; Lith2_Qualifier; mas  Lithology3; SBX	Pmt	
D	12BLDD0016	668.28	676.2	P	bed	<F	itb	STD		0			MD	GRY	GRY	fg	Lith2pc : 50 Lith2ColourTone : L Lith2Colour1 : GY Lith2Colour2 : WH   	Pmt	
D	12BLDD0016	676.2	682.7	P	bed			STD		0			DK	GRY	GRY	fg	Thin medium grained sandy beds up to 3cmLith2pc : 20 Lith2ColourTone : M Lith2Colour1 : GN Lith2Colour2 : GY   ; Lithology3; SSD	Pmt	
D	12BLDD0016	682.7	691.2	P	bed	<F	itb	STD		0			MD	GRN	GRN	fg	fine mm scale banding of alternating dolomite and silty dolomite.Lith2pc : 50 Lith2ColourTone : L Lith2Colour1 : PK Lith2Colour2 : WH   ; Lith2_Qualifier; mas	Pmt	
D	12BLDD0016	691.2	692.38	P	frl			SSD		0			LT	WHT	WHT	mg	Dolomitic sandstone matrix with clasts up to 3cm of dolomiteLith2pc : 50 Lith2ColourTone : L Lith2Colour1 : GN Lith2Colour2 : GY   ; Grainsize_Crystal2; fg  Lith2_Qualifier; mas	Pmt	
D	12BLDD0016	692.38	697.85	P	mas	itb		SDO		0			MD	GRY	GRY	fg	Disturbed beddingLith2pc : 50 Lith2ColourTone : D Lith2Colour1 : GY    ; Lith2_Qualifier; bed	Pmt	
D	12BLDD0016	697.85	709	P	ool	bed	itb	SSD		0			LT	GRY	GRY	fg	Oolitic sandstone.LithStructure :  Vein (undifferentiated); Lith2pc : 45 Lith2ColourTone : L Lith2Colour1 : WH    ; Lith2_Qualifier; mas  Lithology3; STD	Pmt	
D	12BLDD0017	0	26.6	P				NL									Mud rotary collar. Sample caught up in snotty looking muds.	K	
D	12BLDD0017	26.6	38.13	P				SST		4	Residual		MO	CRM	CRM	mg			
D	12BLDD0017	38.13	44.32	P				SST		4	Residual		MD	YEL	YEL	cg			
D	12BLDD0017	44.32	48.67	P				SBX		4	Residual		MO	CRM	CRM	cg	Sub-angular to sub rounded clasts.Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : YE    		
D	12BLDD0017	48.67	56.89	P				SSL		4	Residual		MO	PNK	PNK	cg			
D	12BLDD0017	56.89	80.08	P	bed	bnd		SSL		4	Residual		LT	YEL	YEL	mg	Very mixed observations of bedding. Bleaching around veins and leisergang banding. Some fine bedding observed.		
D	12BLDD0017	80.08	83.85	P				SSL		4	Residual		MO	RED	RED	mg			
D	12BLDD0017	83.85	88.6	P				SSL		3	Residual		MO	YEL	YEL	fg			
D	12BLDD0017	88.6	90.89	P				SSL		3	Residual		LT	CRM	CRM	mg	Could be weathered black shale.		
D	12BLDD0017	90.89	94.82	P				SSH		1	Residual		DK	BLK	BLK	mg		Pmq	
D	12BLDD0017	94.82	98.67	P				SSH		3	Residual		MO	CRM	CRM	cg	Could be weathered black shale.	Pmq	
D	12BLDD0017	98.67	102.69	P				SSH		3	Residual		MD	YEL	YEL	mg		Pmq	
D	12BLDD0017	102.69	104.9	P	grn			SSH		3	Residual		LT	CRM	CRM	fg	Large (~1-2mm) quartz grains within seds.	Pmq	
D	12BLDD0017	104.9	106.59	P				BRE		3	Residual		MD	YEL	YEL	cg	Monomictic. Rounded to sub-angular. Doesnt really look like a sed breccia. Maybe just soft sed stuff.	Pmq	
D	12BLDD0017	106.59	125.85	P				SSH		3	Residual		MD	YEL	YEL	mg	texture:slump folds; Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : YE    ; Grainsize_Crystal2; fg	Pmq	
D	12BLDD0017	125.85	145.15	P				SSH		3	Residual		MD	YEL	YEL	mg	Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : BR   	Pmq	
D	12BLDD0017	145.15	157.46	P	bnd			SSH		3	Residual		DK	YEL	YEL	fg	Textures similar to the mineralised black shale. Could be a weathered example.	Pmq	
D	12BLDD0017	157.46	166.43	P	bnd			SSH		1	Residual		MO	YEL	YEL	mg	Textures similar to the mineralised black shale. Could be a weathered example.Lith2pc : 10 Lith2ColourTone : MT Lith2Colour1 : BL Lith2Colour2 : YE   ; Grainsize_Crystal2; cg  Lith2_Qualifier; bed	Pmq	
D	12BLDD0017	166.43	172.95	P	bnd	bed		SPH		0			MO	BLK	BLK	fg	RegolithProfille :  Fresh rock; Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : YE   ; Grainsize_Crystal2; cg	Pmq	
D	12BLDD0017	172.95	174.81	P	fau			SPH		1	Residual		MO	BLK	BLK	fg	Weathering down a fault.	Pmq	
D	12BLDD0017	174.81	218.07	P	bed			SPH		0			DK	BLK	BLK	fg	Tuff ratios are variable downhole.RegolithProfille :  Fresh rock; Lith2pc : 10  Lith2Colour1 : GY Lith2Colour2 : BK   ; Grainsize_Crystal2; cg	Pmq	
D	12BLDD0017	218.07	223.25	P	bnd			SPH		1	Residual		MO	GRY	GRY	fg		Pmq	
D	12BLDD0017	223.25	225.48	P				VTF		1	Residual		MO	GRY	GRY	mg	Lith2pc : 20 Lith2ColourTone : MT Lith2Colour1 : BK Lith2Colour2 : BR   ; Grainsize_Crystal2; fg	Pmq	
D	12BLDD0017	225.48	229.9	P	grd			VTF		0			LT	GRY	GRY	cg	RegolithProfille :  Fresh rock; Lith2pc : 40 Lith2ColourTone : D Lith2Colour1 : GY    ; Grainsize_Crystal2; fg  Lith2_Qualifier; bnd	Pmq	
D	12BLDD0017	229.9	242.8	P				SSH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 40 Lith2ColourTone : P Lith2Colour1 : GY    ; Grainsize_Crystal2; cg  Lith2_Qualifier; grd	Pmq	
D	12BLDD0017	242.8	243	P	crk	fau		SPH		0			DK	GRY	GRY	fg	Angular; poorly sorted; non-jigsaw fit breccia welded together by qtz. Probably a part of a previous fault zone.RegolithProfille :  Fresh rock	Pmq	
D	12BLDD0017	243	243.7	P	fau			FTZ		0			MD	GRY	GRY	cg	Fault gouge with large clasts.RegolithProfille :  Fresh rock	Pmq	
D	12BLDD0017	243.7	246.4	P	mas			VTF		0			LT	GRY	GRY	fg	Sulphidic shale >70% pyrite.RegolithProfille :  Fresh rock; Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : YE    ; Lith2_Qualifier; bed	Pmq	
D	12BLDD0017	246.4	249.42	P	bnd			SPH		1	Residual		DK	GRY	GRY	fg	Mineralised bsbLith2pc : 20 Lith2ColourTone : P Lith2Colour1 : GY    ; Grainsize_Crystal2; mg  Lith2_Qualifier; grd	Pmq	
D	12BLDD0017	249.42	253.76	P	bnd			SPH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 5 Lith2ColourTone : P Lith2Colour1 : GY    ; Grainsize_Crystal2; mg	Pmq	
D	12BLDD0017	253.76	263.06	P	bed			SPH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : YE Lith2Colour2 : GN   	Pmq	
D	12BLDD0017	263.06	266.53	P	bed			SPH		3	Residual		LT	BLU	BLU	fg	Similar to the previous interval; just weathered. Probably acid leach from the sulphides.Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : YE   	Pmq	
D	12BLDD0017	266.53	269.43	P				SSL		3	Residual		LT	BLU	BLU	fg		Pmq	
D	12BLDD0017	269.43	275.95	P	mas			STD		3	Residual		LT	GRY	GRY	cg		Pmq	
D	12BLDD0017	275.95	280.17	P	bnd			SPH		1	Residual		LT	GRY	GRY	fg	Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed	Pmq	
D	12BLDD0017	280.17	282.08	P	mas			STD		1	Residual		LT	GRY	GRY	cg		Pmq	
D	12BLDD0017	282.08	303.14	P	bnd			SPH		1	Residual		LT	GRY	GRY	fg	Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed	Pmq	
D	12BLDD0017	303.14	303.65	P	bed			SPH		0			MD	YEL	YEL	fg	RegolithProfille :  Fresh rock; Lith2pc : 10 Lith2ColourTone : D Lith2Colour1 : GY    ; Lith2_Qualifier; bnd	Pmq	
D	12BLDD0017	303.65	305.22	P	bnd			SPH		1	Residual		LT	GRY	GRY	fg	Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed  Lithology3; FTZ	Pmq	
D	12BLDD0017	305.22	313.24	P				SPH		1	Residual		LT	GRY	GRY	fg	Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed  Lithology3; FTZ	Pmq	
D	12BLDD0017	313.24	315.48	P				SPH		1	Residual		MD	GRY	GRY	fg	Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed  Lithology3; FTZ	Pmq	
D	12BLDD0017	315.48	320.95	P				SPH		1	Residual		LT	GRY	GRY	fg	Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : RD Lith2Colour2 : BR   ; Lith2_Qualifier; bed  Lithology3; FTZ	Pmq	
D	12BLDD0017	320.95	338.11	P	mas			STD		1	Residual		LT	GRY	GRY	fg		Pmei	
D	12BLDD0017	338.11	345.19	P				SBX		1	Residual		LT	GRY	GRY	mg	Clasts of SDSL.	Pmei	
D	12BLDD0017	345.19	388.75	P	tuf	bxd		STD		1	Residual		LT	GRY	GRY	fg	Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : GY Lith2Colour2 : BL   ; Grainsize_Crystal2; mg   Lithology3; FTZ	Pmei	
D	12BLDD0017	388.75	394.91	P	fau			STD		1	Residual		LT	GRY	GRY	fg		Pmei	
D	12BLDD0017	394.91	411.47	P				STD		0			LT	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : GY Lith2Colour2 : BL   ; Grainsize_Crystal2; cg   Lithology3; FTZ	Pmei	
D	12BLDD0017	411.47	414.73	P				SSL		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock	Pmei	
D	12BLDD0017	414.73	430.63	P	mas			STD		0			LT	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : GY Lith2Colour2 : BL   ; Grainsize_Crystal2; mg   Lithology3; FTZ	Pmei	
D	12BLDD0017	430.63	435.76	P				STD		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock	Pmei	
D	12BLDD0017	435.76	458.19	P				SBX		0			LT	GRY	GRY	cg	Some silicified areas.RegolithProfille :  Fresh rock; Lith2pc : 20 Lith2ColourTone : P Lith2Colour1 : GY Lith2Colour2 : BL   ; Grainsize_Crystal2; fg  Lith2_Qualifier; mas  Lithology3; FTZ	Pmei	
D	12BLDD0017	458.19	472.2	P	sil			FTZ		0			LT	GRY	GRY	fg	Strongly siliceous. Still looks karstic.RegolithProfille :  Fresh rock	Pmea	
D	12BLDD0017	472.2	490.3	P	sil			FTZ		0			LT	CRM	CRM	fg	Possibly stromatilitic. Has stylolites. totally silicified. There are some area of brecciation; but overall very competant and cohesive. EOHStromatolitic; RegolithProfille :  Fresh rock	Pmea	
D	12BLDD0018	0	29.8	P				NL									mud drilling no logging		
D	12BLDD0018	29.8	55.47	P	bed			SPH		4	Residual		MO	YEL	YEL	fg	Possibly weathered black shale. Some liesegang banding.Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : YE    ; Grainsize_Crystal2; mg		
D	12BLDD0018	55.47	56.09	P	bed			SPH		3	Residual		DK	GRY	GRY	fg	Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : YE Lith2Colour2 : BR   		
D	12BLDD0018	56.09	57.36	P	bed			SSL		4	Residual		MD	YEL	YEL	cg			
D	12BLDD0018	57.36	58.24	P				SSL		3	Residual		DK	BRN	BRN	mg	Lith2pc : 10 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : GN   ; Lith2_Qualifier; bed		
D	12BLDD0018	58.24	60.7	P	bed			VTF		1	Residual		MD	GRY	GRY	mg	Well bedded grey rock. Grain size variable between layers. Unidentifiable black flecks up to 5mm in most layers. This rock contains dolomite; but doesnt look like a dolostone. Tuff code based on appearance.		
D	12BLDD0018	60.7	62.47	P	bed			VTF		0			MD	GRY	GRY	mg	RegolithProfille :  Fresh rock; Lith2pc : 40 Lith2ColourTone : D Lith2Colour1 : GY    ; Grainsize_Crystal2; fg   Lithology3; SPH		
D	12BLDD0018	62.47	70.07	P				SDO		0			LT	GRY	GRY	fg	Stylolitic. Some pyrite; but obviously structural remobilised.RegolithProfille :  Fresh rock; Lith2pc : 30 Lith2ColourTone : D Lith2Colour1 : GY    		
D	12BLDD0018	70.07	75.46	P	bed			SSH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GY    ; Lithology3; SPH	Pmq	
D	12BLDD0018	75.46	75.81	P	bed			SSH		0			DK	BLK	BLK	fg	Unit consists of three black shale units; very similar in appearance and may be structurally repeated.  Black shales are heavily CB veined; stronger veining at base of each unit which is unconformable. Top has 3mm py overlain by SDOLRegolithProfille :  Fresh rock; LithStructure :  Vein (undifferentiated); LithStructure :  Folded; Lith2pc : 5 Lith2ColourTone : M Lith2Colour1 : GY    	Pmq	
D	12BLDD0018	75.81	80.25	P	bed			SSH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 15 Lith2ColourTone : M Lith2Colour1 : GY    	Pmq	
D	12BLDD0018	80.25	82.53	P	bed			STD		0			MD	GRY	GRY	fg	bands of disseminated sulphide (mainly py; no other minerals discernable;non-magnetic) up to 11cm thick interbedded with minor black shales.  Dominant unit is dolomitic siltstone. Some CB veins.RegolithProfille :  Fresh rock; LithStructure :  Vein (undifferentiated); Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : GN Lith2Colour2 : YE   ; Lithology3; SBH	Pmq	
D	12BLDD0018	82.53	92.65	P	bed			SSH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 45 Lith2ColourTone : P Lith2Colour1 : CR Lith2Colour2 : GY   	Pmq	
D	12BLDD0018	92.65	104.2	P	bed			SSH		0			DK	GRY	GRY	fg	Lith2pc : 29 Lith2ColourTone : P Lith2Colour1 : CR    	Pmq	
D	12BLDD0018	104.2	107.62	P	bed	bl	fra	SSH		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock; LithStructure :  Folded; Lith1RegolithOverprint : Silicified       	Pmq	
D	12BLDD0018	107.62	107.78	P	fau			STD		0			DK	GRY	GRY	fg	fault gougeRegolithProfille :  Fresh rock		
D	12BLDD0018	107.78	110.35	P	bed	fra		STD		0			MD	GRY	GRY	fg	Stockwork carbonate veining; bedding in sediments is laminar but now broken into blocks; some blocksa re jigsaw fit with CB veins.RegolithProfille :  Fresh rock; LithStructure :  Vein (undifferentiated); Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : CR    		
D	12BLDD0018	110.35	212.96	P	bed			STD					MD	GRY	GRY	fg	Bedded silty doolimitic sediments; major stylolites disrupting bedding.RegolithProfille :  Fresh rock; LithStructure :  Vein (undifferentiated); Lith2pc : 30 Lith2ColourTone : P Lith2Colour1 : CR    		
D	12BLDD0018	212.96	223.2	P	bed			SSH		0			DK	BLK	BLK	fg	Bands of disseminated PY to 3cm thick; minor CP in some transported PY blebs to 1cm long by 0.5cm thick. Minto CB veining; plus some PY veining.  217.42 to 218.9m Galena blebs in thin bandsRegolithProfille :  Fresh rock; LithStructure :  Vein (undifferentiated); Lith2pc : 5 Lith2ColourTone : D Lith2Colour1 : GY    	Pmq	
D	12BLDD0018	223.2	226.75	P	ang			SBX		0			MD	GRY	GRY	cg	Sedimentary breccia consisting of angular dolomite clasts to 15cm plus sulphide clasts to 3cm in dark grey dolomitic silstone matrix.Lith1RegolithOverprint : Silicified       	Pmp	
D	12BLDD0018	226.75	244.1	P	fra			SDO		0			LT	GRY	GRY	fg	Pressure dissolution brecciaRegolithProfille :  Fresh rock; Lith1RegolithOverprint : Silicified       		
D	12BLDD0018	244.1	244.25	P				SBX		0			LT	GRY	GRY	cg	15cm angular breccia includes dolomite; black slale and py clastslithology:dissolution breccia; Lith1RegolithOverprint : Silicified       		
D	12BLDD0018	244.25	255.6	P	mas			SDO		0			LT	GRY	GRY	fg	Massive dolomite; a few pressure dissolution stylolites.RegolithProfille :  Fresh rock; Lith1RegolithOverprint : Silicified       		
D	12BLDD0018	255.6	292.5	P	bed			SDM		0			LT	CRM	CRM	fg	Massive stromatilitic dolomite; mediumgrey to cream colour.  Includes numerous domed and columnar stromatolites.  Some pressure dissolution fractures with recrystallised infill and pyrite.RegolithProfille :  Fresh rock; Lith1RegolithOverprint : Silicified Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : GY Lith2Colour2 : CR   ; Lith2_Qualifier; lam		
D	12BLDD0018	292.5	309.65	P	bnd			SDO		0			LT	CRM	CRM	fg	Moderately solicified dolomite; with moderately intense pressure fracturing.Lith1RegolithOverprint : Silicified       		
D	12BLDD0018	309.65	325.76	P	fra			SDO		0			MD	CRM	CRM	fg	Moderately silicified dolomite with recrystallised pressure dissolution veins to 6cm wide.  Pyramidal calcite crystals in vugs with some pyrite laths.LithStructure :  Deformed; Lith1RegolithOverprint : Silicified Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GY    ; Lith2_Qualifier; bxw		
D	12BLDD0018	325.76	326.5	P	bnd			SDM		1			MD	GRY	GRY	fg	Stromatilitic dolomite which appears moderately intensely fractured and annealed. Minor py associated with stromatolite.  Slight weathering around fractures and increased permeability suggests proximity to fault?RegolithProfille :  Fresh rock; Lith1RegolithOverprint : Silicified       		
D	12BLDD0021	0	53.8	P				NL											
D	12BLDD0021	53.8	58.24	P	bed			SPH		4	Residual		MO	YEL	YEL	fg			
D	12BLDD0021	58.24	65.74	P	bed			SPH		3	Residual		MO	GRY	GRY	fg			
D	12BLDD0021	65.74	68.22	P	bed			STD		4	Residual		MO	YEL	YEL	fg			
D	12BLDD0021	68.22	84.06	P	bed			STD		1			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	84.06	87.68	P				STD		3	Residual		LT	YEL	YEL	fg	Lith1RegolithOverprint : Silicified       		
D	12BLDD0021	87.68	91.86	P				SSH		1	Residual		MO	BLK	BLK	fg			
D	12BLDD0021	91.86	94.25	P	bed			STD		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	94.25	94.94	P	bed			SPH		0			DK	GRY	GRY	fg	Still very dolomitic; just more carbonaceous than units either side.RegolithProfille :  Fresh rock		
D	12BLDD0021	94.94	122.4	P	bed			SPH		0			MD	GRY	GRY	fg	Variable carbonaceous composition and sulphide %. Py never exceeds 2% over a metre.RegolithProfille :  Fresh rock		
D	12BLDD0021	122.4	129.92	P	bed			SPH		0			MD	GRY	GRY	fg	Two small units of sand which have convoluted bedding if bedded at all.RegolithProfille :  Fresh rock; Lith2pc : 20 Lith2ColourTone : M Lith2Colour1 : YE Lith2Colour2 : GY   ; Lithology3; SSD		
D	12BLDD0021	129.92	131.45	P	bed			STD		0			MD	GRY	GRY	fg	Bands of massive pyrite are increasing downhole.RegolithProfille :  Fresh rock		
D	12BLDD0021	131.45	139	P	bed			SPH		0			DK	GRY	GRY	fg	pyritic bands up to 0.5cmRegolithProfille :  Fresh rock		
D	12BLDD0021	139	139.73	P	bed			SDO		0			LT	WHT	WHT	fg	texture:wavy bedding; Lith2pc : 40 Lith2ColourTone : D Lith2Colour1 : GY    ; Lith2_Qualifier; bnd		
D	12BLDD0021	139.73	151	P	bed			STD		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	151	153	P	mas			STD		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith1RegolithOverprint : Silicified       		
D	12BLDD0021	153	160.05	P	bed			STD		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	160.05	160.6	P	bed	itb		SDO		0			MD	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 50 Lith2ColourTone : D Lith2Colour1 : BK Lith2Colour2 : BL   ; Lith2_Qualifier; tuf  Lith2_Qualifie2; bed		
D	12BLDD0021	160.6	188.1	P	bed	itb		STD		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock; Lith2pc : 5 Lith2ColourTone : L Lith2Colour1 : WH Lith2Colour2 : GY   ; Lith2_Qualifier; bnd		
D	12BLDD0021	188.1	218	P	bed			STD		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	218	218.51	P	bnd	tuf		SDO		0			LT	WHT	WHT	fg	Pyrite band occurs at the basal contact of the dolomite with the shale.RegolithProfille :  Fresh rock		
D	12BLDD0021	218.51	243.65	P	mas	bed		SDH		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	243.65	251.67	P	mas			SDH		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	251.67	284.42	P	bed	mas		SDH		0			DK	BLK	BLK	fg	mm scale parallel laminations.RegolithProfille :  Fresh rock		
D	12BLDD0021	284.42	284.78	P	bnd			SDO		0			LT	WHT	WHT	fg	RegolithProfille :  Fresh rock; Lith2pc : 30 Lith2ColourTone : M Lith2Colour1 : BL Lith2Colour2 : GY   		
D	12BLDD0021	284.78	290.18	P	bed	mas		SDH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	290.18	294.56	P	itb	bed		STD		0			MD	GRY	GRY	fg	texture:wavy bedding; RegolithProfille :  Fresh rock; Lith2pc : 50 Lith2ColourTone : D Lith2Colour1 : GY    ; Lith2_Qualifier; mas		
D	12BLDD0021	294.56	346.22	P	mas	bed		SDH		0			DK	BLK	BLK	fg	RegolithProfille :  Fresh rock		
D	12BLDD0021	346.22	348.77	P	bed	itb		SDH		0			DK	GRY	GRY	fg	RegolithProfille :  Fresh rock; Lith2pc : 50 Lith2ColourTone : M Lith2Colour1 : GY    ; Grainsize_Crystal2; mg		
D	12BLDD0021	348.77	349.24	P	ang			SBX		0			MD	GRY	GRY	cg	Jigsaw breccia. pyritic veins and blebs in matrix of brecciaRegolithProfille :  Fresh rock		
D	12BLDD0021	349.24	376.9	P	mas			SDH		0			DK	BLK	BLK	fg	pyritic bands from 349.2-373mRegolithProfille :  Fresh rock		
D	12BLDD0021	376.9	383.04	P	ang	pol		SBX		0			MD	GRY	GRY	cg	Sharp upper contact marked by pyrite band and carbonate veining.RegolithProfille :  Fresh rock		
D	12BLDD0021	383.04	387.8	P	mas			SDO		0			LT	GRY	GRY	fg	EOH. stylolites and disseminated pyrite (<0.01%)RegolithProfille :  Fresh rock		
D	McA20	0	16	P				CLS											
D	McA20	16	30	P				SSL										Kl	
D	McA20	30	82	P				SSL						RED	RED			Pmx	
D	McA20	82	93	P	bed			SSL					LT	GRN	GRN		Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GN Lith2Colour2 : WH   	Pmx	
D	McA20	93	125	P	bxd			SSL					LT	GRN	GRN		Interval mostly Breccia; Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GN Lith2Colour2 : WH   	Pmx	
D	McA20	125	143	P	bed			SSL					LT	GRN	GRN		Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GN Lith2Colour2 : WH   	Pmx	
D	McA20	143	183	P	bxd			SSL					LT	GRN	GRN		Interval mostly Breccia; Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GN Lith2Colour2 : WH   	Pmx	
D	McA20	183	222	P	bed			SSL					LT	GRN	GRN		Lith2pc : 10 Lith2ColourTone : P Lith2Colour1 : GN Lith2Colour2 : WH   	Pmx	
D	McA20	222	282	P	nod	cht		SSL					LT	GRN	GRN		Lith2ColourTone : M Lith2Colour1 : BR    ; Lith2_Qualifier; bed	Pmx	
D	McA20	282	297	P				STD					MD	BRN	BRN			Pmq	
D	McA20	297	318.5	P				SPH					DK	BLK	BLK		Lith2pc : 5 Lith2ColourTone : D Lith2Colour1 : BR    ; Lithology3; SSD	Pmq	
D	McA20	318.5	403.3	P				SPH					DK	BLK	BLK		PYRITE: generally <5% but up to 15%; Bulk forms discrete beds of lam Py  up to 0.85m thick ( upto 60% PY)  but generally about  0.10m thick. PY not as abundant as in MCA17; MCA19. Py beds become less numerous d/hole towards last at 403.5m; Lith2pc : 5 Lith2ColourTone : D Lith2Colour1 : BR    ; Lithology3; SSD	Pmq	
D	McA20	403.3	430	P				STD					DK	BLK	BLK		Lith2pc : 5 Lith2ColourTone : D Lith2Colour1 : BR    ; Lithology3; SSD	Pmq	
D	NBDD005	0	1.2	P	grv	cly		LAL		5		3	MO	BRN	WHT		polymict rounded gravel with white clay matrix and some sandy layers; some clasts are manganese rich;	Q	MDS
D	NBDD005	1.2	7.9	P				SSL		3		3		CRM	TAN		leached interbedded siltstone and clay/shale; pervasive dendritic manganese on fractures and bedding surfaces; minor orange (iron?) staining;	Pmnc	MDS
D	NBDD005	7.9	13.2	P				SSL		3		3		TAN	GRY		leached interbedded siltstone and clay/shale; minor intervals of grey unweathered interbedded siltstone - preserved due to silicification? Some bedding preserved in leached clay rich areas; occasional dendritic manganese; manganese and iron staining (red/orange) fractures and bedding surfaces; voids from 11-12m - after carbonate?	Pmnc	MDS
D	NBDD005	13.2	20.5	P				SSL		3		3		TAN	CRM		leached interbedded siltstone and clay/shale; minor preserved bedded; pervasive dendritic manganese on fractures and bedding surfaces; minor orange (iron?) staining;	Pmnc	DDC
D	NBDD005	20.5	35.2	P				SSL		3		3		TAN	GRY		leached interbedded siltstone and clay/shale; minor intervals of grey unweathered interbedded siltstone - preserved due to silicification? Some bedding preserved in leached clay rich areas; common dendritic manganese; manganese and iron staining (red/orange) fractures and bedding surfaces;	Pmnc	DDC
D	NBDD005	35.2	49.9	P				SSL		3		3		TAN	GRY		leached interbedded siltstone sandstone and clay/shale;  intervals of grey unweathered interbedded siltstone - preserved due to silicification? Some areas of tan/brown are very light (porous?) - highly weathered or de-dolomitised? Occasional dendritic manganese; manganese and iron staining (red/orange) fractures and bedding surfaces; occasional silicified nodules or clasts in siltstone	Pmnc	DDC
D	NBDD005	49.9	51.7	P	lam	<F		SIH		2		4	DK	GRY	TAN		interbedded grey siltstone and black shale; micro-folding and faulting - soft sediment deformation? small (10mm) cross-cutting dykes of sediment with shale deforming around more brittle siltstone; bedding truncated - cross bedding or deformation? partially weathered from top of interval but decreasing downhole - mostly on joints and bedding;	Pmnc	DDC
D	NBDD005	51.7	66	P				SSL		3		3		TAN	GRY		leached interbedded siltstone sandstone and clay/shale;  intervals of grey unweathered interbedded siltstone - preserved due to silicification? Some areas of tan/brown are very light (porous?) - highly weathered or de-dolomitised? Occasional dendritic manganese; manganese and iron staining (red/orange) fractures and bedding surfaces; coarse highly silicified crystalline interval at 54.6 to 54.8 and 60.7 to 60.8; bedding increasely preserved downhole; voids after carbonate(?) in clay rich interval at 63m;	Pmnc	DDC
D	NBDD005	66	71.5	P	lam	<F		SIH		2		4	MD	GRY	TAN		interbedded dominately grey siltstone and black shale;  partially weathered - mostly on joints and bedding; black very silicified interval to 66.4 - forms erosional brecciated contact with lower siltstone; occasional micro faulting and folding in more shaley units; small beds (<5m) of coarse rounded quartz sand in siltstone matrix associated with fine pyrite and alteration that destroys bedding/texture; irregular -angular nodules of carbonate in shaley units at 67.6-67.8 and 70.5-71.5;	Pmnc	DDC
D	NBDD005	71.5	77.9	P				SIH		3		3		TAN	GRY		interbedded dominately grey siltstone and black shale;  mostly weathered to tan colour; manganese specs dendrites and fracture coating common; sandy intervals with occasional coarse rounded quartz grains; irregular -angular nodules of carbonate in shaley units at 74.9-75.1; faulting and carbonate veins at 73.6-74.8; core reduced to soft sand/mush at 76.3-77.5;	Pmnc	DDC
D	NBDD005	77.9	81.7	P	lam			SIH		2		4	MD	GRY	TAN		interbedded dominately grey siltstone and black shale;  partially weathered - mostly on joints and bedding; minor micro faulting and folding at 80m; irregular -angular nodules of carbonate at 78-79m;	Pmnc	DDC
D	NBDD005	81.7	85.1	P	lam			SIH		3		3		TAN	GRY		interbedded dominately grey siltstone and black shale;  mostly weathered to tan colour; manganese specs dendrites and fracture coating common; sandy intervals with occasional coarse rounded quartz grains; Some areas of tan/brown are very light (porous?) - highly weathered or de-dolomitised? Clay in faults/fractures in more compotent grey siltstone;	Pmnc	DDC
D	NBDD005	85.1	86.8	P	lam			SIH		1		4	DK	GRY			interbedded dominately black shale and grey siltstone; forms sharp lower contact between shale and following interval - with increasing siltstone uphole; micro-folding and faulting - soft sediment deformation? bedding truncated - cross bedding or deformation? Occasional carbonate nodules with minor pyrite and disseminated pyrite in shale; minor carbonate veins	Pmnc	DDC
D	NBDD005	86.8	94.8	P	lam			SIH		1		4	MD	GRY	TAN		interbedded grey siltstone black shale and minor sandstone; weathered in parts and on fractures; Occasional angular irregular carbonate nodules - eg at 91-92m; carbonate beds (after sulphate?); minor carbonate veins; some siltstone intervals appear altered as lack texture; occasional minor pyrite blebs; micro-faulting and folding in shaley intervals;	Pmnc	DDC
D	NBDD005	94.8	95.8	P				SSL		0		4	MD	GRY	GRN		minor medium-grained quartz-arenite	Pmnc	LPC
D	NBDD005	95.8	97.2	P	lam			SSH		0		4	DK	GRY	GRN		finely interlaminated; silty beds are more brittle and broken; slumping thrusting and possible dewatering structures break-up thelaminations	Pmnc	LPC
D	NBDD005	97.2	99	P				SSL		2		3	MD	GRY	GRN		orange oxidising alteration from 98-99	Pmnc	LPC
D	NBDD005	99	100.9	P	pyr			SSH		0		4	DK	BLK	GRN		very finely pyritic; including a band at 99.7with finely disseminated Py stratabound over 3cm thickness; secondary Py also	Pmnc	LPC
D	NBDD005	100.9	102	P				SSL		0		4	MD	GRY	GRN		similar to 99.2m: grey siltstonewith orange oxidation interval 101.2-102	Pmnc	LPC
D	NBDD005	102	102.9	P				SSL		0		4	DK	GRY	GRN		finely interlaminated; trace Py including ine grained cubic grains at 102.2m	Pmnc	LPC
D	NBDD005	102.9	104.2	P				SSL		2		4	MD	GRY	GRN		faulted and oxidised to orange at fault	Pmnc	LPC
D	NBDD005	104.2	104.5	P	itb			SSL		0		4	DK	GRY	GRN		interlaminated with 1mm Py cubes in silty layers	Pmnc	LPC
D	NBDD005	104.5	110	P	itb			SSL		0		4	DK	GRY	GRN		sandstone intervals are medium-grained and quartz-rich;  up to c. 1mm with a brown cement; contains interstitial Py; Py also present in siltstone as bleb up to 1 cm in one instance and in veins; 1mm cubes of carbonate interpreted to be after halite at 108m	Pmnc	LPC
D	NBDD005	110	114.1	P	lam			SSL		0		4	MD	GRY			interbedded grey siltstone black shale; some siltstone intervals appear altered as lack texture; strong green+soft (chlorite?) alteration from 109-111m and 112-114m - visibly affecting only siltstone and not shale; occasional minor pyrite blebs/cubes; micro-faulting and folding in shaley intervals; rare carbonate veins	Pmnc	DDC
D	NBDD005	114.1	115	P				SSL		0		4	MD	GRY	GRN		Py in sst and in carb-infilled fractures	Pmnc	LPC
D	NBDD005	115	116.9	P				BFL		0		4	MD	GRY			breccia of interbedded silstone/shale; stratiform sedimentary breccia till 115.7 with sandy interbeds; then becomes jigsaw fit angular clasts of siltstone with carbonate and shale matrix/infill to 117.3; shale visibly intrudes siltstone breccia at 116.2; siltsone altered as lacks texture; micro-faulting/folding in shaley interval; fault gouge at 116.9; blebly pyrite mainly at 115.7 and vein-controlled	Pmnc	DDC
D	NBDD005	116.9	118.9	P				BHC		0		4	MD	GRY			hydrothermal breccia of grey siltstone; carbonate veining with jigsaw fit clasts; intensely veined towards 118.9 with large crystals (open space fill?); minor blebs of chalcopyrite at 117.5-118m; siltstone altered as lacks texture;	Pmnc	DDC
D	NBDD005	118.9	122.3	P				SSL		0		4	MD	GRY	GRN		dominately grey siltstone black shale with minor sandstone and 10 cm pyrtic shale at 119m and trace Py along interval; weak altered as mostly lacks texture - probably chlorite as green and soft; micro-faulting	Pmnc	DDC
D	NBDD005	122.3	123.7	P				SSL		0		4	MD	GRY	GRN		shale interbed containing slumped folds	Pmnc	LPC
D	NBDD005	123.7	128	P				SSL		0		4	MD	GRY	GRN		sandstone layers as everywhere in this core are irregular shaped not well stratabound with parallel tops and bottoms; contains subrounded qtz up to 1mm lithics and 2ndary Py and a fine cement that may also be altered	Pmnc	LPC
D	NBDD005	128	128.7	P				SSL		0		4	MD	GRY	GRN		micro-thrusts and slumping in shale	Pmnc	LPC
D	NBDD005	128.7	135	P				SSL		0		4	MD	GRY	GRN		as interval 123.7-128; vein Py; 10cm shale at 132m with Py	Pmnc	LPC
D	NBDD005	135	135.3	P				SSL		0		4	MD	GRY	GRN		Py in shale is disseminaedand in layer-sub-parallel fractures	Pmnc	LPC
D	NBDD005	135.3	140.7	P				SSL		0		4	MD	GRY	GRN		as other SSL-SST intervals	Pmnc	LPC
D	NBDD005	140.7	141.6	P				SSH		0		4	DK	GRY	GRN		very fine disseminated and blebby Py in shale; shale has disrupted bedding likely soft-sed def	Pmnc	LPC
D	NBDD005	141.6	144.4	P	grd			SSL		0		4	MD	GRY	GRN		minor sst beds are reverse-graded in at least one instance	Pmnc	LPC
D	NBDD005	144.4	146	P				SSL		0		4	MD	GRY	GRN			Pmnc	LPC
D	NBDD005	146	148.2	P	lam			SSL		0		4	MD	GRY	GRN		Py is largely fracture-controlled; partly finely lamineated and in some parts obscured possibly by alteration	Pmnc	LPC
D	NBDD005	148.2	150.2	P	lam			SSH		0		3	DK	GRY	GRN		Shaley fault-gauge at 140.7	Pmnc	LPC
D	NBDD005	150.2	153.5	P	lam	grd		SSL		0		4	MD	GRY	GRN		reverse-graded sandy layers	Pmnc	LPC
D	NBDD005	153.5	155.8	P	lam	cal		SSL		0		4	MD	GRY	GRN		microfractures are infilled with very thin black material; this may be shale squeezed into the fractures; HCl rxn; at 154.7 there is 10 cm interval containing circular to star-shaped dolomite vugs see photo 106-0105 and 0106	Pmnc	LPC
D	NBDD005	155.8	161.3	P				SSL		0		4	MD	GRN	GRN		trace Py and occasional shaley laminae	Pmnc	LPC
D	NBDD005	161.3	161.8	P	lam			SSH		0		3	DK	GRY	GRN		disseminated layer- and fracture-controled Py; minor slumping features	Pmnc	LPC
D	NBDD005	161.8	163.4	P				SSL		0		4	MD	GRY	GRN			Pmnc	LPC
D	NBDD005	163.4	166	P	itb			SSL		0		4	MD	GRY	GRN		minor calcareous sst	Pmnc	LPC
D	NBDD005	166	169	P	itb			SSL		0		4	MD	GRY	GRN			Pmnc	LPC
D	NBDD005	169	171	P	itb			SSL		0		4	MD	GRY	GRN		shale is altered or overprinted in a parculiar way that continues to occur from this depth onward (see photos 106-0109 to 0111); looks like an almost dendritic crystal growth but hand-lens scale reveals it may in fact be a destructive alteration (K?) reducing the shale to patchy black discontinuous spots	Pmnc	LPC
D	NBDD005	171	174	P				SSL		0		4	MD	GRY	GRN		minor fracture Py	Pmnc	LPC
D	NBDD005	174	175.5	P	itb	nod		SSH		0		4	MD	GRN	GRN		2-3 nodules in shale at 175.2 m; disseminated and fracture controlled pyrite as well as Py associated to nodule boundaries	Pmnc	LPC
D	NBDD005	175.5	176.8	P	itb			SSL		0		4	MD	GRY	GRN		minor qtz arenite layer	Pmnc	LPC
D	NBDD005	176.8	178	P	itb			SSH		0		3	DK	GRY	GRN		diss and fractue micro-pyrite	Pmnc	LPC
D	NBDD005	178	186.4	P				SSL		0		4	DK	GRN	GRN		very minor shale	Pmnc	LPC
D	NBDD005	186.4	187.2	P	itb			SSH		0		3	DK	GRY	GRN			Pmnc	LPC
D	NBDD005	187.2	192.8	P	itb			SSL		0		4	DK	GRN	GRN			Pmnc	LPC
D	NBDD005	192.8	195	P				SSL		0		4	DK	GRN	GRN		chloritic siltstone	Pmnc	LPC
D	NBDD005	195	195.8	P	itb			SSH		0		4	DK	GRY	GRN		fracture-Py	Pmnc	LPC
D	NBDD005	195.8	201.3	P				SSL		0		4	DK	GRN	GRN		chlorite silstone;minor dolomite crystals up to 5 mm angular; perhaps infilling or replacing see photo 106-0115	Pmnc	LPC
D	NBDD005	201.3	209.2	P	itb			SSL		0		4	DK	GRN	GRN		some intact shale as well as the altered and overprinted shale as seen at 169m	Pmnc	LPC
D	NBDD005	209.2	210.5	P	itb			SSH		0		4	DK	GRY	GRN		not particularly pyritic	Pmnc	LPC
D	NBDD005	210.5	211.8	P	itb			SSL		0		4	DK	GRN	GRN		minor sed breccia in ssl; sandy minor sandy layers; Shpalerite occurs in little vugs with dolomite very similar to dolomite occurance at 195.8m and photographed there as 106-0115; photo of Sp-Dol occurrence here seen in photos 106-0116 to 118	Pmnc	LPC
D	NBDD005	211.8	216.9	P	itb			SSL		0		4	DK	GRN	GRN			Pmnc	LPC
D	NBDD005	216.9	217.7	P	itb			SSL		0		4	DK	GRN	GRN		shale is microfaulted with bookshelf type displacement	Pmnc	LPC
D	NBDD005	217.7	220.7	P	itb	cal		SSL		0		4	DK	GRN	GRN		altered discontinuous shale layers; weak HCL rxn on siltstone	Pmnc	LPC
D	NBDD005	220.7	225	P	itb			SSH		0		4	DK	GRY	GRN		still very hard despite being mostly shale; perhaps dolomitised; once again Sp occurs in dolomite vugs; perhaps replacing an evaporitic phase. Photo 106-0119	Pmnc	LPC
D	NBDD005	225	230.7	P				SSL		0		4	MD	GRY	GRN		single 4 cm layer of quartz sand; lots of 1mm dolomite vugs perhaps after evaporites	Pmnc	LPC
D	NBDD005	230.7	233.2	P				SSL		0		4	DK	GRN	GRN			Pmnc	LPC
D	NBDD005	233.2	235.9	P	itb			SSH		0		4	DK	GRY	GRN		not really pyritic; dolomite infills irregular veins which are perhaps deformed dewatering channels see photos 106-0122- 123	Pmnc	LPC
D	NBDD005	235.9	243	P	itb			SSL		0		4	DK	GRN	GRN		chlorite altered; in some cases possibly destructive of layering texture	Pmnc	LPC
D	NBDD005	243	248.3	P	itb			SSH		0		4	DK	BLK	GRN		pockets of irregular siltstone within the shale see photos 106-0124 to 0126 maybe from compaction.	Pmnc	LPC
D	NBDD005	248.3	250.8	P	lam			SSL		0		4	DK	GRN			mm scale dolomite vug infill. Occasionally elongated across bedding.	Pmnc	LPC
D	NBDD005	250.8	254.3	P	itb			SSL		0		4	DK	GRN			Irregular dolomite vugs. Minor layer parallel fine pyrite	Pmnc	LPC
D	NBDD005	254.3	255.9	P	itb			SSL		0		4	DK	GRN				Pmnc	LPC
D	NBDD005	255.9	256.9	P	itb	lam		SSH		0		4	DK	GRN			Occasional 5mm sand layers	Pmnc	LPC
D	NBDD005	256.9	265	P	itb	lam		SSL		0		4	DK	GRN			Possible tuff (green) up to 5cm layers x3 layers. Sandstone up to 15cm thick.	Pmnc	LPC
D	NBDD005	265	266.1	P	lam			SSH		0		4	DK	BLK				Pmnc	LPC
D	NBDD005	266.1	268.4	P				SSL		0		4	DK	GRN				Pmnc	LPC
D	NBDD005	268.4	276	P	lam			SSH		0		4	DK	BLK			Disrupted and wavy laminations; occasional pyrite sub-parallel to layering. Minor siltstone; sandstone and dolomite vug infill up to 1cm.	Pmnc	LPC
D	NBDD005	276	277.3	P	lam			SSL		0		4	DK	GRN			Minor sandstone and sedimentary breccias (2cm thick).	Pmnc	LPC
D	NBDD005	277.3	280	P	itb			SIH		0		4	DK	BLK			Inter-laminated (mm scale) between shale and siltstone. Minor pyrite.	Pmnc	LPC
D	NBDD005	280	283.6	P				SSL		0		4	DK	GRN			Sandstone layers up to 15cm thick.	Pmnc	LPC
D	NBDD005	283.6	284.7	P	lam			SSH		0		4	DK	GRN			Wavy laminations (possible soft sediment deformation). 2cm quartz grain. Photo number 106-0127. Pyrite stringers.	Pmnc	LPC
D	NBDD005	284.7	293.8	P	lam			SSL		0		4	DK	GRN			Green tuff (7cm) at 290.7m.	Pmnc	LPC
D	NBDD005	293.8	294.4	P	itb			SIH		0		4	DK	GRN			Slumping and soft sediment deformation observed.	Pmnc	LPC
D	NBDD005	294.4	297.3	P	lam			SSL		0		4	DK	GRN				Pmnc	LPC
D	NBDD005	297.3	298	P	lam			SSH		0		3	DK	BLK			Minor slumping; minor siltstone interbeds; not pyritic.	Pmnc	LPC
D	NBDD005	298	304.4	P	lam			SSL		0		4	DK	GRY			5mm thick vein-dolomitem containing 1mm pyrite cubes.	Pmnc	LPC
D	NBDD005	304.4	304.9	P	lam			SSH		0		3	DK	BLK			minor very fine diss Py	Pmnc	LGS
D	NBDD005	304.9	312.4	P	cal			SSL		0		4	DK	GRY			chlorite alteration is less strong; HCl rxn	Pmnc	LGS
D	NBDD005	312.4	314	P	cal			SSH		0		3	DK	GRY			minor ssl; HCL reaction; calcite infilling wavy channels interpreted to be deformed de-watering structures. Cc also infilling space created by in situ brcciation	Pmnc	LGS
D	NBDD005	314	317.6	P	cal			SSL		0		3	DK	GRN			fault cutting through siltstone with alpha 30 in unoriented core; no visible bedding; perhaps destroyed by chlorite alteration	Pmnc	LGS
D	NBDD005	317.6	318.5	P	lam	<V		SSH		0		3	DK	GRY			soft sed slumping; dolomite infilling minor fractures	Pmnc	LGS
D	NBDD005	318.5	346.1	P	cal	lam		SSL		0		3	DK	GRN			HCL rxn; easy to scratch; laminated in some places and more massive elsewhere perhaps also from alteration overprint by chlorite; pink calcite vein 5mm thick at 344m; XRF did not reveal anomalous Mn but Ti was elevated	Pmnc	LGS
D	NBDD005	346.1	348	P	cal	>V		SIH		0		3	DK	GRN			calcareous and with many cross-cutting calcite veins including pink ones; rare 1mm Py blebs	Pmnc	LGS
D	NBDD005	348	355.4	P	cal	lam		SSL		0		3	DK	GRN			veins and vugs are infilled with calcite; strong HCl rxn in veins and vugs whereas higher up hole it was more dolomite as it onlyfizzes lightly when scratched to a powder	Pmnc	LGS
D	NBDD005	355.4	356.5	P	<V			SSH		0		4	DK	BLK				Pmnc	LGS
D	NBDD005	356.5	357.7	P	bxd	<V		SSL		0		4	DK	GRN			brecciation is sedimentary with clasts sub angular up to 5 cm and some shale matrix	Pmnc	LGS
D	NBDD005	357.7	361.5	P	cal	<V		SSH		0		4	DK	BLK			calcareous shale and calcite in veins including pink ones	Pmnc	LGS
D	NBDD005	361.5	393.3	P	pol	<V		SBX		0		4	DK	GRY			breccia changes styles in this interval; topped by 5cm fine-grained material (see structure table for attitude) top 1.5m is matrix-supported with sub-angular clasts up to 5mm and sandy intervals; below 362.7 it is much coarser with clasts 10cm+ (sometimes taking up the whole core) still with shaley matrix in most cases usually angular to sub-angular clasts with mix of liths including lam and non-lam siltstone and some shale; may be a debris flow; calcareous: weak HCl rxn	Pmnc	LGS
D	NBDD005	393.3	397	P	lam	cal		SSL		0		4	DK	GRY			minor calite infilled vugs and veins	Pmnc	LGS
D	NBDD005	397	405.2	P	bxd	>V		SSL		0		4	MD	GRY			only very minor laminations as measured in structural table; possibly breccaited from a fault but no main structure	Pmnc	LGS
D	NBDD005	405.2	407.3	P	cal			BFL		0		4	DK	GRY			minor vein breccia in an overall breciated interval; this has some aspects of being a sedimentary breccia of accummulation of angular clasts but also some fault-related in-situ brecciation; containing siltstone and shale clasts see photo107-0175	Pmnc	LGS
D	NBDD005	407.3	410.1	P	cal	itb		SIH		0		4	MD	GRY			finely interlaminated; fine calcite veins; lower contact is a calcite vein with small pore space and 1mm pyrite cubes	Pmnc	LPC
D	NBDD005	410.1	413	P	cal	itb		SSL		0		4	MD	GRY				Pmnc	LPC
D	NBDD005	413	422	P				SSL		0		4	MD	GRY			"intervals of in situ brecciation with shaley matrices and calcite veining conatining Py cubes; calcite infills veins and ""vugs"" which may be veinlets/dewatering structures made dicontinuous by deformation and slumping"	Pmnc	LPC
D	NBDD005	422	422.7	P	cal			SSL		0		4	MD	GRY			lots of calcite infilling pore space of irregular shapes; perhaps evaporitic in origin; see photo 107-177	Pmnc	LPC
D	NBDD005	422.7	453.5	P	cal			SSL		0		4	MD	GRY			minor brecciation and 30mm calcite vein at 446m see structure table	Pmnc	LPC
D	NBDD005	453.5	455	P	cal			SSL		0		4	MD	GRY			1mm sphalerite mixed with carbonate? At 454.8 in 1mm cubes and thin fractures see photo 107-0179;	Pmnc	LPC
D	NBDD005	455	456.1	P	vug	evp		SIH		0		4	DK	GRY			calcite in vugs and in layer-parallel bands perhaps pseudomorphed after evaporites especially in bottom metre of interval see photo 107-0180	Pmnc	LPC
D	NBDD005	456.1	473.2	P	cal			SSL		0		4	MD	GRY			wealy calcareous (weak HCl rxn over most of interval); minor 40 cm interlaminated SIH interval at 470m with wavy and disrupted blaminae; minor bxd intervals	Pmnc	LPC
D	NBDD005	473.2	476	P	cal			SSL		0		4	DK	GRN			20 cm interval at the top of possible tuff (bright chloritic green fg interval) and another less bright green intervals between 475 and 476 which may be tuff; sandy intervals are also frequent as usual in the siltstone	Pmnc	LPC
D	NBDD005	476	477	P	itb			SIH		0		4	DK	GRY			fine interlaminations	Pmnc	LPC
D	NBDD005	477	484.8	P	vug	<V		SSL		0		4	DK	GRY			minor sandy layers and shaley layers both less than 5%; calcite in veins and vugs	Pmnc	LPC
D	NBDD005	484.8	486.6	P	vug	evp		SIH		0		4	DK	GRY			calcite vugs possibly as evaporite pseudomorph and in layer parallel bands	Pmnc	LPC
D	NBDD005	486.6	488.5	P	vug	san		SSL		0		4	DK	GRY				Pmnc	LPC
D	NBDD005	488.5	489.7	P	vug	evp		SIH		0		4	DK	BLK			calcite as vugs and layer parallel bands with a Sphalerite layer see photo 107-0184	Pmnc	LPC
D	NBDD005	489.7	496.9	P	vug	cal		SSL		0		4	DK	GRY			minor sandy and shaley intervals	Pmnc	LPC
D	NBDD005	496.9	498.5	P				SSH		0		4	DK	GRY			10-20 cm beds of alternating SSH and SSL	Pmnc	LPC
D	NBDD005	498.5	503.7	P				SSL		0		4	DK	GRY			minor sand	Pmnc	LPC
D	NBDD005	503.7	504.7	P	bxd			SIH		0		4	DK	GRY			disrupted laminations; brecciation may be due to compaction as siltstone component is brittly broken and shale is matrix; Sphalerite is present as 1mm or less specks in and out of breccia clasts; not obviously associated to a fracture or other planar feature but close spatial assoc to pore space from dissolved mineral of vaguely cubic habit: perhaps halite but these pores are 1-2 mm so much larger than any Sp; Sp is not present in these cavities; see photos107-0181 to 0183	Pmnc	LPC
D	NBDD005	504.7	506	P				SSL		0		4	DK	GRN				Pmnc	LPC
D	NBDD005	506	506.8	P	bxd			SSL		0		4	DK	GRY			disrupted laminations and occasionnal clasts	Pmnc	LPC
D	NBDD006	0	5	P	wmd	fer		SSH		3		3	LT	BUF			alternating siltstone and shale; difficult to distinguish the facies with such leaching and alteration but there is a banding of both type; I interpret the softer lighter one to be shale and the harder darker one to be siltstone;iron oxide in fractures	Pmnc	LPC
D	NBDD006	5	29.9	P	wmd	lb		SSH		3		3	LT	BUF			same as above but less broken up and with less Fe oxide in fractures; may all be shale considering that when we get to the unweathered zone (from c.44) there does not appear to be anymore siltstone; patchy dendritc Mn throughout; leisegang banding	Pmnc	LPC
D	NBDD006	29.9	39	P	wmd			SSL		2		3	MD	MUV			less altered than above and comparatively more siltstone weathered to a kind of weak purplish/mauve brown colour; at 38.5-39 there are siliceous spherical nodules in a shale bed; see photo	Pmnc	LPC
D	NBDD006	39	44.7	P	cal	bnd		SSH		1		3	MD	GRY			banded between calcareous medium grey and non-calcareous darker shale; buff-colours weathering remains in patches	Pmnc	LPC
D	NBDD006	44.7	46.2	P				SSH		0		3	MD	BLK			alternatively massive and laminated; minor irregular dolomite vugs	Pmnc	LPC
D	NBDD006	46.2	50.1	P	cal	nod		SSH		0		3	MD	GRY			shale with calcareous nodules from 1-5 cm or making up bands	Pmnc	LPC
D	NBDD006	50.1	68.7	P	cal	bnd		SSH		0		3	MD	GRY			no longer any discreet nodules but banding of grey calcareous and black non-calcareous intervals alternating on 1-10 cm scale; dolomite veins 3-4 mm thick occur and are always oriented the same direction w.r.t. laminations (see structure table)	Pmnc	LPC
D	NBDD006	68.7	71.8	P				SSH		0		3	MD	GRY			Faulted shale interval containing some fault gauge from 68.7 to 68.9 and some broken core and secondary porosity over much of the interval; Shale has laminar vfg pyrite in a few 1 cm-bands	Pmnc	LPC
D	NBDD006	71.8	81.6	P				SMD		1		2	LT	GRY			relatively softer light grey shale or mudstone which absorbs water; porosity is not visible at hand-lens scale; potential aquifer with some leaching; no oxidation or mineralisation; low s.g. (specific gravity)	Pmnc	LPC
D	NBDD006	81.6	83.7	P	cal			SSH		0		3	DK	GRY			shale with on and off calcareous intervals as above; rare nodules	Pmnc	LPC
D	NBDD006	83.7	93.7	P	cal			SSH					MD	GRY				Pmnc	LPC
D	NBDD006	93.7	94.7	P	cal			FTZ		0		3	MD	GRY			secondary porosity from dissolution of minerals but also an invisible porosity interpreted from water absorbtion; visible pores are Fe-stained on the inside; up to 5mm and cluster in bedding-parallel bands. Interval includes	Pmnc	LPC
D	NBDD006	94.7	96	P				CLS									part of the fault zone; this fault caused water loss in drilling at this depth	Pmnc	LPC
D	NBDD006	96	97.4	P	vug	lam		SSH					DK	BLK			irregular dolomite vugs; perhaps infill of squashed de-watering structures	Pmnc	LPC
D	NBDD006	97.4	101.2	P	lam			SSH					DK	BLK			only minor calcareous interlaminae	Pmnc	LPC
D	NBDD006	101.2	107	P	cal	lam		SSH					DK	GRY			interbedded calcareous and non-calcareous shale	Pmnc	LPC
D	NBDD006	107	120.6	P	lam			SPH					DK	BLK			very fine-grained pyrite finely disseminated along lamination; minor slumping but generally well laminated	Pmnc	LPC
D	NBDD006	120.6	133.1	P	cal	pyr		SSH					DK	GRY			Still a bit pyritic but less ubiuitous than interval above; on and off calcareous intervals 1-10cm thick; transitional contact with calcareous bds coming in gradually	Pmnc	LPC
D	NBDD007	0	1.3	P				CLA		5		1	MD	BRN	CRM		Brown/cream clay with ~5% up-to-gravel-sized grit.	Q	CGI
D	NBDD007	1.3	5	P	bxd			CLA		5		2	LT	CRM	BRN		Weathering-induced matrix-supported breccia composed of up-to-3cm grey; weathered brown and bleached white angular-to-rounded clasts of dolomite(?) in a mottled grey/cream/brown/yellow partially-ferruginous clay-to-sand matrix.	Q	CGI
D	NBDD007	5	18.1	P	dol	lam	san	LSR		3		3	LT	CRM	WHT		Predominantly white dolomitic saprolite to saprock with some faint relict crypt-microbial lamination to ~1cm beds. Less weathered segments of silicified dark grey domal stromatolitic dolomite. ~10cm edgewise conglomerates. Less weathered up-to-40cm beds of porous coarse quartz sandstone. Lesser intervals of weathering-induced clay-matrix-supported breccia with up-to-4cm dolomite clasts. Largely broken core.	Pmnh	CGI
D	NBDD007	18.1	32.7	P	kst			LSL		5		1	LT	CRM			Homogenous unconsolidated cream silt to fine sand with ~5% grit. Possible karst-fill.	Q	CGI
D	NBDD007	32.7	43.5	P	dol	lam		LSP		4		2	LT	CRM	WHT		Cream/white dolomitic saprolite to saprock with faint relict lamination to thin bedding moving downhole. Minor sandier intervals.	Pmnh	CGI
D	NBDD007	43.5	44.1	P	qtz	sil	fer	SST		2		4	MD	GRY	YEL		Grey partially-silicified and partially-porus coarse quartz sandstone with brown/yellow ferrugous fracturing.	Pmnh	CGI
D	NBDD007	44.1	47	P	bl	lam		SDM		2		3	LT	BRN	CRM		Partially-bleached pale brown/cream crypt-microbial laminated to thin-bedded dolomite. Common clast-supported dissolution brecciation. Minor unconsolidated silt/sand/grit which may be karst-fill.	Pmnh	CGI
D	NBDD007	47	53.1	P	bl	lam	bnd	SDM		2		4	MO	RED	GRY		Partially-bleached microbial laminated to thin-bedded dolomite. Maroon colour bands overprinted along some laminae and fractures by a grey/green colour. Minor chert rubble with gouge-like material.	Pmnh	CGI
D	NBDD007	53.1	61.2	P	dol	lam	bnd	LSR		3		2	LT	WHT	GRY		White dolomitic saprock with relict microbial lamination to thin-bedding. ~50% of this interval is composed of pale grey chert rubble.	Pmnh	CGI
D	NBDD007	61.2	65.2	P	lam	nod	sil	SDM		2		3	MD	BRN	CRM		Partially-bleached; stained brown/ferruginous crypt-microbial laminated to thin-bedded dolomite. ~10cm edgewise conglomerates. Up-to-4cm carbonate nodules; possibly after anhydrite. Common clast-supported to matrix-supported dissolution(?) brecciation. Occasional selectively-silcified and partially porous dark grey stromatolites and/or sandier intervals. Mn dendrites in the bottom meter of the interval. Liesegang weathering.	Pmnh	CGI
D	NBDD007	65.2	69.1	P	sil	fer		BRE		2		3	MO	BRN	GRY		Clast-supported to matrix-supported fault(?) breccia composed of polymictic angular-to-subangular clasts of dolomite in a ferruginous brown gouge-to-fine-sand matrix. Rubble composed of silicified clasts and botryoidal manganiferous clasts.	Pmnh	CGI
D	NBDD007	69.1	76.8	P	bxd			SDM		2		3	MD	BRN	GRY		Largely broken core composed predominantly of brown ferruginous crypt-microbial laminated dolomite with Mn dendrites. Lesser intervals of silicified coarse quartz sandstone and of unconsolidated fine sand (possible karst fill).	Pmnh	CGI
D	NBDD007	76.8	88	P	lam	evp	nod	SDM		0		4	MD	GRY	CRM		Microbial laminated to thin-bedded dolomite with occasional cm-scale bioherms; beds of cream recrystalised dolomite through to grey crystaline dolomite. Common edgewise conglomerate intervals typically ~10cm. Common sawtooth-edged gypsum pseudomorph laminae. Occasional up-to-3cm silicified flattened nodules possibly after anhydrite. Occasional intervals with abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. Occasional pressure dissolution brecciation and selective silicification of beds. Minor stylolites. 83-84m is broken core with ferruginous fractures- possible fault zone.	Pmnh	CGI
D	NBDD007	88	89.6	P	evp			SDM		0		5	MD	GRY			Microbial laminated dolomite. ~50% of interval has abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. (An alternate interpretation is that these intervals are sedimentary conglomerates; e.g. storm surge deposit) Minor red hematite.	Pmnh	CGI
D	NBDD007	89.6	94.3	P				SDE		0		5	MD	GRY			Homogenous dolarenite (appears slightly more clastic than other crystaline dolomite intervals) with faint bedding. Occasional stylolites.	Pmnh	CGI
D	NBDD007	94.3	103.7	P	lam	evp		SDM		0		5	MD	GRY			Microbial laminated to thin-bedded dolomite with occasional cm-scale bioherms; beds of cream recrystalised dolomite through to grey crystaline dolomite. Minor sawtooth-edged gypsum pseudomorph laminae. Minor intervals with abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. Minor dissolution brecciation. Occasional stylolites and Mn dendrite.	Pmnh	CGI
D	NBDD007	103.7	115	P	lam	nod		SDM		0		5	LT	GRY	PNK		Crypt-microbial laminated to thin-bedded dolomite; beds of recrystalised dolomite through to crystaline dolomite. Common up-to-3cm silicified flattened nodules possibly after anhydrite. Minor gypsum psedomorph sawtooth laminae. Minor stylolites and Mn dendrites on fracture surfaces.	Pmnh	CGI
D	NBDD007	115	120.9	P	evp			SDM		0		5	LT	GRY	CRM		Crypt-microbial laminated to thin bedded dolomite; beds of cream/pink recrystalised dolomite through to grey crystaline dolomite. Over 50% has abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. Some flattened up-to-3cm carbonate nodules and common sawtooth gypsum pseudomorph laminae. Some selective silicification of beds.	Pmnh	CGI
D	NBDD007	120.9	124.1	P	lam	nod		SDM		0		5	MD	GRY			Faint microbial laminated to thin-bedded mostly grey crystaline dolomite. Common ~2cm flattened carbonate nodules possibly after-anhydrite and up-to-5cm 'blotchy' textured 'patches' of coarse dolomite crystals. Minor selectively silicified beds.	Pmnh	CGI
D	NBDD007	124.1	126.9	P	lam	hmt		STD		0		5	MD	GRY			Transitional from crypt-microbial laminated crystaline dolomite to more planar laminated and possibly more clastic-looking dolomitic siltstone. Common red hematite interlaminae.	Pmnh	CGI
D	NBDD007	126.9	128	P	lam	tuf	xbh	SPH		0		4	DK	BLK	GRY		Laminated black shale with lesser interlaminae of grey dolomitic siltstone increasing in frequency moving downhole. Some hummocky cross-stratification. At ~127m shale is friable- more carbonaceous(?). At 127.7m there is a 2cm cream-coloured K-altered/tuffaceous band.	Pmnc	CGI
D	NBDD007	128	129.7	P	lam	slt	nod	SDM		0		5	MD	GRY			Crypt-microbial laminated to medium bedded dolomite; beds of pale grey recrystalised dolomite through to darker grey crystaline dolomite. Minor dark silty interlaminae. Occasional up-to-3cm flattened carbonate nodules- possibly after-anhydrite. Some of the dolomite has dark thin 'whisps' which are mostly bedding-parallel.	Pmx	CGI
D	NBDD007	129.7	131.1	P	evp	lam		SDM		0		5	MD	GRY			Crypt-microbial laminated to thin-bedded grey crystaline to recrystalised dolomite. Majority of interval has abundant 2-10mm round/lath/pine grey carbonate crystals and an overall 'blotchy' appearance- possible anhydrite/gypsum pseudomorph horizons. Much of this interval has coarse clear dolomite crystal beds etc that appear to be open-space fill. That Evidence for storm surge acivity with black clasts (silt? No acid response) and rare quartz grains. Possible trace pyrite.	Pmx	CGI
D	NBDD007	131.1	132.7	P	lam			SDM		0		5	MD	GRY			Crypt-microbial laminated to thin-bedded dolomite; crystaline through to recrystalised dolomite. Minor interbeds of 2-10mm round/lath/pine carbonate crystals with an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons.	Pmx	CGI
D	NBDD007	132.7	136	P	evp	lam		SDM		0		5	MD	GRY			Crypt-microbial laminated to thin-bedded crystaline dolomite. Majority of interval has abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. Much of this interval has coarse clear dolomite crystal beds and nodules that are appear to be open-space fill.	Pmx	CGI
D	NBDD007	136	138.2	P	lam	tuf		SDM		0		5	MD	GRY			Microbial laminated to thin-bedded crystaline to recrystalised dolomite. Minor <2cm pink k-altered/tuffaceous beds.	Pmx	CGI
D	NBDD007	138.2	146.5	P	evp	lam		SDM		0		5	MD	GRY			Microbial laminated to thin-bedded crystaline to recrystalised dolomite. Common sawtooth-edged gypsum pseudomorph laminae. Common intervals with abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons. Some of the  interval has coarse clear dolomite crystal beds and nodules that appear to be open-space fill. Minor selectively silicified beds. At 139.2m there are conspicuous ~2mm round black nodules; possibly after-anhydrite.	Pmx	CGI
D	NBDD007	146.5	150.5	P	lam	tuf		SDM		0		5	MD	GRY	PNK		Microbial laminated to thin-bedded dolomite; interbeds of grey crystaline dolomite and pink recrystallised dolomite. Occasional <10cm bands of red/cream/orange K-alteration/tuffaceous material (e.g. 150.5m). Minor selective silicification of beds; minor red hematitic laminae. Occasional bedding-parallel stylolites. ~20% is broken core with ferruginous fracture coating.	Pmx	CGI
D	NBDD007	150.5	159.1	P	lam	tur		STD		0		5	MD	GRY			Planar laminated dolomitic siltstone and black shale. Interval is turbiditic (fuzzy-edged parasequences due to recrystallisation) and has an overall 'black tram tracks' appearance. Minor <10cm intervals with abundant ~2mm round/lath/pine carbonate crystals and an overall 'blotchy' appearance- interpreted to be anhydrite/gypsum pseudomorph horizons.	Pmx	CGI
D	NBDD007	159.1	167.7	P	lam	pyr		SSH		0		5	DK	BLK	GRY		Planar laminated black shale with lesser grey dolomitic siltstone interlaminae. Occasional pyrite blebs and ~2mm beds and ~5cm zones of abundant ~3mm round/lath/pine evaporite pseudomorphs. Moderate-intensity late typically ~3mm calcite veining and late micro-faulting.	Pmq	CGI
D	NBDD007	167.7	179	P	lam	slt	tuf	SDM		0		5	MD	GRY			Grey planar laminated dolomitic siltstone becoming crypt-microbial laminated crystaline dolomite with lesser black silty interlaminae and black shale beds. Rare pyrite blebs possibly replacing nodules. Rare <4cm cream/green K-altered/tuffaceous beds that might be associated with black shale beds. Rare <2cm evaporite psedomorph horizons. Minor late calcite + pink carbonate + chlorite(?) veining.	Pmp	CGI
D	NBDD007	179	181.1	P	lam	slt		STD		0		5	LT	CRM	GRN		Interlaminae of red and cream crystaline dolomite with thin silty green interlaminae	PmqW	CGI
D	NBDD007	181.1	181.6	P	lam			SDM		0		5	MD	GRY			Grey crypt-microbial laminated crystaline dolomite with lesser black silty interlaminae and black shale beds.	Pmp	CGI
D	NBDD007	181.6	187.3	P	lam	slt	tuf	SDM		0		5	LT	GRY	CRM		Microbial laminated crystaline dolomite to cream recrystallised dolomite with minor silty interlaminae decreasing moving downhole. Occasional <10cm cream green and orange altered/tuffaceous beds that might be associated with black shale beds. Abundant bedding parallel stylolites. Rare ~1-2cm patches/nodules of coarser open-fill crystaline dolomite with Py or Cpy flecks (e.g. 182.6m).	Pmp	CGI
D	NBDD007	187.3	189.5	P				SDO		0		5	LT	GRY	PNK		Recrystallised dolomite with patchy faint microbial lamination	Pmp	CGI
D	NBDD007	189.5	190.9	P	lam			SDM		0		5	LT	GRY	CRM		Diffuse microbial laminated crystaline dolomite to cream recrystallised dolomite.	Pmp	CGI
D	NBDD007	190.9	197.6	P	tuf			SDO		0		5	LT	GRY	PNK		Pink recrystallised dolomite. Abundant stylolites. At 92.1m there is a ~15cm cream/orange K-alteration/tuffaceous band.	Pmp	CGI
D	NBDD007	197.6	200.8	P	fra	tuf		SDO		0		5	LT	BRN	YEL		Recrystallised dolomite. Mostly broken core with ferruginous brown/yellow colouration. At 199.1m there is a ~2cm dark brown K-altered/tuffaceous band.	Pmp	CGI
D	NBDD007	200.8	209.9	P				SDO		0		5	LT	PNK			Pink recrystallised dolomite. Patchy faint microbial lamination to thin bedding. 208-209m is largely broken core with brown ferruginous fracture coating. Occasional coarse dolomite crystal open-space-fill.	Pmp	CGI
D	NBDD007	209.9	215	P	lam	tuf		SDM		0		5	LT	RED	PNK		Pink and red microbial laminated crystaline to recrystallised dolomite. Occasional <5cm K-altered/tuffaceous brown and orange bands. Common stylolites.	Pmp	CGI
D	NBDD007	215	216.2	P				SDO		0		5	LT	PNK			Pink recrystallised dolomite. Patchy faint microbial lamination to thin bedding	Pmp	CGI
D	NBDD007	216.2	222	P	lam			SDM		0		5	LT	PNK			Pink and red microbial laminated crystaline to recrystallised dolomite.  Common stylolites.	Pmp	CGI
D	NBDD007	222	227.1	P	tuf			SDO		0		5	LT	PNK			Pink recrystallised dolomite. Faint and patchy microbial lamination. Occasional <5cm K-altered/tuffaceous brown and orange bands.	Pmp	CGI
D	NBDD007	227.1	234.9	P	lam			SDM		0		5	LT	PNK			Thin microbial laminated pale crystaline dolomite with darker maroon silty interlaminae becoming more frequent and thicker moving downhole (silty interbeds have a no acid response). Minor fracturing with ferruginous yellow coating and Mn dendrites. Minor calcite veining.	Pmp	CGI
D	NBDD007	234.9	235.8	P	bnd			SDM		0		5	MD	BRN			~2cm rhythmically interbedded dark maroon siltstone and paler microbial laminated crystaline dolomite	Pmp	CGI
D	NBDD007	235.8	237.1	P	bnd			SDO		0		5	MO	BRN	CRM		~2cm rhythmically interbedded dark brown siltstone and cream recrystallised dolomite.	Pmp	CGI
D	NBDD007	237.1	239.6	P	bnd			SDM		0		5	MD	BRN			~2cm rhythmically interbedded dark maroon siltstone and paler microbial laminated crystaline dolomite	Pmp	CGI
D	NBDD007	239.6	243	P	lam			SDM		0		5	MD	BRN			Thin microbial laminated pale brown crystaline dolomite with darker maroon silty interlaminae/interbed reducing in frequency and size moving downhole.	Pmp	CGI
D	NBDD007	243	257	P				SDO		0		5	LT	PNK	GRY		Pink recystallised dolomite to grey crystaline dolomite with patchy faint microbial lamination. Abundant stylolites. Minor <1cm calcite veining.	Pmp	CGI
D	NBDD007	257	259	P	lam	tur		STD		0		5	MD	GRY			Planar lamianted grey (to possible microbial laminated) dolomitic siltstone and lesser black shale. Turbiditic (fuzzy-edged parasequences due to recrystallisation) with 'black tram tracks' appearance.	Pmp	CGI
D	NBDD007	259	267.2	P				SDO		0		5	LT	GRY			Cream/grey/pink recrystalised dolomite with lesser grey crystaline dolomite. Patchy and faint microbial lamination. Minor pink Fe-carbonate open-space-fill. Abundant stylolites.	Pmp	CGI
D	NBDD007	267.2	267.4	P				SDO		0		5	MD	GRY			Blotchy-textured pale grey recrystalised dolomite and dark grey crystaline dolomite. Coxco needles.	Pmc	CGI
D	NBDD007	267.4	276.8	P				SDO		0		5	LT	GRY	PNK		Predominantly grey to pink recrystalised dolomite.	Pmp	CGI
D	NBDD007	276.8	277.4	P				SDO		0		5	MO	GRY	BLK		Blotchy-textured pale grey recrystalised dolomite and black crystaline dolomite. Coxco needles.	Pmc	CGI
D	NBDD007	277.4	287.1	P				SDO		0		5	LT	GRY	PNK		Predominantly grey to pink recrystalised dolomite. Abundant stylolites.	Pmp	CGI
D	NBDD007	287.1	289.9	P				SDO		0		5	MD	GRY			Blotchy-textured pale grey recrystalised dolomite and dark grey crystaline dolomite. Possible Coxco needles.	Pmc	CGI
D	NBDD007	289.9	346	P				SDO		0		5	LT	GRY	PNK		Grey to pink recrystalised and crystaline massive dolomite. Mostly massive. Abundant stylolites. Occasional late carbonate veins.	Pmp	CGI
D	NBDD007	346	351.8	P	lam			SDM		0		5	LT	GRY	CRM		Crypt-microbial laminated grey crystaline and cream recrystalised dolomite	Pmea	CGI
D	NBDD007	351.8	360	P				SDO		0		5	LT	PNK	GRY		Massive pink/grey mostly recrystalised dolomite. Rare faint relict lamination. Broken core and red hematite filled fractures at 365-365.5m may represent a fault zone.	Pmp	CGI
D	NBDD007	360	376.2	P	lam	evp		SDM		0		5	LT	GRY			Microbial laminated medium grey crystaline to pale grey recrystalised dolomite; with some cm-scale bioherms. Blotchy textured zones with <5mm nodular/lath/pine crystals that may represent an evaporite pseudomorph horizon. Some ~10cm edgewise conglomerate intervals. At 365.5m there is a ~10cm interval of ~1mm thick elongate needles (up to 4cm). Minor late Fe-carbonate veining and stylolites.	Pmea	CGI
D	NBDD007	376.2	379.8	P				SDO		0		5	LT	PNK	GRY		Mottled pink/grey largely recrystalised dolomite with faint relict lamination and edgewise conglomerates. Minor stylolites.	Pmp	CGI
EOF