H0002 Version 4 H0003 Date_generated 23-Feb-19 H0004 Reporting_period_end_date 28-Dec-17 H0005 State NT H0100 Tenement_no/Combind_report_no EL31306 H0101 Tenement_holder Bacchus Resources H0102 Project_name Woolwonga H0106 Tenement_operator Bacchus Resources H0150 250K_map_sheet_number SD5208 H0151 100K_map_sheet_number 5271 H0152 50K_map_sheet_number H0153 25K_map_sheet_number H0200 Start_date_of_data_acquisition 11-Nov-17 H0201 End_date_of_data_acquisition 19-Dec-18 H0202 Data_format DL4 H0203 Number_of_data_records 1172 H0204 Date_of_metadata_update 13-Dec-18 H0300 Related_data_file H0301 Location_data_file EL31306_2018_02_drillcollars.txt H0302 Lithology_data_file EL31306_2018_03_drilllith.txt H0303 Assay_data_file EL31306_2018_05_drillassay.txt H0304 Survey_data_file EL31306_2018_04_drillsurvey.txt H0305 SurfGeochem_Data_File EL31306_2018_06_surfacegeochem.txt H0307 Lithology_code_file Logging_Codes H0308 File verification List EL31306_2018_07_Verification_List.txt H0310 Water_data_file H0311 Water data incl in lithology file No H0313 Alteration_data_file H0314 Magsusc_data_file H0315 Vein_data_file H0316 Recovery_data_file H0317 Weathering_data_file H0318 DHQAQC_data_file H0319 SURFQAQC_data_file H0320 Other event_data_file H0400 Drill_code DDH RC H0401 Drill_contractor AMWD AMWD H0402 Description Diamond Drilling Reverse Circulation Drilling H0500 Feature_located Drillhole_collar H0501 Geodetic_datum GDA94 H0502 Vertical_datum Nominal H0503 Projection Map Grid of Australia (MGA) H0508 Local Grid Name H0530 Coordinate_system Projected H0531 Projection_zone 52 H0532 Surface_Location_Survey_Instrument GPS H0533 Surface_Location_Survey_Company H0536 Downhole_Geophysical_Survey_Instrument H0537 Downhole_Geophysical_Survey_Company H0900 Remarks H1000 Hole_id Depth From Depth To Colour Lithology LITH1_% BED_THICKNESS_CM1 LITH2_CODE LITH2_% BED_THICKNESS_CM2 LITH3_CODE LITH3_% BED_THICKNESS_CM3 MIN1 MIN2 COMMENTS PLOT_LITH SOURCE LITH_OXIDATION Alteration ALT1_INT ALT1_STYLE ALT2_CODE ALT2_INT ALT2_STYLE Mineralisation ALT3_INT ALT3_STYLE H1001 NA metres metres NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA H1004 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 D BWD003 0 2.5 RD ROS 100 HEM "Alluvial top cover material, mostly clay minerals" D BWD003 2.5 2.66 WH XQO 100 HEM Highly weathered and oxidised solidified clay minerals with extensive haematite D BWD003 2.66 3.38 RD RTY 90 HEM Highly weathered and more oxidisation and leaching D BWD003 3.38 3.9 GRRD RRR 100 HEM D BWD003 3.9 4.6 GRRD SOO 90 GT D BWD003 4.6 5.62 YEBR SOO 30 RRY 30 XQO 30 QZ Brecciated qtz vein running almost sub parallel with the core axis. Weathering was secondary to the formation of the qz vein D BWD003 5.62 5.77 YEBR SSS 90 QZ Coarser grain sandstone interbedded with clay minerals D BWD003 5.77 6 YEBR RRY 70 QZ Interbedded claystones and sandstones D BWD003 6 6.3 YEBR SSS 100 GT Interbedded claystones and sandstones D BWD003 6.3 6.47 YEBR RRY 90 GT Interbedded claystones and sandstones D BWD003 6.47 6.7 YEBR UOO 100 GT Interbedded claystones and sandstones D BWD003 6.7 7 YEBR RRY 100 GT CLAY Interbedded claystones and sandstones D BWD003 7 7.12 YEBR SSS 100 GT Interbedded claystones and sandstones D BWD003 7.12 8 YEBR RRY 80 GT CLAY Clay minerals making up most of the matrix with small veins consisting of a kaolinite running perpendicular to the core axis D BWD003 8 8.4 YEBR SSS 80 XQO 20 GT Coarse grained oxidised sandstone with brecciated qz vein D BWD003 8.4 9 YEBR SSS 100 GT CLAY Sandstone with clay filled veins D BWD003 9 9.32 YEBR RRY 100 GT D BWD003 9.32 9.9 YEBR SSS 80 XQO 20 GT QZ "Sandstone with a highly fractured, oxidised and weathered qz vein" D BWD003 9.9 10.36 GR RRY 100 CLAY D BWD003 10.36 10.66 GR RTY 100 CLAY Loose rubble zone consisting of mostly transported clay minerals D BWD003 10.66 14.25 GR RRY 100 CLAY D BWD003 14.25 15 YEBR SSS 100 GT Solid sandstone layer D BWD003 15 15.85 YEBR UOO 100 GT CLAY Intensly broken up zone with predominantly rubble and some angular clay fragments D BWD003 15.85 20.15 RDBR RTY 100 CLAY D BWD003 20.15 21.2 YEBR SSK 90 XQO 10 GT HEM Fine grained sedimentary zone with high strain micro deformation taking place with strong iron oxides and qz vein D BWD003 21.2 22.56 GROR RRY 100 CLAY D BWD003 22.56 22.9 GROR UOO 100 HEM CLAY Rubble zone D BWD003 22.9 24.05 GROR SSK 100 CLAY Fine grained siltstone layer with a soapy texture but grains are too large to be clay D BWD003 24.05 24.68 GROR UOO 50 CLAY Rubble sone with larger angular fragments D BWD003 24.68 28.25 GROR SSK 100 CLAY D BWD003 28.25 28.46 GROR UOO 100 Rubble zone D BWD003 28.46 29 GROR SSK 100 D BWD003 29 33.52 GROR UOO 100 Rubble zone D BWD003 33.52 34 WH XQO 100 QZ D BWD003 34 34.5 GR UOO 100 Rubble zone D BWD003 34.5 36 GR SSS 100 GT D BWD003 36 36.5 BRGR IMD 100 GT FE Dolerite matrix alternating between medium to coarse grains D BWD003 36.5 44.8 DKGR IMD 100 FE SI Dolerite matrix alternating between medium to coarse grains D BWD003 44.8 94.5 DKGR IMD 100 PY "Coarser grained with depth, defined by plagioclase crystals. Sulphidic towards base of unit." D BWD003 94.5 95.8 DKGY SIO 70 XQZ 30 PY QTZ VEINIG BRECCIATED 94.5-95M AND 'SWIRLY' 95.4-95.8M D BWD003 95.8 100.58 GYGN SIO 100 PY PORPHYROBLASTIC. SOME BEDDED LAYERS ALTERED TO AN OLIVE GREEN COLOUR - DUE TO DOLERITE INTRUSIVE? MINOR SULPHIDIC VEINS D BWD003 100.58 102.7 DKGY SSG 60 10 SIO 40 5 PY BEDS FROM 1-10CM FOR BOTH UNITS. PORPHYROBLASTIC D BWD003 102.7 105.3 DKGY SSG 100 PY D BWD003 105.3 113.4 DKGY SSG 90 XQZ 10 PY QTZ-SULPHIDE VEINS 3-4/METRE 5-30MM THICK. MINOR INTERVALS OF MUDSTONE. D BWD003 113.4 120.05 DKGY SSG 80 70 SIO 20 15 YOUNGING UP HOLE (GRADED BEDS). D BWD003 120.05 123.9 DKGY SSG 100 FINE GRAINED D BWD003 123.9 125.63 DKGY SSG 80 40 SIO 20 10 INTERMINGLING/MIXING OF TWO LITHOLOGIES D BWD003 125.63 132.76 DKGY SIO 100 PY MINOR COARSER INTERBEDS D BWD003 132.76 135.85 DKGY SIO 70 80 SSG 30 30 D BWD003 135.85 136.35 DKGY SIO 100 D BWD003 136.35 136.95 DKGY SIO 100 ZSZ HIGHLY FRACTURED WITH POSSIBLE FAULT GOUGES 10CM WIDE. D BWD003 136.95 139.38 DKGY SIO 100 PORPHYROBLASTIC INTERBEDS - POSSIBLY MORE SILTY. D BWD003 139.38 140.93 DKGY SIC 100 GR PY POSSIBLE FAULT GOUGE 139.46-139.56M. GRAPHITE APPEARS MOSTLY ON FRACTURES D BWD003 140.93 146 DKGY SIO 50 40 SSG 50 40 PY "OCCASIONAL QTZ-SULPHIDE VEINS. GRADED BEDS, YOUNGING UPHOLE" D BWD003 146 150.8 DKGY SSG 100 D BWD003 150.8 153.46 DKGY SIO 70 70 SSG 30 30 D BWD003 153.46 154 DKGY SIC 100 GR GRAPHTIE MOSTLY ON FRACTURE SURFACES. D BWD003 154 156 DKGY SIC 100 ZSZ GR HIGH STRAIN ZONE. GRAPHITIC. RANDOM QTZ VEINS THROUGHOUT D BWD003 156 158.55 DKGY SSG 45 20 SIO 55 25 D BWD003 158.55 160.03 DKGY SIO 100 D BWD003 160.03 165 DKGY SSG 100 FINE GRAINED. VERY MINOR INTERVALS OF MUDSTONE D BWD003 165 178.1 DKGY SSG 60 100 SIO 40 70 SAND INTERVALS BETWEEN 20-100CM THICK. MUD/SILT INTERVALS 20-70CM. SOME INDICACTION OF TURBIDITIC ENVIRONMENT. D BWD003 178.1 182.3 DKGY SIO 100 HIGH STRAIN ZONE 178.1-178.7M D BWD003 182.3 183.4 DKGY SIO 100 ZFG 100 "POSSIBLE FAULT GOUGE, CORE IS CLAYEY AND VERY SMALL RUBBLE. HIGH STRAIN ZONE" D BWD003 183.4 188.1 DKGY SIO 90 100 SSG 10 15 D BWD003 188.1 194.8 DKGY SSG 50 50 SIO 50 50 D BWD003 194.8 197.8 DKGY SIO 100 PY "MINOR SILTY/VERY FINE GRAINED SANDSTONE INTERVALS, 1CM THICK" D BWD003 197.8 199.2 BK SIC 100 PY GR GRAPHITIC ON FRACTURE SURFACES D BWD003 199.2 202.05 DKGY SSG 50 120 SIO 50 120 ONE SEDIMENTARY SEQUENCE FINING UP HOLE D BWD003 202.05 203.75 DKGY SIO 70 XQZ 30 PY QTZ VEINS UP TO 30CM ~5% SULPHIDES D BWD003 203.75 208.55 DKGY SIO 65 80 SSG 35 50 SOME MIXING OF THE TWO LITHOLOGIES - TURBIDITIC ENVIRONMENT. MUDSTONE IS PORPHROBLASTIC D BWD003 208.55 221.8 BK SIO 100 APY PY PORPHYROBLASTIC. ARSENOPYRITE STARS AND CROSSES VERY COMMON. OCCASIONAL 10CM QTZ/SULPHIDE VEINS D BWD003 221.8 229.33 DKGY SIO 85 200 SSG 15 30 INTERBEDDED WITH SOME MIXING OF THE TWO LITHOLOGIES AT CONTACT. D BWD003 229.33 237.18 DKGY SIO 95 XQZ 5 PY VERY MINOR COARSER GRAINED INTERVALS. COMMON QTZ-SULPHIDE VEINS 1-50MM D BWD003 237.18 244.4 DKGY SSG 90 200 SIO 10 15 PREDOMINANTLY SANDSTONE WITH MINOR MUDSTONE INTERBEDS AND ?MUDBALLS D BWD003 244.4 254.4 DKGY SIO 50 30 SSG 50 30 "OVERTURNED BEDS? GRADED BEDS, FINING DOWNHOLE. SEVERAL SEDIMENTARY SEQUENCES AVERAGING 60CM PER SEQUENCES FROM COARSE TO FINE DOWNHOLE. SOME FINELY LAMINATED INTERVALS ~15CM IN TOTAL" D BWD003 254.4 260.2 DKGY SSG 100 MINOR MUDSTONE. FINE AND COARSER GREYWACKE D BWD003 260.2 269.74 DKGY SSG 60 50 SIO 40 35 "OVERTURNED BEDS? GRADED BEDS, FINING DOWNHOLE. SEVERAL SEDIMENTARY SEQUENCES 70-150CM PER SEQUENCES FROM COARSE TO FINE DOWNHOLE. " D BWD003 269.74 274.15 DKGY SSG 80 400 SIO 20 100 "OVERTURNED BEDS? GRADED BEDS, FINING DOWNHOLE WITH ?FLAME STRUCTURES AT CONTACT WITH SAND AT BOTTOM OF INTERVAL. POSSIBLY INTERVAL IS ONE SEDIMENTARY SEQUENCE DOMINATED BY SAND " D BWD003 274.15 279.34 DKGY SIO 75 85 SSG 25 25 "BEDDING NOT AS CLEAR AS ABOVE, SOME ?MUD BALLS WITHIN SAND AT CONTACT WITH ABOVE SEQUENCE. IMMATURE BRECCIA FORMING AT 275.54-275.64M." D BWD003 279.34 311.45 DKGY SSG 75 60 SIO 25 20 "OVERTURNED BEDS. FLAME STRUCTURES INDICATE YOUNGING DOWNHOLE. GRADED BEDS, FINING DOWNHOLE. SEVERAL SEDIMENTARY SEQUENCES AVERAGING 80CM PER SEQUENCES FROM COARSE TO FINE DOWNHOLE. " D BWD003 311.45 329.17 DKGY SIO 100 MINOR INTERVALS OF COARSER GRAINED LITHOLOGIES. D BWD003 329.17 350.8 DKGY SSG 85 100 SIO 15 20 OVERTURNED BEDS? POSSIBLE FLAME STRUCTURES AND GRADED BEDS. EOH D BWD004 0 1.92 LTGY HMO 100 D BWD004 1.92 2.2 OR UOO 100 UNCONSOLIDATED ?SOIL OR HIGHLY WEATHERED ROCKS D BWD004 2.2 14.1 ORGY SSG 85 100 SIO 15 10 SAPROLITIC INTERBEDDED SANDSTONE AND SILTSTONE D BWD004 14.1 24.6 ORGY SIO 90 200 SSG 10 20 SAPROLITIC VERY CLAY RICH WITH INTERBEDS OF COARSER GRAINED MATERIAL D BWD004 24.6 25.9 BEGY SSG 75 150 SIO 25 60 INTERBEDDED FINE TO MEDIUM GRAINED SANDSTONE AND SILTSTONE. BOCO. D BWD004 25.9 34.92 BEGY SSG 75 150 SIO 25 60 INTERBEDDED FINE TO MEDIUM GRAINED SANDSTONE AND SILTSTONE. SHARP CONTACTS ON UPPER LIMITS OF SILTSTONE/MUDSTONE AMD GRADATIONAL ON LOWER LIMITS - YOUNGING UPHOLE? BASE OF PARTIAL OXIDATION D BWD004 34.92 43 GYOR SSG 80 220 SIO 20 50 INTERBEDDED FINE GRAINED SANDSTONE AND MUDSTONE/SILSTONE D BWD004 43 48.25 GY SSG 100 FINE GRAINED SANDSTONE D BWD004 48.25 49 GYWH XQZ 95 SSG 5 ~3% SULPHIDE CONTENT IN QTZ VEIN WITH INCLUSIONS OF HOSTROCK D BWD004 49 56.4 GY SSG 95 300 SIO 5 5 PREDOMINATELY FINE GRAINED SANDSTONE WITH MINOR INTERBEDS OF SILTSTONE/MUDSTONE D BWD004 56.4 57.02 LTGY ZFG 50 SIO 50 DOMINATELY CLAY AMONGST VERY BROKEN SILTSTONE D BWD004 57.02 64.05 GY SSG 100 VERY FINE GRAINED SANDSTONE. VERY BROKEN GROUND FROM 61.5M D BWD004 64.05 64.2 BEGY ZFG 100 FAULT GOUGE? MOSTLY CLAY D BWD004 64.2 67 GY SSG 100 FINE GRAINED SANDSTONE D BWD004 67 71.8 DKGY SSG 90 200 SIO 10 25 INTERBEDDED SANDSTONE AND SILTSTONE D BWD004 71.8 76.16 DKGY SSG 100 FINE GRAINED SANDSTONE D BWD004 76.16 78.6 DKGY SSG 90 150 SIO 10 60 FINE GRAINED SANDSTONE AND MUD/SILTSTONE. MUD/SILTSTONE BEDS UP TO 60CM THICK D BWD004 78.6 81 DKGY SSG 100 FINE GRAINED SANDSTONE D BWD004 81 81.5 DKGY SIO 90 SSG 10 POSSIBLY FINING UP SEQUENCE. D BWD004 81.5 85.83 DKGY SSG 100 FINE GRAINED D BWD004 85.83 86.36 GYBE SSG 100 FINE GRAINED. LIGHTER GREY WITH SOME ?LIMONITE D BWD004 86.36 88 DKGY SIO 100 SILTSTONE - POSSIBLY MUDSTONE IN PART D BWD004 88 89.24 DKGY SSG 100 FINE TO MEDIUM GRAINED D BWD004 89.24 97.2 DKGY SIO 70 60 SSG 30 40 CHLORITE ON FRACTURES. OCCASIONAL QTZ-SULPHIDE VEINS UP TO 3CM THICK D BWD004 97.2 99.2 DKGY SSG 100 FINE GRAINED D BWD004 99.2 100.63 DKGY SIO 85 SSG 25 GRADATIONAL BOUNJDARIES BETWEEN SILT/MUDSTONE AND VERY FINE GRAINED SANDSTONE D BWD004 100.63 105.58 DKGY SSG 100 FINE GRAINED D BWD004 105.58 112 DKGY SSG 80 150 SIO 20 10 INTERBEDDED SANDSTONE AND MUDSTONE. MILLIMETRIC PORPHYROBLASTS IN FINER GRAINED UNITS D BWD004 112 126.3 DKGY SIO 100 """SLIGHT VARIATIONS IN COLOUR FROM LT TO DK GREYS" MILLIMETRIC PORPHYROBLASTS IN FINER GRAINED UNITS "VERY MINOR COARSER GRAINED INTERBEDS. QTZ-SULPHIDE VEINING COMMON""" D BWD004 126.3 131.66 DKGY SSG 75 SIO 25 """MOSTLY GRADATIONAL BOUNDARIES" "OCCASIONAL SHARP CONTACTS. """ D BWD004 131.66 135.6 DKGY SIO 100 """MILLIMETRIC PORPHYROBLASTS VERY COMMON THROUHGOUT UNIT" "SOMETIMES FORMING BOUNDARIES WHERE THEY HAVE CONGREGATED.""" D BWD004 135.6 137.4 DKGY SSG 100 FINE GRAINED SANDSTONE D BWD004 137.4 138.1 DKGY SIO 100 D BWD004 138.1 157.95 DKGY SSG 85 50 SIO 25 20 INTERBEDDED SILTSTONE AND SANDSTONE. SILT/MUDSTONE BEDS RANGE IN THICKNESS FROM 5-30CM IN THICKNESS. TOWARDS BASE OF UNIT SANDSTONE AND MUDSTONE APPEAR TO INTERMINGAL (TURBIDITIC?) D BWD004 157.95 165.7 DKGY SSG 100 D BWD004 165.7 165.9 GY ZSZ 50 SSG 50 """VERY FRACTURED ZONE" POSSIBLE GOUGE "ABUNDANT CLAY""" D BWD004 165.9 169.77 DKGY SSG 100 D BWD004 169.77 171.9 DKGY SSG 85 70 SIO 15 25 D BWD004 171.9 174.65 DKGY SSG 100 MINOR QTZ-SULPHIDE VEINS 1-3CM THICK D BWD004 174.65 176.34 DKGY SSG 90 50 SIO 10 5 ?TURBIDITIC SEQUENCE? VERY FINE TO FINE SANDSTONE AND THIN INTERVALS OF MUD/SILTSTONE D BWD004 176.34 181.55 GYGN SIO 100 DARK GREY TO OLIVE GREEN CHLORITIC MUD/SILTSTONE. PORPHYROBLASTS COMMON AND DARKER IN COLOUR D BWD004 181.55 182.94 GYGN SSG 100 CHLORITIC OLIVE GREENISH GREY MINOR QTZ-SULPHIDE VEINING AND QTZ-CARBONATE VEINING D BWD004 182.94 184.04 DKGY SIO 100 D BWD004 184.04 184.4 DKGY SSG 100 D BWD004 184.4 189.92 DKGY SIO 100 BECOMING LIGHTER GREY WITH DEPTH. MINOR SULPHIDE VEINS TOWARDS BASE OF UNIT D BWD004 189.92 190.15 YEWH XZO 95 XQO 5 PREDOMINATELY A VUGGY SULPHIDE VEIN WITH VERY MINOR QTZ. D BWD004 190.15 190.65 DKGY SSG 100 D BWD004 190.65 195.9 WHGY XQZ 85 SIC 15 PREDOMINANTLY QTZ-SULPHIDE (+/- CARBONATE) VEIN WITH INTERVALS OF CARBONACEOUS MUDSTONE AND OCCASIONALLY FINE SANDSTONE 1CM TO 20CM THICK. GRAPHITIC D BWD004 195.9 196.3 DKGY SSG 100 D BWD004 196.3 197.65 WHGY XQZ 90 SIO 5 3 SSG 5 3 """DOMINANTLY QTZ-SULPHIDE VEIN CONTAINING PYRITE" "ARRSENOPYRITE AND ?CHALCOPYRITE""" D BWD004 197.65 199.07 DKGY SSG 95 XQZ 5 MINOR VEINS 1CM THICK D BWD004 199.07 200.24 WHGY SSG 70 XQZ 30 SOME VEINS ENTIRELY SULPHIDES D BWD004 200.24 201 WHGY XQZ 100 SOME INCLUSIONS OF HOST ROCK D BWD004 201 201.2 DKGY SIO 70 XQZ 30 QTZ VEIN ALMOST ENTIRELY SULPHIDES D BWD004 201.2 202.08 DKGY SSG 70 XQZ 30 SULPHIDE RICH VEINS 1-8CM THICK D BWD004 202.08 202.56 DKGY SIO 75 XQZ 25 VEINING MORE COMMON WITH DEPTH D BWD004 202.56 203.96 WH XQZ 100 QTZ VEIN WITH VERY ABUNDANT SULPHIDES. IN PART COMPLETELY SULPHIDES UP TO 30CM THICK D BWD004 203.96 205.58 DKGY SSG 60 80 SIO 40 80 APPEARS TO BE A FINING UP SUCCESSION D BWD004 205.58 206.5 DKGY SIO 100 D BWD004 206.5 207.33 DKGY SIO 95 XQZ 5 PORPHYROBLASTS COMMON IMMEDIATELY SURROUNDING SULPHIDE VEIN AT 206.5M D BWD004 207.33 207.82 WH XQZ 100 MINOR REMNANTS OF HOST ROCK D BWD004 207.82 208.95 DKGY SIC 100 GRAPHITIC PARTICULARLY ON JOINT SURFACES D BWD004 208.95 209.33 DKGY XQZ 90 SIC 10 VERY MINOR SULPHIDES D BWD004 209.33 210.27 DKGY SIC 100 D BWD004 210.27 214.2 DKGY SSG 70 80 SIO 40 20 MOSTLY MIXING OF TWO LITHOLOGIES - TURBIDITIC? MUDSTONE BEDS 5-10CM D BWD004 214.2 214.84 GY SSG 100 LIGHTER IN COLOUR D BWD004 214.84 215.75 GYWH SSG 80 XQO 20 """SANDSTONE ALTERED BY QTZ VEINS" "VEINS ARE ERRATIC""" D BWD004 215.75 215.96 DKGY ZFG 100 SSG VERY BROKEN GROUND AND CLAY RICH D BWD004 215.96 216.7 WHGY XQZ 85 SSG 15 """ERRATIC QTZ-SULPHIDE VEINING 215.96-216.3M" "THEN COMPLETE QTZ-SULPHIDE VEIN 216.3-216.7M """ D BWD004 216.7 218 DKGY SSG 100 FEW ERRATIC QTZ VEINS IN UPPER PART OF UNIT. BECOMING LIGHTER GREY WITH DEPTH D BWD004 218 218.4 WHGY XQO 98 SSG 2 MINOR ORIGINAL ROCK REMAINS D BWD004 218.4 219.45 DKGY SIC 100 PORPHYROBLASTS COMMON D BWD004 219.45 220.92 GY SSG 100 D BWD004 220.92 221.62 DKGY SIO 100 D BWD004 221.62 228.1 GY SSG 100 D BWD004 228.1 230.55 GYWH SSG 90 XQO 10 20 SOLID QTZ VEINS 228.8-229.06M AND 230.36-230.55M D BWD004 230.55 233 DKGY SIO 50 60 SSG 50 60 D BWD004 233 233.27 WH XQO 100 VERY MINOR REMNANTS OF ORIGINAL ROCK D BWD004 233.27 234.65 DKGY SIC 100 D BWD004 234.65 235.92 GY SSG 100 D BWD004 235.92 236.45 GYWH SSG 65 XQZ 35 BROKEN GROUND. D BWD004 236.45 237.5 DKGY SIO 100 D BWD004 237.5 240.73 DKGY SSG 50 60 SIO 50 60 MULTIPLE MIXING AND GRADING BEDS D BWD004 240.73 241.56 GYWH SIO 80 XQZ 20 VEINS 4CM TO 12CM THICK D BWD004 241.56 247.5 DKGY SIO 60 50 SSG 40 50 INTERBEDDED AND INTERMINGLED SANDSTONE/MUDSTONE. BEDS FROM 5 TO 50CM THICK D BWD004 247.5 248.27 GY ZSZ 100 SIO VERY CLAY RICH AND FRACTURED SILT/MUDSTONE D BWD004 248.27 249.46 DKGY SIO 50 20 SSG 50 20 D BWD004 249.46 252.01 GY SSG 100 D BWD004 252.01 252.46 DKGY SIO 100 D BWD004 252.46 255.7 GY SSG 100 QTZ VEIN 253.57-253.72M D BWD004 255.7 258.6 DKGY SIO 50 40 SSG 50 40 INTERMINGLING AND INTERBEDDED D BWD004 258.6 259.9 GYWH SIO 65 XQO 35 BRECCIATED QTZ VEINING D BWD004 259.9 261.8 LTGY SSG 100 ALTERED FINE GRAINED SANDSTONE. LIGHTER IN COLOUR WITH ABUNDANT PORPHYROBLASTS D BWD004 261.8 263.28 GYGN SSG 100 """PALE GREY GREEN IN COLOUR" "ALTERED. STRONGER ALTERATION THAN ABOVE. ALTERATION DUE TO BELOW INTRUSION. GRAIN SIZE IS VERY FINE HOWEVER COULD BEDUE TO PARTIAL MELT ON CHILL MARGINS""" D BWD004 263.28 268.92 BK IMD 100 COARSE GRAINED DOLERITE. END OF HOLE. D BWD005 0 1.93 LTGY HMO 100 D BWD005 1.93 2.27 OR UOO 100 UNCONSOLIDATED ?SOIL OR HIGHLY WEATHERED ROCKS D BWD005 2.27 4.27 ORYE SSG SAPROLITIC SANDSTONE D BWD005 4.27 8.13 ORYE SSG 75 60 SIO 25 30 SAPROLITIC INTERBEDDED SANDSTONE AND SILTSTONE D BWD005 8.13 9.1 ORGY SSG 100 PREFERENTIALLY WEATHERED ALONG FRACTURES CREATING A 'BRECCIATED' APPEARANCE D BWD005 9.1 10.2 GYOR SIO 95 SSG 5 5 AS ABOVE HOWEVER LESS WEATHERED. SANDY INTERVAL HIGHLY WEATHERED AND FRIABLE. D BWD005 10.2 12.4 OR SSG 100 D BWD005 12.4 14 OR SSG 100 WEATHERED TO SAND AND CLAY. NO REMNANT ROCK TEXTURE REMAINS. D BWD005 14 20.33 OR SSG 75 60 SIO 25 40 SAPROLITIC INTERBEDDED SANDSTONE AND SILTSTONE. SILTSTONE IS LESS WEATHERED IN COMPARISON. SOME INTERVALS UP TO 20CM COMPLETELY WEATHERED TO CLAY ANND SAND. D BWD005 20.33 30.7 ORGY SSG 40 60 SIO 40 40 """MOTTLED ORANGE" GREY "PURPLE. 28.7-29.1M PREFERENTIALLY REDUCED WITH MINOR OXIDATION ON FRACTURE SURFACES WITHIN SANDSTONE. VERY RARE PRESERVED QTZ VEIN. BOCO""" D BWD005 30.7 31.95 GYOR SSG 100 OXIDATION ONLY ON FRACTURES D BWD005 31.95 32.45 OR SIO 60 XQO 40 RELICT VUGGY QTZ VEIN WITHIN MUD/SILTSTONE. BECOMING MORE REDUCED WITH DEPTH. D BWD005 32.45 40.93 GYOR SSG 85 100 SIO 15 10 SILT/MUDSTONE BEDS 5-20CM IN THICKNESS. BASE OF PARTIAL OXIDATION D BWD005 40.93 43.8 GYBE SSG 50 1 SIM 50 1 INTERBEDDED CENTIMETER SCALE GRADED BEDS. SOME INTERVALS UP TO 15CM APPEAR BLEACHED D BWD005 43.8 44.15 DKGY SIO 100 COMPLETELY ALTERED TO CLAY D BWD005 44.15 45 GYBE SSG 50 1 SIM 50 5 INTERBEDDED CENTIMETER SCALE GRADED BEDS. SOME INTERVALS UP TO 15CM APPEAR BLEACHED D BWD005 45 45.25 DKGY SIO 100 COMPLETELY ALTERED TO CLAY D BWD005 45.25 48.25 DKGY SIO 60 1 SSG 40 5 VERY BROKEN GROUND. MINOR BLEACHING D BWD005 48.25 48.55 BE SIO 100 VERY ALTERED AND FRIABLE. PREDOMINANTLY CLAYS D BWD005 48.55 49.7 DKGY SIO 80 25 SSG 20 5 D BWD005 49.7 52.16 DKGY SSG 100 MEDIUM GRAINED SANDSTONE D BWD005 52.16 57 DKGY SSG 60 80 SIO 40 15 INTERBEDDED SANDSTONE AND SILT/MUDSTONE BEDS BETWEEN 5-80CM THICK D BWD005 57 60 DKGY SSG 100 MEDIUM GRAINED SANDSTONE D BWD005 60 90.6 DKGY SSG 60 80 SIO 40 15 INTERBEDDED SANDSTONE AND SILT/MUDSTONE BEDS BETWEEN 5-80CM THICK D BWD005 90.6 96.2 GY SIO 70 5 SSG 30 3 LIGHT AND DARK GREY LAMINATED MUDSTONE AND SANDSTONE. APPEARS TO BE FINING UP HOLE. D BWD005 96.2 98 BEGY SSG 60 15 SIO 40 5 INTERBEDDED VERY FINE GRAINED SANDSTONE AND MUD/SILTSTONE. ALTERED/BLEACHED TO BEIGE COLOUR. ALTERATION PREDOMINANTLY IN COARSER GRAINED UNITS D BWD005 98 100.38 GYBE SIO 80 15 SSG 20 5 WEAKLY TO MODERATELY ALTERED TO BEIGE COLOUR. SILTSTONE AND VERY FINE GRAINED SANDSTONE. PORPHYROBLASTIC IN PART. D BWD005 100.38 101.65 BEGY SIO 80 15 SSG 20 5 """AS ABOVE HOWEVER HIGHLY ALTERED. VERY CLAY RICH" "WEAK ROCK.""" D BWD005 101.65 106.5 GYBE SIO 80 15 SSG 20 5 WEAKLY TO MODERATELY ALTERED TO BEIGE COLOUR. SILTSTONE AND VERY FINE GRAINED SANDSTONE. PORPHYROBLASTIC IN PART. D BWD005 106.5 108 DKGY SIO 75 15 SIM 25 3 INTERBEDDED SILTSTONE AND MUDSTONE D BWD005 108 109.5 BEGY SIO 75 10 SSG 25 5 INTERBEDDED VERY FINE GRAINED SANDSTONE AND MUD/SILTSTONE. WEAKLY ALTERED/BLEACHED TO BEIGE COLOUR. D BWD005 109.5 112.4 DKGY SSG 70 70 SIO 30 30 INTERBEDDED FINE GRAINED SANDSTONE AND SILTSTONE. THICKER BEDS THAN ABOVE AND BELOW D BWD005 112.4 115.1 DKGY SIO 75 5 SSG 25 2 FINELY LAMINATED SILTSTONE AND SANDSTONE D BWD005 115.1 120.74 DKGY SSG 75 80 SIO 25 40 INTERBEDDED FINE/MEDIUM GRAINED SANDSTONE AND SILTSTONE. THICKER BEDS THAN ABOVE AND BELOW. D BWD005 120.74 121.9 DKGY SIO 75 5 SSG 25 2 FINELY LAMINATED SILTSTONE.MUDSTONE AND VERY FINE GRAINED SANDSTONE D BWD005 121.9 124.06 DKGY SSG 100 FINE TO MEDIUM GRAINED SANDSTONE D BWD005 124.06 125.1 DKGY SSG 75 25 SIO 25 15 """INTERBEDDED FINE GRAINED SANDSTONE" "SILTSTONE AND MUDSTONE""" D BWD005 125.1 125.9 DKGY SSG 100 D BWD005 125.9 127.16 DKGY SSG 45 30 SIO 40 20 XQZ 15 10 PY GR """TWO QTZ-SULHIDE VEINS WITH ABUNDANT SULPHIDES" "DEEPER VEIN IS COMPLETELY PYRITE AND ALONG A FRACTURE""" D BWD005 127.16 130.57 DKGY SSG 100 D BWD005 130.57 134.6 DKGY SSG 80 100 SIM 20 25 SOME MUDSTONE LENSES WITHIN SANDSTONE UNITS D BWD005 134.6 138.1 DKGY SIO 80 80 SIM 20 5 D BWD005 138.1 140.52 DKGY SSG 100 POORLY SORTED SANDSTONE WITH COARSE QTZ GRAINS IN A FINE MATRIX - GREYWACKE D BWD005 140.52 142 DKGY SSG 100 FINE TO MEDIUM GRAINED SANDSTONE D BWD005 142 144.5 DKGY SSG 100 POORLY SORTED SANDSTONE WITH COARSE QTZ GRAINS IN A FINE MATRIX - GREYWACKE D BWD005 144.5 145.6 DKGY SSG 100 FINE TO MEDIUM GRAINED SANDSTONE D BWD005 145.6 150.3 DKGY SSG 60 70 SIO 20 30 SIM 20 30 FINING UPWARD SUCCESSIONS FROM SANDSTONE TO SILTSTONE TO MUDSTONE. SUCCESSIONS ~1.5m. THREE SUCCESSIONS NOTED IN THIS INTERVAL. D BWD005 150.3 151.5 DKGY SIO 50 30 SSG 50 30 AS ABOVE WITH SMALLER FINING UP SUCCESSIONS ~65CM D BWD005 151.5 154.9 DKGY SIO 100 VERY MINOR SANDSTONE INTERVALS <5CM D BWD005 154.9 167 DKGY SSG 65 80 SIO 35 45 INTERBEDDED SANDSTONE AND SILT/MUDSTONE D BWD005 167 171.18 DKGY SIO 80 80 SSG 20 20 D BWD005 171.18 176.9 DKGY SSG 70 80 SIO 30 30 GRADING UPWARDS? D BWD005 176.9 185.25 DKGY SIO 75 60 SSG 25 20 D BWD005 183.14 195.38 DKGY SIC 90 XQZ 10 PY APY VEINS MOSTLY 1CM THICK WITH ONE VERY SULPHIDE RICH VEIN 15CM D BWD005 185.25 187.1 DKGY SIO 100 GRAPHITIC IN PART D BWD005 187.1 190.95 WH XQZ 100 APY PY SOME PARTS OF THE QTZ VEIN ENTIRELY ARSENOPYRITE 15CM THICK. JOINTS PERPENDICULAR TO CORE AXIS VERY COMMON D BWD005 190.95 191.7 GYWH SIC 85 XQZ 15 APY PY D BWD005 191.7 192.43 DKGY SIC 100 GR MINOR QTZ-SULPHIDE VEINS D BWD005 192.43 195.38 DKGY SIO 100 MINOR QTZ-SULPHIDE VEINS D BWD005 195.38 196.74 DKGY SIO 100 D BWD005 196.74 197 WH XQZ 100 PY ~3% SULPHIDES D BWD005 197 200.85 DKGY SIC 100 GR PORPHROBLASTS COMMON. FEW QTZ VEINS WITH MINOR SULPHIDES D BWD005 200.85 201.9 GYGR SIO 92 XQZ 8 CL STRONGLY ALTERED MUD/SILTSTONE. CHLORITIC. LIGHT OLIVE GREEN/GREY IN COLOUR. D BWD005 201.9 203.58 GY SIO 100 PY ALTERED GREY TO OLIVE GREEN MUD/SILTSTONE. PORPHYROBLASTS COMMON WHICH ARE HALOED BY SULPHIDES. SOME PORPHYROBLASTS HAVE A LIGHT OLIVE GREEN HALO AROUND THEM D BWD005 203.58 203.9 GYGR XQZ 70 SIM 30 FRACTURED QTZ VEIN WITH ~4% SULPHIDES D BWD005 203.9 204.54 GYGR SIO 100 ALTERED GREY TO OLIVE GREEN MUD/SILTSTONE. PORPHYROBLASTS HAVE A LIGHT OLIVE GREEN HALO AROUND THEM D BWD005 204.54 205.66 DKGY SIO 100 FEW QTZ-SULPHIDE VEINS 1-3CM THICK. D BWD005 205.66 206 GYWH SIO 40 XQZ 30 XQZ 30 D BWD005 206 207.73 DKGY SIO 100 FEW QTZ AND QTZ-SULPHIDE VEINS D BWD005 207.73 227.77 DKGY SSG 50 60 SIO 25 30 SIM 25 30 FINING UP SEQUENCES FROM SANDSTONE TO SILTSTONE TO MUDSTONE. FEW QTZ-SULPHIDE VEINS D BWD005 227.77 233.1 DKGY SIO 50 SIO 50 INTERBEDDED AND INTERMINGLED SILTSTONE AND MUDSTONE D BWD005 233.1 233.95 DKGY SSG 100 FINE GRAINED D BWD005 233.95 235.1 DKGY SIO 100 GR D BWD005 235.1 236.8 GY SSG 60 45 SIO 40 30 XQO 10 """ERRATIC QTZ VEINLETS THROUGHOUT UNIT. POSSIBLY ALTERED" "SANDSTONE IS LIGHTER GREY""" D BWD005 236.8 238.15 DKGY SIC 90 XQZ 10 QTZ VEINS AS ABOVE WITH 4-8 CM ?LITHOLOGICAL QTZ-SULPHIDE VEINS D BWD005 238.15 238.9 GY SIO 95 XQO 5 """?STRUCTURALLY ALTERED" "CLAYEY IN PART WITH POSSIBLE FAULT GOUGES. """ D BWD005 238.9 249 GY SSG 100 FINE GRAINED SANDSTONE/GREYWACKE. FEW 2-3CM QTZ VEINS THROUGHOUT D BWD005 249 254.4 DKGY SIC 100 GR GRAPHITE MOSTLY ON FRACTURE SURFACES. PORPHYROBLASTS COMMON. D BWD005 254.4 255.5 WHGY XQZ 95 SIC 5 PY PREDOMINATLY SULPHIDE RICH QTZ VEIN WITH INCLUSIONS OF HOST ROCK D BWD005 255.5 256.08 GYWH XQZ 75 SIC 25 ZFO PY AS ABOVE WITH DECREASE OF QTZ AND INCREASED SULPHIDE AND HOST ROCK CONTENT. ZONE APPEARS HIGH STRAIN. D BWD005 256.08 256.45 WHGY XQZ 95 SIC 5 PY PREDOMINATLY SULPHIDE RICH QTZ VEIN WITH INCLUSIONS OF HOST ROCK D BWD005 256.45 256.9 DKGY SIO 80 XQZ 20 PY CL CHLORITIC AS BASE D BWD005 256.9 261 DKGY SIC 100 GR GRAPHITE MOSTLY ON FRACTURE SURFACES. PORPHYROBLASTS COMMON. D BWD005 261 261.77 DKGY SSG 80 5 SIM 20 1 INTEREBEDDED SANDSTONE AND SILTSTONE/MUDSTONE D BWD005 261.77 262.55 WHGY XQZ 100 PY SWIRLY' QTZ VEIN WITH ABUNDANT SULPHIDES. SWIRLS DEFINED BY DARK MILLIMETRIC LAYERS. D BWD005 262.55 263.35 GYWH SIO 85 XQZ 15 SULPHDIE RICH QT VEIN. HOST ROCK HAS AN OBVIOUS FABRIC D BWD005 263.35 267.15 DKGY SIO 70 25 SIC 30 10 GR GRAPHITE MOSTLY ON FRACTURE SURFACES. PORPHYROBLASTS COMMON. D BWD005 267.15 268.33 LTGY SSG 90 40 SIO 10 5 """LIGHT GREY GREEN IN COLOUR. ALTERED" "TEXTURE OF ROCK REMAINS""" D BWD005 268.33 275.37 DKGY SIO 60 25 SIM 40 15 INTERBEDDED AND INTERMINGLED SILTSTONE AND MUDSTONE D BWD005 275.37 276 GYGR SIO 100 ALTERED TO A LIGHT OLIVE GREEN - CHLORITIC? D BWD005 276 286.65 DKGY SIO 100 D BWD005 286.65 288 GRGY SIO 100 """ALTERED SILT/MUDSTONE" "FEW ERRATIC QTZ VEVINS AND VEINLETS. ALTERED BY DOLERITE INTRUSION BELOW.""" D BWD005 288 295.9 BK IMD 100 APHANITIC IN UPPER PART BECOMING COARSER WITH DEPTH. PINK ?FELDSPAR AREOLES FROM ~294M BECOMING LIGHTER PINK/ORANGE WITH DEPTH. END OF HOLE D BWD006 0 3.45 GY HFO 100 WASTEE PILE ROCKS D BWD006 3.45 9.45 OR SSG 100 SAPROLITIC WEATHERED SANDSTONE D BWD006 9.45 10.5 OR SSG 50 SIO 50 COMPLETELY WEATHERED AND FALLEN APART. CLAY WITH SAND. PROTOLITH PROBABLY INTERBEDDED SANDSTONE AND SILT/MUDSTONE D BWD006 10.5 12.45 OR SSG 100 D BWD006 12.45 17.3 ORBE SSG 100 COMPLETELY WEATHERED AND FALLEN APART. SAND AND CLAY. D BWD006 17.3 19 GYOR SSG 100 D BWD006 19 19.35 ORBR SSG 100 COMPLETELY WEATHERED AND FALLEN APART. SAND AND CLAY. D BWD006 19.35 22.85 ORBE SSG 100 D BWD006 22.85 27.85 ORBE SSG 50 20 SIO 50 20 SOME 10CM INTERVALS COMPLETELY WEATHERED TO CLAY AND SAND. D BWD006 27.85 32.2 GYOR SSG 65 50 SIO 35 30 D BWD006 32.2 35.6 GYOR SSG 100 SOME INTERVALS UP TO 10CM COMPLETELY WEATHERED TO CLAY AND SAND D BWD006 35.6 39.26 GYOR SSG 62 50 SIM 35 30 D BWD006 39.26 43.25 DKGY SSG 100 ORANGE DISCOLOURATION ON FRACTURES D BWD006 43.25 44.14 DKGY SIO 60 30 SSG 40 20 D BWD006 44.14 46.5 DKGY SSG 100 D BWD006 46.5 52.2 DKGY SSG 70 75 SIM 30 35 D BWD006 52.2 53.15 DKGY SSG 70 75 SIM 30 35 D BWD006 53.15 60 DKGY SSG 100 D BWD006 60 66.3 DKGY SSG 60 45 SIM 40 25 FLAME STRUCTURES - YOUNGING UP HOLE D BWD006 66.3 72.1 DKGY SSG 100 D BWD006 72.1 75.43 DKGY SSG 75 50 SIO 25 15 INTERBEDDED SANDSTONE AND MUD/SILTSTONE. D BWD006 75.43 84.1 DKGY SIO 55 7 SIM 45 6 D BWD006 84.1 122.87 DKGY SSG 60 35 SIO 40 20 INTERBEDD SANDSTONE AND MUD/SILTSTONE AT VARYING THICKNESS INTERVALS. SANDSTONE FROM 10-140CM AND SILTSTONE FROM 5 TO 60CM D BWD006 122.87 128.13 GYWH SIO 90 XQZ 10 PY """VEINS 3-8CM WIDE" ~0.5-3% SULPHIDES "APPEAR TO BE PARALLEL TO BEDDING WITH INCLUSIONS OF HOST ROCK WHICH IS SILT/MUDSTONE""" D BWD006 128.13 129 GYBE SIO 100 ALTERED SILTSTONE MORE YELLOWISH IN COLOUR D BWD006 129 131.13 DKGY SIO 50 5 SIO 50 5 NOT CLEAR BOUNDARIES BETWEEN SILTSTONE AND MUDSTONE D BWD006 131.13 131.65 GYWH SIO 95 XQZ 5 VEINS 2CM UP TO 10CM THICK ~1% SULPHIDES D BWD006 131.65 132.8 GYBN SIO 100 """ALTERED SILSTONE TO GREY-BROWN COLOUR" "TETURE OF ROCK REMAINS. MINOR VEIN WITH ERRATIC ?BRECCIATED QTZ""" D BWD006 132.8 137.28 DKGY SIO 50 5 SIM 50 5 NOT CLEAR BOUNDARIES BETWEEN SILTSTONE AND MUDSTONE D BWD006 137.28 138.4 GYWH SIO 70 XQZ 30 PY APY VEINS 10-15CM WIDE. D BWD006 138.4 142.55 DKGY SSG 75 60 SIO 25 20 D BWD006 142.55 146.55 DKGY SIO 65 50 SSG 35 30 D BWD006 146.55 167.28 DKGY SSG 65 80 SIO 35 40 BED WIDTH VARIES FOR BOTH UNITS FROM 5 CM TO 100CM D BWD006 167.28 167.6 WH XQZ 100 PY ~3% SULPHIDES D BWD006 167.6 172.22 DKGY SSG 60 70 SIM 40 50 D BWD006 172.22 179.4 DKGY SSG 100 D BWD006 179.4 185.15 GNGY SSG 100 CL ALTERED SANDSTONE - VERY CHLORITIC. BROKEN GROUND - ?HIGH STRAIN ZONE D BWD006 185.15 187.95 GYGN SSG 100 SLIGHTLY CHLORITIC BUT LESS THAN ABOVE D BWD006 187.95 194.58 GY SSG 70 75 SIO 30 35 D BWD006 194.58 195 GYGN SSG 100 CL ALTERED SANDSTONE TO OLIVE COLOUR. APPEARS BLEACHED ALONG SOME FRACTURES PERVASIVELY INTO ROCK D BWD006 195 198.34 DKGY SSG 60 80 SIO 40 50 STILL SLIGHTLY ALTERED AT TOP OF UNIT D BWD006 198.34 201.66 DKGY SSG 100 MEDIUM TO COARSE GRAINED SANDSTONE D BWD006 201.66 203 GYGN SSG 50 45 SIO 50 45 CL SLIGHTLY ALTERED D BWD006 203 208.78 GY SSG 100 """BRECCIATED AT 207-207.1M" "INCREASE OF QTZ VEINING ABOVE AND BELOW THIS ZONE""" D BWD006 208.78 209.1 DKGY SIO 100 D BWD006 209.1 211.66 GNGY SSG 100 CL """ALTERED TO LIGHT GREEN OLIVE COLOUR" "ABUNDANT CLOSED FRACTURES. CLAY RICH ZONE 211.1-211.35M.""" D BWD006 211.66 217.46 DKGY SSG 75 100 SIO 25 30 D BWD006 217.46 220.9 DKGY SSG 100 FINE TO MEDIUM GRAINED SANDSTONE D BWD006 220.9 232.65 DKGY SSG 60 80 SIO 40 50 SILT/MUDSTONE INTERVALS 10-50CM AND SANDDSTONE 10-80CM D BWD006 232.65 246.75 DKGY SIO 50 SIM 50 NOT INTERBEDDED D BWD006 246.75 256.23 GY SSG 100 MEDIUM TO COARSE SANDSTONE WITH VERY MINOR INTERVALS OF SILTSTONE D BWD006 256.23 256.76 DKGY SIO 100 D BWD006 256.76 258 GYGN SIO 50 SSG 50 BEDDING IS INTISTINGUISHABLE DUE TO ALTERATION. HIGHLY FRACTURED AND DISJOINTED (MOSTLY CLOSED) D BWD006 258 258.5 GYWH SSG 90 XQO 10 VERY MINOR SULPHIDES IN SOME VEINS. QTZ VEINS AND VEINLETS THROUGHOUT - CHAOTIC IN PATTERN SOME DISPLACED BY FRACTURES. D BWD006 258.5 260.5 DKGY SIO 100 D BWD006 260.5 266 GYPI SSG 100 PINK ?ALTERATION PERVASIVE BETWEEN GRAINS AS WELL AS FILLING CLOSED FRACTURES - BECOMING STRONGER WITH DEPTH. D BWD006 266 267.3 PIGY SSG 90 XQO 10 """VERY ALTERED SANDSTONE" "PREDOMINANTLY PINKORANGE IN COLOUR. QTZ VEINS COMMON AND BRECCIATED IN PART. SOME QTZ SHOWS GROWTH PATTERNS. FRACTURED GROUND AND VERY BROKEN 266.9-267.1M""" D BWD006 267.3 268.95 DKGY IMD 100 APHANITIC DOLERITE D BWD006 268.95 270.2 PIGY IMD 100 PERVASIVE PINK/ORANGE ALTERATION RUNNING SUB-PARALLEL TO CORE AXIS POSSIBLY FOLLOWING A FRACTURE AND ALTERING THE ROCK 2CM EITHER SIDE OF CLOSED FRACTURE. QTZ VEINING ALSO ASSOCIATED WITH SOME PARTS OF THE FRACTURE D BWD006 270.2 272.9 DKGY IMD 100 END OF HOLE D BWD007 0 2 DKGY HMO 100 WASTE ROCK D BWD007 2 2.5 ORBR SSG 70 XQO 30 SAPROLITIC SANDSTONE WITH REMNANT QTZ VEINS D BWD007 2.5 4.8 ORBR SSG 100 HIGHLY WEATHERED SAPROLITIC SANDSTONE - HIGH IN CLAYS D BWD007 4.8 8.1 OR SSG 85 70 SIO 15 10 SAPROLITIC MUD/SILTSTONE AND SANDSTONE. HIGHLY WEATHERED AND IN PART BRECCIATED DUE TO PREFERENTIAL WEATHERING ALONG FRACTURE ZONES AND MORE POROUS UNITS D BWD007 8.1 19 ORBE SSG 100 WEATHERED SAPROLITIC SANDSTONE D BWD007 19 30.65 ORGY SSG 75 15 SIO 25 5 SANDSTONE PREFERENTIALLY WEATHERED - DUE TO POROSITY? D BWD007 30.65 31.6 GYBE SIM 100 D BWD007 31.6 34.34 GY SSG 100 MEDIUM TO COARSE GRAINED SANDSTONE D BWD007 34.34 35 DKGY SIO 100 OCCASIONAL MUD BALLS 3CM IN SIZE D BWD007 35 36.7 DKGY SSG 100 MEDIUM TO COARSE GRAINED SANDSTONE D BWD007 36.7 37.15 GYOR SSG 100 D BWD007 37.15 44 DKGY SSG 100 MEDIUM TO COARSE GRAINED SANDSTONE D BWD007 44 46.67 DKGY SIO 80 70 SSG 20 20 ?TWO FINING UPWARDS SEQUENCE D BWD007 46.67 70 DKGY SSG 50 40 SIO 50 40 SANDSTONE BEDS 15-40CM THICK AND SILT/MUDSTONE BEDS 40CM D BWD007 70 72.4 DKGY SIM 100 "GRAPHITIC IN PART, PARTICULARLY NEAR STRUCTURES? " D BWD007 72.4 78.6 GYBE SIM 100 ZSZ "SOME INTERVALS HAVE BEEN ?BLEACHED TO A LIGHTER GREY/BEIGE COLOUR. HIGH DEGREE OF FRACTURING, POSSBLY IN SHEAR ZONE." D BWD007 78.6 79.65 BEGY SIM 100 ZSZ ZFG "HIGH CLAY CONTENT, POSSIBLE FAULT GOUGE 79.45-79.65M. VERY BROKEN." D BWD007 79.65 81.05 DKGY SIM 100 D BWD007 81.05 81.32 BE SSG 50 SIM 50 "GRADED BED, YOUNGING UPHOLE. ALTERED TO BEIGE COLOUR." D BWD007 81.32 89.8 GY SIO 50 20 SSG 50 20 SANDSTONE BEDS FROM 1-20CM AND MUD/SILTSTONE BEDS 1-20CM D BWD007 89.8 92.6 GY SSG 100 MEDIUM GRAINED SANDSTONE D BWD007 92.6 104.1 DKGY SSG 60 100 SIO 40 65 SANDSTONE MEDIUM TO COARSE GRAINED. MUD/SILTSTONE BEDS FROM 20-80CM IN THICKNESS. FINING UP HOLE. SEVERAL SUCCESSIONS. D BWD007 104.1 116.7 DKGY SIO 60 30 SSG 40 20 "MOSTLY SILSTONE/MUDSTONE, FINE GRAINED SANDSTONE, GRADINNG UP HOLE. SEVERAL SEDIMENTARY SUCCESSIONS." D BWD007 116.7 122.05 DKGY SSG 50 60 SIO 30 35 SIM 20 25 SANDSTONE VERY COARSE AT BASE OF SEDIMENTARY SEQUENCE. EACH FINING UPWARD SEQUENCE ~120CM. D BWD007 122.05 123.9 DKGY SIO 100 PORPHYROBLASTS VERY COMMON. D BWD007 123.9 150.7 DKGY SSG 50 40 SIO 50 40 MUD/SILTSTONE INTERVALS ARE BETWEEN 5-80 CM. SANDSTONE INTERVALS 30-70CM. SEVERAL SEDIMENTARY SEQUENCES FROM 80 - 180CM EACH. D BWD007 150.7 163.6 DKGY SIO 70 20 SIM 30 10 "PORPHYROBLASTIC, MINOR INTERVALS OF ?VERY FINE GRAINED SANDSTONE." D BWD007 163.6 168.7 DKGY SSG 40 40 SIO 60 70 SILT/MUDSTONE BEDS UP TO 100CM. D BWD007 168.7 174.44 DKGY SIM 70 10 SSG 30 4 FINELY INTERBEDDED SANDSTONE AND MUD/SILTSTONE. YOUNGING UPHOLE. PORPHYROBLASTIC IN FINER SEDIMENTS. D BWD007 174.44 175 WHGY XQZ 100 PY QTZ VEIN WITH ~80-90% SULPHIDES D BWD007 175 176 DKGY SSG 40 40 SIM 60 60 "ONE GRADED SEDIMENTARY SEQUENCE, YOUNGING UPHOLE" D BWD007 176 181 DKGY SIM 75 30 SIO 25 10 1-2CM QTZ-SULHIDE VEINS THROUGHOUT D BWD007 181 191.5 DKGY SSG 45 70 SIO 55 90 "SOME INTERVALS ARE FINELY LAMINATED MUDSTONE/SILTSTONE. YOUNGING UP HOLE, SEDIMENTARY SEQUENCES ~160CM" D BWD007 191.5 194.78 DKGY SIC 90 8 SIO 10 1 GR "VERY GRAPHITIC. MINOR SILTSTONE INTERBEDS (1CM), 10CM SEDIMENTARY SEQUENCE OF FINING UPWARDS." D BWD007 194.78 198.06 GYWH XQZ 65 SIC 35 PY SP "SULPHIDES WITHIN VEIN AND ALSO THROUGHOUT HOST ROCK WHICH IS VERY GRAPHITIC. ~10-15% SULPHIDES, PREDOMINANTLY PYRITE WITH MINOR SPHALERITE" D BWD007 198.06 199.67 WH XQZ 100 APY PY "~3% SULPHIDES, MOSTLY ARSENOPYRITE AND MINOR PYRITE" D BWD007 199.67 199.9 DKGY SIC 80 XQZ 20 APY VERY GRAPHITIC MUDSTONE WITH ABUNDANT ARSENOPYRITE WITHIN QTZ VEINS AND WITHIN HOST ROCK D BWD007 199.9 200.23 WHGY XQZ 100 APY PY MINOR INCLUSIONS OF GRAPHITIC MUDSTONE. 95% ARSENOPYRITE IN UPPER 9CM OF VEIN AND LOWER PART IS 5% SULPHIDES ARSENOPYRITE AND PYRITE. CARBONATE VEINING IN QTZ RICH PART OF VEIN D BWD007 200.23 201.85 DKGY SIC 85 110 SSG 15 20 GR PY MINOR QTZ-SULPHIDE VEINING. GRAPHITIC MUDSTONE IS PORPHYROBLASTIC. D BWD007 201.85 202.03 GYWH SIC XQZ APY PY "VERY GRAPHITIC, 7-10% SULPHIDES WITHIN QTZ VEINS" D BWD007 202.03 203.18 DKGY SIC 100 GR FRACTURE SURFACES ARE SHINY FROM GRAPHITE - NO SLICKEN SIDES ON THEM. D BWD007 203.18 205.3 DKGY SIC 75 10 SIO 25 3 XQZ 5 GR PY QTZ VEIN TOWARDS BASE OF UNIT WITH ~10% SULPHIDE CONTENT. INTERBEDDED SILSTONE AND GRAPHITIC MUDSTONE. D BWD007 205.3 209.25 DKGY SSG 80 55 SIC 20 15 PY GRADED BEDS. YOUNGING UPHOLE. QTZ-SULPHIDE VEINS COMMON. LESS GRAPHITE THAN ABOVE. D BWD007 209.25 213.76 GY SSG 100 GR GRAPHITE ON FRACTURE SURFACES. RANDOM QTZ AND CARBONATE VEINLETS COMMON. D BWD007 213.76 227.5 DKGY SSG 75 100 SIC 20 25 XQZ 5 "GRAPHITIC MUDSTONE 20-30CM INTERVALS, SANDSTONE 50-150CM, QTZ-SULPHIDE VEINING 5-20CM." D BWD007 227.5 228.54 DKGY SSG 100 D BWD007 228.54 228.8 WH XQZ 100 PY CARB "~10% SULPHIDES, COMMON CARBONATE" D BWD007 228.8 235.24 DKGY SSG 100 FEW MUD BALLS THROUGHOUT UNIT D BWD007 235.24 238.77 DKGY SSG 60 30 SIC 40 20 XQZ 5 PY COMMON QTZ-SULPHIDE VEINS AND VEINLETS. APPEARS STRUCTURALLY ALTERED DUE TO CHAOTIC NATURE OF VEINING AS WELL AS 'BRECCIATION/MIXING' OF MUDSTONE AND SANDSTONE D BWD007 238.77 240 DKGY SIC 95 XQZ 5 PY CARB D BWD007 240 240.5 WH XQZ 100 PY CARB 50-60% SULPHIDES D BWD007 240.5 245.4 DKGY SSG 80 100 SIC 20 25 ABUNDANT CARBONATE VEINLETS D BWD007 245.4 249.7 DKGY SSG 100 CARB "ABUNDANT CARBONATE VEINLETS, FILLING VOIDS IN PART. MINOR QTZ-SULPHIDE VEINS" D BWD007 249.7 251.15 DKGY SSG 85 100 SIO 15 15 CLAYEY/HIGHLY FRACATURED INTERVALS 5-10CM THROUGHOUT WITH CHAOTIC VEINS AND VEINLETS. D BWD007 251.15 251.45 GYWH ZSZ 80 ZFG 20 "?BRECCIATED QTZ WITH MINOR SULPHIDES, CLAYEY HIGHLY FRACTURED INTERVAL" D BWD007 251.45 252.8 WH XQZ 100 PY 25-30% SULPHIDES D BWD007 252.8 256.33 DKGY SIC 100 PY APY D BWD007 256.33 256.8 GY SSG 100 D BWD007 256.8 261.35 DKGY SIC 100 D BWD007 261.35 262.22 DKGY SSG 65 40 SIO 25 15 SIM 10 5 GRADED BEDS. YOUNGING UP HOLE D BWD007 262.22 262.4 WH XQZ 100 PY 50-60% SULPHIDES D BWD007 262.4 271.2 DKGY SSG 60 60 SIM 40 40 LITHOLOGIES INTERBEDDED AND MIXED D BWD007 271.2 285.2 DKGY SSG 95 200 SIO 5 5 Craig Mc takes over logging responibilities 35CM QZ VEIN @ 278.5 D BWD007 285.2 288.1 DKGY SSG 97 SIC 3 10 CARBONACEOUS MUDSTONE ON HANGING WALL OF 50CM QZ VEIN D BWD007 288.1 289.57 DKGY SIC 90 10 SSG 10 10 NOT CLASSIC CARB-GRAPHITIC MUDSTONE ROCK COLOUR BLACK-GREY D BWD007 289.57 296.55 DKGY SSG 95 SIO 5 10 D BWD007 296.55 309.7 BK SIC 90 20 SSG 10 APY PY GRADUAL GRADING FROM MUD TO VERY FINE SANDS. MAYBE NOT CLASSIC GRAPHITIC MUDSTONE BUT DOES HAVE A BLACK STREAK D BWD007 309.7 320.95 DKGY SSG 95 SIO 5 20 PY D BWD007 320.95 331.95 BK SIC 80 SSG 20 APY PY NOT CLASSIC IE SHINY BLACK GRAPHITE MUDSTONE D BWD007 331.95 345.1 GYBN IMD 100 CHILLED MARGIN EXTENDS METRE OR SO DOWNHOLE. SMALL PATCHES OF PINKING UP TO 5MM. Dolerite gets coarser with depth. UNKNOWN DISSEMINATED SILVER MINERAL PRESENT COULD BE FRESH MAGNETITE eoh @ 345.1-DRILLERS HAVE 345.18M D BWD008 0 4.8 HFO 100 4.1M LOSS SANDSTONE FRAGS PLUS QTZ FRAGS COULD BE ANYTHING D BWD008 4.8 21 GYBN SSG 100 200 MASSIVE LOOKING FINE/MED GRAINED SANDSTONE D BWD008 21 32 GYBN SSG 90 200 SSZ 10 1 INDIVIDUAL BEDS 1CM WIDE PACKAGES UP TO 40CM YOUNGING UPHOLE D BWD008 32 40.6 BNGY SSG 99 200 SSZ 1 3 MASSIVE FINE-MED SANDSTONE D BWD008 40.6 76.25 DKGY SSG 99 200 SSZ 1 5 DOMINATED BY FINE GRAINED SANDSTONE D BWD008 76.25 85 DKGY SIO 95 3 SSG 3 5 MUCH MORE SILTSTONE THAN MUDSTONE D BWD008 85 105 DKGY SSG 95 SIO 5 20 GENERALLY BETWEEN 2 TO 3M OF GREYWACKE BETWEEN UNITS OF FINE GRAINED SEDS ACTUAL BEDS MIGHT BE THINNER THAN 20CM D BWD008 105 126.6 DKGY SSG 75 SIO 25 15 MUDSTONE BEDS PROBABLY THINNER THAN 15CM D BWD008 126.6 130 DKGY SSG 60 SIO 40 5 SIMILAR TO ABOVE INTERVAL EXCEPT FOR CALCITE VEINING/STOCKWORK D BWD008 130 133.4 DKGY SSG 80 SIO 20 5 BLACK-GREY IN COLOUR. SEDS FINER GRAINED THAN TYPICAL GREYWACKE D BWD008 133.4 143.3 GYBE SIO 80 10 SSG 20 5 MEDIUM-LIGHT BROWN GREY. AGAIN GREYWACKE UNITS FINE GRAINED D BWD008 143.3 184.55 DKGY SSG 95 SIO 5 5 """TYPICAL"" GREYWACKE IE FINE GRAINED BUT NOT TOO FINE" D BWD008 184.55 185.6 DKGY SIO 80 SSG 20 VERY FINE GRAINED SEDS WITH GHOSTED PORHYOBLASTS TO 3MM D BWD008 185.6 192.7 DKGY SSG 95 SIO 5 5 STANDARD GREYWACKE D BWD008 192.7 193 BEBR SSG 100 SERICITE -CARBONATE ALTERED UNIT? D BWD008 193 218.3 DKGY SSG 85 SIO 15 STANDARD GREYWACKE WITH MUDSTONE/SILTSTONE BEDS INTERSPERSED THROUGHOUT. Hard to determine bed thickness as they grade into each other. D BWD008 218.3 232.5 DKGY SIO 98 3 SSG 2 VERY FINE GRAINED GREYWACKE D BWD008 232.5 238.1 DKGY SSG 98 SIO 2 STANDARD GREYWACKE. MAYBE SLIGHTLY FINE GRAINED D BWD008 238.1 247 DKGY SIO 98 SSG 2 MUDSTONE-SILTSTONE DOMINATED UNIT D BWD008 247 266.6 DKGY SIO 95 SSG 5 AS ABOVE EXCEPT THE MUDSTONE NOW HAS PORPHYOBLASTS-SPOTTING TO 3MM D BWD008 266.6 267.5 WH XQZ 100 QUARTZ-ARSENOPYRITE-PYRITE VEIN D BWD008 267.5 272.8 DKGY SIO 70 SIO 30 CONTINUATION OF MUDSTONE/SILTSTONE DOMINATED SEQUENCE D BWD008 272.8 298 DKGY SSG 80 SIO 20 5 DOMINATED BY STANDARD GREYWACKE MARKED INCREASED IN QZ VEIN VOLUME D BWD008 298 298.8 GY SSG 100 PREDOMINANTLY GREYWACKE WITH A SMALL BAND OF FINER GRAINED MATERIAL D BWD008 298.8 299 XQZ 100 QZ PY MASSIVE QZ VEIN WITH SOME PYRITE MINERALIATION PARALLEL TO THE CORE AXIS D BWD008 299 299.23 GY SSG 80 XQZ 20 QZ PY GREYWAKCE WITH W/ SUB-PARALELL QZ/SULPHIDE VEIN D BWD008 299.23 299.9 LTGY SIO 80 XQZ 20 QZ PY FINE GRAINED SILT/MUDSTONE ZONE WITH SOME SMALLER QZ/SULPHIDE VEINS D BWD008 299.9 300.17 XQZ 100 QZ PY MASSIVE QZ VEIN WITH MOSTLY PYRITE MINERALISTION AND SOME TRACES OF ARSENOPYRITE D BWD008 300.17 300.48 DKGY SIO 95 XQO 5 QZ APY SILTSTONE WITH QZ VEINLETS FORMING IN FOLIATION JOINTS WITH TRACES OF SPY D BWD008 300.48 300.85 XQZ 80 SSG 20 QZ PY MASSIVE QZ VEIN WITH A SMALL BAND OF GREYWACKE D BWD008 300.85 301.44 GY SIO 90 XQO 10 CARBONACEOUS SILTSTONE ZONE W/ GRAPHITIC FRACTURE SURFACES D BWD008 301.44 301.64 XQO 100 PY MASSIVE QZ VEIN D BWD008 301.64 302.64 LTGY SSG 100 APY LARGE GREYWACKE ZONE W/ DISSEMINATED APY FOUND ON FRACTURE SURFACES D BWD008 302.64 304.4 GY SIC 90 XQZ 10 GR APY CARBONACEOUS FINE GRAINED SECTION W/ A SMALL MINERALISED QZ VEIN ON THE CONTACT OF THE SSG AND SIC D BWD008 304.4 305.3 LTGY SSG 98 XQO 2 GREYWACKE ZONE WITH MINOR QZ VEINING D BWD008 305.3 306 DKGY XQO 90 SIC 10 QZ MASSIVE QZ VEIN WITH A LARGE PROPORTION OF GRAPHITIC MATERIAL INSIDE VEIN JOINTS AND EVIDENCE OF HIGH STRESS AND DEFORMATION D BWD008 306 306.9 DKGY SIC 100 D BWD008 306.9 307 XQO 100 QZ D BWD008 307 308.4 DKGY SSG 95 XQO 5 QZ PY SOME SULPHIDE MINERALISATION D BWD008 308.4 308.8 XQZ 100 QZ APY MASSIVE QZ VEIN WITH SOME STRONG ARSENOPYRITE MINERALISATION D BWD008 308.8 310.8 GY SSG 80 XQZ 20 QZ PY GREYWACKE SECTION WITH SOME MINOR QZ/SULPHIDE VEINS D BWD008 310.8 311 GY SIO 100 SMALL FINE GRAINED SILTSTONE BEDDING D BWD008 311 316.54 GY SSG 98 XQO 2 QZ THICK GREYQACKE SECTION COMPRISED OF MEDIUM GRAINED MATRIX D BWD008 316.54 317.3 GY SIO 100 SILTSTONE LAYER W/ SOME MINOR QZ VEINING D BWD008 317.3 319.55 GY SSG 100 COARSER GRAINED SEDIMENTARY LAYER D BWD008 319.55 324 GY SIO 90 SSG 10 D BWD008 324 324.2 GY XQZ 100 APY QZ SMALL QZ VEIN WITH SOME EVIDENCE OF ARSENOPYRITE MINERALISATION WITH DISSEMINATED SULPHIDE PORPHYRYOBLASTS D BWD008 324.2 327.65 GY SIO 90 XQO 10 APY QZ SILTSTONE/SEDIMENTARY ZONE WITH DISSEMINATED SULPHIDE PORPHYRYOBLASTS D BWD008 327.65 336.8 GY SIO 90 XQZ 10 QZ PY FINER GRAINED ZONE WITH EVIDENCE OF INCREASED STRUCTURAL DEFORMATION RESULTING IN EXCESSIVE BROKEN UP CORE AND FRAGMENTS FROM A HIGH STRESS ENVIRONMENT ON THE CONTACT OF A SHEAR ZONE D BWD008 336.8 342.7 ZSZ 80 XQO 20 QZ CL SHEAR ZONE W/ HIGHLY FRAGMENTED CORE W/ BROEKN UP QZ VEINS CLSER TO THE FAULT ZONE. EVIDENCE OF BRECCIATED FRAGMENTS ON THE CONTACT OF THE FINE GRAINED SEDIMENTARY ROCK AND THE QZ VEIN D BWD008 342.7 344.3 GY ZFZ 100 HIGH STRESS FAULT ZONE W/ EVIDENCE OF CLAY MINERALS AND A RUBBLEZONE W/ GOUGING THROUGHOUT MOST OF THE FAULT D BWD008 344.3 344.8 GY ZSZ 60 XQZ 40 QZ PY SHEAR ZONE ON THE CONTACT OF THE FAULT ZONE AND THE FINE GRAINED SEDIMENTARY STRATIGRAPHY D BWD008 344.8 345.65 GY SIO 90 XQO 5 XZO 5 1.5 QZ PY CONTACT BETWEEN THE SEDIMENTARY STRATIGRAPHY AND THE SHEAR ZONE CONTAINS A FEW QZ VEINS WITH SOME SULPHIDE VEINING AS WELL D BWD008 345.65 346.07 XQZ 100 QZ PY MASSIVE QZ VEIN WITH SOME PYRITIC MINERALISATION D BWD008 346.07 347.9 GY SIO 100 XQO QZ D BWD008 347.9 355.5 LTGY SSG 90 XQZ 5 SIO 5 QZ PY COARSER GRAINED SEDIMENTARY ROCK (GREYWACKE) W/ SOME SMALL QZ-SULPHIDE VEINING D BWD008 355.5 357.57 GY SIO 95 XQZ 5 QZ PY FINER GRAINED SILTSTONE/MUDSTONE WITH SOME QZ-SULPHIDE VEINING D BWD008 357.57 358.1 LTGY SSG 99 XQZ 1 QZ PY GREYWACKE SECTION D BWD008 358.1 359 GY SIO 85 XQZ 15 QZ PY D BWD008 359 361.57 GY SSG 80 XQZ 20 QZ PY GREYWACKE SECTION D BWD008 361.57 366.4 GY SIO 70 XQZ 20 SSG 10 QZ PY FINE GRAINED SEDIMENTARY ZONE WITH QZ-SULPHIDE VEINS AND SOME INTERBEDDED GREYWACKE D BWD008 366.4 371.7 DKGY SIO 70 XQZ 20 SSG 10 22 QZ APY SILTSTONE ZONE WITH A SMALL BAND OF COARSER GRAINED GREYWACKE. APY SUBHEDRAL FRAGMENTS AS WELL AS DS PY. D BWD008 371.7 372.75 XQZ 100 QZ APY MASSIVE QZ VEIN WITH APY SUBHEDRAL FRAGMENTS AND COATINGS OF PY. D BWD008 372.75 377.4 GY SIO 95 XZO 2.5 XQZ 2.5 QZ PY D BWD008 377.4 378.33 DKGY SIO 50 XZO 50 PY HALF SILTSTONE ZONE AND HALF SULPHIDE VEIN PREDOMINANTLY CONSISTING OF PY. D BWD008 378.33 379 DKGY SSG 100 PY DISSEMINATED AND PATCHES OF SULPHIDES INSIDE GREYWACKE D BWD008 379 380.8 GY SIO 90 XQZ 10 QZ PY D BWD008 380.8 382.36 LTGY XQO 50 SIO 50 QZ COMPLEX QZ VEINING THROUGHOUT A FINE GRAIN SEDIMENTARY MATRIX W/ BRECCIATED QZ VEINS AND OBVIOUS CLEAVAGES AND JOINTING WITHIN THE VEINS D BWD008 382.36 389.77 LTGY SIO 80 XQZ 10 SSG 10 QZ PY LIGHT GREY SILTSTONE SECTION WITH A BAND OF GREYWACKE AND SEVERAL SMALL QZ-SULPHIDE VEINS W/ DS SULPHIDES IN THE SS AND QZ VEINS AS WELL AS PB WITHIN THE SEDIMENTARY MATRIX D BWD008 389.77 390.9 XQZ 98 SIO 2 QZ APY MASSIVE QZ VEIN WITH CONSISTENT STRINGERS AND PATCHES OF SILTSTONE INSIDE THE QZ VEIN D BWD008 390.9 391.46 GY XZO 60 SIO 40 PY MASSIVE SULPHIDE VEINS D BWD008 391.46 392.66 GY SIO 100 D BWD008 392.66 393.45 LTGY SSG 90 XZO 10 TICK BANDED SULPHIDE VEIN IN AMONGT A GREYWACKE D BWD008 393.45 394.42 GY SIO 90 XZO 5 XQO 5 QZ PY D BWD008 394.42 397.8 LTGY SSG 95 XQO 5 D BWD008 397.8 399.88 GY SIO 80 XQO 20 QZ PY D BWD008 399.88 400.28 XQO 100 MASSIVE QZ VEIN D BWD008 400.28 402 GY SIC 40 SIO 30 XQO 30 QZ GR CARBONACEOUS ZONE WITH QZ VEINING AND COARSER GRAINED SECTIONS D BWD008 402 467.33 DKGY IMD 100 DOLERITE DYKE D BWD008 467.33 469.7 GY SIO 100 QZ SILTSTONE CONTACT W/ MINUTE QZ VEINLETS D BWD008 469.7 470.4 XQO 80 SIO 20 QZ MASSIVE QZ VEIN WITH CARBONACEOUS MATERIAL ON THE CONTACT OF THE QZ AND SILTSTONE BEDDING D BWD008 470.4 472.4 DKGY SIC 90 XQO 10 CARBONACEOUS MUDSTONE WITH SOME QZ VEINING D BWD008 472.4 482 GY SIO 90 XQZ 10 ARSENOPYRITE MINERALISATION APPROX @ 481M IN DEPTH WITHIN A QZ VEIN. QZ VEIN IS OF LIGHTER MORE TRANSLUCENT ROCK TYPE COMPARED TO THE QZ VEIN INSIDE THE MUDSTONE ZONE. D BWD008 482 487.8 LTGY SSG 100 QZ COARSE GRAIN SEDIMENTARY ROCK LIGHTER IN COLOUR AND MORE CONSISTENT IN FRACTURE TYPE AND ORIENTATION D BWD008 487.8 496.7 GY SIO 95 XQZ 5 APY PY SMALL QZ VEINS WITH PYRITE AND ARSENOPYRITE MINERALISATION. ARSENOPYRITE IS MORE SYNONYMOUS WITH VEINS THAT CONTAIN VOIDS OR CAVITIES D BWD008 496.7 501.6 LTGY SSG 50 SIO 30 XQZ 20 APY QZ STRONG SULPHIDE MINERALISATION WITHIN A QZ VEIN IN THIS PREDOMINANTLY GREYWACKE ZONE D BWD008 501.6 504.25 GY SIO 90 XQO 10 QZ APY SOME APY SUBHEDRAL FRAGMENTS FOUND WITHIN THE SILTSTONE MATRIX D BWD008 504.25 514.26 GY SIO 50 SSG 50 QZ APY D BWD008 514.26 516.62 GY SSG 95 XQO 5 QZ APY D BWD008 516.62 523 GY SIO 45 SSG 45 XQZ 10 QZ APY SULPHIDE-QZ VEIN IS LOOKS HIGHLY SHEARED WITH TRACES OF CLAY MINERALS BINDING THE QZ FRAGMENTS TOGETHER @522.6M IN DEPTH. D BWD008 523 555.3 GY SIO 90 XQZ 10 QZ APY EXTENSIVE SILTSTONE LAYER WITH SPARSE QZ VEINS WITH MINOR SULPHIDE MINERALISATION D BWD008 555.3 566 GY SIO 80 SSG 10 XQO 10 QZ PY D BWD008 566 576.8 GY SSG 100 EOH @576.8m D BWD009 0 7.2 RD UOO 100 TOPSOIL UNCONSOLIDATED MATERIAL D BWD009 7.2 27 BN RRR 100 WEATHERED ROCK/SANDSTONE D BWD009 27 37.5 BN RRR 60 RRSU 40 D BWD009 37.5 55 LTGY SSG 90 SIO 210 QZ FE LIGHT GY GREYWACKE ALTERNATING BETWEEN A FINER GRAINED MATRIX AND SOME COARSE GRAINS W/ INTERBEDDED SILTSTONE LAYERS D BWD009 55 68.2 LTGY SSG 50 SIO 50 QZ D BWD009 68.2 70.3 GY SIO 100 D BWD009 70.3 99.67 GY SSG 50 SIO 50 QZ D BWD009 99.67 100.05 XQZ 100 PY QZ 36CM THICK QZ VEIN WITH CHLORITE ALTERATIO AND BOXWORK. CLUSTERS OF ARSENOPYRITE AND PYRITE MINERALISATION SITUATED CLOSE TO THE CONTACT OF THE QZ AND SEDIMENTARY ROCK ON BOTH THE UPPER AND LOWER SIDE OF THE VEIN D BWD009 100.05 105.45 GY SSG 95 SIO 5 D BWD009 105.45 110.68 GY SIO 95 SSG 5 19 CAL PY SMALL 19CM BAND OF GREYWACKE INTERBEDDED IN THE SILTSTONE D BWD009 110.68 111.42 GY SIO 70 XQZ 30 QZ PY QZ VEIN IS RUNNING PARALLEL TO THE CORE AXIS AND CONTAINS PATCHES OF APY-PY-CHLORITE D BWD009 111.42 115.46 GY SIO 98 XZO 2 APY QZ SILTSTONE UNIT WITH SOME SMALL SULPHIDE VEINS RUNNING THROUGH IT. SOME BROKEN UP FRAGMENTS SUGGESTING THAT THERE WAS SOME HIGH STRESS DEFORMATION -SHEARING D BWD009 115.46 118.09 GY SSG 95 SIO 5 6 CAL PY D BWD009 118.09 118.8 GY SIO 98 XQZ 2 QZ PY D BWD009 118.8 119.04 GY SSG 100 D BWD009 119.04 122.15 GY SIO 50 SSG 50 PY QZ SMALL SPECKS OF PY FOUND ON THE FRACTURE SURFACE OF THE FINER SEDIMENTARY ROCKS D BWD009 122.15 132.23 GY SSG 85 SIO 10 XQO 5 QZ D BWD009 132.23 134.16 GY SSG 100 D BWD009 134.16 138.7 GY SIO 50 SSG 50 APY QZ D BWD009 138.7 139.3 GY SIM 98 XQO 2 QZ D BWD009 139.3 145.7 GY SIO 50 SSG 50 QZ APY SMALL QZ VEINLETS THROUGH CONTACTS OF SSG AND SIO WITH SOME CONTAINING SULPHIDES D BWD009 145.7 145.88 GY SIO 100 SILICA ALTERATION IN A SMALL SILTSTONE ZONE WITH EXTENSIVE SMALL QZ VEINLETS SITUATED ON THE HIGHER SIDE OF THE SILTSTONE BAND D BWD009 145.88 147.45 GY SIM 100 REALLY FINE GRAINED SEDIMENTARY MATRIX AND BROKEN UP IN SOME SECTIONS EXPOSING CALCITE AND APY NEEDLES ON THE FRACTURE SURFACES D BWD009 147.45 154.72 GY SIO 50 SSG 50 QZ CAL D BWD009 154.72 158.55 GY SIO 45 SSG 45 XQZ 10 QZ PY D BWD009 158.55 159 GY SIO 98 XQO 2 SILICIFICATION OF SILTSTONE WITH TRACES OF K-FELDSPAR ALTERATION D BWD009 159 171.98 GY SIO 90 XQO 5 XQZ 5 PY QZ SLIGHTLY SILICIFIED SILTSTONE UNIT WITH INCREASED QZ VEINING D BWD009 171.98 181.7 DKGY SIO 60 20 SSG 40 BEDS VARY IN THICKNESS FROM CM'S TO 10'S CM D BWD009 181.7 188.4 DKGY SIO 90 SSG 10 D BWD009 188.4 204.7 DKGY SSG 90 SIO 10 DOMINATED BY FINE GRAINED GREYWACKE D BWD009 204.7 207.9 DKGY SIO 98 SSG 2 WHAT GREYWACKE IS THERE IS VERY FINE GRAINED D BWD009 207.9 233.6 DKGY SSG 95 SIO 5 5 DOMINATED BY FINE GRAINED GREYWACKE D BWD009 233.6 240.9 DKGY SIO 80 20 SSG 20 POSSIBLY THICK BEDS OF MUDSTONE/SILTSTONE. GREYWACKE IS FINE GRAINED D BWD009 240.9 250.9 DKGY SSG 90 SIO 10 10 FINE GRAINED GREYWACKE D BWD009 250.9 265.5 DKGY SIO 95 SSG 5 D BWD009 265.5 270.4 DKGY SSG 95 SIO 5 FINE GRAINED GREYWACKE D BWD009 270.4 275.9 DKGY SIO 98 5 SSG PORPHYROBLASTS PRESENT TO 2-3MM. SOME LAMINATED BEDS D BWD009 275.9 276.85 DKGY SSG 100 D BWD009 276.85 278.5 DKGY SIO 100 ABUNDANT PORPHYROBLASTS. FOLIATED? D BWD009 278.5 279.45 DKGY SSG 100 D BWD009 279.45 284.8 DKGY SIO 100 SELECTED BEDS WITH CARB?-SERICITE? ALTERATION BUFF BROWN IN COLOUR. ONLY SELECTED BEDS UP TO 30CM WIDE IN PLACES D BWD009 284.8 297.1 DKGY SIO 98 4 SSG 2 MORE MUD/SILT DOMINATED BUT WITHOUT THE COLOURED ALTERATION. PATCH OF BROWN MINERAL AT 288.2. SOME MINOR AREAS CONTAINING SMALL PORPHYROBLASTS (<1MM) D BWD009 297.1 312.7 DKGY SIO 80 SSG 20 AS ABOVE. INCREASE IN PORPHYROBLAST ABUNDANCES. VERY SUBTLE CHANGES BETWEEN SAND AND MUD BEDS-MAYBE DUE TO COLOUR AND PERHAPS ALTERATION? D BWD009 312.7 315 GYBN SIO 80 SSG 20 WEAK PERVASSIVE SERICITE?-CARB? ALTERATION COLOURING ROCK???? D BWD009 315 317 DKGY SSG 80 SIO 20 RETURN TO NORMAL BUT NOT FOR LONG… D BWD009 317 318.8 GYBN SIO 100 SE-CB ALT? D BWD009 318.8 326.9 DKGY SIO 90 SSG 10 MOSTLY FINE GRAINED D BWD009 326.9 331.3 GYBN SIO 100 SILTSTONE D BWD009 331.3 335.3 DKGY SIO 100 SILT + MUD D BWD009 335.3 336.4 GY XQZ 100 QZ-CL-CAL-PY VEIN D BWD009 336.4 345.9 DKGY SIO 90 5 SSG 19 D BWD009 345.9 363.45 DKGY SSG 95 SIO 5 10 """STANDARD"" GREYWACKE-SILT/MUD SEQUENCE" D BWD009 363.45 365.2 DKGY SIO 100 5 RUBBLY CORE BETWEEN 364.2-365.2 D BWD009 365.2 379 DKGY SSG FINE GRAINED GREYWACKE D BWD009 379 381.5 DKGY SSG 80 SIO 20 D BWD009 381.5 382.8 GYBN MHO 100 HANGING WALL CONTACT ZONE TO DOLERITE D BWD009 382.8 386.6 BNGY IMD 100 CHILLED ZONE FINE GRAINED D BWD009 386.6 432 GY IMD 100 MED-COARSE GR DOLERITE D BWD009 432 433.7 GY IMD 100 FINE GRAINED CHILLED DOLERITE MARGIN D BWD009 433.7 434.98 DKGY SSG 100 FINE GRAINED GREYWACKE D BWD009 434.98 446 BK SIO 90 1 SSG 10 SOME MASSIVE SECTIONS. WHERE THERE IS BEDDING IT IS 1CM BANDS D BWD009 446 446.7 BK SSG 100 HANGING WALL OF A BIG STRUCTURE. PORPHYROBLASTS? D BWD009 446.7 447.15 BK ZFC 100 MAJOR STRUCTURE. Mostly INTACT D BWD009 447.15 459.9 BK SIC 98 1 SSG 2 XQZ MAYBE NOT CLASSIC GRAPHITIC MUDS ALTHOUGH GRAPHITE ON FRACTURE SURFACES WITH QZ ASP VEINS D BWD009 459.9 462.65 BRBE OOO 100 SE CARB MAYBE CARBONATE-SERICITE ALT. LOOKS LIKE A ALT'D SSG BUT BEAN THINKS IT MIGHT BE VOLCANIC. D BWD009 462.65 468.2 BEBR SSG 100 SE CARB VERY SIMILAR ALT TO ABOVE INTERVAL BUT WITH POSS GHOSTED BEDDING??? D BWD009 468.2 470.55 DKGY SSG 80 SIO 20 VERY FINE GRAINED GREYWACKE D BWD009 470.55 472.35 BK SIC 100 0.5 XQZ GHOSTED BEDS???? QZ-ASP VEINS D BWD009 472.35 476.4 BK SIC 100 APY PORPHYROBLASTIC. OCMMON 5-40MM QTZ VEINS WITH MINOR SULPHIDES D BWD009 476.4 477.4 BK SIC 100 ZSZ 85 HIGHLY FRACTURED WITH RUBBLE ZONES. QUARTZ VEINING. D BWD009 477.4 478.45 BK SIC 100 PORPHROBLASTIC. MINOR FINE GRAINED SANDSTONE BEDS D BWD009 478.45 488.2 DKGY SSG 80 200 SIO 20 50 GRADED BEDS FROM COARSE SANDSTONE TO MUDSTONE. YOUNGING UP HOLE. SEQUENCE +2M D BWD009 488.2 513.68 DKGY SIO 60 160 SSG 40 120 BEDDING PARALLEL TO CORE AXIS D BWD009 513.68 517.7 DKGY SIO 40 50 SSG 40 50 XQZ 20 PY APY POSSIBLY GALENA? VEINS 20-200MM THICK D BWD009 517.7 522.3 DKGY SSG 70 200 SIO 30 80 BEDDING SUBPARALLEL TO CORE AXIS D BWD009 522.3 530.15 DKGY SIO 50 SSG 50 CARB CARBONATE VEINLETS THROUGHOUT. BEDDING PARALLEL TO CORE AXIS THEREFORE HARD TO DETERMINE BED THICKNESS D BWD009 530.15 533.75 DKGY SSG 100 MINOR MUD/SILTSTONE D BWD009 533.75 539.84 DKGY SSG 85 160 SIO 15 20 XQZ PY APY "QZ-SULPHIDE VEINS 30-100MM WIDE, ABUNDANT SULPHIDES WITHIN" D BWD009 539.84 543.1 DKGY SSG 65 70 SIO 35 40 GRADED BEDS YOUNGING UPHOLE D BWD010 118.57 GY SSG 100 CARB D BWD010 0 4.1 BG UOO 100 QZ PY Waste material is overlying the alluvial clays and gravels for the first few meters as the drillhole sits on top of the old mineralised waste dump on the ROM pad D BWD010 4.1 5.1 RD UOO 100 HEM Sopsoil clay zonr consisting of Fe oxides D BWD010 5.1 5.23 BN RRY 100 CLAY D BWD010 5.23 5.8 BN SSG 80 RRY 20 CLAY Clay and sand zone with leached clay minerals D BWD010 5.8 5.9 BG SSG 100 Sandstone to clay younging D BWD010 5.9 6.06 BN UGO 100 CLAY Unconsolidated rubble/gravel zone D BWD010 6.06 27.7 BN UCO 70 SSO 30 CLAY Deep sedimentary zone consisting of msotly clay and with interbedded sandstone zones D BWD010 27.7 30 GY SSG 80 Greywacke zone with alternating finer and coarser grain clasts D BWD010 30 31.2 GY SSG 50 12 SSG 50 12 D BWD010 31.2 31.56 GY SSG 80 13 UCO 20 Greywacke zone with interbedded clay minerals D BWD010 31.56 31.74 GY SSG D BWD010 31.74 32.9 GY SSG 60 15 SSG 40 15 D BWD010 32.9 33.64 GY SSG 100 D BWD010 33.64 34.58 GY SSG 90 UCO 10 CLAY D BWD010 34.58 36.67 GY SSG 70 42 SSO 30 28 D BWD010 36.67 37.17 GY SSG 100 D BWD010 37.17 38.2 GY SSG 100 D BWD010 38.2 44 D BWD010 44 45 BL SYC 100 Fine grained carbonaceous mudstone D BWD010 45 55.4 GY SSG 50 SSG 50 SERI PY Large greywacke/siltstone unit. Traces of sericite forming on the fracture surfaces at 47.50. Crystalline veinlets of Pyrite also found on a joint surface inside a siltstone zone at 52.15m. D BWD010 55.4 72.02 GY SSG 100 SIC 15 PY SI Disseminated PY and silicified patches on some of the fracture zones as well as PY coating on fractures D BWD010 72.02 72.2 W ZVQ 100 Massive quartz/sulphide vein approximately 18cm thick. Carbonate vein within the secondary vein sitting on the bottom side of the vein D BWD010 72.02 81 BL SIC 100 GR SI Carbonaceous graphitic zone with calcium carbonate veining and pyrite veinlets D BWD010 81 85.3 GY SSG 60 40 SIC 38 20 XQZ 2 1 D BWD010 85.3 94.9 GY SSG 100 PY QZ Highly deformed and fractured zone from 81.8m to 83.5m in depth due to rock type (more carbonaceous/graphitic matrix) and high strain D BWD010 94.9 96.4 GY SSG 100 Coarse grained graywacke/sandstone D BWD010 96.4 97.29 GY SSG 100 D BWD010 97.29 97.73 GY SIC 70 12 SSO 30 4 CARB PY Finer grained more carbonaceous zone with disseminated sulphides found on the fractures as well as a few carbonate veinlets D BWD010 97.73 100.65 GY SSG 100 CARB GR Graphitic planar fracture surfaces with calcium carbonate fracture filling and specks of sulphides D BWD010 100.65 101.54 GY SSG 95 57 XQZ 5 1 QZ CARB Two qtz veins amongst a siltstone matrix with traces of sulphides forming on the fracture surfaces D BWD010 101.54 101.9 GY SSG 100 PY D BWD010 101.9 104.1 GY SSG 100 Coarse grained greywacke D BWD010 104.1 104.95 GY SSG 95 35 XQC 5 0.5 CARB PY Small carbonate veinlets with disseminated sulphides amongst the matrix around the veinlets D BWD010 104.95 105.9 GY SSG 100 45 D BWD010 105.9 106.15 GY SSG 95 XQZ 5 0.8 PY QZ Small fine grained matrix unit with two qtz veins running perpendicular to the core axis with specks of sulphides in the vein D BWD010 106.15 107.6 GY SSG 100 D BWD010 107.6 108.14 GY SSG 90 34 XQZ 10 2.5 D BWD010 108.14 108.42 GY SSG 100 D BWD010 108.42 109.17 GY SSG 100 D BWD010 109.17 109.43 GY SSG 80 12 XQZ 20 1 Qtz vein with some sulphides in the form of specks inside the vein D BWD010 109.43 109.87 GY SSG 100 D BWD010 109.87 110.13 GY SSG 75 15 XQZ 25 1.5 D BWD010 110.13 111.2 GY SSG 100 D BWD010 111.2 113.82 GY SSG 70 70 SSO 30 5 Predominantly a greywacke but there is some interbedded siltstone matrix D BWD010 113.82 116.1 GY SSG 100 QZ D BWD010 116.1 GY SSG 100 D BWD010 118.57 119 GY SSG 90 XCO 10 CARB Small carbonate veinlets crosscutting running both parallel to the core axis and perpendicular D BWD010 119 119.2 GY SSG 60 14 XQZ 40 6 QZ PY Qtz vein has been crosscutted by post fault leaving an oblique slip of a sinistral nature D BWD010 119.2 119.73 GY SSG 100 D BWD010 119.73 119.85 GY SSG 80 XQZ 20 QZ Small qtz vein alteration D BWD010 119.85 120.6 GY SSG 100 PY D BWD010 120.6 120.8 GY SSG 95 XCO 5 CARB D BWD010 120.8 120.9 GY SSG 90 XQZ 10 PY QZ D BWD010 120.9 121.68 GY SSG 100 D BWD010 121.68 121.89 GY SSG 80 XQO 20 QZ Zone of high stress with some qtz veins running through with sulphides present in the vein and on the fracture surfaces D BWD010 121.89 121.95 WH XQZ 100 QZ PY Massive qtz vein with patches of sulphide mineralisation D BWD010 121.95 122.3 GY SSG 100 D BWD010 122.3 123.25 WH ZFZ 100 CARB GR High stress fault zone with carbonate veinlets and graphitic carbonaceous material on and around fracture surfaces D BWD010 123.25 123.7 GY SSG 100 D BWD010 123.7 123.9 GY SSG 90 XQZ 10 PY QZ D BWD010 123.9 124 WH XQZ 100 QZ PY Massive qtz vein with both pyrite and arsenopyrite mineralisation making up 20% of vein compositon D BWD010 124 124.36 GY SSG 100 CARB D BWD010 124.35 124.5 GY SSG 70 XQZ 30 D BWD010 124.5 124.94 GY SSG 100 D BWD010 124.94 125.17 BL SIC 100 GR PY Carbonaceous zone with traces of graphite and sulphides in the form of blebs D BWD010 125.17 126.79 GY SSG 100 PY CARB Small veinlets of carbonates amongst the matrix as well as sulphides coating the fracture surfaces D BWD010 126.79 126.85 WH XQZ 100 QZ PY Massive qtz/sulphide vein D BWD010 126.85 127.14 BL SIC 95 XZO 5 GR PY Carbonaceous zone with veinelts of sulphides D BWD010 127.14 127.54 GY SSG 90 XCO 5 XZO 5 APY CARB Veinlets of carboantes and veinlets of sulphides running along the foliation bedding with the apex alongside the orientation line D BWD010 127.54 127.8 GY SSG 75 XQZ 25 QZ PY Arsenopyrite and pyrite forming in veins and qtz veins D BWD010 127.8 128 GY SIC 90 XCO 5 XQZ 5 QZ CARB D BWD010 128 128.54 GY SSG 60 XQZ 40 QZ PY D BWD010 128.54 129.08 BL SIZ XCO ZSO CARB Sulphidic mudstone inside a high stress zone. Probably the result of a fault shear as mudstone is broken up into rubble D BWD010 129.08 129.7 GY SSG PY Pyrite forming in patches and specks on the surfaces of fractures D BWD010 129.7 130.1 GY SSG 90 XQZ 9 XCO 1 PY Sulphides forming in matrix as blebs and on fracture surfaces as coating D BWD010 130.1 132.22 GY SSG 100 D BWD010 132.22 132.25 WH XQZ 100 QZ PY D BWD010 132.25 132.72 GY SSG 100 D BWD010 132.73 132.74 GY XQZ 100 QZ PY Small qtz/sulphide vein D BWD010 132.74 132.81 GY SSG 100 D BWD010 132.81 134.12 GY SSG 95 XCO 5 CARB D BWD010 134.12 134.79 GY SSG 100 D BWD010 134.79 138.15 GY SSG 95 XCO 5 CARB PY Small veinlets of calcium carbonate and pyrite porphyry blasts D BWD010 138.15 138.7 GY SSG 98 XCO 2 CARB EOH D BWD011 0 3.9 VOO 100 Unconslidated material D BWD011 3.9 4.3 RRS 100 Weathered rock and clay D BWD011 4.3 4.6 RRR 100 Highly weathered sandstone D BWD011 4.6 16.1 SSG 100 Oxidised greywacke D BWD011 16.1 18.2 SIO 100 D BWD011 18.2 20.5 SSG 100 Fine-medium grained sandstone D BWD011 20.5 22.2 SIO 100 Siltstone rare fine sandstone D BWD011 22.2 27.2 SSG 100 Base of weathering D BWD011 27.2 41.2 GY SSG 100 Fairly massive D BWD011 41.2 42.9 GY SIO 100 D BWD011 42.9 82 GY SSG 100 Fine grained sandstone and siltstone. Younging uphole. Grainsize coarsening dhole in each metre plus unit. D BWD011 82 87.4 GY SSG 100 FINER GRAINED UNIT DOM'D BY SILSTONE-MUDSTONE WITH MM SIZED PORPHRIOBLASTS D BWD011 87.4 130.4 GY SSG 100 FINE GRAINED SANDSTONE DOMINATED. Mm sized Porphyroblasts in siltstone/mudstone beds D BWD011 130.4 140.5 DKGY SIO 98 200 SSG 2 10 DOM BY MUDSTONE/SILTSTONE. RARE FINE GRAINED SANDY BEDS. MM SCALE PORHYROBLASTS D BWD011 140.5 146.1 DKGY SSG 60 100 SIM 40 100 DOM BY FINE GRAINED SANDSTONE BUT WITH BLACKISH GREY MUD/SILT D BWD011 146.1 184 DKGY SSG 90 100 SIO 10 20 DOM BY FINE GRAINED SANDSTONE VERY RARELY MEDIUM GRAINED OCCASIONAL FINE GRAINED MUD/SILT BEDS GRADING INTO SANDY UNITS. YOUNGING UPHOLE D BWD011 184 194.2 DKGY SSG 90 100 SIO 5 20 DOM BY FINE GRAINED SANDSTONE BUT WITH BLACKISH GREY MUD/SILT. SAME AS UNIT ABOVE BUT WITH INCREASE IN LARGE QZ VEINS D BWD011 194.2 200.3 DKGY SIO 100 ALMOST BLACK COLOURED MUD/SILTSTONE LARGE STRUCTURE @198.2-199.0. VERY FEW QZ VEINS D BWD011 200.3 222.45 DKGY SSG 95 199 SIO 5 20 FINE GRAINED SANDSTONE WITH OCCASIONAL FINE GRAINED BEDS D BWD011 222.45 227.45 DKGY SIO 95 SSG 5 "DOM BY FINE GRAINED SEDS, SMALL AMOUNT OF VERY F GRAINED SAND OR COARSE SILT" D BWD011 227.45 300 DKGY SSG 98 SIO 2 TYPICAL FINE GRAINED SANDSTONE D BWD011 300 301.85 DKGY SIO 90 SSG 10 DOMINATED BY MUDSTONE WITH GRADATIONAL CONTACT WITH VERY FINE SANDSTONE TOWARDS BOTTOM OF HOLE. 3-10CM QTZ-SULPHIDE VEINS. D BWD011 301.85 306.5 DKGY IMD 100 FINE GRAINED POSSIBLY CHILL MARGIN OF DOLERITE OR 'BAKING ZONE' OF COUNTRY ROCK. FELDSPAR COMMON AS INTERGRANULAR OR HALOS AROUND BLACK SPOTS. D BWD011 306.5 316.8 GYPI IMD 100 "COARSE GRAINED DOLERITE. ABUNDANT PLAGIOCLASE INCREASING WITH DEPTH, POSSIBLY ANORTHITE. END OF HOLE." D BWD012 0 2 RD RRS 100 "HIGHLY WEATHERED, SOIL DEVELOPMENT IN TOP 20-30CM" D BWD012 2 31.35 RD SSG 55 75 SIO 45 50 HIGHLY WEATHERED SAPROLITE/SAPROCK WITH SECTIONS PRESERVING ORIGINAL ROCK TEXTURE. SOME INTERVALS COMPLETELY WEATHERED TO CLAYS OR SANDS D BWD012 31.35 34.67 BN IMD 100 "HIGHLY WEATHERED DOLERITE, CONTACT COULD BE HIGHLY HOWEVER CANNOT DETERMINE DUE TO WEATHERING. TEXTURE OF DOLERITE." D BWD012 34.67 60.5 DKGY IMD 100 MGT WEAKLY MAGNETIC. MINOR INTERVALS OF K-SPAR ?ALTERATION. SOME FRACTURES ARE CLAYEY D BWD012 60.5 79.25 DKGY IMD 100 MGT WEAKLY MAGNETIC D BWD012 79.25 85.56 GYBE SIO 100 ALTERED SILT/MUDSTONE DUE TO DOLERITE DYKE. BROKEN GROUND D BWD012 85.56 89.95 GY SIO 100 PY PARTIALLY ALTERED SILT/MUDSTONE. QTZ-PYRITE VEIN D BWD012 89.95 97.95 DKGY SSG 75 150 SIO 25 40 "GRADED BEDS, YOUNGING UPHOLE. SEVERAL SEDIMENTARY SUCCESSIONS" D BWD012 97.95 99.95 DKGY SSG 100 ZSZ 85 HIGHLY FRACTURED WITH 'WHISPY' ALTERATION QTZ VEINS. GRAPHITE ON FRACTURE SURFACES D BWD012 99.95 105.8 DKGY SSG 90 300 SIO 10 25 PREDOMINANTLY SANDSTONE WITH MINOR MUDSTONE. SOME MIXING OF MOTH LITHOLOGIES TOWARDS BASE D BWD012 105.8 110.13 DKGY SIO 75 50 SSG 25 15 D BWD012 110.13 125.45 DKGY SSG 60 100 SIO 40 70 HIGHLY FRACTURED D BWD012 125.45 126.9 DKGY SSG 100 ZSZ 100 HIGHLY FRACTURED WITH 'WHISPY' ALTERATION QTZ VEINS. APPEARS TO BE FAULT GOUGE IN SECTIONS WITH A VERY FINE MATRIX AND FLOATING CLASTS D BWD012 126.9 165.2 DKGY SSG 55 55 SIO 45 50 SOME INTERVALS SHOW YOUNGING UPHOLE DIRECTION THROUGH GRADED BEDDING. MIXING OF SAND AND MUDS TOWARDS BASE OF UNIT - ?TURBIDITIC D BWD012 165.2 180.9 DKGY SIO 95 XQZ 5 "COMMON QZ-SULPHIDE VEINS, 1-2 PER METRE FROM 2MM TO 50MM THICK." D BWD012 180.9 190.2 DKGY SSG 50 100 SIO 50 100 "INTERVALS A MIX OF SANDSTONE/MUDSTONE, TURBIDITIC ENVIRONMENT. LOAD CASTS AT 188.75M INDICATE YOUNGING DOWNHOLE. RIP UP CLASTS COMMON ALSO." D BWD012 190.2 196.55 DKGY SIO 100 ONE QZ-SULPHIDE VEIN 15CM WIDE. D BWD012 196.55 227.23 DKGY SSG 60 120 SIO 35 80 XQZ 5 PY SEVERAL SEDIMENTARY SEQUENCES OF SAND AND SILT/MUDSTONE WITH VARYING INTERVAL LENGTHS FROM 120-400CM SSG AND 20-140CM SIO. GRADED BEDDING INDICATES YOUNGING DOWNHOLE SMALL INTERVALS SHOW MIXING OF THE TWO LITHOLOGIES INDICATING A MORE TURBIDITIC ENVIRONME D BWD012 227.23 227.47 DKGY XQZ 100 PY VUGGY QZ-PYRITE VEIN ~8% SULPHIDES D BWD012 227.47 240 DKGY SSG 60 120 SIO 40 80 D BWD012 240 294.35 DKGY SSG 65 120 SIO 45 60 "LESS DEFINED BEDDING, MORE TURBIDITIC ENVIORNMENT, VERY 'SWIRLY' MIX OF SAND AND MUDSTONE" D BWD012 294.35 297.35 DKGY SIC 100 ZSZ GR "CARBONACEOUS MUDSTONES, GRAPHITIC ON FRACTURE SURFACES. VERY FRACTURED WITH ALTERATION CARBONATES THROUGHOUT." D BWD012 297.35 299.56 DKGY SIO 100 D BWD012 299.56 301.98 DKGY SIO 90 200 SSG 10 23 D BWD012 301.98 313.77 DKGY SIO 100 "MINOR SAND INTERVALS, MOSTLY MUDSTONE WITH SILTSTONE" D BWD012 313.77 347.44 DKGY SSG 90 100 SIO 10 10 EVIDENCE OF OVERTURNED BEDS WITH FLAME TRUCTURES INDICATING A YOUNIGNG DOWNHOLE DIRECTION D BWD013 0 2.7 CORE LOSS D BWD013 2.7 6.5 ORBE RRM 100 MOTTLED SAPROLITIC CLAYS WITH REMNANT PROTOLITH FRAGMENTS. D BWD013 6.5 17.17 ORGY SSG 100 "STRONGLY WEATHERED GREYWACKE, POSSIBLY MINOR MUDTSONE. " D BWD013 17.17 35.9 ORBE SSG 60 120 SIO 20 60 XQO 20 REMNANT QTZ VEINS FROM 10-80CM THICK D BWD013 35.9 40.35 GYOR SSG 100 OXIDISED FRACTURES. MINOR 1-2 CM QTZ VEIN. D BWD013 40.35 46.3 GYOR SIO 65 100 SSG 35 50 "MINOR OXIDATION ON FRACTURES, DOES NOT PERMEATE INTO ROCK" D BWD013 46.3 51.35 DKGY SSG 100 D BWD013 51.35 62.7 DKGY SIO 85 400 SSG 15 50 "COARSER GRAINED TOWARDS THE BASE OF UNIT, POSSIBLY A GRADED BED" D BWD013 62.7 64.93 GYWH ZFX 100 "IMMATURE BRECCIA, CLAST SUPPORTED, QTZ ALTERATION." D BWD013 64.93 81.28 DKGY SSG 85 150 SIO 15 30 APPEARS SLIGHTLY ALTERED?? 79-80.5M (TEXTURE). SOME BEDS SHOW AN UPWARD FINING SEQUENCE D BWD013 81.28 85.9 DKGY SIO 60 100 SSG 40 70 COMMON 1CM QTZ VEINS D BWD013 85.9 86.57 WH XQO 95 SSG 5 PY MINOR SULPHIDES WHICH LOOK LIKE A LATER EVENT ON IN A SMALL PROPORTION OF THE VEIN D BWD013 86.57 87.7 DKGY SIO 100 VERY MINOR COARSER GRAINED INTERVALS D BWD013 87.7 89.12 WHGY XQZ 90 SIO 10 PY APY "15CM INTERVALS OF SOLID SULPHIDES, REST OF VEIN IS ~15% SULPHIDES" D BWD013 89.12 93.35 DKGY SIO 100 "LIGHTER AND DARKER LAYERSWIHTIN, COULD BE SLIGHTLY SILTIER IN THESE INTERVALS" D BWD013 93.35 98.7 DKGY SSG 80 70 SIO 20 15 D BWD013 98.7 104.18 DKGY SIO 65 100 SSG 35 60 D BWD013 104.18 105.6 GY SSG 90 XQO 10 ALTERED SANDSTONE/SILTSTONE WITH AUNDANT 'CHAOTIC' QTZ VEINS AND VEINLETS D BWD013 105.6 173.8 DKGY IMD 100 WEAKLY MAGNETIC IN PARTS. D BWD013 173.8 175.9 DKGY SSG 85 120 SIO 15 20 WEAKLY ALTERED SANDSTONE/MUDSTSONE CHARACTERISED BY A LIGHTER GREY/PINK COLOURATION ALONG CLOSED FRACTURES. D BWD013 175.9 177.9 LTGY SSG 100 ALTERED SANDSTONE CHARACTERISED BY PERVASIVE DISCOLOURATION TO THE BULK ROCK TO A LIGHTER GREY/BEIGE COLOUR D BWD013 177.9 181.14 DKGY SSG 55 100 SIO 45 80 COARSER GRAINED INTERVALS LIGHTER IN COLOUR. WEAK ALTERATION AS ABOVE ON FRACTURES D BWD013 181.14 184.6 DKGY SIO 100 "PORPHYROBLASTIC. MUDSTONE LAYERED WITH SILTSTONE, 10CM BEDS" D BWD013 184.6 185.36 DKGY SSG 100 D BWD013 185.36 190 GYWH SIO 40 XQZ 20 ZSZ 40 GR PY "PORPHYROBLAASTIC IN FINER GRAINED UNITS. SULPHIDIC QTZ VEINS UP TO 30CM IN WIDTH. ?FAULT GOUGES COMMON UP TO 10CM THICK, GRAPHITIC ON FRACTURE SURFACES. " D BWD013 190 191 GYWH XQZ 50 SSG 50 PY APY ~20% SULPHIDES WITHIN VEINS. TWO VEINS UP TO 30CM THICK. D BWD013 191 199.35 DKGY SSG 60 40 SIO 40 30 GREYWACKE 30-60CM THICK AND MUDSTONE UP TO 20-40CM D BWD013 199.35 199.75 WH XQZ 100 PY ~30-40% SULPHIDES D BWD013 199.75 204 DKGY SSG 100 PY COMMON QZ-SULPHIDE VEINS D BWD013 204 213.75 DKGY SSG 75 65 SIO 25 20 5-10CM QZ-SULPHIDEVEINS WITH A FREQUENCY OF 1/M D BWD013 213.75 219.7 DKGY SSG 100 MINOR INTERVALS OF MIXED SAND AND MUD AND MUDBALLS. YOUNGING UPHOLE (LOAD CASTS) D BWD013 219.7 222.74 DKGY SSG 50 50 SIO 50 50 FINING UPHOLE D BWD013 222.74 226.2 DKGY SIO 60 50 SSG 40 30 FINE UNITS PORPHYROBLASTIC D BWD013 226.2 226.85 WH XQZ 100 APY PY ~30% SULPHIDES D BWD013 226.85 230.45 DKGY SIO 60 30 SSG 40 20 FINER UNITS ARE PORPHYROBLASTIC D BWD013 230.45 238.85 DKGY SSG 85 XQZ 15 PY "COMMON QZ-SULPHIDE VEINS 5-25CM THICK, FREQUENCY 1/1.5M" D BWD013 238.85 240.5 WHGY SIO 55 XQZ 45 APY PY HOSTROCK 'CLASTS' WITHIN QZ VEIN. D BWD013 240.5 253.15 DKGY SSG 85 200 SIO 15 35 POSSIBLE SHEAR ZONE 241.85-242.2M CHARACTERISED BY HIGH FRACTURE RATE AND 'RANDOM' QTZ STRINGERS. FLAME STRUCTURES INDICATE FINING UPHOLE SEQUENCE. D BWD013 253.15 264.8 DKGY SSG 95 XQZ 5 PY COMMON QZ-SULPHIDE VEINS 1-3CM THICK WITH A FREQUENCY OF 2/M D BWD013 264.8 265.7 WHGY XQZ 75 SIC 25 PY MINOR SULPHIDES. 'CLASTS' OF HOST ROCK AMONGST QTZ VEIN D BWD013 265.7 267.85 DKGY SIC 90 XQZ 10 ZSZ APY PY QZ IS 'BRECCIATED' AND 'CHAOTIC' AND POSSIBLE DUE TO STRUCTURAL ZONE. Yep confirmed structural zone D BWD013 267.85 273.4 DKGY SSG 98 SIO 2 1 LOAD CASTS OF MUDSTONE D BWD013 273.4 279.25 DKGY SIC 70 SSG 28 4 XQZ 2 MAYBE NOT TEXT BOOK GRAPHITIC MUDSTONE BUT GRAPHITE ON JOINTS ETC D BWD013 279.25 284.5 DKGY SSG 98 SIO 2 MINOR WISPY MUDSTONE BEDS D BWD013 284.5 294.3 DKGY SIO 50 2 SSG 50 SOME THICKER MUD BEDS D BWD013 294.3 298.7 DKGY SSG 98 SIO 2 10 D BWD013 298.7 347.9 DKGY SSG 80 2 SIO 20 NOT SURE IF I'VE BULKED THIS OUT TOO MUCH? MUDSTONE/SILTSTONE HAS SPARSE PORPHYROBLASTS TO 2MM D BWD013 347.9 364.3 DKGY SIO 98 10 SSG 2 2 V HARD TO SEE BEDDING. DISRUPTED BY POOR ROCK MASS AND STRUCTURE @ 351.2 D BWD013 364.3 394 DKGY SSG 97 SIO 3 10 STANDARD LOOKING GREYWACKE WITH VERY OCCASIONAL MUDSTONE BEDS D BWD013 394 458.7 DKGY SIO 70 3 SSG 30 20 MORE SILTSTONE DOMINATED distinctive WELL BEDDED APPEARANCE. EOH @ 458.6 D BWD014 0 1 LTBN ROS LIGHT ORANGE BROWN SOIL D BWD014 1 2.2 ODM 1.2M MISSING CORE D BWD014 2.2 3.6 LTOR RRM D BWD014 3.6 9.5 LTOR SSG D BWD014 9.5 33.7 BE SIO 95 SSG 5 D BWD014 33.7 47 GY SSG FEOX ON JOINTS/FRACTURES. FINE GRAINED GREYWACKE D BWD014 47 49 GY SSG D BWD014 49 50 BEGY SSG CARBONATE ALTERATION? ASSOC WITH VEINING D BWD014 50 57.6 DKGY SSG 98 SIO 2 FINE GRAINED UNIT ASSOC WITH STRUCTURE? D BWD014 57.6 61.3 BK SIO 100 1 VARIABLE THICKNESS BEDS IN SOME PLACES LOOKS MASSIVE D BWD014 61.3 64 GNGY SSG 100 EPIDOTE?? ALTERATION (GRASS GREEN) IN THICK BANDS D BWD014 64 67.8 DKGY SSG 100 D BWD014 67.8 71.5 DKGY SIO 95 3 SSG 5 D BWD014 71.5 74.5 DKGY SIO 100 PORPHYROBLASTIC SPOTS UP TO 5MM IN PLACES. MOSTLY 3MM D BWD014 74.5 76.9 DKGY SIO 100 LOOKS MASSIVE PROBABLY ISN'T BEDDING JUST OBSCURED? D BWD014 76.9 84.3 DKGY SSG 100 D BWD014 84.3 90.9 BK SIO 85 5 SSG 14 XQZ 1 D BWD014 90.9 98.4 DKGY IMD CHILLED MARGIN D BWD014 98.4 103.3 DKGY SSG 100 DOING MY HEAD IN TRYING TO FIGURE OUT IF IT'S DOLERITE OR GREYWACKE. NON MAGNETIC AND SLIGHTLY UNIFORMALLY GRAINY BUT LOW CONFIDENCE D BWD014 103.3 200.48 DKBN IMD 100 CHILLED MARGIN D BWD014 200.48 203 DKBN XQZ 85 SSG 15 WHITE QZ ALMOST A BRECCIA WITH CARB ALT GREYWACKE D BWD014 203 207.1 DKBN SSG 100 PERVASSIVE CARB? ALTERATION D BWD014 207.1 211.25 DKGY SSG 100 STANDARD LOOKING GREYWACKE D BWD014 211.25 216.2 DKGY SIO 95 2 SSG 5 D BWD014 216.2 226.7 DKGY SIC 80 3 XQZ 20 SSG 5 PORPHYROBLASTS COMMON IN MUDSTONE. NICE LOOKING MINERALISED ZONE D BWD014 226.7 232.7 LTGY XQZ 95 SIC 5 WHITE QZ WITH APY & PY D BWD014 232.7 233.3 BK SIC 100 D BWD014 233.3 246.9 DKGY SSG 70 80 SIO 25 3 XQZ 5 QZ PY ALMOST BUT NOT QUITE RHYMMICALY BEDDED. STD GREYWACKE AND MUDSTONE/SILTSTONE D BWD014 246.9 249.3 GY SIO 80 XQZ 20 QZ PY OBVIOUS FOLIATION WITHIN THE SILTSTONE BEDDING D BWD014 249.3 252.3 GY SSG 100 GREYWACKE ZONE D BWD014 252.3 256.38 GY SIO 70 SSG 30 QZ D BWD014 256.38 266.6 GY SSG 90 SIO 5 25 XQZ 5 D BWD014 266.6 270.9 GY SIO 90 SSG 5 13 XQZ 5 QZ PY FINER GRAINED MATRIX WITH SOME QZ VEINING AND SSG BEDDING D BWD014 270.9 274.35 DKGY SIC 85 XZO 2 XQO 8 QZ PY MASSIVE SULPIDE VEINS WITHIN THE GRAPHITIC CARBONACEOUS ZONE D BWD014 274.35 276.6 GY SIO 100 D BWD014 276.6 302 GY SSG 70 SIO 25 XQO 5 QZ PY PREDOMINANTLY GREYWACKE WITH INTERBEDDED SILTSTONE LAYERS AND A FEW QZ-SULPHIDE VEINS D BWD014 302 302.46 DKGY SIC 90 XQZ 20 QZ PY DARK FINE GRAINED SEDIMENTARY ROCK WITH SOME XULPHIDIC VEINS D BWD014 302.46 303.1 XQZ 90 SIO 10 QZ APY 45CM THICK QZ VEIN WITH MASSIVE PYRITE AND BRECCIATED QZ FRAGMENTS WITH A SUBHEDRAL SHAPE D BWD014 303.1 309.5 GY SIO 85 XQZ 10 XZO 5 QZ APY SULPHIDE AND QZ VEINS AMONGST A SILTSTONE ZONE D BWD014 309.5 314.7 GY SSG 50 42 SIO 30 41 XQZ 20 32 QZ PY D BWD014 314.7 328.7 GY SIO 80 D BWD014 328.7 330 GY XQZ 50 ZFO 50 LARGE QZ VEIN OVER 1M WITH SULPHIDES AND HIGHLY FRAGMENTED D BWD014 330 335 GY SSG 50 SIO 50 D BWD014 335 336.5 GY SSG 80 XQC 20 INTENSE CARBONATE AND QZ VEINING GOING THROUGH THIS ZONE D BWD014 336.5 341.3 GY SIO 40 SSG 40 XQO 20 QZ PY D BWD014 341.3 345.7 GY ZFO 90 XQC 10 INTENSE CARBONATE AND QZ VEINING THROUGH THIS SECTION WITH MORE FRACTURES AND FAULTING D BWD014 345.7 348 LTGY SSG 100 D BWD014 348 352 GY SIO 90 XQC 5 ZFO 5 ANOTHER INTENSE VEINING ZONE D BWD014 352 360.5 GY SSG 90 SIO 10 D BWD014 360.5 363 GY SIO 100 D BWD014 363 372.5 GY SSG 70 SIO 20 XQO 10 QZ PY D BWD014 372.5 382.3 LTGY SSG 90 SIO 10 35 PREDOMINENTLY GREYWACKE D BWD014 382.3 385.69 DKGY SIC 33 SIO 33 SSG 33 INTERBEDDED MUDSTONES-SILTSTONES-GREYWACKE D BWD014 385.69 386.15 XQZ 100 QZ APY D BWD014 386.15 387.8 GY SIO 60 SSG 40 D BWD014 387.8 388.2 XQO 90 SSG 10 QZ PY VUGGY QZ WITH SOME PYRITIC MINERALISATION ON THE CONTACT OF THE QZ VEIN AND GREYWACKE D BWD014 388.2 401.75 GY SSG 60 SIO 30 XQZ 10 QZ PY D BWD014 401.75 404.4 GY SSG 100 APY SPECKS OF DISSEMINATED APY THROUGHOUT THE GREYWACKE D BWD014 404.4 405.18 GY SIO 90 XQO 10 PY CL CHLORITE STAINING AND PYRITIC MINERALISATOIN WITHIN THE QZ VEIN D BWD014 405.18 407.25 GY SSG 100 APY D BWD014 407.25 408.22 GY SIO 100 D BWD014 408.22 410.48 GY SSG 80 SIO 20 D BWD014 410.48 411.46 GY SIO 90 SSG 10 D BWD014 411.46 426.8 GY SSG 70 SIO 20 XQZ 10 QZ APY PREDOMINANTLY GREYWACKE UNIT WITH INTERBEDDED SILTSTONE AND QZ VEINING D BWD014 426.8 438.7 GY SIO 98 XQO 2 SILTSTONE ZONE WITH SOME QZ VEINING IN SAME ORIENTATION AS FOLIATION AND BEDDING PLANES D BWD014 438.7 443.07 GY SIO 100 D BWD014 443.07 447.2 GY SSG 80 SIO 20 D BWD014 447.2 450.6 GY SSG 70 SIO 25 XQO 5 D BWD014 450.6 451 DKGY SIC 95 XQO 5 QZ SERI DARK CARBONACEOUS ZONE WITH SERICITE FORMING ON THE FRACTURE SURFACES AS COATING D BWD014 451 462 GY SSG 60 SIO 25 SIC 15 QZ MOSTLY GREYWACKE AND SILTSTONE WITH SOME QZ VEINING AND ONE BAND OF HIGHLY GRAPHITIC SLICKENSIDE FRACTURESURFACE MUDSTONE D BWD014 462 465.5 GY SIO 60 SSG 30 XQO 10 QZ EOH D BWD015 0 1 RD RTC 100 FE CL "Top cover of transported material, highly weathered with excessive Fe oxides" D BWD015 1 2.85 BN UOO 100 Unconsolidated material D BWD015 2.85 6.7 BN RRR 100 Saprolitic sandstone D BWD015 6.7 9.2 BG RRSL 95 XQO 5 QZ FE Lower saporolite D BWD015 9.2 12.4 BG RRY 100 FE Consolidated clay zone w/ FE staining on the fracture surfaces. D BWD015 12.4 23.3 BG SSG 90 RRY 10 FE D BWD015 23.3 31.25 GY SSG 60 SIO 40 D BWD015 31.25 33.15 GY SSG 100 QZ Coarse grained greywacke D BWD015 33.15 41.6 GY SIO 100 Varying greywacke and siltstone D BWD015 41.6 43.6 GY ZSO 60 ZFG 20 ZFX 20 Shear zone with evidence of fault gouges from fracture filling gouge with brecciated fragments within the gouge matirx D BWD015 43.6 47.6 GY SIO 100 CA Siltstone zone with minor calcium carbonate veinlets D BWD015 47.6 53.7 GY SSG 90 SIC 10 Greywacke with some traces of carbonaceous material seen within the fracture surfaces D BWD015 53.7 56 GY SIO 100 CA Siltstone zone with minor calcium carbonate veinlets D BWD015 56 60 GY ZFO 100 CA GR Shear zone with graphitic material and brecciated rock fragments D BWD015 60 68.65 GY SIO 100 CA Siltstone layer with interbedded fine grained and coarse grained zones D BWD015 68.65 69 XQO 100 QZ APY 20CM THICK QZ VEIN WITH TRACES OF ARSENOPYRITE D BWD015 69 85.3 LTGY SIO 60 SSG 35 XQO 5 QZ CL PREDOMINANTLY SILTSTONE AND GREYWACKE WITH SOME QZ VEINLETS AND SOME CHLORITISATION IN ONE OF THE QZ VEINS. SEEMS AS THOUGH THERE MAYBE EITHER A SERICITE OR COLICA ALTERATION AT THE START OF THIS ZONE D BWD015 85.3 85.57 XQZ 50 SIO 50 QZ APY SMALL QZ-SULPHIDE VEIN D BWD015 85.57 87 GY SIO 100 D BWD015 87 89 BG SIO 100 SERI SILTSTONE UNDERGONE HEAVY SERICITE-CARBONATE ALTERATION D BWD015 89 94.3 GY SIO 90 XQO 10 QZ SILTSTONE WITH MODERATE DEFORMATION AS IT SITS ON THE CONTACT OF A FAULT ZONE. THERE ARE TRACES OF SERICITE ALTERATION IN THE FORM OF HALOS-BLEBS D BWD015 94.3 96 GY ZFZ 70 SIO 30 HIGH BROKEN UP-FRAGMENTED FAULT ZONE D BWD015 96 97 GY SIO 100 D BWD015 97 97.6 GY ZFG 100 FAULT GOUGE D BWD015 97.6 98.6 GY SIO 100 QZ D BWD015 98.6 128 GY ZFN 100 EXTENSIVE FAULT ZONE W/ HIGHLY FRACTURED MATERIAL INTERBEDDED WITH THICK QZ VEINS AND MOSTLY COMPRISED OF A FINE GRAINED MATRIX BUT HAVE ZONES OF COARSER GRAINED MATRIX. NO ORIENTATION LINE WAS OBTAINED WITHIN THIS ZONE D BWD015 128 148.62 GY SSG 50 SIO 50 D BWD015 148.62 166.2 GY SIO 100 D BWD015 166.2 168.77 GY XZO 50 SIC 50 APY SULPHIDE VEIN ON THE CONTACT OF A SILTSTONE AND A CARBONACEOUS MUDSTONE D BWD015 168.77 175.4 GY SSG 70 SIO 30 QZ CL SEDIMENTARY STRATIGRAPHY WITH SOME CHLORITISATION AND VEINLETS OF QZ D BWD015 175.4 177.51 XQZ 90 SIO 10 8 QZ PY THICK BAND QZ VEIN WITH SOME PYRITIC SULPHIDES AND SERICITISATION IN AMONGST SOME OF THE QZ FRACTURES D BWD015 177.51 179.13 GY SIO 90 SSG 10 D BWD015 179.13 180.2 XQO 80 SIO 20 SERI QZ D BWD015 180.2 183.47 GY SSG 70 SIO 20 XQZ 10 PY SERI QZ VEIN WITH SURROUNDING SERICITE ALTERATION AS WELL AS SOME TRACES OF SERICITE AND PATCHES OF PYRITE WITHIN THE VEIN D BWD015 183.47 183.95 GY SIO 100 QZ D BWD015 183.95 186.7 GY SSG 100 D BWD015 186.7 187.72 XQZ 80 SIO 20 QZ PY D BWD015 187.72 190.1 DKGY SIC 80 SIO 20 PY DARK COLOURED MUDSTONE-CARBONACEOUS ZONE WITH PYRITE FORMING IN AMONGST THE SEDIMENTARY MATRIX D BWD015 190.1 190.33 XQO 70 SIC 30 D BWD015 190.33 204 GY SSG 70 SIO 30 D BWD015 204 205.32 XQO 95 SIC 5 QZ SERI APPROX 1M THICK QZ VEIN WITH TRACES OF SERICITE ALTERATION D BWD015 205.32 213.7 GY SIO 60 SSG 30 XQO 10 QZ SERI SOME SERICITISATION WITHIN THE QZ VEINS AND TRACES OF GRAPHITE ON SOME OF THE FRACTURE SURFACES D BWD015 213.7 214.26 GY SSG 100 VERY COARSE GRAINED GREYWACKE D BWD015 214.26 215.78 GY SIO 60 SSG 35 XQO 5 QZ SERI SOME TRACES OF CHLORITE WITHIN THE QZ VEIN D BWD015 215.78 216.45 GY XZO 80 SIO 20 PY QZ D BWD015 216.45 231.17 GY SIO 60 SSG 30 XQZ 10 APY SERI SILTSTONE LAYER WITH QZ VEINS AND SERICITISATION ALTERATION D BWD015 231.17 248.8 LTGY SIO 48 SSG 48 XQO 4 QZ D BWD015 248.8 249.5 GY SSG 100 COARSER GRAINED GREYWACKE D BWD015 249.5 271.64 GY SIO 80 SSG 20 LARGER SILTSTONE PROPORTION WITH SOME BANDS OF COARSER GRAINED (GREYWACKE) SEDIMENTARY ROCK D BWD015 271.64 272.85 GY SSG 95 SIO 5 D BWD015 272.85 291.1 GY SIO 85 SSG 10 XQO 5 QZ CL D BWD015 291.1 294.41 GY SIO 95 XQZ 5 APY QZ Section is predominantly fine grained siltstone and is characterised by several fractures and small veins/veinlets. Fractures tend to folllow 2 main orientations although a single 250 mm long fracture runs oblique to core axis at the 294m mark. Veins are D BWD015 294.41 306.47 GY SIO 50 SSG 50 CAL SERI Alternating interbedded silltstone and greywacke dominate. The top 3m of section is characterised by alternating bands of phorphyblasts (perhaps chloritic) which feature in the darker grey units. Very minor fracturing is observed but seem to be in a predo D BWD015 306.47 321.46 GY SSG 100 PREDOMINANTLY FINE GRAINED GREYWACKE WITH COARSER INTERVALS. PORPHYROBLASTIC IN PART - CHLORITIC? D BWD015 321.46 324.08 GY SSG 85 SIO 15 SI MIXINNG IN PART OF SANDSTONE WITH MUD/SILTSTONE. SOME INTERVALS MAY APPEAR FINER GRAINED DUE TO A SILICICEOUS ALTERATION D BWD015 324.08 365.9 GY SSG 100 SI "FINE TO COARSE GRAINED GREYWACKE. SILICEOUS ALTERTION IN PART, PERVASIVE FROM FRCTURES. ?BLEACHING ALONG THESE AREAS. PORPHYROBLASTIC IN SECTIONS - CHLORITIC" D BWD015 365.9 379.85 GY SIO 50 SSG 50 SI SILICA ALTERATION POSSIBLY LEADING TO FINER GRAINED APPEARANCE. MILLIMETRIC VEINS COMMON. LIGHT GREY/GREEN/GREY D BWD015 379.85 381.6 LTGY SIO 100 SI STRONGLY SILICIFIED. BLEACHED ALONG FRACTURES AND PERVASIVELY IN ROCK FROM FRACTURES. LIGHT OLIVE GRAY. D BWD015 381.6 388.12 LTGY SSG 75 SIO 25 SI "FINER GRAINED APPEARANCE COULD BE DUE TO SILICIFICATION. MOSTLY FINE TO COARSE GRAINED GREYWACKE, PORPHYROBLASTIC IN PART - CHLORITIC? MODERTELY SILICIFIED AND ALTERED." D BWD015 388.12 394.83 DKGY SSG 80 SIO 20 BEDDING ALMOST PARALLEL TO CORE AXIS. COARSE GRAINED GREYWACKE INTERBEDDED WITH FINER GREYWACKE AND LESSER PERCENTAGE OF SILT/MUDSTONE. FLAME STRUCTURES INDICATE YOUNGING UPHOLE D BWD015 394.83 397.63 DKGY SSG 100 FINE TO MEDIUM GREYWACKE. POSSIBLY ONE SEQUENCE FROM MEDIUM GROUND TO FINE GRAINED - ?YOUNGING DOWNHOLE? D BWD015 397.63 399.57 DKGY SIO 50 SSG 50 BEDDING ALMOST PARALLEL TO CORE AXIS WITH VERY COARSE GRAINED GREYWACKE AND VERY FINE GREYWACKE TO SILTSTONE. D BWD015 399.57 408.7 DKGY SSG 100 "COARSE GREYWACKE AT TOP OF SEQUENCE TO FINER GREYWACKE DOWNHOLE - GRADED BEDDING, YOUNGING ?DOWNHOLE. END OF HOLE." D BWD016 0 0.2 ORBR ROS 100 TOP SOIL D BWD016 0.2 4.02 ORBE RRM 100 "MOTTLED ZONE, VERY FRIABLE. POSSIBLY HIGHLY WEATHERED GREYWACKE/MUDSTONE" D BWD016 4.02 9.9 ORGY SSG 50 SIO 50 RRM 100 "MOTTLED SANDSTONE AND SILTSTONE, MOTTLED WITH A PREFERENTIAL WEATHERING ON MORE POROUS LITHOLOGIES FORMING A 'BRECCIATED' OR 'CONGLOMERATIC' APPEARANCE OF CORE" D BWD016 9.9 11.06 ORGY XQO 85 SIO 15 PY "REMNANT QTZ VEIN, WITH OXIDISED SILTSTONE NETWORK THROUGH VEINING. PITTING IN REMNANT QTZ VEIN, POSSIBLY REMNANT OF PYRITE. VERY FEW PYRITE WITHIN QTZ VEIN." D BWD016 11.06 12.74 ORBE SIO 100 MOTTLED SILT/MUDSTONE. OXIDISED AND FRIABLE. D BWD016 12.74 18.24 GYOR SIO 50 140 SSG 50 140 PERVASIVE OXIDATION FROM FRACTURES. FEW REMNANT QTZ VEINS UP TO 8CM THICK. SOME INTERVALS MORE FIRABLE THAN OTHERS OTHERWISE ORIGINAL ROCK TEXTURE IS PRESERVED. D BWD016 18.24 19 ORGY SIO 80 XQO 20 FRIABLE. REMNANT FRAGMENTS OF QTZ - POSSIBLE VEINING D BWD016 19 19.93 GYOR SIO 100 OXIDISED FRACTURES. D BWD016 19.93 22.6 GYOR SSG 60 70 SIO 40 10 BEDDING SUBPARALLEL TO CORE AXIS D BWD016 22.6 25.28 GYOR SIO 100 OXIDATION ALONG FRACTURES. VERY PORPHYROBLASTIC AND PITTED FROM ?WEATHERED PORPHYROBLASTS. BEDDING AT HIGH ANGLE TO CORE AXIS D BWD016 25.28 28.5 GYOR SIO 50 40 SSG 50 40 VERY PORPHYROBLASTIC WITHIN FINER LITHOLOGY. BEDDING IS AT A HIGH ANGLE TO THE CORE AXIS. D BWD016 28.5 35.14 GY SIO 50 40 SSG 50 40 AS ABOVE WITH NO OXIDATION D BWD016 35.14 35.4 GY ZFG 100 SIO 100 PY CLAY RICH WITH REMNANTS OF QUARTZ AND SULPHIDES. POSSIBLE FAULT GOUGE? OXIDISED ON FRACTURES D BWD016 35.4 44.9 GY SIO 100 "MINOR OXIDATION ON FRACTURE SURFACES. VERY CLAY RICH AND FRIABLE IN SECTIONS, ?ALTERED. PORPHYROBLASTIC. " D BWD016 36.45 98.5 DKGY IMD D BWD016 44.9 47.42 DKGY SIO 95 XQZ 5 PY QZ-SULPHIDE VEIN 10CM WITH OTHER REMNANT QTZ-SULPHIDE VEINS IN ALTERED ZONES. ALTERED ZONES ARE CLAY RICH AND FRIABLE. D BWD016 47.42 57.35 GY SIO 100 ZSZ 100 PY VERY FRACTURED CORE. SOME ZONES HAVE FRACTURES WITH A POLISHED SURFACE (NOT GRAPHITIC). PORPHYROBLASTIC. BEDDING SUB PARALLEL TO CORE AXIS. SULPHIDES FORMING VEINLETS AS ?INFILL OF FRACTURES D BWD016 57.35 59.8 DKGY SIO 100 CARB CARBONATE VEINING AND FRACTURE COATING. PORPHYROBLASTIC D BWD016 59.8 74.15 DKGY SIO 80 50 SSG 20 50 PY BEDDING AT HIGH ANGLE TO CORE AXIS. PORPHYROBLASTIC. DISSEMINATED PYRITE IN SOME ZONES. FINE GRAINED GREYWACKE D BWD016 74.15 81.73 DKGY SIO 100 D BWD016 81.73 83.34 DKGY SSG 70 50 SIC 30 20 GR D BWD016 83.34 84.65 BK SIC 100 GR PY MOSTLY GRAPHITIC ON FRACTURE PLANES. FEW 5-8CM THICK QTZ-SULPHIDE VEINS D BWD016 84.65 90.05 DKGY SSG 70 70 SIO 30 30 FRACTURE SURFACES POLISHED (NOT GRAPHITIC). D BWD016 90.05 93.07 DKGY SSG 100 PY QTZ-SULPHIDE VEINS AND VEINLETS COMMON D BWD016 93.07 94.1 DKGY SSG 80 XQZ 20 PY VEINS UP TO 10CM THICK WITH ~30-40% SULPHIDES WITHIN FINE TO MEDIUM GREYWACKE D BWD016 94.1 104.53 DKGY SSG 100 FINE TO COARSE GREYWACKE WITH COMMON QTZ VEINLETS AND OCCASIONAL 1-5CM QTZ-SULPHIDE VEINS D BWD016 104.53 107.4 DKGY SSG 75 150 SIC 25 40 GR COARSE GRAINED GREYWACKE WITH INTERBEDDED CARBONACEOUS MUDSTONE WITH POLISHED FRACTURE SURFACES D BWD016 107.4 108.3 GYWH XQZ 50 SIC 50 GR PY QTZ-SULPHIDE VEINS 25CM THICK D BWD016 108.3 111.53 DKGY SIO 75 60 SSG 25 20 D BWD016 111.53 113.08 DKGY SIO 70 XQZ 30 APY PY QTZ-SULPHIDE VEINS 10-20CM THICK. ~30% SULPHIDES (ARSENOPYRITE AND PYRITE) D BWD016 113.08 114.45 DKGY SSG 0 D BWD016 114.45 116.68 DKGY SIO 20 30 SSG 80 130 COARSE GRAINED GREYWACKE D BWD016 116.68 119.05 DKGY SIO 100 PY APY 10CM QTZ-SULPHIDE VEIN WITH 15% SULPHIDES D BWD016 119.05 122.76 DKGY SIO 60 40 SSG 40 30 D BWD016 122.76 131.05 DKGY SSG 70 100 SIO 30 40 GREYWACKE 20-100+ CM THICK INTERVALS WITH BALLS AND 'SWIRLS' OF MUDSTONE. SILT/MUDSTONE UP TO 60CM THICK D BWD016 131.05 139 DKGY SIO 65 90 SSG 35 55 ?HIGH STRAIN ZONE? D BWD016 139 156.5 DKGY SSG 100 FINE TO MEDIUM GRAINED GREYWACKE D BWD016 156.5 185.23 DKGY SSG 60 170 SIO 40 110 FINE TO COARSE GRAINED GREYWACKE. D BWD016 185.23 185.98 GYWH XQZ 90 SIO 10 CARB APY "MINOR SULPHIDES 2-3% APY. CARBONATE COMMON AND PINK MINERAL, POSSIBLY CARBONATE ALSO" D BWD016 185.98 206 DKGY SSG 83 150 SIO 17 30 PY APY DOMINATED BY COARSE GRAINED GREYWACKE WITH MUD/SILTSTONE INTERBEDS 15-50CM THICK. QTZ-SULPHIDE VEINING GENERALLY RESTRICTED TO FINE GRAINED INTERVALS. GREYWACKE INTERVALS TYPICALLY 150-200CM THICK. D BWD016 206 212.33 DKGY SIO 85 250 SSG 15 40 DOMINATED BY MUD/SILTSTONE WITH INTERBEDDED COARSE GRAINED SANDSTONE. SOME FINELY LAMINATED INTERVALS ON A MILLIMETRIC SSCLE MUD AND SILTSTONE. D BWD016 212.33 215.86 GYGN SIO 65 30 SSG 35 15 PY "ALTERED MUD/SILTSTONNE AN FINE GRAINED GREYWACKE, LIGHTER GREEN GREY IN APPEARANCE, VEINLETS AND STRINGERS COMMON, DISSEMINATED SULPHIDES." D BWD016 215.86 223 DKGY SSG 75 150 SIO 25 50 "MUDSTONE IS POSSIBLE WEAKLY GRAPHITIC, SILTSTONE OR VERY FINE GRAINED GREYWACKE." D BWD016 223 226.43 BK SIO 100 PY QUARTZ +/- SULPHIDE VEINING COMMON. VEINING POSSIBLY DUE TO STRUCTURE. D BWD016 226.43 227.77 GNGY SSG 100 PY "ALTERED VERY FINE GRAINED GREYWACKE? LITHOLOGY HARD TO DETERMINE DUE TO ALTERATION BUT APPEARS MORE COARSE THAN ABOVE. ALTERED TO A GREENISH GREY COLOUR, COMON QTZ +/- SUPHIDE VEINS AND QUARTZ STRINGERS. " D BWD016 227.77 228.2 BK SIO 100 QTZ VEINING/STRINGERS COMMON AND APPEARS DO TO POSSIBLE STRUCTURAL ALTERATION. D BWD016 228.2 230.34 DKGY SSG 100 MINOR MUDSTONE D BWD016 230.34 234 DKGY SIO 100 ZSZ 100 "HIGHLY FRACTURED. MINOR GRAPHITE, ON FEW FRACTURE PLANES." D BWD016 234 236.9 DKGY SSG 70 50 SIO 30 20 GREYWACKE IS VERY PORPHYROBLASTIC GIVING A COARSER GRAINED APPEARANCE HOWEVER IT IS FINE GRAINED - POSSIBLY SILTSTONE. D BWD016 236.9 252.25 DKGY SIO 75 90 SSG 25 30 VERY FINE GRAINED GREYWACKE. SHARP LITHOLOGICAL CONTACTS - WELL BEDDED D BWD016 252.25 253.34 BK SIC 55 35 SSG 45 30 GR INTERVALS OF CARBONACEOUS/GRAPHITIC MUDSTONE AND FINE GRAINED GREYWACKE D BWD016 253.34 259 DKGY SIO 50 SIC 30 XQZ 20 PY APY "MUDSTONE, GRAPHITIC IN PART AND SILTSTONE. COMMON QTZ-SULPHIDE VEINING. SULPHIDES ALSO PRESENT IN HOST ROCK." D BWD016 259 275.77 DKGY SSG 53 170 SIO 47 150 FINE GRAINED GREYWACKE. D BWD016 275.77 278.16 DKGY SIO 100 D BWD016 278.16 285.63 DKGY SIO 62 25 SSG 38 15 WELL BEDDED. POSSIBLE FAULT GOUGE AT 282.9-283M. D BWD016 285.63 296.87 DKGY SSG 80 150 SIO 20 20 "MUDSTONE BEDS 10-30CM, COARSER GRAINED BEDS ARE PORPHYROBLASTIC? COARSER AT BASE FINING UPHOLE. BEDDING IS WELL DEVELOPED. BASE ROCK IS FINE GRAINED - POSSIBLY SILTSTONE." D BWD016 296.87 300.85 DKGY SIO 100 PORPHYROBLASTIC. BEDDING WITH MUDSTONE AND SILTSTONE. CONTACT WITH ABOVE GREYWACKE HAS FLAME STRUCTURES AND LOAD CASTS INDICATING YOUNGING UP HOLE. D BWD016 300.85 305.53 DKGY SSG 80 100 SIO 20 20 "MUD/SILTSTONE 15-50CM INTERVALS, GREYWAWCKE IS FINE TO COARSE GRAINED ~100CM THICK" D BWD016 305.53 322.53 DKGY SSG 100 BOUNDARY WITH ABOVE UNIT IS GRADUAL. FINE TO COARSE GRAINED GREYWACKE. PORPHYROBLASTIC D BWD016 322.53 341.42 DKGY SSG 60 100 SIO 40 60 "PORPHYROBLASTIC. MUD/SILTSTONE TYPICALLY 60 CM THICK, GREYWACKE IS >100CM. DIFFICULT TO DETERMINE THICKNESSES DUE TO BEDDING BEING SUB PARALLEL TO CORE AXIS" D BWD016 341.42 345.4 DKGY SIO 60 70 SSG 40 50 PY QTZ SULPHIDE VEINING 344.0-344.7M ~10% SULPHIDES WITHIN VEIN. D BWD016 345.4 353.7 DKGY SIO 100 PREDOMINANTLY SILTSTONE (POSSIBLY VERY FINE GRAINED GREYWACKE) WITH MINOR MUDSTONE D BWD016 353.7 362.46 DKGY SIO 70 70 SSG 30 30 BEDDING SUBPARALLEL TO CORE AXIS THEREFORE DIFFICULT TO DETERMINE THICKENSSES OF SEQUENCES. GREYWACKE FINE TO MEDIUM GRAINED D BWD016 362.46 366.05 DKGY SSG 100 D BWD016 366.05 380.22 DKGY SSG 65 90 SIO 35 50 SERI "GREYWACKE BEDS RANGING FROM 50 TO 100+ CM, MUD/SILTSTONE FROM 3 TO 100+ CM. GREYWACKE IS MEDIUM TO COARSE GRAINED. STRONG SERICITE ALTERATION IN ZONES. BRECCIA ?FAULT BRECCIA 379.9-380.22" D BWD016 380.22 393.5 DKGY SIO 100 PY APY "MUDSTONE AND SILTSTONE. PREDOMINANTLY SILTSTONE WHICH IS VERY PORPHYROBLASTIC. PORPHYROBLASTS HAVE A FABRIC. ALTERATION VEINING COMMON WITHIN MUDSTONE. SILTSTONE LIGHTER IN COLOUR, POSSIBLY SERICITISED? LITHOLOGIES." D BWD016 393.5 396.55 DKGY SIO 65 60 SSG 35 30 "STRANGE ROCK 396-396.5M COARSER GRAINED, BLACK WITH WHITE SPECKS (LOOKS LIKE ?LAMPROPHYRE) AND SLIGHTLY SOFTER THAN SURROUNDING ROCKS. " D BWD016 396.55 402.18 DKGY SIO 100 SILTSTONE IS VERY PORPHYROBLASTIC WHICH FORMS A FABRIC. MOSTGLY SILTSTONE D BWD016 402.18 407.56 DKGY SIO 100 SERI PY "ALTERED DUE TO ?STRUCTURE BELOW. 'VEINING' OF ALTERATION WHEREBY IT IS LIGHTER AND APPEARS COARSER THAN SURROUNDING ROCK, SERICITISED? SULPHIDES COMMON WITHIN 'ALTERATION' AND HOST ROCK" D BWD016 407.56 409.6 DKGY SIO 100 ZSZ FRACTURED. TOP OFO ?SHEAR ZONE D BWD016 409.6 411.8 GY ZFG 100 "FAULT GOUGE, CLASTS IN A CLAY MATRIX. VERY FRIABLE. QTZ VEINING COMMON" D BWD016 411.8 415.2 DKGY ZSZ 100 SIO 100 VERY BROKEN GROUND. CORE LOSS. D BWD016 415.2 418.6 DKGY ZFX 100 SIO 80 SIC 20 CARB FAULT BRECCIA. CARBONATE VEINING COMMON. FAULT PLANE ALONG BEDDING SURFACE? D BWD016 418.6 420.45 DKGY SIO 100 PORPHYROBLASTIC D BWD016 420.45 424.25 GYGN ZSZ 100 SIO 100 ZFX 15 BROKEN GROUND WITH COMMON VEINING. FAULT BRECCIA/GOUGE 420.45-420.9M. PARENT ROCK IS ALTERED TO A LIGHTER COLOUR ?SERICITISED AND PORPHYRBLASTS REMAIN UNALTERED BY THIS PROCESS. D BWD016 424.25 428.1 DKGY SIO 75 SIC 25 ZSZ 100 GR PY "VERY FRACTURED, GRAPHITIC ON FRACUTRE PLANES, POSSIBLY SOME GREYWACKE (PITTED SURFACE COULD BE MAKING IT APPEAR COARSER GRAINED THAN IT IS). COMMON DISSEMINATED PYRITE IN 'COARSER GRAINED' UNITS" D BWD016 428.1 430.2 DKGY SSG 100 FRACTURED BUT LESS THAN ABOVE D BWD016 430.2 435.35 DKGY SIO 75 SIC 25 ZSZ 100 GR POSSIBLE FAULT GOUGE 433.5-433.8M. MINOR FAULT BRECCIA D BWD016 435.35 437.3 DKGY ZFX 100 D BWD016 437.3 458 GYGN SIO 100 ZSZ 100 FRACTURED. DENSE STOCKWORK OF VEINLETS. VARYING DEGREES OF ALTERATION WITH A GREEN TINGE TO ROCK. MINOR RAPHITE ON FRACTURE SURFACES. D BWD016 458 462 DKGY SIO 70 45 SSG 30 20 SOME PERVASIVE LTERATION MAKING ROCK OLIVE GREEN IN PART. MORE COMPETENT THAN ABOVE AND BELOW ROCKS D BWD016 462 465.17 DKGY SIO 70 45 SSG 30 20 ZSZ AS ABOVE WITH INCREASE OF FRACTURING AND CLAY D BWD016 465.17 467.63 DKGY SIO 100 "COMPETENT ROCK, SILTIER INTERBEDS ARE SLIGHTLY ALTERED" D BWD016 467.63 485.42 DKGY SIO 50 40 SSG 50 40 MUD/SILTSTONE BEDS FROM 6-80CM THICK AND MEDIUM TO COARSE GRAINED GREYWACKE BEDS 3-90CM THICK. APPEARS TO BE A FINING UPWARDS SERIES OF SUCCESSIONS D BWD016 485.42 489.93 DKGY SIO 100 D BWD016 489.93 490.8 GYBE SIO 100 ALTERED ?SERICITISED. PALE GREY/YELLOW/GREEN IN COLOUR EXCEPT FOR PORPHYROBLASTS WHICH REMAIN UNALTERED. ROCK TEXTURE (I.E. BEDDING) IS RETAINED. MICAS IN QTZ VEINLETS WITH A SLIGHT IRRIDESCENCE D BWD016 490.8 509.82 DKGY SIO 100 INTERBEDDED MUDSTONE AND SILTSTONE. MINOR ZONES OF ALTERATION (504.7-504.9M) D BWD016 509.82 516 GY SIO 100 "ALTERED ?SERICITISED, 'BLEACHED' IN PART. HIGH DENSITY OF QUARTZ VEINING, STOCKWORK VEINING. " D BWD016 516 522.88 DKGY SIO 100 POSSIBLY ?SERICITISED IN MINOR INTERALS D BWD016 522.88 530 DKGY SSG 100 "QTZ VEINING COMMON, 1-2CM WIDE. RARE STOCKWORKED VEINS. MEDIUM TO COARSE GRAINED" D BWD016 530 537.9 DKGY SIO 100 PY DISSEMINATED SULPHIDES VERY COMMON. SERICITISED PREFERENTIALLY ON ?SILTIER BEDS - PYRITE ASSOCIATED WITH THESE ?BEDS. D BWD016 537.9 540 DKGY SIO 80 XQZ 20 PY GREENISH MINERAL WITH 3% Mg ASSOCIATED WITH FELDSPAR? SPOTS. ?GLAUCONITE. STOCKWORKED VEINS. D BWD016 540 548.44 DKGY SSG 100 MEDIUM TO COARSE GREYWACKE D BWD016 548.44 558.5 DKGY SSG 75 100 SIO 25 30 FLAME STRUCTURES INDICATE YOUNGING UPHOLE. END OF HOLE. D BWD017 0 5.6 RDBR RTO 100 mottled clay with rounded qz frags D BWD017 5.6 20.5 BE SIO 100 D BWD017 20.5 21.85 OR SSG 100 possible greywacke? Not sure D BWD017 21.85 34 OR SSG 100 Extremely weathered and 6m core loss. Loss associated with hypothesised fault? D BWD017 34 35.6 GYOR SSG 100 D BWD017 35.6 36.35 GY SSG 100 NOT sure if dolerite or greywacke?? D BWD017 36.35 98.4 GY IMD 100 def dolerite. D BWD017 98.4 100.4 DKGY SSG 100 D BWD017 100.4 103 BE SSG 80 SIO 20 SE SERICITE ALT? D BWD017 103 111 DKGY SSG 100 SMALL SPOTS D BWD017 111 121.5 DKGY SSG 80 SIO 20 D BWD017 121.5 125.65 DKGY SIC 60 SSG 40 MAYBE NOT CLASSIC SIC LITH TYPE D BWD017 125.65 146.1 DKGY SSG 90 SIO 10 10 D BWD017 146.1 148.15 BK SIC 100 GR STRETCHED PORPHYROBLASTS TO 1MM D BWD017 148.15 158.1 DKGY SIO 100 10 D BWD017 158.1 168.05 DKGY SIO 70 5 SSG 30 INTERBEDDED BUT DOM BY FINE GRAINED SEDS D BWD017 168.05 171.85 DKGY SSG 100 D BWD017 171.85 180.25 BK SIC 95 5 SSG 5 D BWD017 180.25 198.35 DKGY SIO 80 5 SSG 20 20 SOME SIO CLOSE TO BEING SIC D BWD017 198.35 200.75 DKGY SIO 60 SIC 30 SSG 10 MAJOR STRUCTURE ROCK CATACLASITE. CLAST SUPPORTED TECTONIC BRECCIA D BWD017 200.75 206.3 DKGY SSG 80 SIO 20 BRECCIATED ROCKS IN THE FOOTWALL OF MAJOR STRUCTURE ABOVE D BWD017 206.3 217.9 DKGY SSG 90 SIO 10 D BWD017 217.9 222.7 DKGY SIO 100 D BWD017 222.7 241.1 BK SIC 100 FOLIATION DEFINED BY PORPHYROBLASTS BUT HARD TO SEE DEFINITIVE BEDDING D BWD017 241.1 246.45 DKGY SSG 85 SIO 10 SIC 5 CRACKLE-MOSAIC BRECCIA TEXTURE IN PLACES D BWD017 246.45 247 BK SIC 100 D BWD017 247 248 DKGY SIO 100 10 D BWD017 248 248.15 BK SIC 100 D BWD017 248.15 255.25 DKGY SIO 95 3 SSG 5 D BWD017 255.25 262.2 DKGY SSG 80 SIO 20 5 D BWD017 262.2 269.5 DKGY SIO 100 VERY SPOTTY WITH PORPHYROBLASTS TO 1-2MM D BWD017 269.5 273 DKGY SSG 66 10 SIO 34 FINE GRAINED SSG D BWD017 273 312.9 DKGY SSG 90 SIO 10 20 GARNET PORPHYROBLASTS? AROUND 274???? D BWD017 312.9 313.25 BK SIC 100 POSSIBLE CARBONACEOUS MUDSTONE D BWD017 313.25 322.1 DKGY SSG 100 D BWD017 322.1 322.75 DKGY SIO 100 3 D BWD017 322.75 328.5 DKGY SSG 95 SIO 5 3 D BWD017 328.5 347.05 DKGY SIO 95 2 SSG 5 D BWD017 347.05 354.35 DKGY SIC 6 6 SIO 92 8 SSG 2 NOT TYPICAL BUT BLACK MUDSTONES INTERBEDDED WITH MUDSTONE/SILTSTONE BEDS. POSSIBLE CARBONACEOUS UNITS. EOH @354.35M D BWD018 0 2 BR ROO D BWD018 2 10.98 BE SSG SIO D BWD018 10.98 12.6 BR SIO VERY WEATHERED SILTSTONE? D BWD018 12.6 26.4 BE SSG D BWD018 26.4 34 DKGY SSG 90 SIO 10 8 TRANSITION FROM WEATHERED TO FRESH IS RAZOR SHARP D BWD018 34 38.9 DKGY SIO D BWD018 38.9 41.4 DKGY SSG 100 D BWD018 41.4 42.41 DKGY SSG 80 SIO 20 5 VERY DARK GREY ALMOST BLACK SILTSTONE/MUDSTONE. NOT QUITE CARBONACEOUS MUDSTONE (SIC) BUT IF IT NEEDS TO FIT THE MODEL THEN IT COULD AT A PINCH D BWD018 42.41 54.31 DKGY SSG 100 D BWD018 54.31 56 DKGY SSG 85 SIC 12 10 SIO 3 POSSIBLE SIC BUT NOT CLASSIC D BWD018 56 73.25 DKGY SSG 95 SIO 5 5 D BWD018 73.25 77.7 DKGY SIO 95 5 SSG 5 D BWD018 77.7 83.5 DKGY SIC 15 5 SIO 80 5 SSG 5 NOT FULL ON CARBONACEOUS MUDSTONE BUT DEF BLACKER THAN DK GREY MUDSTONE D BWD018 83.5 89.7 DKGY SIO 60 5 SSG 40 D BWD018 89.7 89.9 BK SIC 100 D BWD018 89.9 97.5 DKGY SSG 80 SIO 20 5 D BWD018 97.5 99 DKGY SIO 50 3 SSG 50 DARK GREY MUDSTONE BUT NOT BLACK ENOUGH FOR SIC D BWD018 99 119.3 DKGY SSG 90 SIO 10 5 D BWD018 119.3 122.7 DKGY SIC 20 2 SIO 5 SSG 75 MAYBE NOT CLASSIC SIC BUT BLACKISH MUDSTONE INTERBEDDED WITH GREYWACKE AND MUD/SILTSTONE D BWD018 122.7 145.91 DKGY SSG 90 SIO 10 5 LOOKS LIKE YOUNGING UP HOLE D BWD019 0 2 RDBR UOO 100 D BWD019 2 23.9 BE SSG 95 SIO 5 D BWD019 23.9 34 DKGY SSG 100 FE OX ON JOINTS OTHERWISE FRESH D BWD019 34 48.5 DKGY SSG 95 SIO 5 BLOCKY AND VERY JOINTY D BWD019 48.5 55.5 DKGY SSG 90 SIO 10 4 D BWD019 55.5 61.7 DKGY SIO 90 SSG 10 D BWD019 61.7 63.8 DKGY SIC 33 SSG 33 SIO 33 MOSAIC/CRACKLE BRECCIA D BWD019 63.8 67.2 DKGY SSG 30 SIO 70 D BWD019 67.2 75.5 DKGY SIC 15 20 SSG 20 SIO 65 D BWD019 75.5 87.2 DKGY SSG 100 SERI crackle to mosaic breccia. Fairly intact rock mass apart from structures hosted within. WEAK PERVASIVE SERICITE ALT D BWD019 87.2 92.6 DKGY SSG 80 SIO 20 MOSTLY MOSAIC BRECCIA. BACKGROUND ROCK MASS LARGELY INTACT. PERVASIVE SERICITE ALTERATION D BWD019 92.6 101 DKGY SSG 80 SIO 20 25 D BWD019 101 108 DKGY SIC 50 SIO 50 XCO CAL QZ INTERBEDDED SILTSTONE AND MUDSTONE WITH SOME SERICITISATION AND BRECCIATED CARBONATE VEIN D BWD019 108 113.9 GY SIO 50 SSG 50 SERI D BWD019 113.9 116 GY SIO 40 SSG 40 XQO 20 QZ SERI D BWD019 116 122.8 GY SSG 70 SIO 25 XQO 5 SERI D BWD019 122.8 133.68 LTGY SSG 60 SIO 30 XQO 10 QZ PY MOSTLY INTERBEDDED GREYWACKE AND SILTSTONE WITH SOME PYRITE FORMING IN THE MORE CARBONACEOUS FRACTURES ALONG WITH TRACES OF CHLORITE D BWD019 133.68 145.1 DKGY SIC 80 SIO 10 XQO 10 QZ GR INTENSELY FAULTED ZONE WITH LOTS OF RUBBLE-GOUGES AND FRAGMENTED CARBONACEOUS MATERIAL WITH TRACES OF SERICITE AROUND 139M D BWD019 145.1 147.41 DKGY XQZ 50 SIC 50 QZ PY INTENSLEY FRACTURED ZONE WITH A LARGE QZ VEIN AND SOME SULPHIDES WITHIN THE VEIN D BWD019 147.41 149.51 LTGY SIC 50 CLAY GR LIGHT GREY CLAY FILLED FRACTURE ZONE THAT MAY HAVE BEEN A FAULT WITH SOME CLAY MINERALS ACCUMULATING D BWD019 149.51 156.61 GY SIO 40 SSG 40 XQO 10 QZ PY D BWD019 156.61 159.46 DKGY SIC 100 GR PY PY DISSEMINATED WITHIN THE FINE GRAINED MATRIX AND ON THE FRACTURE ZONES D BWD019 159.46 163.2 GY SIC 70 SSG 30 GR APY D BWD019 163.2 170 GY SSG 60 SIC 35 XQZ 5 QZ APY D BWD019 170 171 XQZ 80 SIO 20 QZ APY PREDOMINANTLY A QZ VEIN D BWD019 171 174.92 GY SSG 50 SIO 50 D BWD019 174.92 175 XQZ 100 D BWD019 175 184.78 GY SSG 60 SIO 30 XQZ 10 QZ APY D BWD019 184.78 185.9 DKGY SIC 80 XQZ 20 APY QZ THICK 20CM QZ-SULPHIDE VEIN D BWD019 185.9 189.5 GY SIO 80 SSG 20 GR CAL D BWD019 189.5 200.1 GY SSG 90 SIO 9 XQZ 1 GR CAL D BWD019 200.1 201.41 GY SIO 65 XQZ 35 QZ APY D BWD019 201.41 206.08 GY SSG 100 QZ APY D BWD019 206.08 213.05 DKGY SIO 70 XQO 30 QZ CAL D BWD019 213.05 221.75 GY SSG 90 XQO 10 SERI QZ D BWD019 221.75 230.3 DKGY SSG 60 SIO 30 XQZ 10 QZ PY D BWD019 230.3 233 LTGY SSG 90 SIO 10 D BWD019 233 234.41 GY SIO 45 SSG 45 XQZ 10 QZ PY D BWD019 234.41 236.3 LTGY SSG 98 XQO 2 QZ D BWD019 236.3 238.2 GY SSG 90 SIO 10 D BWD019 238.2 275.2 LTGY SSG 45 SIO 45 XQO 10 QZ CL TRACES OF PYRITE WITHIN A QZ -CHLORITE-SULPHIDE VEIN AT APPROXIMATELY 258.5M IN DEPTH D BWD019 275.2 276 LTGY SSG 70 XQO 30 QZ PL CHLORITE FORMING ON SOME OF THE QZ VEIN SELVAGES AS WELL AS A K-FELDSPAR VEIN CROSSCUTTING A QZ VEIN D BWD019 276 291.02 GY SSG 60 SIO 35 XQO 5 QZ PY D BWD019 291.02 302.65 DKGY SIO 95 XQO 5 QZ PY 6CM THICK QZ-SULPHIDE VEIN AS WELL AS VISIBLE GRAPHITIC MATERIAL D BWD019 302.65 315.59 LTGY SIO 60 SSG 40 MINOR GRAPHITE ON FRACTURE SURFACES D BWD019 315.59 324.41 DKGY SIO 70 15 SIC 30 10 PY INTERBEDDED MUD/SILTSTONE AND CARBONACEOUS MUDSTONE. PORPHYROBLASTS ASSOCIATED WITH CARBONACEOUS UNITS. SHARP BOUNDARIES APART FROM 30CM ZONE AT 321.6M WHERE MIXING OF TWO UNITS OCCURS WITH ABUNDANT SULPHIDES. END OF HOLE @ 324.41M D BWD020 0 1.5 RDBR UOO 100 D BWD020 1.5 3.1 BN SSG 100 D BWD020 3.1 5 RDBR RRR 100 D BWD020 5 26.47 BN SSG 95 XQO 5 QZ SOME QZ VEINING THROUGHOUT THE MODERATELY WEATEHRED SANDSTONE D BWD020 26.47 33.3 GY SSG 90 SIO 9 XQO 1 QZ D BWD020 33.3 50.9 GY SSG 50 SIO 45 XQZ 5 QZ APY D BWD020 50.9 62.3 GY SIO 70 SSG 25 XQO 5 QZ GR SEDIMENTARY UNIT IS PREDOMINANTLY FINER GRAINED D BWD020 62.3 66.4 DKGY SIC 60 SIO 30 SSG 10 GR D BWD020 66.4 72.2 GY SIO 70 SSG 30 D BWD020 72.2 75.2 GY SIO 50 SIC 50 GR D BWD020 75.2 82.4 GY SSG 60 SIO 30 XQZ QZ PY D BWD020 82.4 91.8 DKGY SIO 95 XQO 5 QZ PY SMALL QZ VEIN AND A CONSIDERABLE AMOUNT OF DISSEMINATED PYRITE IN THE FORM OF PORPHYRY BLASTS AND FRACTURE COATING IN THE FINER GRAINED MATERIAL D BWD020 91.8 92.1 XQO 90 SIO 10 QZ PY D BWD020 92.1 95.3 DKGY SIO 55 SSG 40 XQZ QZ PY PTIGMATIC QZ VEIN RUNNING PARALLEL TO THE CORE AXIS D BWD020 95.3 96.1 GY SSG 50 XQZ 50 QZ APY BRECCIATED SUBHEDRAL ARSENOPYRITE FRAGMENTS WITHIN THE SEDIMENTARY ROCK D BWD020 96.1 97.4 GY SSG 50 SIO 50 APY BRECCIATED SUBHEDRAL ARSENOPYRITE FRAGMENTS WITHIN THE GREYWACKE UNIT D BWD020 97.4 100.7 GY SSG 45 SIO 55 XQZ QZ PY D BWD020 100.7 103.4 LTGY SIO 100 FINERGRAINED ZONE WITH SOME CLAY MINERALS AND HIGHLY FRACTURED DUE TO A FAULT D BWD020 103.4 105 XQZ 100 QZ PY THICK QZ VEIN WITH STRINGER VEINS OF PYRITE THROUGHOUT SECTION OF THE VEIN D BWD020 105 106.36 LTGY SSG 100 D BWD020 106.36 107.35 DKGY SSG 60 XQO 40 QZ PY D BWD020 107.35 133.4 DKGY SSG 80 SIO 20 MUDSTONE BEDS 1-20CM AND SANDSTONE 15 TO >1M. OCCASIONAL RIPUP CLASTS D BWD020 133.4 142.7 DKGY SSG 80 80 SIC 20 20 YOUNGING UPHOLE (FLAME STRUCTURES/LOAD CASTS). D BWD020 142.7 146.07 GY SSG 70 SIO 30 D BWD020 146.07 147.55 DKGY SIO 75 40 SIC 25 15 GR ?CARBONACEOUS MUDSTONE INTERBEDS D BWD020 147.55 151.05 DKGY SIO 100 ZSZ 100 HIGHLY FRACTURED ZONE WITH MINOR FAULT GOUGE @ 148.8M D BWD020 151.05 155.1 DKGY SIC 55 15 SIO 45 10 GR CARBONACEOUS MUDSTONE INCREASING WITH DEPTH. GRAPHITE ON FRACTURE SURFACES. D BWD020 155.1 168.5 GY SSG 90 100 SIO 10 15 MOSTLY MEDIUM TO COARSE GRAINED GREYWACKE WITH INTERBEDS AND LAMINATED MUDSTONE WITH OCCASIONAL RIP UP CLASTS. D BWD020 168.5 177 DKGY SSG 75 20 SIC 15 5 SIO 10 3 YOUNGING UPHOLE INDICATED BY FLAME STRUCTURES AND LOAD CASTS. SEQUENCES OF INTERBEDDED CARBONACEOUS MUDSTONE AND MUD/SILSTONE AND MEDIUM TO COARSE GRAINED GREYWACKE. D BWD020 177 193 GY SSG 75 100 SIO 20 30 SIC 5 2 "MEDIUM TO COARSE GRAINED GREYWACKE WITH INTERBEDDED MUD/SILSTONE PACKAGES, POSSIBLY MINOR CARBONACEOUS BEDS. YOUNGING UPHOLE" D BWD020 193 208.25 GY SSG 85 100 SIO 15 10 MEDIUM TO COARSE GRAINED GREYWACKE WITH INTERBEDDED MUDSTONE/SILTSTONE. D BWD020 208.25 220.95 GY SIO 90 100 SSG 10 15 "GRADED BEDS, YOUNGING UPHOLE FROM MEDIUM/COARSE GRAINED GREYWACKE TO MUDSTONE" D BWD020 220.95 228.5 DKGY SSG 75 100 SIO 20 15 SIC 5 2 ?SHEAR ZONE 223.35-223.85M. D BWD020 228.5 229.86 DKGY SIC 70 20 SIO 15 15 SSG 10 10 SOME BEDS ARE OFFSET BY 1-2CM D BWD020 229.86 236 DKGY SSG 100 VERY MINOR RIP-UP CLASTS D BWD020 236 254.7 DKGY SSG 70 100 SIO 30 15 COARSE GRAINED GREYWAKCE WITH INTERBEDDED (SOMETIMES FINELY LAMINTED DARK AND LIGHT GREY) SILT/MUDSTONE D BWD020 254.7 260.4 DKGY SIO 100 FINELY LAMINATED SILTSTONE AND MUDSTONE. BEDS ARE 1-5CM THICK. D BWD020 260.4 266.1 BK IMD 100 BI BIOTITE RICH DOLERITE. BIOTITE IS COARSE GRAINED. TOWARDS BOTTOM OF UNIT IT BECOMES FINER GRAINED WITH GRADATIONAL CONTACT WITH UNDERLYING SILT/MUDSTONE D BWD020 266.1 269.23 DKGY SIO 90 30 SIC 10 1 ZSZ GR "FRACTURED GROUND, INTERBEDS AND ?RIP-UP CLASTS OF ?CARBONACEOUS MUDSTONE WITHIN MUD/SILTSTONE. QUARTZ VEINS COMMON" D BWD020 269.23 272.12 DKGY SSG 90 100 SIO 10 10 MUDSTONE INTERBEDS FROM 0.5-10 CM D BWD020 272.12 274.48 DKGY SIO 100 0.5 FINELY LAMINATED SILTSTONE AND MUDSTONE. BEDS ARE FROM 2MM TO 30MM THICK. D BWD020 274.48 312.97 DKGY SSG 85 40 SIO 15 10 SERIES OF FINING UP SUCCESSIONS. SEDIMENTARY SEQUENCES ARE ~50-60CM IN UPPER PART OF UNIT TO 150CM LOWER DOWN IN HOLE. OCCASIONAL LAMINATED MUDSTONE/SILTSTONE D BWD020 312.97 324.75 DKGY SIO 100 MILDLY ALTERED (?SERICITISE/BLEACHED) IN PART UP TO 10CM. REMAINDER UNALTERED. 320.4-320.6M FAULT GOUGE. D BWD020 324.75 329.77 DKGY SSG 60 50 SIO 40 30 "SEVERAL SEDIMENTARY SUCCESIONS FROM GREYWACKE TO MUDSTONE, FINING UPHOLE." D BWD020 329.77 337.1 DKGY SIO 80 SSG 20 PARTIALLY ALTERED (?SERICITISED/BLEACHED). PORPHYROBLASTIC IN PART D BWD020 337.1 338.22 PIGY SIO 85 SSG 15 SE "ALTERED TO PINKISH/YELLOW GREY, POSSIBLE SERICITISATION, BLEACHING, SILICIFICATION. " D BWD020 338.22 348.82 GY SIO 80 SSG 20 "PARTIALLY ALTERED (?SERICITISED/BLEACHED), PREFERENTIALLY ALONG BEDDING IN MORE COARSER GRAINED INTERVALS I.E. SILTSTONE. PORPHYROBLASTIC IN PART" D BWD020 348.82 351.08 GY SIO 100 ZSZ HIGHLY FRACTURED SILTSTONE WITH SOME MINOR 2CM THICK FAULT GOUGES. D BWD020 351.08 354.4 GY SIO 80 SSG 20 "SEDIMENTARY SEQUENCE FROM GREYWACKE TO MUDSTONE, YOUNGING UPHOLE." D BWD020 354.4 359.84 GY SSG 100 COARSE GRAINED GREYWACKE. VERY MINOR MUD/SILTSTONE D BWD020 359.84 383.82 GY SSG 80 100 SIO 20 5 COARSE GRAINED GREYWACKE GRADING (UPHOLE) INTO SILT/MUDSTONE. SILT/MUDSTONE BEDS ARE 5-15CM THICK. D BWD020 383.82 390.95 DKGY SIO 100 XQZ PY QZ-SULPHIDE VEINS COMMON WITH ~5% SULPHIDE CONTENT. POSSIBLY CARBONACEOUS IN PART. D BWD020 390.95 396.72 GY SSG 85 100 SIO 15 20 "SEVERAL SEDIMENTARY SUCCESIONS FROM GREYWACKE TO MUDSTONE, FINING UPHOLE." D BWD020 396.72 404.5 DKGY SIO 100 MUDSTONE AND SILTSTONE. PORPHYROBLASTIC IN PART. D BWD020 404.5 407.75 DKGY SIO 80 50 SIC 20 10 INTERBEDDED DARK AND LIGHT MUD/SILSTONE. DARKER INTERVALS MAY BE CARBONACEOUS D BWD020 407.75 413.66 DKGY SIO 100 INTERBEDDED DARK AND LIGHT MUD/SILSTONE. DARKER INTERVALS NOT AS ?CARBONACEOUS AS ABOVE UNIT. D BWD020 413.66 422.27 LTGY SIO 90 100 SSG 10 5 PARTIALLY ALTERED LTHOLOGICALLY BOUND TO A LIGHTER GREY YELLOW. POSSIBLY SILICIFIED IN PART. D BWD020 422.27 425 DKGY SIO 100 ZFX 75 ZFZ 100 GR FAULT BRECCIA/FAULT GOUGE. QTZ ALTERATION AND INFILL COMMON. GRAPHITE ON FRACTURE SURFACES. STOCKWORK/RANDOMLY ORIENTED QTZ VEINING AND QUARTZ AS FRAGMENTS IN FAULT BRECCIA/GOUGE. MINOR SULPHIDES WITHIN MATRIX. D BWD020 425 428.1 GYWH SSG 100 XQO 50 ZFZ 100 GR CL "STRUCTURALLY ALTERED ZONE. ABUNDANT STOCKWORKED/RANDOMLY ORIENTED QUARTZ VEINING THROUGHOUT, DRUZY IN PART, WHITE AND GENERALLY NOT ASSOCIATED WITH SULPHIDES. CHLORITE? EPIDOTE? FORMING LIGHT GREEN 'STAINING' IN PART. SULPHIDES IN MATRIX AND RARE VEINLE" D BWD020 428.1 430.3 DKGY SSG 100 ZFX 80 GR PY MODERATE STRUCTURAL ALTERATION. VEINING COMMON WITH HOST ROCK CONTAINING APPEARANCE OF QUARTZ 'MOTTLING'. ROCK HAS A SLIGHT FABRIC DEFINED BY QUARTZ 'MOTTLING'. DISSEMINATED PYRITE COMMON. D BWD020 430.3 434.4 DKGY SIO 60 100 SSG 40 90 "SEVERAL SEDIMENTARY SUCCESIONS FROM GREYWACKE TO MUDSTONE, FINING UPHOLE." D BWD020 434.4 434.95 DKGY SIC 50 20 SIO 50 20 D BWD020 434.95 436.9 DKGY SIO 60 SSG 40 SEVERAL SEDIMENTARY SUCCESIONS FROM GREYWACKE TO MUDSTONE. D BWD020 436.9 447.7 GY SSG 100 MEDIUM TO COARSE GRAINED GREYWACKE. POLISHED FRACTURE SURFACES. D BWD020 447.7 450 GYWH SIO 100 XQO 45 ZFZ 100 GR STRUCTURALLY ALTERED ZONE. FAULT BRECCIA/ IN PART WITH QTZ VEINING FRAGMENTED INPART. POND SLIME GREEN MINERAL OVERPRINT ON QTZ VEINS AND HOST ROCK. QTZ VERY COMMON. GRAPHITE ON FRACTURE SURFACES. STOCKWORK/RANDOMLY ORIENTED QTZ VEINING AND QUARTZ AS FRAG D BWD020 450 451.78 DKGY SIC 60 SIO 40 GR CARBONACEOUS MUDSTONE AND DARK POSSIBLY CARBONACEOUS SILTSTONE. GRAPHITE ON FRACTURE SURFACES. HIGHLY FRACTURED IN UPPER PART. D BWD020 451.78 452.88 GYWH XQO 95 SSG 5 CHLORITE ON FRACTURE SURFACES AND 'CLASTS' OF GREYWACKE D BWD020 452.88 465.7 DKGY SSG 60 280 SIO 40 200 THICK BEDS OF COARSE GRAINED GREYWACKE AND SILTSTONE. MUDSTONE PROPHYROBLASTIC D BWD020 465.7 473.55 DKGY SSG 50 SIC 35 SIO 15 PY GR DARKER IN COLOUR - POSSIBLY SLIGHTLY CARBONACEOUS. QTZ-SULPHIDE VEINS COMMON. CONTACTS ARE GRADATIONAL OR MIXED/SWIRLY. GRAPHITIC ON SOME FRACTURE SURFACES. D BWD020 473.55 489.5 DKGY SSG 60 100 SIO 40 50 SEVERAL SEDIMENTARY SUCCESIONS FROM GREYWACKE TO MUDSTONE. D BWD020 489.5 492.3 DKGY SIO 100 POSSIBLY CARBONACEOUS AS IT IS DARKER THAN ABOVE. D BWD020 492.3 494.9 DKGY SIO 80 SIC 20 ZSZ 100 GR PY STRUCTURALLY/HYDROTHERMALLY? ALTERED ZONE. ROCK HAS TAKEN ON A 'STETCHED' APPEARANCE WITH AGILISATION BETWEEN FRACTURES (2CM THICK). D BWD020 494.9 497.36 DKGY SIO 100 PORPHYROBLASTIC. INTERBEDDED SILTSTONE AND MUDSTONE. D BWD020 497.36 505.25 GYBE SIO 100 "ALTERED SILTSTONE, ?BLEACHED TO A LIGHT GREY/YELLOW IN PART. ?SILICIFIED. ABUNDANT CLOSED FRACTURES - PERVASIVE BLEACHING FROM FRATURES ~2-3MM INTO HOST ROCK." D BWD020 505.25 524.4 DKGY SIO 80 60 SSG 20 30 D BWD020 524.4 541.36 GYBE SSG 60 SIO 40 ALTERED GREYWACKE AND SILT/MUDSTONE. ?BLEACHED TO A LIGHT GREY/YELLOW IN PART. ?SILICIFIED. 50% ALTERED D BWD020 541.36 547.5 DKGY SIO 100 D BWD020 547.5 558.3 DKGY SSG 80 100 SIO 20 25 SEDIMENTARY SUCCESSIONS OF MEDIUM GRAINED GREYWACKE TO MUDSTONE. GRADED BEDS AND FLAME STRUCTURES INDICATE YOUNGING UPHOLE. D BWD020 558.3 561.35 GYBE SSG 80 100 SIO 20 25 "AS ABOVE HOWEVER ALTERED/?BLEACHED TO A LIGHT GREY/YELLOW COLOUR IN PARTS, PERMIATING FROM FRACTURES." D BWD020 561.35 588.03 GY SSG 65 100 SIO 35 50 SEDIMENTARY SUCCESSIONS OF MEDIUM GRAINED GREYWACKE TO MUDSTONE. D BWD020 588.03 597.1 DKGY SIO 70 100 SSG 40 20 SEDIMENTARY SUCCESSIONS OF MEDIUM GRAINED GREYWACKE TO MUDSTONE. YOUNGING UPHOLE D BWD020 597.1 624.3 DKGY SSG 60 100 SIO 40 80 SEDIMENTARY SUCCESSIONS OF MEDIUM GRAINED GREYWACKE TO MUDSTONE. YOUNGING UPHOLE. END OF HOLE.