H0002 Version 1 H0003 Generated 11-Aug-2021 H0004 Reporting Period End_Date 16-Jun-2021 H0005 State NT H0100 Tenement_No EL 31350 H0101 Tenement_holder Newmont Exploration Pty Ltd H0102 Project_name Fenton South H0106 Tenement_Operator Newmont Exploration Pty Ltd H0150 Map_sheet_number  250000 SD52-08 H0151 Map_sheet_number 100000 5170 H0200 Start_date_of_acquisition 22-Jun-2017 H0201 End_date_of_acquisition 16-Jun-2021 H0202 Template_format DG1 H0203 Number of data_records 739 H0204 Date of Metadata_update 11-Aug-2021 H0300 Related_data_filenames H0301 Location_Data_File EL31350_2021_S_03_DrillCollars.txt H0302 Geology_Data_File EL31350_2021_S_06_DrillholeLithologyLogs.txt H0303 DHAssay_Data_File EL31350_2021_S_04_DownholeAssays.txt H0304 Survey_Data_File EL31350_2021_S_05_DownholeSurveys.txt H0307 Lithology_Code_File EL31350_2021_S_07_LithologyCodeList.txt H0400 Drill_Code CORE H0402 Description Diamond drill core H1000 HOLE_ID START DEPTH END DEPTH DRILL_TYPE TN_Colour TN_Lith1_Code TN_Lith1_GrainSize TN_Lith1_Texture TN_Lith2_Code TN_Lith2_GrainSize TN_Lith2_Texture TN_ORIENTED_CORE TN_Arsenopyrite_Pct TN_Arsenopyrite_Style TN_Pyrite_Pct TN_Pyrite_Style TN_Pyrrhotite_Pct TN_Pyrrhotite_Style TN_Sed_Structure TN_STRUC_TYPE TN_Structure_Comments TN_Structure_Intensity TN_Structure_Type TN_VeinSet1_Density TN_LITH_COMMENTS H1001 Meters Meters D KAD0001 0 3 CORE YE CLY MUD MAS LATT MSD MAS YES D KAD0001 3 8 CORE LGY SDST FS MAS YES D KAD0001 8 13.85 CORE RDBN CLY MUD MAS YES D KAD0001 13.85 15.4 CORE RDBN SLST SLT MAS YES D KAD0001 15.4 26.6 CORE GY SLST SLT LAM YES Planar to irregularly laminated siltstone. D KAD0001 26.6 34.2 CORE LGY SLST SLT LAM SLST SLT MAS YES D KAD0001 34.2 38.1 CORE YE SLST SLT LAM SLST SLT MAS YES D KAD0001 38.1 39.4 CORE RDBN SDST EFS LAM SDST EFS MAS YES D KAD0001 39.4 42.3 CORE RDBN SDST EFS MAS YES D KAD0001 42.3 48 CORE LGY SDST EFS MAS YES D KAD0001 48 51 CORE RDBN SDST EFS MAS YES D KAD0001 51 57.5 CORE LGY SDST EFS MAS YES D KAD0001 57.5 65.9 CORE LGY SLST SLT MAS YES W FRS D KAD0001 65.9 95.5 CORE GY CNGL MUD MAS LMST MUD MAS YES D KAD0001 95.5 95.75 CORE GY CNGL MUD MAS LMST MUD MAS YES M FO D KAD0001 95.75 98.85 CORE GY CNGL MUD MAS LMST MUD MAS YES D KAD0001 98.85 103.5 CORE LGY LMST MUD LAM LMST MUD MAS YES D KAD0001 103.5 103.8 CORE LGY SLST SLT MAS YES Clast-supported monomictic-siltstone breccia. M FBH D KAD0001 103.8 107.2 CORE LGY SLST SLT LAM YES D KAD0001 107.2 108 CORE LGY SLST SLT MAS SLST SLT LAM YES D KAD0001 108 110 CORE RDBN SLST SLT MAS SLST SLT LAM YES D KAD0001 110 110.2 CORE RDBN SLST SLT MAS SLST SLT LAM YES Minor monomictic conglomerate horizon. D KAD0001 110.2 110.9 CORE RDBN SLST SLT MAS SLST SLT LAM YES D KAD0001 110.9 111.5 CORE RDBN SDST EFS MAS YES D KAD0001 111.5 112.45 CORE RDBN SDST CS MAS YES D KAD0001 112.45 112.7 CORE RDBN SDST EFS MAS YES D KAD0001 112.7 113.7 CORE LGY SDST EFS MAS YES D KAD0001 113.7 114.25 CORE LGY SDST EFS MAS SDST EFS BX YES D KAD0001 114.25 114.35 CORE GY FZ EFS BX YES Clast-supported polymictic breccia. S FBH D KAD0001 114.35 114.9 CORE YE SLST SLT MAS YES D KAD0001 114.9 115 CORE YE SLST SLT MAS SLST SLT BX YES Healed matrix-supported (calcite) monomictic breccia. W FBH D KAD0001 115 115.3 CORE YE MDST MUD MAS YES D KAD0001 115.3 115.4 CORE YE MDST MUD MAS SLST SLT BX YES Healed matrix-supported (calcite) monomictic breccia. W FBH D KAD0001 115.4 116.4 CORE YE MDST MUD MAS YES D KAD0001 116.4 119 CORE GY SLST SLT MAS SLST SLT BX YES Clast-supported monomictic (mud or silt) and polymictic (mud and silt) phases of brecciation. D KAD0001 119 119.2 CORE GY SDST EFS MAS YES D KAD0001 119.2 120.75 CORE LGY SDST EFS MAS YES D KAD0001 120.75 122.9 CORE RDBN SDST FS MAS YES D KAD0001 122.9 123 CORE GY SDST FS MAS YES D KAD0001 123 123.2 CORE LGY SLST SLT MAS SLST SLT BX YES Clast-supported polymictic (siltstone and mudstone) breccia. W FBH D KAD0001 123.2 123.5 CORE LGY SLST SLT MAS YES D KAD0001 123.5 123.55 CORE LGY SLST SLT MAS SLST SLT BX YES Clast-supported polymictic (laminated siltstone and limestone) breccia. S FBH D KAD0001 123.55 123.8 CORE LGY SLST SLT MAS YES Generally matrix-supported monomictic (mud) breccia. D KAD0001 123.8 123.9 CORE LGY MDST MUD MAS YES Generally matrix-supported monomictic (mud) breccia. D KAD0001 123.9 124.6 CORE LGY MDST MUD MAS SLST SLT BX YES Generally matrix-supported monomictic (mud) breccia. W FBH D KAD0001 124.6 125.13 CORE LGY SLST SLT MAS SLST SLT BX YES Generally matrix-supported monomictic (mud) breccia. W FBH D KAD0001 125.13 125.3 CORE YE MDST MUD MAS SLST SLT BX YES Generally matrix-supported monomictic (mud) breccia. W FBH D KAD0001 125.3 126.85 CORE YE MDST MUD MAS YES D KAD0001 126.85 127.2 CORE LGY SLST SLT BX YES Clast-supported polymictic (mud and laminated siltstone) breccia. D KAD0001 127.2 128.35 CORE GY CNGL MUD MAS LMST MUD MAS YES D KAD0001 128.35 128.5 CORE LGY LMST MUD MAS SLST SLT LAM YES D KAD0001 128.5 129.2 CORE LGY LMST MUD MAS YES D KAD0001 129.2 129.5 CORE GY LMST MUD MAS YES D KAD0001 129.5 129.9 CORE DGY LMST MUD MAS YES Dirty limestone (dark coloured). D KAD0001 129.9 130 CORE GY LMST MUD MAS SLST SLT LAM YES D KAD0001 130 130.05 CORE GY LMST MUD MAS YES D KAD0001 130.05 131.1 CORE LGY LMST MUD MAS YES D KAD0001 131.1 131.45 CORE DGY LMST MUD MAS YES Dirty limestone (dark coloured). D KAD0001 131.45 131.7 CORE LGY LMST MUD MAS YES D KAD0001 131.7 132.95 CORE GY CNGL MUD MAS LMST MUD MAS YES D KAD0001 132.95 133.8 CORE LGY SLST SLT LAM YES Irregular laminated siltstone. D KAD0001 133.8 133.9 CORE LGY SLST SLT MAS SLST SLT BX YES Clast-supported monomictic (silt) breccia. W FBH D KAD0001 133.9 134.1 CORE LGY SLST SLT MAS YES D KAD0001 134.1 134.7 CORE LGY SLST SLT BX LMST MUD BX YES Clast-supported polymictic (silt and limestone) breccia. W FBH D KAD0001 134.7 136.8 CORE GY SLST SLT LAM YES D KAD0001 136.8 137.4 CORE LGY SLST SLT MAS YES D KAD0001 137.4 138.85 CORE LGY SLST SLT BX YES Clast-supported monomictic and polymictic (silt and limestone and mud) phase brecciation. W FBH D KAD0001 138.85 139.35 CORE GY CNGL MUD MAS LMST MUD MAS YES D KAD0001 139.35 140.3 CORE LGY SLST SLT LAM YES D KAD0001 140.3 141.05 CORE LGY LMST MUD BX YES D KAD0001 141.05 142.1 CORE LGY SLST SLT LAM YES D KAD0001 142.1 143 CORE LGY LMST MUD BX YES D KAD0001 143 143.5 CORE LGY LMST MUD MAS YES D KAD0001 143.5 144.4 CORE LGY LMST MUD BX SLST SLT BX YES Clast-supported polymictic (silt and limestone) breccia. W FBH D KAD0001 144.4 144.6 CORE LGY SLST SLT LAM YES D KAD0001 144.6 145.1 CORE LOR SLST SLT BX LMST MUD BX YES "Clast-supported polymictic (mud, silt, and limestone) breccia." W FBH D KAD0001 145.1 145.2 CORE LGY SLST SLT LAM YES "Clast-supported polymictic (mud, silt, and limestone) breccia." W FBH D KAD0001 145.2 145.55 CORE LOR SLST SLT BX MDST MUD BX YES "Clast-supported polymictic (mud, silt, and limestone) breccia." W FBH D KAD0001 145.55 145.9 CORE LGY SDST CS MAS YES D KAD0001 145.9 148.35 CORE LOR MDST MUD MAS YES D KAD0001 148.35 154.75 CORE LGY MDST MUD BX LMST MUD MAS YES Clast-supported monomictic (dominated by mud) and polymictic (dominated by mud and minor limestone and silt) phased brecciation. W FBH D KAD0001 154.75 158 CORE DGY LMST MUD MAS YES Dirty limestone (dark coloured). D KAD0001 158 166.5 CORE GY LMST FG MAS SDST FG MAS YES "common vuggy calcite veins," M FRS massice calcitic limestone with abundant bedds id terrigenious lithix sandstone influx. D KAD0001 166.5 172.3 CORE BNGY LMST FG CBED SLST SLT CBED YES D KAD0001 172.3 173.5 CORE LGY LMST MAS YES vuggy limestone D KAD0001 173.5 185.3 CORE LGY LMST FG MAS SLST SLT CBED YES M FRS massive vuggy limestone with common - brown grey interbedded silts. presence of silts increases competency of unit. D KAD0001 185.3 192 CORE BNGY SLST SLT CBED LMST FG BX YES RUC "planar to convilute bedded silt stones with abundant, coarser grained sub angular limeestone clasts. silt supported breccia. " D KAD0001 192 194.6 CORE LOR LMST CG BX SLST CS BX YES RUC angular - sub angular sedimentairy breccia. clast supported with limestone clasts dominent over siltstone. D KAD0001 194.6 195 CORE GY BX YES M FRU D KAD0001 195 195.8 CORE GY SLST SLT LAM BX YES interbedded fine and coarser silts. cross cuty by abundant vuggy calcite fractures. D KAD0001 195.8 200.3 CORE RDBN SDST FS MAS BX YES fine matrix supported pollylithic sandstone. andular clasts. possibly a volcaniclastic? D KAD0001 200.3 200.5 CORE RDBN SDST FS BX YES RUC "polylithic, angular - sub angular, clast supported sedimentary breccia. " D KAD0001 200.5 208.5 CORE RDBN SDST FS CBED SLST SLT BX YES "very fine beddes sand with clear up hole younging. bedding discontiuous. red - poly lithick. possibly a volcaniclastic? unit displays rare, angular - subangular rotated siltstone glasts (grey). " D KAD0001 208.5 218 CORE RDBN SDST FS CBED SLST BX YES increased breccia content. angiular rip up clasts forming base of bed. D KAD0001 218 225 CORE RDBN SDST FS MAS CBED YES "decreased clast content, bedding extremly conviluted. " D KAD0001 225 225.8 CORE RDBN SDST FS LAM BX YES ibcreased angular clasts including quartz. D KAD0001 225.8 228.8 CORE LOR SDST FS LAM FO YES "foliated, micacious sandstone. common finbe, elongate lathes - possibly pummice. cross cut by narrow .05cm - 1cm quartz veins. " D KAD0001 228.8 236.8 CORE YES D KAD0001 236.8 245.2 CORE PI GRT CG BX YES down hole contact is sharp. baked margin is neglagable. "k spar rich granite intrusive, cross cut by abundant slbite - kspar fractures. common muscovite and ?tourmaline. " D KAD0001 245.2 246 CORE GYGN SDST FS MAS YES D KAD0001 246 247 CORE GYGN SDST FS BX YES D KAD0001 247 251.2 CORE GYGN SDST FS FO MAS YES "dominent, core axis parallell foliation defined by narrow lathes of dark mineral (pummice/ ash?). " D KAD0001 251.2 254.8 CORE GY SDST MG MAS FO YES dominent foliation defined by core axis parallell light coloured mineral - possibly cordirite? D KAD0001 254.8 255.2 CORE QZVN CRN YES buck quartz vein D KAD0001 255.2 256.2 CORE GY SDST CG FO YES filiation defined by amphibole and cordirite? D KAD0001 256.2 257.3 CORE BNGY SDST FS FO YES D KAD0001 257.3 257.5 CORE PI SDST FS PBED YES D KAD0001 257.5 260.5 CORE GY SDST FS MAS FO YES massive sandstone with ?foliation defined by elongate cordirite. is this foliation of overprint of remanent bedding. D KAD0001 260.5 263 CORE CR SLST SLT MAS FO YES decreased cordirite increased hornblend. foliation/ remanent bedding defined by hornblend growth. D KAD0001 263 267 CORE WH QZVN CRN YES large buck quartz vein cross cut by moderate - strong chlorite - hamatite fractures. sulphide associated with these fractures. D KAD0001 267 269.2 CORE LOR SDST MAS BX YES unhealed hematite fractures. S FRS D KAD0001 269.2 275.5 CORE LGY SDST FS PBED FO YES possible remanent bedding/ foliation defined by amphibole +-Garnet. D KAD0001 275.5 276 CORE PI QZVN CRN YES large buck quartz vein with strong k-spar upper and lower salvage. D KAD0001 276 282 CORE WH QZVN CRN YES large buck quartz vein with strong k-spar upper and lower salvage. D KAD0001 282 282.67 CORE PI QZVN CRN YES large buck quartz vein with strong k-spar upper and lower salvage. D KAD0001 282.67 284 CORE GY SDST MAS YES D KAD0001 284 297 CORE PI GRT CG MAS YES "course grained granite - k-spar - quartz +- albite. accessory muscovite, xenochristic chlorite. tourmaline?/hornblend. " D KAD0001 297 305 CORE PI GRT CG CRN YES D KAD0001 305 320 CORE PI GRT CG CRN BX YES "zone of increased quartz veining cross cutting granite. veining associated with sphalerite? = dark euhedral/ sub euhedral mineral forming on vein salvages and within rock mass - individual crystals 0.5 - 2cm. Sphaletite/ pyrrhotite / tourmaline? possible arseno pyrite disseminated throught grounf mass? or is this just fine muscovite? " D KAD0001 320 325.6 CORE PI GRT CG CRN YES D KAD0001 325.6 330.2 CORE LGY SDST FS MAS BX YES S FRS D KAD0001 330.2 330.6 CORE GRT YES abundant dark mineral - tourmaline / pyroxene/ spalerite? D KAD0001 330.6 332 CORE LGY SDST FS MAS BX YES S FRS D KAD0001 332 332.4 CORE GRT YES D KAD0001 332.4 336.5 CORE GY SDST FS BX CBED YES "strongly fractured, hunhealed -brittle. massive moving down hole to planar/ convilute bedded (convilutions on 1cm scale) sandstone. bedding defined by darker mineral, no younging direction apparent. " D KAD0001 336.5 342 CORE LGY SDST FS PBED CBED YES planar bedded fine sand. bedding defined by over growth of darker mineral (amphibole?). possible younging down hole? unit cross cut by several sheetes qtz veins with -.1 - 0.5 cm wide chlorite - pyrite selvage. D KAD0001 342 342.5 CORE LGY SDST FS PBED YES D KAD0001 342.5 343 CORE LGY BI FG MAS YES possible fine grained dolerite/ massive sediment. displays lack of cordiorite. D KAD0001 343 344 CORE GYGN SLST SLT LAM YES D KAD0001 344 345.1 CORE LGY BI FG MAS BX YES "broken, unhealed. " S FRS D KAD0001 345.1 346.7 CORE GYGN SLST SLT LAM BX YES S FRS "laminated silts, bedding at low - moderate angle to core axis. pervasive sericite alteration. bedding defined by dark mineral (amphibole?) abundnant diseminated sulfide locally related to amphibole - chlorite beds. " D KAD0001 346.7 350.3 CORE GY SDST FS MAS BX YES S FRS "fine to medium grained sandstone. strongly fractured. abundent diseminated sulphide throughout. sulphides are sub euhedral and 1mm - 8mm in diameter. rare quartz veining. so no direct corelation to veins," D KAD0001 350.3 357 CORE LGY SLST SLT PBED BX YES S FRS D KAD0001 357 358.1 CORE GYGN HFL CG CRN SDST MAS YES S FRS "massive corsley crystalin e Hornfels (?) possibly after sandstone/ dolerite? loss of sulphide. hornblend - muscovite -staurolite? " D KAD0001 358.1 361.5 CORE GYGN SLST SLT LAM BX YES S FRS laminated to localy massive silts. increasing sulphide. - bedding parallell to diseminated. unit is cross cut by a large milky quartz vein. selvage of dark mineral (chlorite?) and inkreased k - spar towasds salvage. incresed pyrite. dark brown - black mineral - possibly sphalerite/ oxidised pyrrhotite. D KAD0001 361.5 364.5 CORE LGY SLST SLT BX SDST BX YES S FRS D KAD0001 364.5 365 CORE LGY BI FG MAS BX YES fine grained dolerite? displays lack of sed texture - lack of sulphide. S FRS D KAD0001 365 366 CORE SLST SLT BX SDST FS BX YES S FRS interbedded filts and fine sands strnglt fractured. possibly faulted? D KAD0001 366 366.5 CORE FZ FA YES S FRU interbedded filts and fine sands strnglt fractured. possibly faulted? D KAD0001 366.5 366.8 CORE SLST SLT BX SDST FS BX YES S FRS interbedded filts and fine sands strnglt fractured. possibly faulted? D KAD0001 366.8 367 CORE FZ FA YES S FRU interbedded filts and fine sands strnglt fractured. possibly faulted? D KAD0001 367 367.2 CORE GY SLST SLT BX SDST FS BX YES S FRS interbedded filts and fine sands strnglt fractured. possibly faulted? D KAD0001 367.2 370 CORE GY GYWK FS BX YES S FRS D KAD0001 370 371.6 CORE PI SYN CG MAS YES "massive, cours crystaline felsic intrusive dominated by KSpar lesser albite and lesser qtz. posibly accessory muscovite. " D KAD0001 371.6 372.6 CORE PI SYN CG MAS YES D KAD0001 372.6 372.8 CORE FZ FA YES M FRU faulted contact - fault flour. D KAD0001 372.8 374 CORE LGY GYWK FS BX MAS YES styongly fractured/ jointed. unhealed. massibe GW. moderate serricite overprint. albite/ calcite throughout groundmass? D KAD0001 374 374.5 CORE GYWK FS MAS BX YES D KAD0001 374.5 375.6 CORE GYGN GYWK FS PBED YES chloritic greywakey. cross cut by sone of intense sheeted veins - 14 D KAD0001 375.6 376 CORE LGY GYWK BX YES S FRS D KAD0001 376 384.4 CORE LGY GYWK FS PBED YES well bedded sand stone - displays a dominent siderate pervasive alteration with lesser k-spar. overgrowth of albite. D KAD0001 384.4 386.5 CORE LGY SLST FS PBED BX YES planar bedded silts and wake moving down into massive wakey. silts display a strong albite/ cordirite overprint and pervasive siderite. chlorite is very week and only occures bedding parallell in silts. D KAD0001 386.5 391.3 CORE LGY GYWK FS MAS BX YES planar bedded silts and wake moving down into massive wakey. silts display a strong albite/ cordirite overprint and pervasive siderite. chlorite is very week and only occures bedding parallell in silts. D KAD0001 391.3 394.8 CORE LGY GYWK FS MAS PBED YES D KAD0001 394.8 395.5 CORE GY SLST SLT LAM YES D KAD0001 395.5 397.4 CORE LGY GYWK FS PBED YES D KAD0001 397.4 398.5 CORE LGY GYWK FS MAS YES D KAD0001 398.5 398.9 CORE GYGN SLST SLT MAS YES posibly a protolithic silt/ chlorite overprint pervasive. near complete replacment by disseminated euhedral pyrite. D KAD0001 398.9 402 CORE PI SYN CG MAS BX YES D KAD0001 402 402.8 CORE PI SYN CG MAS YES D KAD0001 402.8 406 CORE LGY GYWK FS MAS YES D KAD0001 406 409.7 CORE LGY GYWK FS PBED YES D KAD0001 409.7 411 CORE GYGN SLST SLT PBED YES D KAD0001 411 412 CORE BNGY GYWK FS PBED YES D KAD0001 412 412.2 CORE FZ FA YES M FBH D KAD0001 412.2 413.4 CORE BNGY GYWK FS MAS YES D KAD0001 413.4 414.3 CORE GYGN SLST SLT LAM YES D KAD0001 414.3 415.3 CORE LGY GYWK FS MAS YES D KAD0001 415.3 418.5 CORE LGY GYWK FS PBED YES D KAD0001 418.5 418.8 CORE GYGN FZ FA YES M FRS D KAD0001 418.8 421.5 CORE BNGY GYWK FS MAS YES D KAD0001 421.5 425.4 CORE BNGY GYWK MUD PBED YES D KAD0001 425.4 426 CORE SYN YES D KAD0001 426 426.5 CORE LGY SLST SLT BX LAM YES D KAD0001 426.5 426.7 CORE SYN YES D KAD0001 426.7 435 CORE PI SDST FS PBED YES olanar to massive sand stones cross cut by numerous syanitic intrusions / veins..pervasive k-spar throughout. D KAD0001 435 435.3 CORE LGY FZ FA YES M SED olanar to massive sand stones cross cut by numerous syanitic intrusions / veins..pervasive k-spar throughout. D KAD0001 435.3 437.7 CORE PI SDST FS PBED YES olanar to massive sand stones cross cut by numerous syanitic intrusions / veins..pervasive k-spar throughout. D KAD0001 437.7 442 CORE PI SLST SLT PBED BX YES planar bedded silt stones cross cut by intense stock work of qtz veins. larger buck quarts veins possess abundant pyrite and are associated with a 5cm wide albite alteration halo. . rock flooded by k-spar - pink. D KAD0001 442 444.7 CORE GYGN SDST SLT MAS YES "bedded silts and sands. moving down hole more quarts veins - buck and laminated. laminated veins possess abundant diseminated, dirty pyrite. k sapar alteration increeases accociated with buck qtz veins. " D KAD0001 444.7 446.5 CORE GYGN SDST SLT PBED YES "bedded silts and sands. moving down hole more quarts veins - buck and laminated. laminated veins possess abundant diseminated, dirty pyrite. k sapar alteration increeases accociated with buck qtz veins. " D KAD0001 446.5 448.2 CORE PI SDST SLT PBED YES "bedded silts and sands. moving down hole more quarts veins - buck and laminated. laminated veins possess abundant diseminated, dirty pyrite. k sapar alteration increeases accociated with buck qtz veins. " D KAD0001 448.2 448.6 CORE WH QZVN CRN YES large buck qtz vein - late stage - cross cuts qtz - kspar veins. D KAD0001 448.6 449 CORE BNGY SLST SLT MAS BX YES D KAD0001 449 449.3 CORE PI SYN MAS YES D KAD0001 449.3 450 CORE WH QZVN MAS YES massive buck qtz vein ewxploiting granite contact. D KAD0001 450 454.4 CORE PI SLST SLT PBED BX YES laminated to locally massive siltstone cross cut by numerous qtz - kspar veins and rare syanitic veins. D KAD0001 454.4 455 CORE PI SYN CG MAS BX YES course grained syanitic intrusion cross cut by strong stock work of qtz - zb veins. kicks out pervasive k-spar alteration into surrounding country rock 0.5m -1m either side. D KAD0001 455 456 CORE SLST LAM YES D KAD0001 456 456.3 CORE PI QZVN YES D KAD0001 456.3 460.3 CORE PI SDST FS PBED BX YES D KAD0001 460.3 462 CORE GYGN SLST SLT PBED YES D KAD0001 462 465.3 CORE PI SDST FS PBED PBED YES planar bedded silts to sands cross cut by several qtz - kspar veins - srong potassic alteration throughout. D KAD0001 465.3 470.6 CORE GYGN SLST SLT PBED CH PBED YES interbedded greywake and siltstone. strong albite . cordirite crystal overgrowth. bedding at 3mm - 1 cm.strong bedding parallell diseminated pyrite D KAD0001 470.6 471.2 CORE CR SLST SLT BX CH PBED YES strongly fractured and breciated by adjacent pegmatite. intense siderite - silica - epidote pervasive. D KAD0001 471.2 471.5 CORE PEG CG CRN YES D KAD0001 471.5 473.6 CORE LGY SLST SLT PBED CH PBED YES interbedded chert and silt. is this chert or just silica alteration? D KAD0001 473.6 474 CORE PEG CG CRN YES D KAD0001 474 474.4 CORE LGY SLST SLT LAM YES D KAD0001 474.4 474.6 CORE PEG YES D KAD0001 474.6 474.7 CORE YES D KAD0001 474.7 475 CORE PEG YES D KAD0001 475 476.5 CORE GY SLST SLT LAM YES D KAD0001 476.5 477 CORE LGY CH PBED SLST SLT LAM YES interbedded chert and siltstone. very week siderite - chlorite alteration in silts. D KAD0001 477 479.8 CORE LGY SLST SLT LAM GYWK FS PBED YES interbedded silts and gw.silts are dominent . unit displays a strong amphibole overprink in the silt and albite in thw wake. seiderite pervasive. D KAD0001 479.8 480.5 CORE BNGY MDST MUD LAM CH NLR YES D KAD0001 480.5 480.7 CORE FZ FA YES S FBU D KAD0001 480.7 483.9 CORE BNGY MDST MUD LAM CH NLR YES D KAD0001 483.9 486.5 CORE CR SLST SLT PBED YES strongly altered / silica overprinted. D KAD0001 486.5 487.8 CORE WH FIRK CG CRN YES pegmatitic vein. Qtz - kspar - albite - biotite D KAD0001 487.8 488.4 CORE CR SLST SLT PBED YES silica -kspar flooded silt. sedimentary structur largely oliterated. D KAD0001 488.4 490 CORE CR FIRK CG CRN YES vein changes from being more k-spar rich up hole to increasingly quartz - albite rich down hole. D KAD0001 490 490.5 CORE DGY FZ FA YES S FBU D KAD0001 490.5 491 CORE GY MDST MUD LAM BX YES laminated carbonacious mudstone. strongly fractured by adjacent fault. D KAD0001 491 491.2 CORE LGY PEG CG CRN BX YES laminated carbonacious mudstone. strongly fractured by adjacent fault. D KAD0001 491.2 492.3 CORE GY MDST MUD LAM BX YES laminated carbonacious mudstone. strongly fractured by adjacent fault. D KAD0001 492.3 492.5 CORE DGY FZ FA YES S FRU D KAD0001 492.5 494 CORE GY MDST MUD BX BX YES cross cut by stockwork qtz veining and associate pyrite. S FRS laminated carbonacious mudstone. strongly fractured by adjacent fault. D KAD0001 494 497 CORE GYGN SLST SLT BX YES D KAD0001 497 499.3 CORE GYGN SDST SLT LAM CH PBED YES planar bedded cloriotic silts - abundant bedding parallell quarts veinf. D KAD0001 499.3 499.7 CORE PI SYN CG MAS YES D KAD0001 499.7 503.2 CORE GYGN SLST SLT LAM CH PBED YES planar bedded cloriotic silts - abundant bedding parallell quarts veinf. possibly chert banding. D KAD0001 503.2 512 CORE PI FIRK CG CRN YES course grained granitic intrusion. qtz - kspar - albite - tourmaline. unit becomes increasingly fine grained and quartx rich down hole. D KAD0001 512 513.7 CORE GYGN SLST MG PBED YES sreongly fracdtured and altered silts. several cross cuting granitic veins. D KAD0001 513.7 514.7 CORE WH QZVN CRN YES D KAD0001 514.7 516.2 CORE BNGY SLST FS MAS BX YES D KAD0001 516.2 516.6 CORE WH QZVN CRN YES D KAD0001 516.6 524 CORE BNGY SLST SLT LAM YES laminated silts. lamminations defined by bedding parallell biotite. first occurance of biotite. unit cross cut by abundant buck qtx veuns 1 - 10cm across. D KAD0001 524 524.4 CORE GYGN SLST BX YES S FRS fractured sediment up against large healed fault breccia. D KAD0001 524.4 525 CORE GYGN FZ FA YES angular clasts and fault flower. breciated quattz veins = multiple stages of movment S FBH D KAD0001 525 533.2 CORE GYGN DLT FG FO BX YES D KAD0001 533.2 533.5 CORE GYGN FZ FA YES M SED D KAD0001 533.5 534 CORE DLT FG FO BX YES M FRS D KAD0001 534 534.3 CORE GYGN FZ FA YES S SED D KAD0001 534.3 535.6 CORE GYGN DLT FG FO BX YES M FRS D KAD0001 535.6 535.9 CORE GYGN FZ FA YES fault clay fill and large angular clasts- significant moment and fluid flow. S SED D KAD0001 535.9 537.2 CORE GYGN DLT FG FO BX YES M FRS D KAD0001 537.2 541.2 CORE GY SDST SLT BX LAM YES D KAD0001 541.2 549.5 CORE LGY SDST SLT LAM YES D KAD0001 549.5 555 CORE BNGY SLST PBED YES bedding at 2 -5cm defined by bedding parallell biotite over print. moving down hole a corse grained albite overprint becomes prominent . albite breaksdown into dark mineral - hornblend / chlorite. D KAD0001 555 558.3 CORE BNGY SLST SLT BX YES "planar bedded sints, strongly fractured / jointed. " D KAD0001 558.3 560 CORE BNGY DLT FG BX YES "planar bedded sints, strongly fractured / jointed. " D KAD0001 560 560.3 CORE BNGY FZ FA YES W FBH D KAD0001 560.3 564 CORE BNGY SLST SLT BX LAM YES "strongly fractured silts. cross cut by several 1cm wide quartz veins these possess a stronc 0.5cm wide chlorite selvage, " D KAD0001 564 565.6 CORE GYGN DLT FG FO FO YES "chilled upper margin. very fine grained, foliated. stromg amphibole overprint. " D KAD0001 565.6 568.8 CORE GYGN DLT MG FO YES D KAD0001 568.8 569 CORE GYGN MG FA YES narrow qtz and clay filled shear. S SED D KAD0001 569 574.4 CORE GYGN DLT MG FO YES D KAD0001 574.4 574.7 CORE PI DLT FG GRA YES M SED increased k-spar and clinozoisite(?) parallell to foliation. possibly a narrow ductile shear inducint alteration? or possibly granopheric core? D KAD0001 574.7 577.5 CORE GYGN DLT MG FO YES D KAD0001 577.5 578.6 CORE PIRD FIRK CG GRA YES "dolerite intruded by granitic vein - k-spar - qtz. upper boundary displays strong, corse amphibole growth. vein/ intrusion possessed abundant dolerite xenolits. gronopheric texture is inturn cross cut by buck quartz veins possessing abundant chlorite - pyrite., " D KAD0001 578.6 582.3 CORE LGY DLT FG FO YES moderatly altered dolwrite - protolithic texture distroyed by alteration from crosscuting quartz - kspar veins. D KAD0001 582.3 585 CORE GYGN DLT MG FO YES D KAD0001 585 586.3 CORE BNGY DLT FG BX FO YES dolerite cross cut by sheeted and stockwork qtx veins. distruction of crystal structure. increased biotie and disseminated sulphide. D KAD0001 586.3 587 CORE BNGY DLT FG FO YES dolerite cross cut by sheeted and stockwork qtx veins. distruction of crystal structure. increased biotie and disseminated sulphide. D KAD0001 587 593 CORE GYGN DLT MG FO YES D KAD0001 593 593.3 CORE BNGY DLT FG FO YES D KAD0001 593.3 594.4 CORE GYGN DLT FG FO YES D KAD0001 594.4 595 CORE GYGN SLST SLT LAM YES D KAD0001 595 596.5 CORE PI DLT MG FO QZVN FO YES dolerite and contact intruded by foliation parallell qtz - k-spar veining. D KAD0001 596.5 604 CORE GYGN DLT FG FO YES D KAD0001 604 605 CORE GYGN DLT FG FO YES W FRS D KAD0001 605 606 CORE GY FZ FG FA BX YES S FBH "strong fault breccia, clay rich with broad deformation zone either side" D KAD0001 606 606.4 CORE DLT FG BX SH YES W FRS defomration sheared zone proximal to fault D KAD0001 606.4 617 CORE GYGN DLT FG FO YES D KAD0001 617 619.2 CORE BNGY FZ FG FA BX YES M F "several faults through interval, brittle brecciation exploited by veins. Some pug formed along fractures and discrete shears" D KAD0001 619.2 620 CORE GYGN DLT FG FO YES D KAD0001 620 620.5 CORE GYGN DLT FG FO BX YES W FRS D KAD0001 620.5 622.4 CORE GYGN DLT FG FO YES D KAD0001 622.4 623.4 CORE PI SYN MG CRN YES D KAD0001 623.4 624.3 CORE GYGN DLT FG FO YES D KAD0001 624.3 625.2 CORE GYGN FZ FG FA SH YES S F strongly sheared zone with high clay content D KAD0001 625.2 633.1 CORE GYGN DLT FG FO YES weakly foliated dolerite with weak crackle brecciation textures infilled by thin carbonate stringers D KAD0001 633.1 633.3 CORE GYGN SLST SLT SH FO YES "possible sheared sediment along contact with fault zone, possible sheared dolerite with strong fabric " D KAD0001 633.3 633.6 CORE GYGN SLST SLT SH FO YES S FO D KAD0001 633.6 635.2 CORE GYGN FZ FG FA BX YES "strongly sheared, high clays with angular clasts " S F "Broad fault zone with angular clast in puggy clay rich matrix, strong deformation textures " D KAD0001 635.2 637 CORE PI FIRK VCG CRN YES "coarse grained felsic intrusive, high K spar and albite growth with strongly sheared margins " D KAD0001 637 638.2 CORE GYGN FZ FG FA BX YES fault rubble S FRS "fault rubble zone " D KAD0001 638.2 639.4 CORE GYGN DLT FG FO FIRK YES "several thin feldspar rich intrusives through interval " D KAD0001 639.4 639.8 CORE GYGN SLST FG SH SH YES "possible sediment " D KAD0001 639.8 640.5 CORE GY FZ VCG FA SH YES "strong shear or fault with high caly along contact " S SED "sheared contact with intrusive, pug formation" D KAD0001 640.5 643.98 CORE PI FIRK VCG CRN YES M SED "coarse grained felsic intrusive exploiting fault zone, sheared contacts. Strong Qtz, feldspar, albite, tourmaline growth. " D KAD0001 643.98 644.3 CORE DGY FZ FG FA SH YES clay rich strongly sheared zone S F small clasts of country rock caught up in clay rich sheared zone D KAD0001 644.3 647.2 CORE PUGY GRT MG CRN YES "microgranite, finer grained than Felsic intrusives. qtz kspar and biotite" D KAD0001 647.2 647.9 CORE PI FIRK VCG CRN YES "very coarse intrusive within microgranite with similar composition " D KAD0001 647.9 653 CORE PUGY GRT MG CRN YES "microgranite, finer grained than Felsic intrusives. qtz kspar and biotite " D KAD0001 653 654.5 CORE PUGY GRT MG CRN YES D KAD0001 654.5 661.95 CORE PI GRT MG CRN YES stronger Kspar colouring D KAD0001 661.95 662.4 CORE PI FIRK VCG CRN YES D KAD0001 662.4 666.7 CORE PUGY GRT MG CRN BX YES "very weak brittle deform textures " D KAD0001 666.7 674.15 CORE PUGY GRT MG CRN YES D KAD0001 674.15 674.6 CORE PI FIRK VCG CRN YES D KAD0001 674.6 675 CORE PUGY GRT MG CRN YES D KAD0001 675 675.6 CORE PI FIRK VCG CRN YES D KAD0001 675.6 679.6 CORE PUGY GRT MG CRN FIRK YES thin felsic intrusives within interval of granite D KAD0001 679.6 680 CORE PI FIRK VCG CRN YES D KAD0001 680 680.75 CORE PUGY GRT MG CRN YES D KAD0001 680.75 680.9 CORE GY FZ MG SH YES M SED "Thin shear structure within granite wiht minor pyrite " D KAD0001 680.9 682.7 CORE PUGY GRT MG CRN YES "discrete zones of coarse grained felsic intrusive within interval " D KAD0001 682.7 683.3 CORE PI FIRK VCG CRN YES D KAD0001 683.3 684 CORE PUGY GRT MG CRN YES D KAD0001 684 686.7 CORE GY GRT MG CRN YES D KAD0001 686.7 687.25 CORE DGY GRT MG SH BX YES M SED brittle deformation textures with small shear zone D KAD0001 687.25 688.45 CORE GY GRT MG CRN YES D KAD0001 688.45 690.05 CORE PI FIRK VCG CRN YES D KAD0001 690.05 691.5 CORE GY GRT MG CRN YES D KAD0001 691.5 691.9 CORE PI FIRK VCG CRN YES D KAD0001 691.9 693.5 CORE GY GRT MG CRN YES D KAD0001 693.5 694.4 CORE PI FIRK VCG CRN YES D KAD0001 694.4 695.6 CORE PUGY GRT MG CRN YES D KAD0001 695.6 695.95 CORE PI FIRK VCG CRN YES D KAD0001 695.95 698.8 CORE PUGY GRT MG CRN YES D KAD0001 698.8 700.1 CORE PI GRT FG CRN YES "stronger silica and Kspar colouring over finer almost chert-like zone " D KAD0001 700.1 700.5 CORE PUGY GRT MG CRN YES W SED "Weak shear within granite " D KAD0001 700.5 703.05 CORE PUGY GRT MG CRN YES D KAD0001 703.05 706.2 CORE GY GRT FG CRN YES "Weak Kspar colouring, finer grained with more amphibole, possible dolerite " D KAD0001 706.2 707.1 CORE PUGY GRT MG CRN YES D KAD0001 707.1 707.6 CORE PI QZVN FG CRN YES "fine grained vein or intrusion of silica and Kspar " D KAD0001 707.6 715 CORE PUGY GRT MG CRN YES D KAD0001 715 716.2 CORE PUGY GRT MG CRN YES W FRS "Weak microfracturing " D KAD0001 716.2 725 CORE PUGY GRT MG CRN YES D KAD0001 725 737.4 CORE PUGY GRT MG CRN YES D KAD0001 737.4 738.5 CORE PI FIRK VCG CRN YES D KAD0001 738.5 747 CORE PUGY GRT MG CRN YES D KAD0001 747 750 CORE PUGY GRT MG CRN YES D KAD0001 750 762.6 CORE PUGY GRT MG CRN YES D KAD0001 762.6 764.05 CORE PI FIRK CGV CRN YES D KAD0001 764.05 775.1 CORE PUGY GRT FG CRN YES D KAD0002 0 65.5 PC D KAD0002 65.5 84.5 CORE GY CNGL MUD FBD SLST MUD LAM YES lighter discontinuous cherty bands of blobs through laminated darker muds D KAD0002 84.5 85.5 CORE GY CNGL MUD FBD SLST MUD LAM YES M SED lighter discontinuous cherty bands of blobs through laminated darker muds D KAD0002 85.5 87.5 CORE GY CNGL MUD FBD SLST MUD LAM YES lighter discontinuous cherty bands of blobs through laminated darker muds D KAD0002 87.5 89 CORE GY CNGL MUD FBD SLST MUD LAM YES W SED D KAD0002 89 92.5 CORE GY CNGL MUD FBD SLST MUD LAM YES D KAD0002 92.5 98 CORE LGY CNGL MUD FBD SLST MUD LAM YES W FRS "minor faults through interval with preferential weathering, structures appear subparallel to core" D KAD0002 98 100 CORE LGY CNGL FS BX SLST MUD LAM YES SLB monomict breccia conglomerate D KAD0002 100 103.3 CORE LGY SDST FS MAS PBED YES quartz rich sandstone D KAD0002 103.3 104.3 CORE OR SDST FS MAS PBED YES quartz rich sandstone D KAD0002 104.3 104.5 CORE LGY SDST FS MAS PBED YES quartz rich sandstone D KAD0002 104.5 104.8 CORE LGY SDST FS MAS PBED YES "small rubble zones in interval " W FRS quartz rich sandstone D KAD0002 104.8 106 CORE GY SLST MUD LAM YES "small rubble zones in interval " W FRS D KAD0002 106 107.3 CORE GY SLST MUD LAM YES D KAD0002 107.3 108.8 CORE OR LMST FS MAS YES D KAD0002 108.8 115.4 CORE GY SLST MUD LAM YES D KAD0002 115.4 117.2 CORE OR LMST MUD LAM CNGL MUD MAS YES D KAD0002 117.2 118.25 CORE GY SLST MUD LAM YES D KAD0002 118.25 121 CORE GY CNGL MUD MAS LMST MUD LAM YES D KAD0002 121 122.1 CORE BNOR CNGL VCG MAS LMST MUD LAM YES "Polymict conglomerite, clast supported limestones" D KAD0002 122.1 123.6 CORE GY SDST CS MAS YES "Coarser sandstone " D KAD0002 123.6 125.15 CORE GY SDST MSD LAM YES W FRS Interbedded sands and silts D KAD0002 125.15 127.05 CORE BNOR SDST MSD MAS YES "weathered sands, so qtz growth in cavities. patchy strongly weathered clay zones" D KAD0002 127.05 130 CORE PUGY SDST FS MAS YES "fine to medium massive sandstone, moderately weathered " D KAD0002 130 135 CORE PUGY SDST FS MAS YES W FRS "fine to medium massive sandstone, moderately weathered " D KAD0002 135 145 CORE BNOR LMST FS MAS YES D KAD0002 145 151 CORE GY LMST MUD CBED CNGL YES D KAD0002 151 156.2 CORE GY LMST MUD CBED YES D KAD0002 156.2 157 CORE GY LMST MUD CBED NLR YES calcite blobs D KAD0002 157 159 CORE GY LMST MUD CBED LAM YES D KAD0002 159 164.3 CORE GY LMST MUD LAM YES D KAD0002 164.3 164.5 CORE DGY SLST MUD LAM LMST YES SLB W FRS D KAD0002 164.5 165 CORE DGY SLST MUD LAM LMST YES SLB S F D KAD0002 165 171.3 CORE DGY SLST MUD LAM LMST YES SLB W FRS D KAD0002 171.3 172 CORE DGY SDST FS LAM SLST MUD YES W FRS "Vuggy interbedded silts and sands " D KAD0002 172 177.5 CORE GY SDST FS MAS YES DW D KAD0002 177.5 183 CORE BNOR SDST FS MAS LMST YES DW D KAD0002 183 188.4 CORE GY SDST FS MAS YES DW D KAD0002 188.4 192.1 CORE DGY SDST FS MAS YES MDD W FRS "Vuggy sandstone with small inclusions of mud, as well as fine mud laminations" D KAD0002 192.1 195.5 CORE GY LMST MUD PBED CNGL YES D KAD0002 195.5 196.3 CORE DGY SLST MUD LAM YES D KAD0002 196.3 197.3 CORE GY CNGL MUD MAS YES Monomict conglomerate D KAD0002 197.3 199.5 CORE DGY SLST MUD LAM YES D KAD0002 199.5 201.2 CORE LGY SLST MUD LAM CNGL YES D KAD0002 201.2 201.5 CORE PUGY LMST MUD PBED YES D KAD0002 201.5 215 CORE PUGY LMST MUD CBED CNGL YES "Iron oxidation colouring, pacthy beds of conglomerate " D KAD0002 215 222.3 CORE RDBN LMST MUD CBED CNGL YES DW "Vuggy towards the end, infill with calcite?" D KAD0002 222.3 222.5 CORE RDBN CNGL CGV MAS CNGL YES "Unconformity, gravel of granite within limestone mud" D KAD0002 222.5 224 CORE RDBN CNGL CGV MAS YES "Unconformity, gravel of granite within limestone mud" D KAD0002 224 226.9 CORE PI GRT CG CRN YES Kspar flooded mod weathered granite D KAD0002 226.9 229 CORE CR GRT CG CRN YES darker granite with occasional planar vein D KAD0002 229 229.9 CORE PI FZ MG FA YES rubbly deformation zone M FRU D KAD0002 229.9 233 CORE PI GRT CG CRN YES Patchy weathered zones through strongly Kspar flooded granite D KAD0002 233 246.5 CORE PI GRT CG CRN YES "Coarse grained, Kspar, qtz, micas and tourmailine?" D KAD0002 246.5 248.7 CORE PI GRT CG CRN YES D KAD0002 248.7 250.1 CORE PI GRT CG CRN YES M FRS D KAD0002 250.1 251.55 CORE PI GRT CG CRN YES D KAD0002 251.55 258.5 CORE RDBN SDST FS LAM PBED YES W FRS redbbrown iron oxide coloured laminated to planar bedded with some brittle deformation textures D KAD0002 258.5 259.4 CORE RDBN SLST SLT XBED LAM YES TCB D KAD0002 259.4 259.5 CORE RDBN FZ SLT SH FA YES TCB Strongly sheared contact S SED sheared silt contact with qtz D KAD0002 259.5 259.6 CORE RDBN FZ FG SH SLST FA YES Strongly sheared contact S SED sheared silt contact with qtz D KAD0002 259.6 261.7 CORE RDBN QZVN FG CRN SLST BX YES W FRS "Brittley deformed strained qtz with Fe oxide colouration, rare narrow slivers of siltstone " D KAD0002 261.7 262 CORE GY SLST SLT SH QZVN BX YES M SED chaotic brecciated veining through sheared sediment D KAD0002 262 262.9 CORE RDBN QZVN FG CRN BX YES W FRS D KAD0002 262.9 266 CORE RDBN SDST FS PBED MDST SH YES S SED "Sediment weathered to FE oxidised clays, appears quite strongly sheared but overall quite rubbley" D KAD0002 266 267.3 CORE RDBN SDST FS MAS MDST YES S FRS "Sediment weathered to FE oxidised clays, appears quite strongly sheared but overall quite rubbley" D KAD0002 267.3 274 CORE RDBN SDST FS MAS MDST YES M FRS "appears to be a weathered consolidated mudstone, possibly still Cambrian? difficult to define textures due to weathering, possibly the metamorphic overprint of tuff " D KAD0002 274 274.5 CORE GY SDST SLT SH YES "Tuffaceous textures, possibly strong fabric through dolerite?" D KAD0002 274.5 275 CORE PI FIRK FG CRN SLST YES M F "Tuffaceous textures, possibly strong fabric through metamorphic overprint" D KAD0002 275 276 CORE GNGY TUFF SLT FO YES D KAD0002 276 276.4 CORE GNGY FZ SLT FA SH YES S F D KAD0002 276.4 276.7 CORE GNGY TUFF SLT FO YES D KAD0002 276.7 279.7 CORE PI FIRK VCG CRN YES "strong Kspar and silica rich felsic intrusive with finder grained margins, similar composition to prev granite, occasional epidote and tourmaline " D KAD0002 279.7 283 CORE CR SDST EFS FO YES 7 DS "strongly sericite flooded, with bands of qtz kspar and zones of massive sulphide ppt, some smaller Felsic intrusives through interval although boundaries not well defined " D KAD0002 283 288.1 CORE CR SDST EFS FO YES 15 DS "strongly sericite flooded, with bands of qtz kspar and zones of massive sulphide ppt, some smaller Felsic intrusives through interval although boundaries not well defined " D KAD0002 288.1 289.1 CORE PI FIRK VCG CRN YES 7 DS "strongly sericite flooded, with bands of qtz kspar and zones of massive sulphide ppt, some smaller Felsic intrusives through interval although boundaries not well defined " D KAD0002 289.1 291.5 CORE CR SDST EFS FO YES 25 DS "strongly sericite flooded, with bands of qtz kspar and zones of massive sulphide ppt, some smaller Felsic intrusives through interval although boundaries not well defined " D KAD0002 291.5 299 CORE CR SDST EFS FO YES 15 DS "fine dissem sulphides, some massive sulphides formed along fractures. similar Kspar banding to prior" D KAD0002 299 300 CORE GY SDST EFS FO SH YES 10 DS M FRS broken ground D KAD0002 300 310 CORE GY SDST EFS FO YES 15 DS "Decreased pink Kspar colouration, still silica and py rich. massive pyrite along fractures and disseminated. Still appears to have metamorphic banding of felsic and amphibole? richer more mafic bands. occasional brown colouring but not convinced its biotite - no micacious" D KAD0002 310 311 CORE GY SDST EFS FO QZVN BX YES 10 DS "Decreased pink Kspar colouration, still silica and py rich. massive pyrite along fractures and disseminated. Still appears to have metamorphic banding of felsic and amphibole? richer more mafic bands. occasional brown colouring but not convinced its biotite - no micacious" D KAD0002 311 312 CORE GY SDST EFS FO YES 10 DS "Decreased pink Kspar colouration, still silica and py rich. massive pyrite along fractures and disseminated. Still appears to have metamorphic banding of felsic and amphibole? richer more mafic bands. occasional brown colouring but not convinced its biotite - no micacious" D KAD0002 312 315.6 CORE GY SDST EFS FO YES 15 DS Similar metamorphic banding as previous D KAD0002 315.6 316 CORE BK CSH MUD SH YES 20 BEDP "Strong rubbley weathered zone " S FRU "Sheared black shale, rubbley" D KAD0002 316 316.7 CORE GNGY SDST EFS BX QZVN BX YES 30 DS "Mild green colouring, possibly sericite, amphibole formed along fractures" D KAD0002 316.7 318 CORE BK CSH MUD SH YES 50 DS Strong rubbley weathered zone S FRU D KAD0002 318 319.2 CORE GY QZVN BX CSH MUD LAM YES 25 DS "Large qtz vein, strongly sheared through cabronaceous shale, strong pyrite overprint " D KAD0002 319.2 321.1 CORE DGY CSH MUD CBED YES 50 DS More consolodated mudstone with abundant Py overprint D KAD0002 321.1 323 CORE DGY SLST SLT PBED BX YES 30 DS "increased silica, mild green colouring, ? chl or sericite " D KAD0002 323 325.5 CORE GNGY SLST SLT PBED BX YES 20 DS "weak amphibole overprint, and some large blebs of biotite, soft black mineral. " "increased silica, mild green colouring, ? chl or sericite " D KAD0002 325.5 326.4 CORE GYGN QZVN BX SLST SLT SH YES 7 DS M SED "almost like a breccia of altered vein sheared through sediment, which has been healed and overprinted, moderate silica flooding " D KAD0002 326.4 326.8 CORE GYGN FZ FA SLST SLT SH YES 7 DS S F "almost like a breccia of altered vein sheared through sediment, which has been healed and overprinted, moderate silica flooding " D KAD0002 326.8 328.5 CORE GYGN QZVN BX SLST SLT SH YES 7 DS M SED "almost like a breccia of altered vein sheared through sediment, which has been healed and overprinted, moderate silica flooding " D KAD0002 328.5 329 CORE GYGN QZVN BX SLST SLT SH YES 7 DS rubble zone S FRU "almost like a breccia of altered vein sheared through sediment, which has been healed and overprinted, moderate silica flooding " D KAD0002 329 330 CORE GYGN QZVN BX SLST SLT SH YES 7 DS M SED "almost like a breccia of altered vein sheared through sediment, which has been healed and overprinted, moderate silica flooding " D KAD0002 330 334.1 CORE DGY TUFF SLT PBED YES 15 DS "tuffaceous sediment, actinolite and pyrite overprint and along fabric. weak sericite" D KAD0002 334.1 345.4 CORE PI GRT VCG CRN YES "Very course grained granite, Kspar and qtz dominant with lesser tourmaline. biotite growth between crsytals" D KAD0002 345.4 348 CORE PI GRT VCG CRN YES 15 DS increased in darker minerals and patches of increased disseminated pyrite. possible raft of sediment 348-349 D KAD0002 348 349 CORE PUGY GRT VCG CRN SLST YES 15 DS increased in darker minerals and patches of increased disseminated pyrite. possible raft of sediment 348-349 D KAD0002 349 350 CORE PI GRT VCG CRN YES 15 DS increased in darker minerals and patches of increased disseminated pyrite. possible raft of sediment 348-349 D KAD0002 350 356 CORE PI GRT VCG CRN YES 2 VF "similar to pervious granite, minor albite and pyrite" D KAD0002 356 366.4 CORE PI GRT CG MAS YES D KAD0002 366.4 366.7 CORE PI FZ FA YES "narrow, dark clay filled shear. " W SED D KAD0002 366.7 368 CORE PI GRT CG MAS YES D KAD0002 368 369.3 CORE PI GRT CG BX FO YES 5 FF course grained grainite 0-n localy foliated. strongly fractured. fractures filled by dark grey mineral with abundant sulphide. D KAD0002 369.3 370 CORE PI FZ FA FO YES 5 FF course grained grainite 0-n localy foliated. strongly fractured. fractures filled by dark grey mineral with abundant sulphide. D KAD0002 370 370.5 CORE PI GRT CG BX FO YES 5 FF course grained grainite 0-n localy foliated. strongly fractured. fractures filled by dark grey mineral with abundant sulphide. D KAD0002 370.5 374.4 CORE PI GRT CG MAS YES D KAD0002 374.4 375 CORE PI GRT VE CG MAS YES vuggy granite - weathered out calcite vugs in cours granite. D KAD0002 375 377 CORE PI GRT CG MAS YES D KAD0002 377 378.3 CORE PI GRT CG MAS YES 2 DS D KAD0002 378.3 380.4 CORE BK BI FG MAS YES 15 DS very fine grained dark vein / mineral intruding and cross cutting granite. soft - possibly tourmaline? abundant course (3-5mm) pyrite disseminated through oit. upper contack is diduse over 1.5m. lower contact is abrupt. D KAD0002 380.4 381 CORE PI GRT CG MAS YES 2 DS D KAD0002 381 388 CORE PI GRT CG MAS YES D KAD0002 388 389.7 CORE GY GYWK FG MAS YES narrow rsaasft of sediment within granite. cross cut by k -spar veins. D KAD0002 389.7 390 CORE RDBN GRT CG MAS GYWK YES granite with several small xenoliths of greywake. D KAD0002 390 391.5 CORE BNOR FZ FA GRT FA YES strongly fractured and altered granite. fluid flow along fracture zone resulted in granite weathering to clays and sandy material. M FBU D KAD0002 391.5 399.4 CORE PI GRT CG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 399.4 399.6 CORE PI FA YES narow flour filed shear. W SED "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 399.6 400 CORE PI GRT CG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 400 401.5 CORE PI GRT FG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 401.5 405 CORE PI GRT CG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 405 405.5 CORE PI GRT FG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 405.5 410 CORE PI GRT CG MAS YES "dark pink -red, feldspar dominated granite - abundant course grained tourmaline throughout. " D KAD0002 410 413 CORE LOR GRT CG MAS YES granite displays a crecrease in k -spar content - becomes increasingly quartz ritch. D KAD0002 413 420.5 CORE PI GRT CG MAS YES D KAD0002 420.5 421 CORE PI GRT VCG MAS YES D KAD0002 421 422 CORE WH FZ FG FA GRT YES SED sheared granite - displays crystal deformation into fine grained shear pattern. D KAD0002 422 426 CORE PI GRT VCG MAS YES D KAD0002 426 426.3 CORE WH FG FA YES SED sheared granite - displays crystal deformation into fine grained shear pattern. D KAD0002 426.3 449 CORE PI GRT VCG MAS YES D KAD0002 449 453.7 CORE GNGY DLT FG MAS YES 7 DS chilled margin within dolerite. massive dolerite lacks foliation. is this a very late stage - post cullen intrusive? D KAD0002 453.7 457 CORE PI GRT VCG MAS YES D KAD0002 457 457.3 CORE LOR FZ FG FA YES M SED sheared granite - displays crystal deformation into fine grained shear pattern. D KAD0002 457.3 458.5 CORE PI GRT VCG MAS YES D KAD0002 458.5 459.3 CORE LOR FZ FG FA YES M SED sheared granite - displays crystal deformation into fine grained shear pattern. D KAD0002 459.3 461 CORE PI GRT VCG MAS YES massive granite - vcg. displays an almost flow banded texture in mplaces. is this flow banfing or exolution laminellie? most prominent in k - spar. D KAD0002 461 463.3 CORE PI GRT VCG MAS YES D KAD0002 463.3 464.6 CORE GNGY DLT FG MAS YES 10 DS D KAD0002 464.6 465.8 CORE RDBN PEG CG MAS YES 20 DS corse grained intrusive abundent qtz - abbite - tourmaline. 3-5mm pyrite disemionated throughout. D KAD0002 465.8 467.2 CORE PI GRT CG MAS YES 10 DS D KAD0002 467.2 468 CORE RDBN PEG VCG MAS YES 15 DS corse grained intrusive abundent qtz - abbite - tourmaline. 3-5mm pyrite disemionated throughout. D KAD0002 468 474 CORE PI GRT CG MAS YES D KAD0002 474 475.1 CORE RDBN PEG CG BX YES 10 DS corse grained pegamtite with abundant sulphide development at crystal boundary fractures. sulphide strongly associated with tourmaline at crystal boundaries. D KAD0002 475.1 475.4 CORE BNOR FZ FA PEG YES 20 DS clay - flour filled fault and surrounding shear through pegmatite/ granite. associated with increased biotite - tourmaline. abundant fracture fill pyrite throughout. M SED D KAD0002 475.4 476.4 CORE RDBN GRT CG BX YES 5 DS D KAD0002 476.4 477.3 CORE PI FZ FA YES S FRU "significant damage zone - granite ground up to unhealed, grevel . samd. " D KAD0002 477.3 478.5 CORE PI PEG VCG BX YES corse grained pegamtite with abundant sulphide development at crystal boundary fractures. sulphide strongly associated with tourmaline at crystal boundaries. D KAD0002 478.5 481.3 CORE PIRD SYN CG MAS YES D KAD0002 481.3 482.7 CORE PI PEG CG MAS YES 10 DS corse grained pegamtite with abundant sulphide development at crystal boundary fractures. sulphide strongly associated with tourmaline at crystal boundaries. D KAD0002 482.7 484.8 CORE PI GRT CG MAS YES D KAD0002 484.8 485 CORE GY FZ FA YES buck qtz vein exploiting narrow flour foll - chlorite rich fault zone. D KAD0002 485 485.5 CORE WH QZVN CRN YES buck qtz vein exploiting narrow flour foll - chlorite rich fault zone. D KAD0002 485.5 485.7 CORE GY FZ FA YES buck qtz vein exploiting narrow flour foll - chlorite rich fault zone. D KAD0002 485.7 487 CORE WH GRT FG BX YES D KAD0002 487 489.4 CORE PI GRT CG MAS YES D KAD0002 489.4 490.1 CORE GNGY DLT YES 7 DS D KAD0002 490.1 490.6 CORE PI PEG VCG MAS YES qtz -ab-kspar -tourmaline pegmatite. purple tinge to mineral - flourite? D KAD0002 490.6 493.4 CORE GNGY DLT YES 5 DS 2 DS D KAD0002 493.4 501 CORE PI PEG VCG MAS YES D KAD0002 501 505.7 CORE PI GRT CG MAS YES D KAD0002 505.7 506 CORE GYGN SDST FS PBED YES D KAD0002 506 508.5 CORE GYGN SDST FS PBED YES 3 DS well bedded sandstone - hornblend decreasing down hole. disseminated pyrite. cross cut by common - k-spar stringers. D KAD0002 508.5 509.4 CORE GR SDST FS PBED YES D KAD0002 509.4 510.5 CORE GR DLT CG MAS YES D KAD0002 510.5 511.5 CORE GYGN SDST FS PBED YES 5 DS D KAD0002 511.5 514 CORE GYGN SDST FS PBED YES 5 DS 3 DS D KAD0002 514 514.3 CORE GYGN SDST FS PBED YES 5 DS D KAD0002 514.3 515.5 CORE BNGY SLST FS LAM YES laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 515.5 517 CORE BNGY SLST FS LAM YES 2 FF laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 517 520 CORE BNGY SLST FS LAM YES laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 520 522 CORE BNGY SLST FS LAM YES 2 VF laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 522 523 CORE BNGY SLST FS LAM YES laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 523 523.5 CORE BNGY SLST FS LAM YES 3 DS laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 523.5 525.5 CORE BNGY SLST FS LAM YES laminated light coloured silts and darker sands. not a true silt - silty sand. well laminated. weak pervasive chlorite. D KAD0002 525.5 527.6 CORE BNGY SDST FS PBED MAS YES interbedded massive and planar bedded sands. increased biotite. biotite is present as both a pervasive regional mineral and a bedding paralell over growth. localy strong cordirite/ albite overprint. D KAD0002 527.6 528 CORE PI FIRK CG MAS YES D KAD0002 528 528.9 CORE LGY SDST FS PBED YES 1 FF D KAD0002 528.9 530 CORE PI FIRK CG MAS YES D KAD0002 530 530.6 CORE PI FIRK CG MAS YES 3 VF D KAD0002 530.6 532 CORE GNGY SLST SLT LAM HFL YES 3 VF hornfels after siltstone. moderate bedding parallell amphibole overprint. D KAD0002 532 532.7 CORE PI FIRK CG MAS YES D KAD0002 532.7 540.6 CORE LGY SLST SLT LAM YES 2 VF 5 FF "very fine siltstones well laminated to localy massive - masive portios display strong, course garnet over growth. " D KAD0002 540.6 541 CORE DGY FZ FA YES completly clay altered fault zonr S FRU D KAD0002 541 541.3 CORE GNGY SDST FS MAS YES D KAD0002 541.3 541.4 CORE DGY FZ FA YES D KAD0002 541.4 541.8 CORE PIRD SYN MG BX YES breciated syanite exploiting faultzone - indicate moment post intrusion / cooling. D KAD0002 541.8 542.3 CORE DGY FZ FA YES S FBU D KAD0002 542.3 543.2 CORE BNOR SYN BX SLST YES interfingered felsic intrusive and assimilated siltstone. D KAD0002 543.2 545.3 CORE GNGY DRT FG FO HFL YES dolerite overprinted to hornfels - moderate ampibole overprint. D KAD0002 545.3 545.7 CORE BNOR HFL FG FO YES Amhibole - albite hornfels with moderate hematite overprint adjacent to narrow healed fracture. D KAD0002 545.7 549 CORE BNOR HFL FG PBED YES Amhibole - albite hornfels with moderate hematite overprint adjacent to narrow healed fracture. D KAD0002 549 549.6 CORE GNGY HFL MG PBED YES Amphibole - albnite hornfels. D KAD0002 549.6 551.2 CORE GRBR HFL MG PBED YES amphibole - kspar overprinted sandstone/ greywacke. partial assimilation of sediment within 0.5m of granite. D KAD0002 551.2 561 CORE PI GRT VCG CRN YES massive granite course ceytaline - Qtz 0 Ab - Kspar - cross cut by k- spar stringers. unit is inturn cross cut by late stage buck qtz veins. D KAD0002 561 562 CORE BNOR GRT VCG CRN GYWK YES course grained k -spar granite with several siltstone xenoliths. xenoliths are partialy assimilated. 3% diseminated pyrite throughout. xenoliths possess pre-granite qtz - carbonate stringers. D KAD0002 562 564 CORE PI GRT VCG CRN YES D KAD0002 564 565.3 CORE PI GRT CG CRN YES D KAD0002 565.3 566.6 CORE GY SDST FG MAS YES D KAD0002 566.6 567.4 CORE GY FZ FA YES completly brecciated / gouged fault zone. fault zone filled with milky qtz veins. broken zones and unbroken qzt veins suggests multiple stages of movment. S FBH D KAD0002 567.4 567.7 CORE SLST SLT BX YES 10 DS D KAD0002 567.7 568 CORE C/LOSS YES D KAD0002 568 568.5 CORE GY SLST SLT BX YES D KAD0002 568.5 569.5 CORE LBR DAS FG BX YES posibly micro dacite / qtz micro diorite. posibly corse grained quartzose sandstone. D KAD0002 569.5 571.5 CORE GY FZ FA YES 7 FF significant fault zone and damage zone at moderate angle to core axis. exploted by multiple buck qtz veins. pyrite within veins and disseminated within fault rock. S FBU D KAD0002 571.5 573.5 CORE GY MDST MUD BX YES 1 FF 10 FF D KAD0002 573.5 574.9 CORE WH QZVN LAM MDST MUD BX YES 2 DS 10 DS laminated milky qtz vein cross cuting carbonacious mudstone. abundant pyrite and trace arsenopyrite associated with country roack xenoliths. D KAD0002 574.9 575.4 CORE GY FZ FA YES S FBU D KAD0002 575.4 576.6 CORE GY SLST SLT BX YES 7 DS 5 DS needles of arseno pyrite forming foliation. D KAD0002 576.6 577.6 CORE LGY SDST FS BX YES 10 FF fine sand - silt coss cut by abundant qtz veins. largely buck with a few narrow laminated veins. strong pyrite sill. pyrite dominenty forms in narrow fractures in country rock. within veins close to selvage. or diseminated in country rock D KAD0002 577.6 578.2 CORE GY FZ FA YES 7 DS S SED D KAD0002 578.2 579.5 CORE GNGY SLST SLT LAM YES 3 DS 15 BEDP lamminated sandly silt. pervasive chlorite and moderate albite over print. anundant bedding parallell dulphide. cross cut by several moderate to low angle qtz veins. D KAD0002 579.5 581.9 CORE GYGN DLT FG FO YES 7 FF D KAD0002 581.9 584 CORE LGY SLST SLT LAM YES 15 DS laminated albitic silts. disseminated pyrite throughout. down hole boundary with dolerite exploted by several sheeted qtz veins. D KAD0002 584 584.6 CORE GYGN DLT FG MAS YES D KAD0002 584.6 586 CORE GY MDST MUD LAM YES 2 FF 7 SE D KAD0002 586 587 CORE GY MDST MUD LAM YES 2 FF 7 SE 1 D KAD0002 587 587.3 CORE GY FZ FA YES 2 FF 7 SE 1 D KAD0002 587.3 588 CORE GY MDST MUD LAM YES 2 FF 7 SE 1 D KAD0002 588 589 CORE PI SYN FG MAS YES D KAD0002 589 590 CORE GNGY SLST SLT LAM HFL YES 3 VF D KAD0002 590 596 CORE GYGN DLT MG MAS YES D KAD0002 596 599.6 CORE GYGN DLT MG MAS YES 5 FF D KAD0002 599.6 599.9 CORE GY FZ FA YES D KAD0002 599.9 603 CORE LGY DLT FG MAS YES 3 FF D KAD0002 603 604 CORE LGY SLST FS MAS YES D KAD0002 604 607 CORE LGY DLT FG MAS YES D KAD0002 607 617.4 CORE GY DLT FG MAS YES D KAD0002 617.4 617.6 CORE WH SH YES laminated sheared qtz vein - possesses ubundent xenolits of country rock. lamination parallell pyrrhotite and pyroite. D KAD0002 617.6 618.3 CORE GY DLT FG BX MAS YES D KAD0002 618.3 618.5 CORE WH SH YES laminated qtz vein within shear abundant pyrite - pyrrhotite. D KAD0002 618.5 619.3 CORE GY DLT FG MAS YES D KAD0002 619.3 623.4 CORE LGY DLT FG MAS YES D KAD0002 623.4 627.6 CORE GNGY SLST FG SH DLT FG SH YES 5 DS 3 DS unsure if this is just a strongly sheared dolerite or potentialy interfingered dolerite and sediment. cross cut by abunfant qtz veins with significant pyrrhotite pyriyte in both vein and disseminated in rock. D KAD0002 627.6 632.1 CORE GR DLT CG SH YES 3 FF 15 DS strongly sheared doletir - versy strong cousr and pervasive chlorite overprint. huge amounts of pyrrhotite in groundmass. cross cut by several 3 -10cm wide quartz veins - commonly contain pyrrhotite. D KAD0002 632.1 646 CORE GNGY DLT FG FO YES 1 VF D KAD0002 646 646.5 CORE WH QZVN BX YES 25 VF D KAD0002 646.5 648.6 CORE GNGY DLT FG FO YES D KAD0002 648.6 648.8 CORE SH YES quartz vein filled shear zone. M SED D KAD0002 648.8 651 CORE GNGY DLT FG FO YES D KAD0002 651 653 CORE GNGY DLT MG FO YES D KAD0002 653 654.5 CORE GNGY DLT FG FO YES D KAD0002 654.5 660.4 CORE GNGY DLT MG MAS YES D KAD0002 660.4 663.5 CORE GY SLST SLT CBED YES 2 FF D KAD0002 663.5 668 CORE GNGY DLT MG FO YES D KAD0002 668 669 CORE GNGY DLT MSD MAS YES D KAD0002 669 674 CORE GNGY DLT MG FO YES D KAD0002 674 676 CORE GNGY DLT FG FO YES D KAD0002 676 677 CORE DGY DLT FG FO YES 10 VF D KAD0002 677 682.5 CORE GYGN DLT FG FO YES D KAD0002 682.5 684 CORE GNGY DLT MG FO YES D KAD0002 684 685.7 CORE GNGY DLT FG MAS YES D KAD0002 685.7 689.5 CORE LGY DLT FG BX FO YES cross cut by low angle calxite fractures. percasive calcite alteration. D KAD0002 689.5 695.6 CORE GNGY DLT MG MAS YES D KAD0002 695.6 696 CORE WH QZVN YES D KAD0002 696 697 CORE GY DLT FG FO YES D KAD0002 697 706 CORE GNGY DLT MG FO YES D KAD0002 706 709.6 CORE LGY DLT FG BX YES D KAD0002 709.6 710.2 CORE PI GRT MG FO YES D KAD0002 710.2 711.8 CORE LGY DLT MG MAS YES cros cut by set of veins at low angle to core axis. D KAD0002 711.8 712 CORE GY FZ FA YES S FBU exploited by laminated qtz vein. D KAD0002 712 712.3 CORE DGY MDST MUD SH YES D KAD0002 712.3 714.1 CORE PIRD MDST MUD BX YES 2 DS possible mud stone witha very strong potassic overprint. alteration cross cut by qtz veining. D KAD0002 714.1 714.5 CORE WH FZ FA QZVN YES S SED D KAD0002 714.5 721 CORE GY DLT FG BX FO YES 7 FF very fine grained dolerite. cross cut by calcite stock and qtz veining.. veining associated with diseminated pyrrhotite. moderated tourmaline overprint assocuated with veining. D KAD0002 721 723.4 CORE GY SDST FG LAM FO YES 7 FF "not sure if this is a fine grained, altered folerite or a tourmaline overprinted dandstone. " D KAD0002 723.4 723.7 CORE PI GRT FG MAS YES D KAD0002 723.7 725.8 CORE RDBN SLST SLT LAM YES moderat k -spat pervasive overprint to possible siltstone (ro highly altered dolerite). serricite pervasive. tourmaline following bedding / foliation. D KAD0002 725.8 727 CORE PI GRT FG MAS YES contact exploited by set of sheeted veind and moderate angle - one of these possesses abundant pyrite ans posibly vis AU? D KAD0002 727 731.8 CORE PI GRT MG MAS YES D KAD0002 731.8 732 CORE PI FIRK CG MAS YES D KAD0002 732 735.3 CORE PI GRT MG MAS YES D KAD0002 735.3 735.4 CORE GY FZ FA YES D KAD0002 735.4 736.2 CORE PI GRT MG MAS YES D KAD0002 736.2 737 CORE PI FIRK CG MAS YES D KAD0002 737 738.7 CORE RDBN GRT MG MAS YES D KAD0002 738.7 739.2 CORE PI FIRK CG MAS YES D KAD0002 739.2 741 CORE RDBN GRT MG MAS YES D KAD0002 741 742.5 CORE PI FIRK MG MAS YES D KAD0002 742.5 744.5 CORE PI GRT FG BX YES D KAD0002 744.5 745.5 CORE CR QZVN YES D KAD0002 745.5 746.3 CORE RDBN GRT MG MAS YES 1 FF D KAD0002 746.3 746.6 CORE GNGY FZ FA YES 2 FF S SED quartz - chlorite filled shear zone D KAD0002 746.6 747.4 CORE CR QZVN YES 3 FF D KAD0002 747.4 749 CORE GY GRT MG MAS YES D KAD0002 749 750 CORE PI GRT MG MAS YES D KAD0002 750 753.7 CORE PI GRT MG MAS YES D KAD0002 753.7 754 CORE PI FIRK CG MAS YES D KAD0002 754 755.8 CORE PI GRT MG MAS YES D KAD0002 755.8 756.1 CORE PI FIRK CG MAS YES D KAD0002 756.1 757.2 CORE PI GRT MG MAS YES D KAD0003 0 26.6 CORE C/LOSS mud rotary drilling 0m - 26.6m D KAD0003 26.6 28.5 CORE CR SLST SLT LAM D KAD0003 28.5 30 CORE BNOR SDST MSD MAS D KAD0003 30 32.7 CORE BNOR SLST SLT MAS D KAD0003 32.7 42.2 CORE LBR SDST FS MAS D KAD0003 42.2 44.2 CORE CR SLST SLT CBED MDST CBED D KAD0003 44.2 51 CORE BNOR LMST FS MAS CNGL angular clasts of sand stone within fine orange matrix. D KAD0003 51 75.4 CORE BNGY SLST SLT CBED LMST FG NLR D KAD0003 75.4 85.7 CORE RD SLST SLT CBED LMST NLR D KAD0003 85.7 94.2 CORE SLST SLT PBED LMST NLR D KAD0003 94.2 96 CORE MDST SLT CBED LMST NLR D KAD0003 96 100.3 CORE SLST SLT CBED LMST NLR limestone clasts becoming more angular. D KAD0003 100.3 106 CORE SLST SLT CBED LMST BX lime stone clasts become angular. D KAD0003 106 117.8 CORE LMST FG NLR SLST CBED D KAD0003 117.8 120.8 CORE BNGY SLST SLT MAS MDST BX siltstone with abundant lamminated siltstone rip up clasts. angular - 2 - 5cm. matrix supported. D KAD0003 120.8 124 CORE BNGY SLST SLT LAM possible large paleoprot carbonacious mud stine clast in angulat breccia. D KAD0003 124 130.5 CORE BNOR CNGL BX SDST sanddtone cambrian matrix supporting 1 - 8cm clasts of angular lamminated carbonacious siltstone - possibly proterozoic rip up clasts. D KAD0003 130.5 132 CORE LGY SLST SLT BX LAM clast supported. D KAD0003 132 132.8 CORE SDST CG MAS D KAD0003 132.8 137.4 CORE BNGY MDST MSD BX LMST BX "matrix supporterd sedimentary breccia - - polylithic, limestonbne clasts and lamminated silts / muds. silts + muds - possibly proterozoic. " D KAD0003 137.4 143.4 CORE CR MDST MSD CBED LMST NLR D KAD0003 143.4 149.4 CORE BN SDST FS MAS LMST BX sandstone supporting angular limestone clasts in breccia. D KAD0003 149.4 156 CORE BN SDST FS MAS D KAD0003 156 159.6 CORE BNGY SDST FS BX VN massive sand sctone cross cut by stock work vuggy clacite veins. D KAD0003 159.6 165 CORE LBR SLST SLT LAM CBED D KAD0003 165 167.6 CORE BN SLST SLT MAS MDST BX sub angular 0.5 -2cm mudstone clasts in brown siltstone matrix. matric supported. D KAD0003 167.6 175.5 CORE BNGY MDST MSD MAS BX SKD sedimentary mudstone breccia cross cut by stoclwork calcitye veins. D KAD0003 175.5 179 CORE BNOR SLST SLT MAS MDST BX massive oxidesed siltstone containing significant angulat clasts of lamminated mudstone. D KAD0003 179 183 CORE BNGY CNGL MSD BX MDST LAM clast supported angular mudstones within mudstone matrix D KAD0003 183 203.1 CORE BNOR CNGL SLT MAS MDST LAM oxidised siltstones - massive containing abundant sub rounded to sub angulat greywacke and mudstone clasts - matrix supported to localy clast supported. clast size varies from 5cm in matrix dominated area to 0.5cm in clast supporterd areas. D KAD0003 203.1 205 CORE BN SLST SLT LAM D KAD0003 205 206.6 CORE BNOR SLST SLT LAM D KAD0003 206.6 210 CORE BNOR CNGL SLT MAS SLST LAM D KAD0003 210 213.4 CORE BNOR SDST FS MAS D KAD0003 213.4 216 CORE PI GRT MG MAS D KAD0003 216 216.8 CORE PI GRT MG MAS D KAD0003 216.8 227 CORE PI GRT MG MAS D KAD0003 227 231 CORE PI GRT FG MAS D KAD0003 231 234 CORE PI GRT CG MAS D KAD0003 234 235 CORE PI GRT CG MAS D KAD0003 235 237.5 CORE PI GRT CG MAS D KAD0003 237.5 240.5 CORE PI GRT MG MAS interdigitating syano and leuco granite D KAD0003 240.5 243.5 CORE LGY GRT MG MAS "leuco granite " D KAD0003 243.5 249 CORE PI GRT MG MAS D KAD0003 249 250.2 CORE PI FIRK CG MAS D KAD0003 250.2 252.4 CORE PI SYN MG MAS D KAD0003 252.4 252.8 CORE PI FIRK CG BX D KAD0003 252.8 264 CORE PI SYN FG MAS D KAD0003 264 271 CORE PIRD SYN MG MAS D KAD0003 271 272 CORE PIRD SYN MG MAS D KAD0003 272 273 CORE PIRD SYN MG MAS D KAD0003 273 274 CORE PIRD SYN MG MAS D KAD0003 274 275 CORE PIRD SYN MG MAS D KAD0003 275 276 CORE PIRD SYN MG MAS D KAD0003 276 279 CORE PIRD SYN MG MAS D KAD0003 279 280 CORE PIRD SYN MG MAS D KAD0003 280 282 CORE PIRD SYN MG MAS D KAD0003 282 283 CORE PIRD SYN MG MAS D KAD0003 283 285 CORE PIRD SYN MG MAS D KAD0003 285 286 CORE PIRD SYN MG MAS D KAD0003 286 290 CORE PIRD SYN MG MAS D KAD0003 290 291 CORE PIRD SYN MG MAS D KAD0003 291 292 CORE PIRD SYN MG MAS D KAD0003 292 298 CORE PIRD SYN MG MAS D KAD0003 298 298.5 CORE PIRD SYN MG MAS D KAD0003 298.5 299 CORE PI FIRK CG MAS D KAD0003 299 299.2 CORE PI FIRK CG MAS D KAD0003 299.2 301 CORE PIRD SYN MG MAS D KAD0003 301 302 CORE PI FIRK CG MAS D KAD0003 302 303 CORE PIRD SYN MG MAS D KAD0003 303 304 CORE PIRD SYN MG MAS D KAD0003 304 305 CORE PIRD SYN MG MAS D KAD0003 305 308 CORE PIRD SYN MG MAS D KAD0003 308 309 CORE PIRD SYN MG MAS D KAD0003 309 310 CORE PIRD SYN MG MAS D KAD0003 310 311 CORE PIRD SYN MG MAS D KAD0003 311 312 CORE PIRD SYN MG MAS D KAD0003 312 313 CORE PIRD SYN MG MAS D KAD0003 313 315 CORE PIRD SYN MG MAS D KAD0003 315 321 CORE PI GRT MG MAS D KAD0003 321 329.8 CORE PIRD GRT MG MAS D KAD0003 329.8 331.3 CORE GRGY BX FG BX GRT MG BX Faulted Polymictic Bx. Major Fault Zone. Rock is Friable and turned completely to Fault Gauge Clay is parts. D KAD0003 331.3 332.6 CORE GRGY BX FG BX GRT MG BX "Polymictic Bx. Jumbled clasts (Angular to rounded) of Chert, Siltstones and dolerite. Numerous generations of veining & Bx." D KAD0003 332.6 337.4 CORE GYPI GRT FG MAS "Silica-flooded, pale grey, bleached granite. " D KAD0003 337.4 348.5 CORE PIRD GRT MG MAS "Transitions to Potassic red/pink massive granite @ 337.4m. Qtz +/-Cb veining present, planar & anastomosing." D KAD0003 348.5 349.35 CORE PIRD GRT MG BX "Vn density increases, crackle texture Bx, mimnor trace Pyrite" D KAD0003 349.35 350 CORE PIRD GRT MG BX "As Above with 15mm wide Qtz & fine sulphide vein @ 349.35-.55. Strong Bx, silica flooding, matrix supported angular clasts of granite." D KAD0003 350 357.8 CORE PIRD GRT MG BX Increased Pyrite Offset veins D KAD0003 357.8 362.3 CORE GYPI GRT MG MAS Minor veining D KAD0003 362.3 362.7 CORE GYPI GRT MG MAS Dark grey pink D KAD0003 362.7 362.9 CORE GRGY SDST MG MAS "Feldspar rich sandstone, assimilated upper & lower contacts" D KAD0003 362.9 374.9 CORE PIGY GRT MG BX "Silica-flooded, pale grey, bleached granite. Planar & Anastomosing Qtz vns, strong BX 2m before contact." D KAD0003 374.9 375.7 CORE GY GRT MG BX Igneous Contact. Strong veining / Bx & Silica flooding. D KAD0003 375.7 377.4 CORE GY FZ FA GRT MG BX Sandstone & siliceous siltstone incorporated into granite. D KAD0003 377.4 396 CORE PIGY GRT MG MAS Vuggy open Qtz/cb vns after 387m D KAD0003 396 397 CORE PI FIRK CG MAS D KAD0003 397 419.2 CORE GY GRT MG M D KAD0003 419.2 422.2 CORE GYPI GRT MG MAS Leucocratic D KAD0003 422.2 422.6 CORE PI FIRK CG MAS Pegmatitic D KAD0003 422.6 425.3 CORE GYPI GRT MG MAS Leucocratic D KAD0003 425.3 426 CORE PI FIRK CG MAS Pegmatitic D KAD0003 426 428 CORE GYPI GRT MG MAS D KAD0003 428 433 CORE PI FIRK CG BX Silica Flooded. Upper Contact looks assimilated & subsequently Bx with (Zamu?) Dolerite. Late vuggy Qtz/Cb vns sub paralle to core axis. D KAD0003 433 434.6 CORE GR DLT MG MAS Dolerite incorporated into granite body. Orthocumulate. Foliated in direction of contacts and veining. Epidote Alt. D KAD0003 434.6 435.6 CORE PI FIRK CG MAS D KAD0003 435.6 440.3 CORE PI GRT MG MAS D KAD0003 440.3 442 CORE PIRD FIRK CG MAS D KAD0003 442 452 CORE PI GRT MG MAS D KAD0003 452 453 CORE PIRD FIRK CG MAS D KAD0003 453 455.5 CORE PI GRT MG MAS D KAD0003 455.5 456.4 CORE PIRD FIRK CG MAS D KAD0003 456.4 457.3 CORE PI GRT MG MAS D KAD0003 457.3 457.8 CORE PIRD FIRK CG MAS D KAD0003 457.8 465 CORE PI GRT MG MAS D KAD0003 465 465.3 CORE PIRD FIRK CG MAS D KAD0003 465.3 476 CORE PIGY GRT MG MAS D KAD0003 476 480 CORE PIGY GRT MG MAS Vuggy Qtz/cb veining sub paralle to core axis D KAD0003 480 483 CORE PIGY GRT MG MAS D KAD0003 483 483.4 CORE PIGY GRT MG BX Minor Bx D KAD0003 483.4 493 CORE PIGY GRT MG MAS EOF