Elliott Creek 1:100 000 Geological Series Map · 04 May 2006 07:28:19...
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300 300 300 320 380 420 400 400 340 300 300 340 320 380 320 300 340 320 320 400 420 420 440 360 400 400 320 400 420 340 400 320 400 440 380 300 360 400 400 420 460 340 320 340 360 400 400 400 460 400 400 460 380 400 440 400 380 360 360 460 400 360 360 340 400 400 420 400 460 420 420 440 500 400 520 500 360 540 420 420 480 460 440 400 400 420 460 500 540 560 420 440 460 480 460 500 460 580 500 460 460 440 420 500 480 480 500 500 600 600 500 460 440 480 420 400 420 440 460 460 560 460 460 580 440 400 420 440 440 460 440 440 420 420 400 380 380 420 560 Irregully Creek Muntharra Creek Muntharra Creek Creek Irregully Irregully Creek Creek Koorabooka Elliott Creek Creek Koorabooka Wanna Yard GODFREY RANGE KENNETH RANGE MINNIERRA RANGE Cobbina Yard (abd) SALLY TABLETOP JAMES TABLETOP Yard Yard landing ground Yard M I N N I E R R A R A N G E landing ground (Hoppys Strip) ALICIA TABLETOP landing ground landing ground EDNEY HILL Yard (abd) JESSICA TABLETOP landing ground Yard landing ground Stevens Yard M I N N I E R R A R A N G E landing ground (Macs Strip) landing ground landing ground Yard STEVENS HILL Yard (abd) landing ground landing ground Yard Yard Coodardo Gap K E N N E T H R A N G E Yard Yard landing ground landing ground G O D F R E Y WANNA HILL 520 m Yard landing ground Yard landing ground Wanna Yard landing ground Gifford Creek Homestead 30 km WANNA ROAD Yard Gregorys Gap R A N G E landing ground Cobra Homestead 25 km Yard Yard WHITE CLIFFS Damper Spring Dog Pool Bore Salt W ell (abd) (PD) Muntharra Pool McCorrey Bore Thorpe Bore Lee Steere Pool Strama Bore Alicia Bore Minnierra Pool Jessica Bore Dog Pool Dog Pool Bore Terrys Camp Bore Weena Well Damper Spring Bend Bore Bend Waterholes Roy Pool Weedarra Bore (abd) Bandee Well Kulkatharra Springs Python Pool Pretty Pool Coonbaroo Well Pingandi Bore Faithfuls Pool Coodardo Well Cutharra Well (abd) Delia W ell New Bore Suspense Bore (abd) Salt Well (abd) Stockyard Bore Nooneroo Bore Wanna Bore New Wanna Bore Shearing Shed Bore House Well Swamp Bore Moondine Well Eracuotharra Spring Koorabooka Bore (abd) Scotty Bore (abd) Terminus Bore Trinity Well Cain Well Godfreys Well Blue Bush Well (PD) Fault Talga Wanna Syncline od od od od od od od od od od od od od od zq zq zq zq zq od zq zq zq zq zq zq zq zq zq od od od od od od od od od od od od od od od od od od od od ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìMC-s ìMC-s ìMC-s ìMC-s ìMC-s ìMC-s ìMC-s ìME-s ìME-s ìME-s ìME-s ìW-s ìME-s zq od od od od îå46ôôôÜN è50ôôôÜE 52 54 56 58 è60 62 64 66 68 è70 72 74 76 78 è80 82 84 86 88 è90 92 94 96 98 ê00 46 48 îå50 52 54 56 58 îå60 62 64 66 68 îå70 72 74 76 78 îå80 82 84 86 88 îå90 92 94 96 98 îè00 ê00 98 96 94 92 è90 88 86 84 82 è80 78 è70 72 74 64 66 68 56 58 è60 62 è50 52 54 48 îå50 52 54 56 58 îå60 62 64 66 68 îå70 72 74 76 78 îå80 82 84 86 88 îå90 92 94 96 98 îè00 76 ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? 75 S 14 1 M 16 58 M 30 78 1 10 89 2 2 70 15 1 70 S 12 82 1 M 25 70 1 S 43 50 1 20 M 3 4 4 M 80 1 75 od ìMEl-s ìMEl-s od zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq od od zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq zq ìMCb-st ìMCb-st ìMCb-st od od od od od od od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od od od od od od od od ìMEg-s ìMEg-s od od od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od ìMCb-st ìMCb-st ìMCb-st od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od ìMCb-st od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od ìMCb-st ìMCb-st ìMCb-st ìMCb-st od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od od ìMCb-st od od od od ìMCb-st ìMCb-st ìod¿,À ìod¿,À ìMEl-s od od od od od od od ìod¿,À ìod¿,À od od od A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 A2 ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 A3 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 C1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz Rz C1q C1q C1q ìMEk-st ìMEk-st ìMEk-st ìMEk-st ìMEk-st ìMEk-st ìMEk-st C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf Rf ìWa-s ìWa-s ìWa-s ìWa-s ìWa-s ìWa-s Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk Rk od od od od od od od od od od od od od od od od od od od C1c£ C1c£ C1c£ C1c£ C1c£ C1c£ C1c£ C1c£ C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f C1f ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd ìMCb-kd Rzi Rzi Rzi W W W W W W W W W W W W W W W W W W W W W W W W W W W W W W ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st ìMCb-st A A Wf ìMEk-sl ìMEk-sl ìMEk-sl L L L L L L L L ìMEi-st ìMEi-st ìMEi-st ìMEk-kd C1tsµ A1c£ ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìMEi-k ìMEi-k ìMEi-k ìMEi-k ìMEi-k ìMEi-k ìMEi-k ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEm-k ìMEm-k ìMEg-s ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEv-k ìMEp-k ìMEp-k ìMEp-k ìMEp-k ìMEp-k ìMEp-k ìMEp-k ìMEp-k ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMEd-c ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMElc-sf ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEy-s ìMEy-s ìMEy-s ìMEy-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìMEc-s ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìodÀ ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCc-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMCi-s ìMEi-st ìMEi-st Rz ìMEi-k Rz ìMEi-k Rz ìMEi-k Rz ìMEi-k Rf ìMEi-k A2 Rk ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMCb-s C2 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMEc-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCb-s C3 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCc-s C2 ìMCi-s C2 ìMCi-s C2 ìMCi-s C2 ìMCi-s C2 ìMCi-s C2 ìMCi-s C2 ìMCi-s C2 ìMCc-s C3 ìMCc-s C3 ìMCc-s C3 ìMCc-s C3 ìMCc-s C3 C2 ìodÀ C2 ìodÀ Rk C2 Rk C2 Rf ìMEv-k Rk C2 ìWa-s C2 ìMEc-s ìMCi-s C1f ìMCi-s C1f ìMCi-s C1f ìMCi-s C1f Rz ìMEb-sl C2 ìMCb-st C2 ìMCb-st C2 ìMEk-st ìWa-s zq zq od ìMEi-k C2 ìMEk-s C2 ìMEc-s C2 ìMEc-s C2 od od ìMEl-s C3 C3 C3 Rz Rz C2 C3 ìMEk-s Rz Rz Rz C3 C2 C2 C2 ìodÀ C3 C3 C3 C1f ìod¿,À ìMEl-s ìMEl-s C2 C2 C2 C2 ìodÀ ìodÀ ìodÀ ìodÀ C3 C2 C2 C2 C2 C2 C2 C2 C2 C2 C2 ìMEi-st C3 A A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 A1 38 20 29 30 84 40 19 20 36 19 9 23 22 10 71 19 34 16 9 4 31 16 14 13 28 20 14 13 3 7 5 17 8 4 18 7 12 6 14 24 30 14 19 3 16 21 28 20 14 28 24 17 24 20 34 20 70 77 24 22 18 25 11 21 21 33 18 45 90 9 9 16 19 38 19 29 9 17 10 13 16 15 86 8 14 14 50 65 35 4 9 11 8 20 13 5 7 6 11 12 10 10 10 16 16 19 11 9 75 1 22 84 1 41 20 30 57 74 66 69 1 34 73 64 57 67 50 38 20 51 55 52 19 1 79 44 69 5 10 3 81 5 1 66 35 10 6 2 12 25 12 1 13 1 88 30 58 61 4 12 11 8 7 3 8 20 15 12 19 5 20 3 4 25 18 45 77 57 42 42 68 75 1 80 18 48 80 42 65 68 68 57 61 62 54 68 16 60 42 19 1 80 75 68 85 48 1 60 1 78 65 70 55 25 55 46 78 1 70 70 55 48 22 68 30 82 1 42 46 48 82 1 70 62 20 80 1 70 2 44 60 8 48 16 25 4 4 3 1 8 1 1 12 10 22 1 1 38 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 C3 od 212 Dmd 2148 Mn 2149 Mn 2150 Mn 2151 G A S C O Y N E M I N E R A L F I E L D A S H B U R T O N M I N E R A L F I E L D Asbs Asbs Dmd Mn 2149 ? ? ? ? 58 S M 30 15 10 Wanna Syncline 2 Edmundian Orogeny (1070Ê755 MaÝä) Capricorn Orogeny (1805Ê1780 MaÝì) 40À 116°30À 24°00À 50À 117°00À 24°00À 50À 40À 23°30À 117°00À 50À 40À 116°30À 50À 40À 23°30À SHEET 2250 AUSTRALIA 1Ý:Ý100Ý000 GEOLOGICAL SERIES GEOLOGICAL SURVEY OF WESTERN AUSTRALIA Geological boundary exposed........................................................................................................... deformation events, where known e 2 e 1 a a Edmund Fold Belt (DÛÝ ).......................................................................... Edmund Fold Belt (DÕÝ ).......................................................................... Ashburton Fold Belt (DÛÝ )....................................................................... Ashburton Fold Belt (DÕÝ )....................................................................... 4 3 Fault exposed........................................................................................................... concealed........................................................................................................ anticline; exposed, concealed....................................................................... syncline; exposed, concealed....................................................................... Small-scale fold axial surface, showing strike and dip inclined............................................................................................................ vertical............................................................................................................. syncline........................................................................................................... S-vergence...................................................................................................... M-vergence..................................................................................................... Bedding, showing strike and dip inclined............................................................................................................ 36 Cleavage, showing strike and dip inclined............................................................................................................ 80 22 Airphoto lineament Track....................................................................................................................... Homestead............................................................................................................. Yard........................................................................................................................ Contour line, 20 metre interval............................................................................ Spring..................................................................................................................... Windpump.............................................................................................................. Abandoned, position doubtful.............................................................................. Bore........................................................................................................................ Well......................................................................................................................... ¦ TRANSVERSE M ERCATO R PROJECTION Grid lines indicate 1000 m etre interval of the Map Grid Australia Zone 50 H ORIZON TAL DAT UM : GEO CENTRIC D ATU M O F AUS TRALIA 1994 VERTICAL DATUM: AU STR ALIAN H EIGHT DATUM 0 1 2 3 4 5 6 7 8 9 10 Kilom etres M etres 1000 SCALE 1:100Ý000 2048 2049 2050 2051 2148 2149 2150 2151 2248 2249 2250 2251 2348 2349 2350 2351 2448 2449 2450 2451 2548 2549 2550 2551 LOCKIER EUDAMULLAH MANGAROON M AROONAH YINNETHARRA EDMUND ULLAWARRA CAPRICORN CANDOLLE PEEDAWARRA ASHBURTON TEANO BOGGOLA PARABURDOO MULGUL KALLENIA EDMUND TUREE CREEK MOUNT EGERTON MOUNT PHILLIPS SG 50-2 SG 50-3 SF 50-14 SF 50-15 PINK HILLS MOUNT VERNON SNOWY MOUNT KENNETH RANGE ELLIOTT CREEK MOUNT PHILLIPS MOUNT AUGUSTUS MOUNT EGERTON 1:100Ý000 maps shown in black 1:250Ý000 maps shown in brown SHEET INDEX GN MN GRID / MAGNETIC GRID CONVERGENCE True north, grid north and magnetic north are shown diagrammatically for the centre of the map. Magnetic north is correct for TN 0.1¾ Building.................................................................................................................. Mineral field boundary........................................................................................... 4 km 2 km SEA LEVEL SEA LEVEL 2 km 4 km DIAGRAMMATIC SECTION A B Collier Group Edmund Group Wyloo Group concealed........................................................................................................ Fence, generally with track................................................................................... Dolerite dykes and small intrusions COLLIER BASIN EDMUND BASIN Structural symbols are labelled according to the sequence of deformation Capricorn Orogeny (1830Ê1780 Ma) normal, tick on downthrown side................................................................. reverse, triangle on upthrown side............................................................... concealed, position uncertain....................................................................... anticline........................................................................................................... Small-scale fold axis, showing trend and plunge inclined............................................................................................................ ASHBURTON BASIN Watercourse with ephemeral pool or waterhole................................................ Quartz vein Fold, showing axial trace and generalized plunge direction BeddingÊcleavage intersection lineation, showing trend and plunge SHEET 2250 B A The Map Grid Australia (MGA) is based on the Geocentric Datum of Australia 1994 (GDA94) GE OC ENT R IC DA T UM OF A UST R A L IA GDA94 positions are compatible within one metre of the datum WGS84 positions G E O L O G I C A L S U R V E Y W E S T E R N A U S T R A L I A TIM GRIFFIN DIRECTOR Geological Survey of Western Australia 0 5 10 15 20 Kilometres SCALE 1:Ý500Ý000 W Wf A L W Wf A L Sandy and clayey distal sheetwash and slope deposits, no clearly defined drainage Ferruginous sand and silt Silt, sand, and gravel in active drainage channels and adjacent to floodplains; includes ferruginous deposits C1 C1c£ C1f C1q C1tsµ C1 C1c£ C1f C1q C1tsµ A1 A1c£ A1 A1c£ Quartz and rock fragments in an unconsolidated silt and sand matrix; includes ferruginous deposits Unconsolidated ferruginous rubble and scree Quartz fragments in an unconsolidated silt and sand matrix, derived from quartz veins and quartzose rock Sandstone fragments in a silt and sand matrix, derived from sandstone Unconsolidated silt, sand, and gravel in active drainage channels; includes ferruginous deposits Swelling clay (gilgai) developed on alluvial flats C2 C2 A2 A2 Quartz and rock fragments in a partly consolidated silt and sand matrix Partly consolidated silt, sand, and gravel; partly dissected by present-day drainage C3 A3 C3 A3 Sheetwash units Alluvial unit Lacustrine unit Colluvial units, third generation Alluvial units, third generation Colluvial units second generation Alluvial unit, second generation Colluvial unit first generation Alluvial unit, first generation Residual or relict units Rf Rk Rz Rf Rk Rz Ferruginous deposits, including lateritic, ferruginous, and manganiferous duricrust Silcrete and brecciated siliceous caprock od zq ìodÀ Quartz veins, of various ages c. Dolerite and gabbro sills intruded into ìMCi-s ìMCc-s ìMCb-s ìMCb-st ìMCb-kd ILGARARI FORMATION: BACKDOOR FORM ATION: CALYIE FORMATION: siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone siltstone, mudstone, and fine-grained sandstone quartz sandstone, siltstone, mudstone, conglomerate, and dolostone Thin- to thick-bedded sandstone and siltstone ìod¿,À Edmund Group c. c. COODARDOO FORMATION: ULLAWARRA FORMATION ULLAWARRA FORMATION: DEVIL CREEK FORMATION: DISCOVERY FORMATION: Curran Member: thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills; has gradational contacts with underlying laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite ìod¿,À MUNTHARRA FORMATION: ìMEc-s ìMElc-sf ìMEl-s ìMEv-k ìMEd-c ìMEm-k ìMEk-s ìMEk-st thin- to thick-bedded dolostone and stromatoloitic dolostone, and sandstone and siltstone KIANGI CREEK FORMATION: ìMEk-kd Dolostone, siltstone, and sandstone ìMEk-sl CHEYNE SPRINGS FORMATION: dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstone ìMEp-k ìMEb-sl BLUE BILLY FORMATION: siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic ìMEg-s GOORAGOORA FORMATION: fine- to coarse-grained sandstone and siltstone; minor conglomerate, dolostone, and dolomitic siltstone ìMEi-k IRREGULLY FORMATION: stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate ìMEi-st ìMEy-s YILGATHERRA FORMATION: ìWa-s Rzi Rzi Ferruginous silcrete and brecciated siliceous caprock ASHBURTON FORMATION Unassigned QUATERNARY CAINOZOIC PHANEROZOIC Collier Group MESOPROTEROZOIC c. 1070 MaÝåÝè Bangemall Supergroup PALAEOPROTEROZOIC _ MESOPROTEROZOIC Edmund Group PROTEROZOIC c. 1620 MaÝê Wyloo Group COLLIER BASIN EDMUND BASIN ASHBURTON BASIN PALAEOPROTEROZOIC ìodÀ ìodÀ ìodÀ ìMEb-sl ìMEb-sl ìMEb-sl ìMEb-sl ìMEv-k ìMEv-k ìMEg-s ìMEg-s ìMEp-k ìMEp-k ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEk-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEl-s ìMEd-c ìMEd-c ìMEd-c ìMEc-s ìMEc-s ìMEl-s ìMElc-sf ìMElc-sf ìMCb-s ìMCb-s ìMCb-s ìMCb-s ìMCb-st ìMCb-st ìMCb-st ìMCc-s ìMCc-s ìMCi-s ìMEk-st ìMEk-st od od od ìMEi-k ìWa-s ìWa-mh W.A. N.T. S.A. N.S.W . Vic. Qld Tas. A.C.T. ìMCb-kd Department of CLIVE BROWN, M.L.A. MINISTER FOR STATE DEVELOPMENT JIM LIMERICK DIRECTOR GENERAL Industry and Resources FIRST EDITION 2004 Precious mineral Steel industry metal Industrial mineral MINERAL AND ROCK COMMODITY GROUPS MINERAL OCCURRENCES MINERAL AND ROCK COMMODITIES Asbestos, serpentine (chrysotile)............................... OPERATING STATUS AND SITE IDENTIFICATION NUMBER Regolith hosted Mineral occurrence or prospect e.g. MINERALIZATION STYLESÝ Diamond....................................................................... Manganese................................................................... ìMEb-sl ìMEg-s ìMEi-st ìMEb-sl ìMEp-k ìMEk-st ìMEp-k ìMEi-st ìMEg-s ìMEi-k ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À ìod¿,À Unconsolidated, fine-grained deposits in claypans, perennial lakes, and swamps; low-lying areas with internal drainage; usually thickly vegetated Swelling clay (gilgai) and rock fragments, mostly developed over dolerite Weakly cemented and compacted silt, sand, and gravel; deeply dissected valley-fill deposits Calcrete, developed in and adjacent to alluvial channels; locally silicified; dissected by major present-day drainage lines Dolerite dykes, sills, and small intrusions, of various ages; one suite dated at 755 MaÝâ; dashed where interpreted from aer omagnetic data Thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite, and siltstone ìod¿ ìodÀ and overlying COODARDOO FORMATION siltstone, fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills ( ) massive or laminated chert, and silicified mudstone, and siltstone; local silicified sandstone and conglomerate siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate Medium to very thick bedded quartz sandstone and siltstone Siltstone; minor fine-grained sandstone sandstone, siltstone, conglomerate, and dolostone ìWa-mh ìWa-s ìWa-mh zq ìod¿,À Dolerite and gabbro sills Dolerite and gabbro sills ìMC-s ìME-s ìW-s Version 1.0 _ June 2004 Western Australia 2004 Western Australia Geological Survey, 1:100Ý000 Geological Series The recommended reference for this map is: 100 Plain Street, East Perth, WA, 6004. Phone (08) 9222 3459, Fax (08) 9222 3444 Published by the Geological Survey of Western Australia. Digital and hard copies of this map are available from the Information Centre, Department of Industry and Resources, (1) M. T. D. Wingate and J. W. Giddings, 2000, Precam brian Research, v. 100, p. 335Ê357. Geochronology by: Interpreted geochronology by: (3) M. T. D. Wingate, 2002, GSW A Record 2002/4. (5) D. R. Nelson, 1998, GSW A Record 1998/2, p. 194Ê197. (4) D. R. Nelson, 2001, GSW A Record 2001/2, p. 10Ê20. WebÝ www.doir.wa.gov.au/gswa EmailÝ [email protected] (2) D. McB. M artin and A. M. Thorne, 2004, Precam brian Research, v. 128, p. 385Ê409. (6) S. Sheppard, et al., 2001, GSW A Record 2001/5, p. 3Ê4. (7) C. E. Hall, et al., 2001, Australian Journal of Earth Sciences, v.48, p. 731Ê744. (9) K. N. Sircom be, 2003, Australian Journal of Earth Sciences, v. 50, p. 967Ê974. ìMCb-st od ìMCb-st ìMElc-sf od unspecified...................................................................................................... 1829Ê1806 MaÝîÝðÝò (8) GSWA, in prep., G SW A Record. 2004 and moves easterly by about 0.1^ in For further details, refer to main reference Quartz and rock fragments in a weakly cemented and compacted silt and sand matrix; deeply dissected valley-fill deposits and Edmund Collier Groups Dolerite and gabbro sills intruded into Ý; oldest suite ( ) dated at 1465 MaÝåÝè and youngest suite ( ) dated at 1070 MaÝåÝè Bangemall Supergroup Bangemall Supergroup Fault DATA DIRECTORY Theme Agency Data Source Data Currency Geology 1998ÝÊÝ2001 GSWA Topography DLI and GSWA field survey 2001 Structural data WAROX GEONOMA Cadastre TENGRAPH APR 2004 MAY 2004 GESMAR Horizontal control Topographic nomenclature Dept of Industry and Resources Dept of Industry and Resources Dept of Industry and Resources Dept of Industry and Resources Dept of Land Information Dept of Land Information Dept of Land Information MAY 2004 MAY 2004 APR 2004 WAMIN MAY 2004 Dept of Industry and Resources Mineral occurrences (non-confidential) Geology by D . M cB. Martin, A. M . Thorne, and I. A . Copp 1997-98, and D. M cB. Martin 2003 Edited by F. Eddison and G. Loan Cartography by P. Taylor and B.Williams MARTIN, D. McB., THORNE, A. M., and COPP, I. A., 2004, Elliott Creek, W.A. Sheet 2250 Edmundian Orogeny (1070Ê755 Ma) Fold axes INTERPRETED BEDROCK GEOLOGY concealed, interpreted from aeromagnetic data........................................ Stratabound sedimentary ANGLE 1.1¾ 1 years. Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist facies Interbedded psammite and pelite; includes quartzÊmuscoviteÊbiotiteÊcordieriteÊandalusiteÊgarnet schist and quartzÊmuscoviteÊbiotiteÊstaurolite schist; upper greenschist to amphibolite facies (Section only) MINEDEX ìMEy-s ìMEy-s ìMEy-s Road, unsealed...................................................................................................... Sandstone, conglomerate, siltstone, and dolostone
Transcript of Elliott Creek 1:100 000 Geological Series Map · 04 May 2006 07:28:19...
04 May 2006 07:28:19 U:\CAMP\Projects\Archived\100_000\Elliott_Creek\2250-GDA.dgn
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ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEv-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEp-k
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMEd-c
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sfìMElc-sf
ìMElc-sf
ìMElc-sf
ìMElc-sf
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-s
ìMEk-sìMEk-s
ìMEk-s
ìMEk-s
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ìMEy-s
ìMEy-s
ìMEy-s
ìMCb-s
ìMCb-s
ìMCb-s ìMCb-s
ìMCb-sìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-sìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-s
ìMCb-sìMCb-s
ìMCb-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
ìMEc-s
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ìMCc-sìMCc-s
ìMCc-s
ìMCc-s
ìMCc-s
ìMCc-s
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ìMCc-s
ìMCc-s
ìMCc-s
ìMCc-s
ìMCi-sìMCi-s
ìMCi-s
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ìMEi-st
ìMEi-st
RzìMEi-k
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RzìMEi-k
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ìMCb-sC2 ìMCb-s
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ìMEc-sC3
ìMEc-sC3
ìMEc-sC3
ìMEc-sC3
ìMEc-sC3
ìMEc-sC3
ìMEc-sC3
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ìMCb-sC3
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ìMCi-sC2
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ìMCc-sC3
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C2ìodÀ
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RkC2
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RfìMEv-k
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C2ìWa-s
C2ìMEc-s
ìMCi-sC1f
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C2ìMCb-st
C2ìMCb-st
C2ìMEk-st ìWa-s
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ìMEk-sC2ìMEc-s
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ìMEc-sC2
odod
ìMEl-s
C3
C3C3
Rz
Rz
C2
C3
ìMEk-s
Rz
Rz
Rz
C3
C2
C2
C2
ìodÀ
C3
C3
C3
C1f
ìod¿,À
ìMEl-s
ìMEl-s
C2
C2
C2
C2ìodÀ
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C3C2
C2
C2
C2
C2
C2
C2
C2
C2
C2
ìMEi-st
C3
A
A1
A1
A1
A1
A1
A1A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
38
20
29
30
84
40
19
20
36
19
9
23
2210
71
19
34
16
9
4
31
16
14
13
28
20
14
13
3
7
5
17
8
4
18 7
12
6
14
24
30
14
19316
21
282014
28
24
17
24
20
34
20 7077
24
22
18
25
11
21
21
3318
45
90
9
9
16
19
38
19
29
9
17
10
13
16
15
868
14
1450
65
35
4
9
11
8
20
13
5
7
6
11 12
10
10 10
16
16
19
119
751
22
84
1
41
20
3057
74
66
69
1
34
73 64 57
67
50
38
2051
55
5219
1 79
44
69
5 10
381
5 166 35
10
6
2
12
25
12
1
13
1 88
30
5861
4
12
11
87
3
8
20
15
12
19
5
20
3
4
25
18
45
77
57
42
42
68
75 1
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18
4880
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65
68
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57
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166042
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75
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8548
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55
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801
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2
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25
4
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10
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38
C3
C3C3
C3
C3
C3C3
C3 C3
C3
C3
C3C3
C3
C3
C3
C3
od
212
Dmd
2148
Mn
2149Mn
2150Mn
2151
G A S C O Y N E M I N E R A L F I E L D
A S H B U R T O N M I N E R A L F I E L D
Asbs
Asbs
Dmd
Mn
2149
? ?
? ?
58
SM 30
15
10
Wanna Syncline
2
Edmundian Orogeny (1070Ê755 MaÝä)
Capricorn Orogeny (1805Ê1780 MaÝì)
40À116°30À
24°00À
50À 117°00À
24°00À
50À
40À
23°30À
117°00À50À40À116°30À
50À
40À
23°30À
SHEET 2250AUSTRALIA 1Ý:Ý100Ý000 GEOLOGICAL SERIES GEOLOGICAL SURVEY OF WESTERN AUSTRALIA
Geological boundary
exposed...........................................................................................................
deformation events, where known
e 2
e 1
a
a
Edmund Fold Belt (DÛÝ )..........................................................................
Edmund Fold Belt (DÕÝ )..........................................................................
Ashburton Fold Belt (DÛÝ ).......................................................................
Ashburton Fold Belt (DÕÝ ).......................................................................
4
3
Fault
exposed...........................................................................................................
concealed........................................................................................................
anticline; exposed, concealed.......................................................................
syncline; exposed, concealed.......................................................................
Small-scale fold axial surface, showing strike and dip
inclined............................................................................................................
vertical.............................................................................................................
syncline...........................................................................................................
S-vergence......................................................................................................
M-vergence.....................................................................................................
Bedding, showing strike and dip
inclined............................................................................................................36
Cleavage, showing strike and dip
inclined............................................................................................................80
22
Airphoto lineament
Track.......................................................................................................................
Homestead.............................................................................................................
Yard........................................................................................................................
Contour line, 20 metre interval............................................................................
Spring.....................................................................................................................
Windpump..............................................................................................................
Abandoned, position doubtful..............................................................................
Bore........................................................................................................................
Well.........................................................................................................................
¦
TRANSVERSE MERCATOR PROJECTION
Grid lines indicate 1000 metre interval of the Map Grid Australia Zone 50
HORIZONTAL DATUM: GEOCENTRIC DATUM OF AUSTRALIA 1994VERTICAL DATUM: AUSTRALIAN HEIGHT DATUM
0 1 2 3 4 5 6 7 8 9 10
KilometresMetres
1000
SCALE 1:100Ý000
2048
2049
2050
2051
2148
2149
2150
2151
2248
2249
2250
2251
2348
2349
2350
2351
2448
2449
2450
2451
2548
2549
2550
2551
LOCKIER
EUDAMULLAH
MANGAROON
MAROONAH
YINNETHARRA
EDMUND
ULLAWARRA CAPRICORN
CANDOLLE
PEEDAWARRA
ASHBURTON
TEANO
BOGGOLA
PARABURDOO
MULGUL
KALLENIA
EDMUND TUREE CREEK
MOUNT EGERTONMOUNT PHILLIPS
SG 50-2 SG 50-3
SF 50-14 SF 50-15
PINK HILLS
MOUNT VERNON
SNOWY MOUNT
KENNETH RANGEELLIOTT CREEK
MOUNT PHILLIPSMOUNT
AUGUSTUS
MOUNT EGERTON
1:100Ý000 maps shown in black
1:250Ý000 maps shown in brown
SHEET INDEX
GNMN
GRID / MAGNETIC
GRIDCONVERGENCE
True north, grid north and magnetic north
are shown diagrammatically for the centre
of the map. Magnetic north is correct for
TN
0.1¾
Building..................................................................................................................
Mineral field boundary...........................................................................................
4 km
2 km
SEA LEVEL SEA LEVEL
2 km
4 km
DIAGRAMMATIC SECTIONA B
Collier Group
Edmund Group
Wyloo Group
concealed........................................................................................................
Fence, generally with track...................................................................................
Dolerite dykes and small intrusions
COLLIER BASIN
EDMUND BASIN
Structural symbols are labelled according to the sequence of deformation
Capricorn Orogeny (1830Ê1780 Ma)
normal, tick on downthrown side.................................................................
reverse, triangle on upthrown side...............................................................
concealed, position uncertain.......................................................................
anticline...........................................................................................................
Small-scale fold axis, showing trend and plunge
inclined............................................................................................................
ASHBURTON BASIN
Watercourse with ephemeral pool or waterhole................................................
Quartz vein
Fold, showing axial trace and generalized plunge direction
BeddingÊcleavage intersection lineation, showing trend and plunge
SHEET 2250
B
A
The Map Grid Australia (MGA) is based on the Geocentric Datum of Australia 1994 (GDA94)
GEOCENTRIC DATUM OF AUSTRALIA
GDA94 positions are compatible within one metre of the datum WGS84 positions
GEOLO
G IC A L SURV EY
WE
ST
E R N A U S T RA
LIA
TIM GRIFFIN
DIRECTOR
Geological Survey ofWestern Australia
0 5 10 15 20
Kilometres
SCALE 1:Ý500Ý000
W Wf A L
WWf
A
L
Sandy and clayey distal sheetwash and slope deposits, no clearly defined drainageFerruginous sand and silt
Silt, sand, and gravel in active drainage channels and adjacent to floodplains; includes ferruginous deposits
C1C1c£C1fC1qC1tsµ
C1 C1c£ C1f C1q C1tsµ A1 A1c£
A1A1c£
Quartz and rock fragments in an unconsolidated silt and sand matrix; includes ferruginous deposits
Unconsolidated ferruginous rubble and screeQuartz fragments in an unconsolidated silt and sand matrix, derived from quartz veins and quartzose rockSandstone fragments in a silt and sand matrix, derived from sandstone
Unconsolidated silt, sand, and gravel in active drainage channels; includes ferruginous depositsSwelling clay (gilgai) developed on alluvial flats
C2
C2 A2
A2
Quartz and rock fragments in a partly consolidated silt and sand matrix
Partly consolidated silt, sand, and gravel; partly dissected by present-day drainage
C3 A3
C3
A3
Sheetwash units
Alluvial unit
Lacustrine unit
Colluvial units, third generation
Alluvial units, third generation
Colluvial units second generation
Alluvial unit, second generation
Colluvial unit first generation
Alluvial unit, first generation
Residual or relict units
Rf Rk Rz
RfRkRz
Ferruginous deposits, including lateritic, ferruginous, and manganiferous duricrust
Silcrete and brecciated siliceous caprock
od
zq
ìodÀ
Quartz veins, of various ages
c.
Dolerite and gabbro sills intruded into
ìMCi-s
ìMCc-s
ìMCb-s
ìMCb-st
ìMCb-kd
ILGARARI FORMATION:
BACKDOOR FORMATION:
CALYIE FORMATION:
siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone
siltstone, mudstone, and fine-grained sandstone
quartz sandstone, siltstone, mudstone, conglomerate, and dolostone
Thin- to thick-bedded sandstone and siltstone
ìod¿,À Edmund Group c.c.
COODARDOO FORMATION:
ULLAWARRA FORMATION
ULLAWARRA FORMATION:
DEVIL CREEK FORMATION:
DISCOVERY FORMATION:
Curran Member:
thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone
siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills; has gradational contacts with underlying
laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite
ìod¿,À
MUNTHARRA FORMATION:
ìMEc-s
ìMElc-sf
ìMEl-s
ìMEv-k
ìMEd-c
ìMEm-k
ìMEk-s
ìMEk-st
thin- to thick-bedded dolostone and stromatoloitic dolostone, and sandstone and siltstone
KIANGI CREEK FORMATION:
ìMEk-kd Dolostone, siltstone, and sandstone
ìMEk-sl
CHEYNE SPRINGS FORMATION: dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstoneìMEp-k
ìMEb-sl BLUE BILLY FORMATION: siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic
ìMEg-s GOORAGOORA FORMATION: fine- to coarse-grained sandstone and siltstone; minor conglomerate, dolostone, and dolomitic siltstone
ìMEi-k IRREGULLY FORMATION: stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate
ìMEi-st
ìMEy-s YILGATHERRA FORMATION:
ìWa-s
Rzi
Rzi Ferruginous silcrete and brecciated siliceous caprock
ASHBURTON FORMATION
Unas
signe
dQU
ATER
NARY
CAIN
OZOI
C
PHAN
EROZ
OIC
Collie
r Gro
up
MES
OPRO
TERO
ZOIC
c. 1070 MaÝåÝè
Bang
emal
l Sup
ergr
oup
PALA
EOPR
OTER
OZOI
C _
MES
OPRO
TERO
ZOIC
Edm
und
Grou
p
PROT
EROZ
OIC
c. 1620 MaÝê
Wylo
o Gr
oup
COLL
IER
BASI
NED
MUN
D BA
SIN
ASHB
URTO
N BA
SIN
PALA
EOPR
OTER
OZOI
C
ìodÀ
ìodÀ
ìodÀ
ìMEb-sl
ìMEb-sl
ìMEb-sl
ìMEb-sl
ìMEv-k
ìMEv-k
ìMEg-s
ìMEg-s
ìMEp-k
ìMEp-kìMEk-sìMEk-s ìMEk-s
ìMEk-s
ìMEk-sìMEk-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEd-c
ìMEd-c
ìMEd-c
ìMEc-s
ìMEc-s
ìMEl-s
ìMElc-sf
ìMElc-sf
ìMCb-s
ìMCb-sìMCb-s
ìMCb-s
ìMCb-st
ìMCb-st
ìMCb-st
ìMCc-s
ìMCc-s ìMCi-s
ìMEk-st
ìMEk-st
od
od
odìMEi-k
ìWa-s
ìWa-mh
W.A.
N.T.
S.A.
N.S.W.
Vic.
Qld
Tas.
A.C.T.
ìMCb-kd
Department of
CLIVE BROWN, M.L.A.
MINISTER FOR STATE DEVELOPMENT
JIM LIMERICK
DIRECTOR GENERAL
Industry and Resources
FIRST EDITION 2004
Precious mineral
Steel industry metal
Industrial mineral
MINERAL AND ROCK COMMODITY GROUPS
MINERAL OCCURRENCES
MINERAL AND ROCK COMMODITIES
Asbestos, serpentine (chrysotile)...............................
OPERATING STATUS AND SITE IDENTIFICATION NUMBER
Regolith hosted
Mineral occurrence or prospect e.g.
MINERALIZATION STYLESÝ
Diamond.......................................................................
Manganese...................................................................
ìMEb-sl ìMEg-sìMEi-st
ìMEb-sl
ìMEp-k
ìMEk-st
ìMEp-k
ìMEi-st
ìMEg-sìMEi-k
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,Àìod¿,À
Unconsolidated, fine-grained deposits in claypans, perennial lakes, and swamps; low-lying areas with internal drainage; usually thickly vegetated
Swelling clay (gilgai) and rock fragments, mostly developed over dolerite
Weakly cemented and compacted silt, sand, and gravel; deeply dissected valley-fill deposits
Calcrete, developed in and adjacent to alluvial channels; locally silicified; dissected by major present-day drainage lines
Dolerite dykes, sills, and small intrusions, of various ages; one suite dated at 755 MaÝâ; dashed where interpreted from aeromagnetic data
Thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite, and siltstone
ìod¿ ìodÀ
and overlying COODARDOO FORMATION
siltstone, fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills ( )
massive or laminated chert, and silicified mudstone, and siltstone; local silicified sandstone and conglomerate
siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate
Medium to very thick bedded quartz sandstone and siltstone
Siltstone; minor fine-grained sandstone
sandstone, siltstone, conglomerate, and dolostone
ìWa-mh
ìWa-sìWa-mh
zq
ìod¿,À
Dolerite and gabbro sills
Dolerite and gabbro sills
ìMC-s
ìME-s
ìW-s
Version 1.0 _ June 2004
Western Australia 2004
Western Australia Geological Survey, 1:100Ý000 Geological Series
The recommended reference for this map is:
100 Plain Street, East Perth, WA, 6004. Phone (08) 9222 3459, Fax (08) 9222 3444
Published by the Geological Survey of Western Australia. Digital and hard copies of thismap are available from the Information Centre, Department of Industry and Resources,
(1) M. T. D. Wingate and J. W. Giddings, 2000, Precambrian Research, v. 100, p. 335Ê357.Geochronology by:
Interpreted geochronology by:
(3) M. T. D. Wingate, 2002, GSWA Record 2002/4.
(5) D. R. Nelson, 1998, GSWA Record 1998/2, p. 194Ê197.(4) D. R. Nelson, 2001, GSWA Record 2001/2, p. 10Ê20.
WebÝ www.doir.wa.gov.au/gswa EmailÝ [email protected]
(2) D. McB. Martin and A. M. Thorne, 2004, Precambrian Research, v. 128, p. 385Ê409.
(6) S. Sheppard, et al., 2001, GSWA Record 2001/5, p. 3Ê4.(7) C. E. Hall, et al., 2001, Australian Journal of Earth Sciences, v.48, p. 731Ê744.
(9) K. N. Sircombe, 2003, Australian Journal of Earth Sciences, v. 50, p. 967Ê974.
ìMCb-st
od
ìMCb-st ìMElc-sf
od
unspecified......................................................................................................
1829Ê1806 MaÝîÝðÝò
(8) GSWA, in prep., GSWA Record.
2004 and moves easterly by about 0.1^ in
For further details, refer to main reference
Quartz and rock fragments in a weakly cemented and compacted silt and sand matrix; deeply dissected valley-fill deposits
andEdmund Collier Groups
Dolerite and gabbro sills intruded into Ý; oldest suite ( ) dated at 1465 MaÝåÝè and youngest suite ( ) dated at 1070 MaÝåÝè
Bang
emal
lSu
perg
roup
Bang
emal
lSu
perg
roup
Fault
DATA DIRECTORY
Theme AgencyData Source Data Currency
Geology 1998ÝÊÝ2001GSWA
Topography DLI and GSWA field survey 2001
Structural data WAROX
GEONOMA
Cadastre TENGRAPH APR 2004
MAY 2004GESMARHorizontal control
Topographic nomenclature
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Land Information
Dept of Land Information
Dept of Land Information
MAY 2004
MAY 2004
APR 2004
WAMIN MAY 2004 Dept of Industry and Resources
Mineral occurrences(non-confidential)
Geology by D. McB. Martin, A. M. Thorne, and I. A. Copp 1997-98, and D. McB. Martin 2003 Edited by F. Eddison and G. Loan
Cartography by P. Taylor and B.Williams
MARTIN, D. McB., THORNE, A. M., and COPP, I. A., 2004, Elliott Creek, W.A. Sheet 2250
Edmundian Orogeny (1070Ê755 Ma)
Fold axes
INTERPRETED BEDROCK GEOLOGY
concealed, interpreted from aeromagnetic data........................................
Stratabound sedimentary
ANGLE 1.1¾
1 years.
Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist faciesInterbedded psammite and pelite; includes quartzÊmuscoviteÊbiotiteÊcordieriteÊandalusiteÊgarnet schist and quartzÊmuscoviteÊbiotiteÊstaurolite schist;
upper greenschist to amphibolite facies (Section only)
MINEDEX
ìMEy-s
ìMEy-s
ìMEy-s
Road, unsealed......................................................................................................
Sandstone, conglomerate, siltstone, and dolostone
