1
100 100 100 100 100 100 100 200 200 100 100 100 100 40 40 60 60 60 60 60 80 80 80 80 80 80 80 80 80 80 140 120 140 140 160 140 140 140 140 120 120 160 180 160 160 80 120 120 120 60 80 80 80 160 160 180 140 160 140 160 140 140 160 160 140 140 120 80 80 80 100 100 40 80 80 120 120 140 200 80 60 120 140 140 120 100 120 120 100 120 80 80 Pilinya Creek TURNER RIVER RIVER TURNER EAST STRELLEY RIVER WEST Tabba Tabba Creek Tabba Tabba Creek Petermarer Creek Beebingarra Creek Beebingarra Creek Fingerpost Creek Bore Creek TURNER RIVER TURNER RIVER Carraba Creek INDIAN OCEAN Bore Creek TUR NER RIVER Beebingarra Creek Tabba Tabba Creek WEST GREAT NORTHERN BULLEN HILL TRIG HILL Indee WALLARINGA PEAK Wallareenya COOKES HILL RED HILL Tabba Tabba transmission line GREAT NORTHERN HIGHWAY INDEE ROAD PUNTANYA RIDGE MAGPIE RANGE TABBA TABBA ROAD TABBA TABBA ROAD WALLAREENYA ROAD WALLAREENYA ROAD OLD MARBLE BAR ROAD WALLAREENYA ROAD PORT HEDLAND WITTENOOM ROAD PORT HEDLAND WITTENOOM ROAD WITTENOOM ROAD NEWMAN PORT HEDLAND RAILWAY HEDLAND NEWMAN RAILWAY PORT HIGHWAY Roebourne 168 km Port Hedland 30 km Port Hedland 59 km Lalla Rookh Homestead 19 km Lalla Rookh Homestead 19 km Marble Bar 139 km Port Hedland 50 km Abydos Homestead 53 km Port Hedland 28 km Pippinga rra Hom estead 5 km Tabba Tabba R122 64m Port Hedland Newman Railway PORT HEDLAND Lalla Rookh Homestead 47 km Great Northern Highway 5 km Great Northern Highway 8 km Road Auski Tourist Village 162 km Woodstock Homestead 78 km landing ground landing ground landing ground landing ground (abd) landing ground (abd) Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard Yard landing ground Cooliarin Pool (PD) Tanks Pooca Pools Puntanya Pool Well Wonnabuckety Well Gerrie Well Junction Well Outcamp Well Yambanya Well Red Bank Well Chituma Well Boundary Well Old Indee Well Florrie Well Wallyanna Well Granite Well Mookareenya Well Shorty Well Bungabar Well Newman Well Anzac Well Pardoo Well Red Hill Well Munda Well Fingerpost Well Newman Well Pinnipindinna Well Carubumya Well Edgar Well Baker Well Carowehyna Well Western Well Talyebinya Well Woggra Well Well Black Tank Well Edenuenya Well Mardacoombania Well Wingina Well Beti Beti Well Calerooloondinya Well Minamonica Well Pilinya Well Wayeranna Well Top Well Coorunya Well Talye Well Poocatche Well South Well Granite Well Pingina Well Merinya Well Peerinya Well Trig Well Howell Well Wodra Well Leehey Well Myanna Well Deep Well Bluff Well Toodigrina Well Shed Well Orchard Well Pookingarra Well (abd) Cralbra Well Kobalana Well (PD) Cosacana Well Hall Well Malindra Well Chillerina Well Rhyne Well Wallareenya Well Box Soak Well Big Hill Well Mac Well Peterson Govt Well Robert Well Donald Well Pedlars Well Box Creek Well Wattle Well Coogiearrina Well Grass Plain Well Claypan Well Murkingana Well Coolie Well Brown Well 9 Mile Well (PD) Mungaleena Well (PD) Culba Well (abd) Wallareenya Well Chookabraneeina Well (PD) No 5 Well (abd) Mindra Well 6 Mile Well (abd) Boundary Well Tank Tank Tank Tank Tank Tank Tabba Bore Trig Hill Well Schillaman Well No 4 Bore (PD) Mount Dove Well Marlbourgh Well (abd) Coolie Coolie Well (abd) Balbryna Well Chookabraneeina Well (abd) Magpie Well (abd) Bore Well Dam Tank (abd) (PD) Pool Jeffery Well T ab b a Sh e a r Z on e Ta b b a Indee Fault ñgIm ñP ñbm ñgIm ñgIm ñog ñog ñD ñD ñu ñGl ñgLpo ñgLpo ñgLpo ñut ñut ñba ñgLut ñP ñu ñGl ñu ñog ñgIwa ñD ñD ñgId ñgIch ñgIch ñgIm ñGl ñogs ñu ñog ñgIm ñog ñWe ñgLpo d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d ñu ñD ñO ñgLmw ñGl d d ñgLmp ñGl d dx dx dx dx dx ñgLm ñgm ñP ñu ñur ñgIlw ñD ñgIch ñbau ñgIch ñDc ñgg ñogs ñgLmp ñgLpo ñgLmi ñgLmp ñgLmp ñgLmw ñgLut ñgLmi ñgLkd ñgId ñD ñgImy ñD ñgIth ñgItt ñgIpr ñgIm îì78ôôôÜN îì80 82 84 86 88 îì90 92 94 96 98 îî00 02 04 06 08 îî10 12 14 16 18 îî20 22 24 26 28 îî30 32 58 ì56ôôôÜE ì60 62 64 66 68 ì70 72 74 76 78 ì80 82 84 86 88 ì90 92 94 96 98 î00 02 04 06 78 îì80 82 84 86 88 îì90 92 94 96 98 îî00 02 04 06 08 îî10 12 14 16 18 îî20 22 24 26 28 îî30 58 ì60 62 64 66 68 ì70 72 74 76 78 ì80 82 84 86 88 ì90 92 94 96 98 î00 02 04 06 08 ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? Z 75 Z 10 Z S 30 S S Z 70 75 30 S S 60 80 80 45 35 40 55 20 30 50 60 70 60 75 70 10 10 50 10 85 75 75 65 75 80 75 62 58 80 80 80 75 80 80 80 20 70 70 65 80 70 70 30 20 85 80 80 85 80 80 60 70 70 45 75 80 80 85 85 82 68 65 70 70 80 75 70 70 70 50 80 83 85 85 86 88 75 70 80 65 70 70 80 88 40 54 60 80 83 75 70 80 55 80 80 70 80 85 80 60 70 75 70 70 80 80 70 75 80 80 85 10 80 85 80 50 80 85 50 65 60 60 85 85 85 80 80 75 50 70 80 80 70 80 85 75 75 75 75 75 75 75 65 65 70 80 80 80 80 80 80 80 80 80 85 60 10 65 70 75 80 75 80 60 70 75 75 80 75 85 85 70 70 85 85 70 70 80 80 75 85 80 80 20 70 70 70 50 80 85 60 80 80 60 70 26 70 70 5 10 60 60 60 45 60 60 60 70 70 70 70 30 70 10 55 70 70 75 60 65 70 70 40 50 85 60 80 50 70 30 70 65 80 80 75 82 60 60 80 65 85 75 65 85 50 55 65 75 70 70 70 70 80 80 80 80 80 80 80 85 85 75 75 75 75 75 55 60 70 60 80 80 80 80 60 75 80 85 70 80 80 80 80 80 80 80 80 80 80 80 80 80 70 70 70 50 70 85 85 85 76 80 75 78 85 60 65 65 50 75 60 58 65 60 55 60 75 50 60 70 75 30 30 30 30 30 20 20 70 70 70 80 75 65 60 60 45 75 75 75 70 70 70 85 85 85 60 60 60 80 80 80 80 80 80 80 75 88 70 60 60 70 70 70 70 80 80 80 80 80 80 80 80 80 80 80 80 85 85 80 75 85 85 80 65 73 70 75 80 80 80 80 80 80 70 80 85 70 70 80 80 85 85 80 80 80 80 85 85 85 85 85 85 84 65 65 70 70 60 75 56 75 80 70 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 80 70 70 70 70 70 70 70 70 70 70 70 70 70 75 85 75 75 75 85 85 65 75 85 80 60 60 85 85 55 75 75 55 50 70 80 85 75 80 80 75 80 80 65 85 80 80 80 80 70 60 75 80 80 80 85 85 80 80 75 75 70 70 55 65 75 70 80 80 80 85 85 75 75 75 75 70 70 65 65 65 50 55 80 85 65 70 85 80 80 80 70 80 80 80 85 85 85 80 75 75 80 80 80 70 70 75 75 65 55 85 85 85 85 80 80 80 80 80 80 80 80 80 80 80 85 85 85 85 85 85 85 65 65 60 60 75 60 80 80 80 80 70 85 85 75 10 70 70 70 70 80 80 50 65 80 80 80 80 80 80 80 80 80 80 80 80 80 70 70 70 85 85 75 20 30 80 80 80 80 80 70 70 75 80 80 80 80 80 80 80 80 15 30 10 65 40 70 75 60 50 30 35 80 80 55 85 85 40 30 70 80 60 55 15 15 60 65 80 Ôao Ôao Ôrg Ôaa Ôrg Ôw Ôaoc Ôrg Ôw Ôaoc Ôc ñOt Ôao Ôaa Ôaoc Ôao Ôaa Ôaoc Ôaoc Ôaa ñgImy ñgImy ñgImy ñgImy Ôaoc Ôaoc Ôaoc Ôaoc Ôao Ôaoc Ôaoc Ôao ñgImy Ôw Ôw Óag Óag Óag Ôrg ñgIchm ñgIpr ñgImy ñgImy ñgImy ñgImy ñgIpe ñgImy ñgImy ñgImy Óak ñgImy Ôrg ñgImy ñgImy Órk Óaf Óak Ôc Ôw Óag ñgIchm Ôaa ñgIpr ñgIpr ñgIpe ñgImy ñgImy ñgImy ñgImy Órk ñgImy Órk Órk Ôrg ñus Óaq Óaq ñgImy Órk ñgImy Ôaoc Ôaoc ñgIpr Ôrg Ôrg Ôao Óak Óag Óag Óag Óag Óag ñgIpr ñgImsl ñgIpr Óaq Ôao ñgLmm Ôw ñbus ñog ñgIpr ñbus ñog Ôao ñuts Ôrg Ôrg ñgIpr ñgIms Ôw ñgIpr Ôrg ñgIpr Óak Ôaa Ôaa Ôao ñur Ôaoc Ôaoc Ôaoc Ôaoc ñDm ñDm Óaf Óaf Óaf Óaf ñDm ñgImq Óag ñurg ñfpx ñfpx ñur ñur ñur ñurs Óag ñDm ñgImq ñfp Ôaoc Ôao Ôao ñgImq ñur ñur ñgImq Ôaoc Órk Órk Órk Órk Órk ñDm Ócf Ócf Ócf Óaf Óaf Óaf Ócf Ócf Ócf Ócf Ócf Ócf Ôc ñog ñog ñgIlw ñgIlw ñgIlw ñgIlw ñgIlw Órk ñgIlw ñgIchn ñgIchn ñog ñgIchn ñgIchn ñbau ñbao ñbao ñut ñut ñgIchn ñgIdi ñog ñgIdh ñgIdi Óaq Óaq Óaq ñgIchp Ôaoc Ôab ñfp ñgIwa Óaq ñgIdl ñgIms ñgIml ñgIch ñgIch Óaq ñgId Órk ñgIchm ñgIchm ñgIchp Óak ñgIchd Órk Ôao Ôao Ôao Ôao Ôao Ôao ñog ñgIchi Órk ñgIchi ñgIms ñgImsx ñgImsx ñgImsx ñgImsx ñgIdc ñgIms Óaq Ôao ñgIdc ñgIms ñgIwa Órk Ôao Ôab ñog ñgLmm ñut ñog ñog ñogm Ôao Ôao Ôao ñgImsl ñgIpr ñgItt Órk Órk Órk Óaq ñgLmp ñgLmp ñgLmp Ôrg Ôao Ôrg ñgLkd ñgLkd ñgLkd Óak Óak Ôao ñog Óaq Ôao ñgLmw ñgLmm Ôao Ôao Óag ñgId Óag Óaq ñogs Ôao ñgLmm ñog Ôao Ôw Ôw ñDcs ñDm ñDm ñDcs ñDcs ñDm Ôao Óaf ñDm ñDm ñDm ñDm Ôaoc Ócf Ócf Ócf ñus ñbus ñgLpe ñgLmf ñgLmp ñogs ñogsf Ôaoc Ôaoc ñgLmp Órk Óaf Ócf Ócf Ócf Ôaa Ócf ñDm ñDmhl ñbus ñogsf ñgLdmf Ôaoc Ôaoc ñgLmf ñgLmf Órk ñgLmi ñgLmi ñgLmi ñgLmi ñgLmi Órk ñgLmi ñgLmi ñgLmp ñgLmf ñgLmp ñgLdmf Órk Ócf ñfs ñgLmf Ócf Ócf Ócf Órk Óaq Ôao ñDm ñgLdmf Ôaa Ôrg Órk ñgLpo ñgLpo Óaf Ôao Ócf Ócf Ócf Ôrg Ôrg Ôrg ñgLmp Ôaa Ôaa ñgLmw ñgLmw ñgLpo Óaf Órk Órk ñgLmw ñgLmf ñgLmw ñfs ñgIwa Ôao Ôao ñfs ñogs ñbus ñogs Ôaa ñgLdmf Ôaa ñgLmp ñgLmp Ôrg Ôrg Ôrg Ôrg Órk Órk ñgLkd ñgLkd Ôaa ñgLkd Ôrg Ôrg Ôaa ñgLmi ñgLmp ñgLmp Órk ñgLmp ñut ñut ñgLut ñgLmi Ôaoc Ôaoc Órk Órk Órk Órk ñut ñut ñut ñut ñogs ñogs ñogs ñgLmi ñgLmi ñgLmi ñgLmi ñgLmi ñgLmp Ôao Ôao Ôrg Ôao Ôao Ôao ñgLmp Ôaa Ôaoc ñgLpo ñgLpo ñgLpo ñgLpo ñgLpo ñgLpo ñgLpo ñgLpo Ôrg Ôrg ñgLmi ñgLmi ñgLmi Órk Ôao Ôao Ôaa ñgLpe ñgLpe ñgLmp ñgLmp ñgLmp ñgLmx ñut ñut ñut Ôrg Ôrg Ôrg Órk ñgLutx Ôrg Ôaa ñut Ôrg ñgLmp ñgLmp Ôrg ñgLutx ñgLutx ñgLutx ñgLutx ñgLutx ñgLutx ñgLut ñgLut ñgLut ñgLut ñut ñut ñut ñut ñut ñgLut ñba ñut Ôc ñs ñubs ñWeb ñOtbc ñgLmb ñgLm ñut ñgIpr ñgLmm Óag Ôaoc Ôao ñgImsl Ôao ñgIms Ôw Ôw Ôw Ôw Óag Óc Óc Óc Óc Óc q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q q d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d d dx dx dx dx dx dx dx dx ñbaog ñbaog ñgIth Óc Óc Óc Óc q ñbao q ñgImy q ñgIpe Órk d ñgIpe Óaq ñgImy ñgIpe q q ñgIpe Órk q ñgIpe ñgIpe q ñgIpe d d d q d q q d ñpf d d q q q q q q d d d q d d ñur 80 80 75 70 q d ñgIms q d q q q q 75 80 d d d d 61 70 70 84 70 d q q q ñgLmp ñgLmp 80 q 65 40 q ñWebk ñud d d q d d q q d d q q d q 70 ñGli ñDm 85 ñbus q Ôao d q q q 80 ñgLmp Ôao 70 d d d d 85 75 70 d q q 65 d ñgIpe ñgIpe ñgIpe q q ñgIpe q d Órk Ócf q ñgLmf ñus ñut d d q q q q ñgIpe ñgIpe ñgIpe ñgIpe d ñgLpe dx Órk Ôc d d d d ñgId ñgIdc ñgIpe ñgIms Óak ñgIchm ñgImy ñgIpe ñbaog ñut ñbao Ôaa ñgIpe ñgIpe ñgImy ñgIpe Óaq ñus Ôrg q q q q ñb ñbm ñbm ñbm ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlc ñGlcw ñGlcw ñGlcw ñci ñGli ñGli ñGli ñGli ñGli ñGli ñGli Ôao Ôao ñD(tqc) Órk q ñgImq ñgIpe ñgIpe ñgIpe ñgImy ñgImy ñgImy ñgIpe ñgIpe ñgIpe ñgIchm ñgImy ñgIchm ñgIdc ñgId ñgIdc ñgIwa d ñut d d q q ñgLmp ñgIdi Ôaoc Ôaa ñD(t) Ôac ñnp ñnp ñWebc 80 ñgIdl ñgIdl ñcil ñcq ñod d d d d d d d ñus ñgImy ñgIpe ñgIpe ñgIpe ñgIpe ñbaog ñus ñus ñgIpe q d ñgIpe ñbaoz ñbau ñbao ñgImy ñgIpe Ôc ñgIpe d ñgIchm ñgIchm d ñgIchm q ñgIchm d q q q ñgIpe ñgIpe d ñgIms ñgIpe d Ôao ñog ñDic ñuts ñog ñGlc ñut d ñgIpe ñgIpe d ñgIpe ñgId q d d d d d d d q q ñogs d d d d d d d d d d d d d d d d q q ñgIwa ñut ñut ñDmhl ñDmhl q q q d q d d d q ñgLut ñgLmp d d d q d ñgLpe d ñGlcw ñbus ñGlc ñGli Ócf Ócf ñfp Óaf Óc Ôac Ôac ñfp ñfp ñfp ñfp 142934 142935 160727 160728 160744 160730 q q ñbao q d ñgIpe ñog ñgIpe ñgIpe ñgIpe ñgIpe d d d d d d d d d d q q q d d d q d d q q q d Óc ñgLmw ñgLmf d d ñgIchm ñgIpr q ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñDmhh ñOcb ñbus ñgIchm ñgIpe Óaq P I L B A R A M I N E R A L F I E L D M A R B L E B A R D I S T R I C T Tabba Tabba Pippingarra Pilgangoora Bore Creek Pippingarra Sn, Ta, Li Li Ta Sn Rm Lynas Find Rm Sn, Ta, Li Rm Rm Rm Cookes Hill Au Au Rm Rm McPhees West Lode Au Tabba Tabba Pb, Ag, Au Mount Berghaus Au Crawfords Ta Boondarrie Station Cu Brl Trig Hill Well Ta Trig Hill Well SE Brl Mount Berghaus Au Malindra Well SW Cu McPhees North West Au, Ta Ta Trig Well Alluvials Turner River Au Fe Indee East Indee West Fe Fe Old Tabba Asbc Last Crusade Au Au Lost Arc Au WMC McPhee's Hill Sn, Ta, Nb, Brl Fe Nb Brl Birthday Gift Wallaringa Peak Pb Au Cu Pb Ag Asbc Fel Mica Fel, Mica, Ta, Brl ? ? 25 30 35 S Z GEOLOGICAL SURVEY OF WESTERN AUSTRALIA 21^00À 118^30À 20^30À 119^00À 20^30À 21^00À 119^00À SHEET 2656 Ôaa Ôac Ôaoc Ôab Ôw Ôc Óag Óaq Óak Ócf Órk Óaf Mixed floodplain deposits with numerous small claypans Alluvial sand, silt, and clay in floodplains, with gilgai surface in areas of expansive clay q d dx ñpf q d dx Quartz vein Dolerite and gabbro dykes; interpreted from aeromagnetic data where dashed ñDm ñDmhl ñDcs MALLINA FORMATION: CONSTANTINE SANDSTONE PHANEROZOIC CAINOZOIC Unassigned units ñD(tqc) ñgImy ñgIpe ñgIth ñgItt ñgImq ñgIml ñgIms ñgImsl ñgImsx ñgIlw ñgIpr ñgIwa ñgId ñgIdc ñgIdh ñgIdi ñgIch ñgIchd ñgIchm ñgIchn ñgIchp ñgIchi PIPPINGARRA GRANITOID COMPLEX CARLINDI GRANITOID COMPLEX ñgLkd ñgLpe ñgLpo ñgLm ñgLmf ñgLmb ñgLmm ñgLmp ñgLdmf Pegmatite; metamorphosed Quartz(Êfeldspar) porphyry dyke; fine-grained; massive Pegmatite; metamorphosed ñgLmi ñgLmw De Grey Group Pilbara Supergroup ARCHAEAN Geological boundary Fold, showing axial trace and generalized plunge direction Small-scale fold axis, showing trend and plunge Bedding, showing strike and dip 25 75 Igneous layering, showing strike and dip 65 Way-up indicator Metamorphic foliation, showing strike and dip Cleavage, showing strike and dip 75 60 89 Óc ñgIpe Airphoto lineament SHEET 2656 FIRST EDITION 2001 0 5 10 15 20 Kilom etres SCALE 1:Ý500Ý000 Topography from the Department of Land Administration Sheet SF 50-4, 2656, Published by the Geological Survey of Western Australia. Copies available from the Information Centre, Department of Minerals and Energy, 100 Plain Street, East Perth, WA, 6004. Phone (08) 9222 3459, Fax (08) 9222 3444 This map is also available in digital form 2354 2355 2356 2357 2454 2455 2456 2457 2554 2555 2556 2557 2654 2655 2656 2657 2754 2755 2756 2757 2854 2855 2856 2857 MILLSTREAM ROEBOURNE DELAMBRE SHERLOCK COSSIGNY HOOLEY SATIRIST YULE THOUIN WODGINA WALLARINGA TAMBOURAH CARLINDIE SPLIT ROCK COONGAN PARDOO ROEBOURNE PYRAMID MARBLE BAR PORT HEDLAND SF 50-3 S F 50-4 SF 50-7 SF 50-8 COOYA POOYA MOUNT WOHLER NORTH SHAW MARBLE BAR WHITE SPRINGS MOUNT BILLROTH PORT HEDLAND DE GREY 40À 118^30À SHEET INDEX 1:100Ý000 maps shown in black 1:250Ý000 maps shown in brown 50À 50À 40À 40À 50À 50À 40À 25 Grid lines indicate 1000 metre interval of the Map Grid Australia Zone 50 VERTICAL DATUM : AUSTRALIAN HEIGHT DATUM 0 1 2 3 4 5 6 7 8 9 10 Kilom etres M etres 1000 SCALE 1:100Ý000 HO RIZO NTAL DATUM : G EO CENTRIC DATUM O F AUSTRALIA 1994 UN IVERSAL TRANSVERSE M ERC ATO R PRO JECTIO N INTERPRETED BEDROCK GEOLOGY GN MN GRID / M AGNETIC GRID CONVERGENCE True north, grid north and m agnetic north are show n diagram m atically for the centre of the m ap. M agnetic north is correct for 2 years. 2001 and m oves easterly by about 0.1^ in TN Cordierite hornfels, strongly contact-metamorphosed shale, siltstone, and wacke Poorly sorted subarkose and wacke; lesser interbeds of shale; metamorphosed Chert; metamorphosed ¦ Western Australia 2001 Colluvium _ sand, silt, and gravel in outwash fans; scree and talus; proximal mass-wasting deposits Ferruginous silt, sand, and gravel; variably consolidated and dissected Colluvium _ dissected consolidated clay, silt, and sand deposits; derived from adjacent rock outcrops Chlorite-rich, laminated shale and siltstone; metamorphosed ñGlc ñGlc ñGlcw ñGlcw CLEAVERVILLE FORMATION Gorge Creek Group MYANNA LEUCOGRANITE: THELMAN MONZOGRANITE: TABBA TABBA LEUCOGRANITE: MALLINDRA WELL GRANODIORITE: PETERMARER MONZOGRANITE: CHILLERINA GRANODIORITE: POOCATCHE MONZOGRANITE: KADGEWARRINA MONZOGRANITE: MINNAMONICA MONZOGRANITE: ñgLmx with modifications from geological field survey AUSTRALIA 1Ý:Ý100Ý000 GEOLOGICAL SERIES Stretching lineation, showing trend and plunge 15 QUATERNARY C D E F G H J K L M SEA LEVEL 2 km 4 km SEA LEVEL 2 km 4 km E F G H J K L M ñGls ñD(t) Turbiditic wacke; medium- to coarse-grained; abundant chert clasts; local graded units; ñgIdl Dolerite dykes, with abundant granite xenoliths locally; potassic alteration minor pebble beds and shale; metamorphosed ñGli ñGli Banded iron-formation; locally includes banded quartzÊmagnetiteÊgrunerite rock; metamorphosed Metamorphosed, fine- to medium-grained wacke; locally interleaved with serpentine- and tremolite-rich schist and metamorphosed iron-formation and ferruginous siltstone fine- to medium-grained biotite(Êmuscovite) granite; seriate to equigranular; massive to weakly foliated; metamorphosed Granodiorite magmatically interleaved with massive to weakly foliated, seriate to K-feldspar-porphyritic leucogranite; injection migmatite; metamorphosed Leucocratic biotite monzogranite; massive to weakly foliated; metamorphosed hornblendeÊbiotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; metamorphosed locally abundant inclusions of CHILLERINA GRANODIORITE; metamorphosed hornblendeÊbiotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; metamorphosed HornblendeÊbiotite diorite and granodiorite; massive to moderately foliated; locally inclusion-rich; metamorphosed Coarse-grained diorite and granodiorite; metamorphosed Hornblende-megacrystic, coarse-grained diorite and gabbro; massive to weakly foliated; metamorphosed Magmatically interleaved metagabbro and coarse-grained diorite and granodiorite; metamorphosed Coarse-grained, leucocratic biotite(Êhornblende) granodiorite and monzogranite; massive to moderately foliated; metamorphosed hornblendeÊbiotite granodiorite to K-feldspar porphyritic monzogranite; massive to moderately foliated; metamorphosed Granodiorite and monzogranite, strongly net-veined by diorite; metamorphosed Plagioclase-porphyritic granodiorite; strongly foliated in shear zones; metamorphosed fine- to medium-grained muscoviteÊbiotite(Êgarnet) monzogranite; equigranular to weakly porphyritic; massive to weakly foliated; metamorphosed muscoviteÊbiotite(Êgarnet) monzogranite; equigranular to weakly porphyritic; massive to weakly foliated; metamorphosed muscoviteÊbiotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite; metamorphosed Fine- to coarse-grained biotite monzogranite; metamorphosed Diorite, granodiorite, monzogranite, and abundant felsic to mafic inclusions and dykes, strongly foliated; metamorphosed massive to weakly foliated; metamorphosed Biotite(Êmuscovite) monzogranite, equigranular to weakly K-feldspar porphyritic; locally highly leucocratic and ghost-banded; massive to weakly foliated; metamorphosed WALLAREENYA GRANODIORITE: Fine- to coarse-grained muscoviteÊbiotite monzogranite; massive to weakly foliated; metamorphosed d ñu ñGl Mafic and ultramafic intrusions Dolerite dykes Pippingarra Granitoid Complex Carlindi Granitoid Complex Other granitoid rocks Constantine Sandstone Cleaverville Formation Euro Basalt ñgImy ñgIth ñgItt ñgIpr ñgIm ñgIch ñgIlw ñgIwa ñgId ñgLkd ñgLmi ñgLpo ñgLmw ñgLmp ñgm ñgg Myanna Leucogranite Thelman Monzogranite Tabba Tabba Leucogranite Petermarer Monzogranite Chillerina Granodiorite Mallindra Well Granodiorite Wallareenya Granodiorite Motherin Monzogranite Kadgewarrina Monzogranite Minnamonica Monzogranite Poocatche Monzogranite Gabbro Schist after gabbro Ultramafic rock, undivided ñog ñogs ñu Pilbara Supergroup, undivided ñba ñbm ñbau ñut Amphibolite High-Mg basalt Interleaved amphibolite and ultramafic rock TalcÊserpentineÊchlorite schist De Grey Group Group Group Gorge Creek Warrawoona ñgImq ñgIchn ñgImq ñbm A B C D ñGli ñGlc ñut Tabba Tabba Shear Zone ñgIms ñgIpr ñgIchp ñgIpr ñbaog ñbau ñut ñut ñbao ñgImsl ñgId ñgId ñgIchn ñgIchi ñgId ñbus ñogs ñGlc ñgIpe ñgId DIAGRAMMATIC SECTIONS ñgLmp ñut ñut ñut ñgLut ñba ñgLm ñud ñWebk ñWeb Pippingarra Granitoid Complex, undivided d d d d d d q ñut ñWec q q ñgImq ñgImq ñgLdmf ñogs ñgIchi ñgIchi ñbus PILBARA CRATON Turbiditic wacke; locally subarkosic; fine- to coarse-grained; abundant chert clasts; well-developed graded units; metamorphosed Monzogranite Monzogranite Monzogranite Granodiorite PILBARA CRATON ñP 142899 ñgImsx ñgImsx q ñgId ñgIpe ñWec K-feldspar porphyritic monzogranite and lesser granodiorite; mesocratic; local inclusions of granodiorite; metamorphosed Edited by N. Tetlaw, K. Greenberg, and G. Loan Fault or shear Diorite, granodiorite, and tonalite ñur TremoliteÊchloriteÊtalc schist ANG LE 3.3¾ 1.6¾ c. c. c. c. c. c. c. Geochronology by: Tabba Tabba Shear Zone 80 Shear-sense indicator, showing dip of foliation ñgIchp Geology by R. H. Smithies 1999; and D. C. Champion, and R. S. Blewett (AGSO) 1998 Ôao Alluvial sand, silt, and clay on floodplains Printed by Frank Daniels Pty. Ltd., Western Australia The recommended reference for this map is: Western Australia Geological Survey, 1:100 000 Geological Series Cartography by A. Veale and J. Dwyer ñgIpe Carlindi Granitoid Complex, undivided SMITHIES, R. H., CHAMPION, D. C., and BLEWETT, R. S., 2001, Wallaringa, W.A. Sheet 2656: interbedded shale, siltstone, and medium- to fine-grained wacke; minor layers of chert; metamorphosed exposed........................................................................................................... concealed, interpreted from aeromagnetic data......................................... exposed........................................................................................................... normal, tick on downthrown side.................................................................. reverse, triangle on upthrown side............................................................... relative displacement...................................................................................... concealed........................................................................................................ concealed, interpreted from aeromagnetic data.......................................... Strongly foliated rock............................................................................................ anticline, exposed........................................................................................... syncline, exposed........................................................................................... overturned anticline; exposed, concealed................................................... unspecified...................................................................................................... S-vergence...................................................................................................... Z-vergence...................................................................................................... inclined............................................................................................................ vertical............................................................................................................. overturned....................................................................................................... inclined............................................................................................................ vertical............................................................................................................. graded bedding.............................................................................................. inclined............................................................................................................ vertical............................................................................................................. inclined............................................................................................................ vertical............................................................................................................. inclined............................................................................................................ vertical............................................................................................................. inclined............................................................................................................ dextral, inclined.............................................................................................. sinistral, inclined............................................................................................ inclined............................................................................................................ structural trend............................................................................................... Isotopic age determination site with identification number.............................. Highway with national route marker................................................................... Formed road.......................................................................................................... Major track............................................................................................................. Track...................................................................................................................... Fence, generally with track.................................................................................. Railway................................................................................................................... Telegraph line........................................................................................................ Homestead............................................................................................................. Building.................................................................................................................. Yard........................................................................................................................ Microwave repeater station.................................................................................. Horizontal control; major...................................................................................... Contour line, 20 metre interval............................................................................ Watercourse.......................................................................................................... Pool........................................................................................................................ Bore, well............................................................................................................... Windpump............................................................................................................. Dam, tank.............................................................................................................. Position doubtful................................................................................................... Abandoned............................................................................................................ Road metal...................................................................................................... Mine........................................................................................................................ Prospect................................................................................................................. Quarry or pit.......................................................................................................... Opencut, abandoned............................................................................................ Mineral occurrence............................................................................................... Gold................................................................................................................. Beryl................................................................................................................ Iron.................................................................................................................. Lithium............................................................................................................. Niobium........................................................................................................... Tantalum......................................................................................................... Opencut.................................................................................................................. Tin.................................................................................................................... Opencut.................................................................................................................. Lineation, unspecified, showing trend and plunge d Coonterunah Group d dx dx (3) D. R. Nelson, 1998, GSWA Record 1998/2. (6) D. R. Nelson, in prep., GSWA Record 2001/2. (1) R. Buick et al., 1995, Nature, v. 375, p. 574Ê577. (2) D. R. Nelson, 1997, GSWA Record 1997/2. (5) D. R. Nelson, 2000, GSWA Record 2000/2. c. ñgLut ñgLutx MOTHERIN MONZOGRANITE: CARLINDI GRANITOID COMPLEX interleaved monzogranite, granodiorite, gneiss, and pegmatite; moderately to strongly foliated; and intruded by abundant sheets of massive to weakly foliated muscovite-bearing monzogranite and pegmatite; metamorphosed c. ñWeb ñWebk ñWec EURO BASALT Fine- to medium-grained mafic schist and amphibolite; after tholeiitic and high-Mg basalt, and dolerite sills ñWebc Carbonate-altered and schistose basalt; local intense silicification; m etam orphosed Komatiitic basalt and komatiite; locally pillowed and with olivine-spinifex texture; metamorphosed Warrawoona Group Carbonate-altered and silicified, fine- to medium-grained mafic schist after basalt ñfp ñfp ñfpx ñfs ñog ñogm ñogs ñogsf ñba ñbao ñbaog ñbaoz ñbau ñbus ñubs ñus ñur ñurg ñurs ñut ñuts ñud Melanogabbro; massive to moderately foliated; metamorphosed QuartzÊsericite(ÊfeldsparÊepidoteÊactinolite) schist Interleaved amphibolite and talcÊtremoliteÊserpentineÊchlorite schist TalcÊtremoliteÊchlorite schist interleaved with amphibolite and actinolite schist TremoliteÊchloriteÊtalc schist TremoliteÊchloriteÊtalc schist; intruded by abundant granitic dykes TalcÊserpentineÊchlorite schist; locally preserved olivine- and pyroxene-spinifex textures Amphibolite; fine- to medium-grained amphiboleÊplagioclaseÊquartzÊsericiteÊepidote rock Unassigned Medium- to coarse-grained metagabbro; foliated to massive High-Mg basalt and olivine basalt; locally preserved pyroxene-spinifex textures; metamorphosed Metabasalt; locally plagioclase-phyric Paragneiss; medium-grained, strongly recrystallized sedimentary rock ñb ñbm Feldspar porphyry; locally with hornblende phenocrysts; metamorphosed Dolerite; metamorphosed Interleaved actinolite schist, talcÊtremoliteÊchlorite schist, and quartzÊsericite schist; locally mylonitized TremoliteÊchloriteÊtalc schist interleaved with metasedimentary rocks ñs ñnp Banded iron-formation; locally includes banded quartzÊmagnetiteÊgrunerite rock; metamorphosed Banded iron-formation; strongly recrystallized and limonitized ñci ñci ñcil ñcq Metamorphosed feldspar porphyry containing abundant greenstone xenoliths ñod Fine- to medium-grained plagioclaseÊhornblendeÊactinoliteÊepidote schist after gabbro; locally includes interleaved talcÊserpentineÊchlorite schist Fine- to medium-grained plagioclaseÊhornblendeÊactinoliteÊepidote schist; includes abundant interleaved quartzÊsericiteÊepidote schist Interleaved talcÊserpentineÊchlorite schist, quartzÊsericite schist, cordierite hornfels, and actinolite schist Coonterunah Group COUCAL FORMATION: mafic schist and amphibolite; locally silicified c. ñOt ñOtbc TABLE TOP FORMATION: fine- to medium-grained amphibolite; after tholeiitic basalt and dolerite Interleaved chlorite schist, amphibolite, talc schist, and metamorphosed banded iron-formation c. (4) D. R. Nelson, 1999, GSWA Record 1999/2. Pilbara Supergroup Pilbara Supergroup, undivided Ôrg Alluvial sand and gravel in rivers and creeks; clay, silt, and sand in channels on floodplains Clay and silt in claypan deposits on floodplains Sheetwash deposits _ silt, sand, and pebbles on distal outwash fans; no defined drainage Alluvial gravel deposits, dominated by vein-quartz debris, unrelated to recent drainage; dissected ñgLmp Biotite monzogranite, strongly foliated; seriate to K-feldspar porphyritic; related to ; metamorphosed ñgLmp Mylonitized monzogranite; related to ; metamorphosed Biotite monzogranite, porphyritic (K-feldspar) to seriate; massive to weakly foliated; locally strong flow-alignment; metamorphosed porphyritic biotite(Êmuscovite) monzogranite; fine- to coarse-grained; quartz and K-feldspar phenocrysts; ñDmhh ñDmhh ñDmhh ñDmhh biotiteÊmuscovite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated; metamorphosed biotite-monzogranite; seriate to strongly K-feldspar porphyritic; massive to weakly foliated; locally with strong flow-alignment; Biotite monzogranite, seriate to porphyritic K-feldspar; fine- to medium-grained; massive to weakly foliated; local strong flow-alignment; metamorphosed Sedimentary rock, undivided; metamorphosed locally includes banded quartzÊgrunerite rock; metamorphosed Medium-grained amphibolite Medium-grained garnetiferous amphibolite Amphibolite; silicified Dunite replaced by serpentine(ÊtalcÊtremoliteÊchlorite) rock; locally preserved, medium-grained olivine-cumulate texture Serpentinite; serpentineÊtremolite(ÊtalcÊchlorite) rock after peridotite; locally preserved, medium-grained olivine-cumulate te xture (7) D. E. L. Baker, written communication, 2001. Quartzofeldspathic eluvial sand with quartz and rock fragments; overlying and derived from granitoid rock Alluvial gravel, unrelated to recent drainage; dissected by present-day drainage Alluvial calcrete; massive, nodular, and cavernous limestone; variably silicified; dissected by present-day drainage Residual calcrete; massive, nodular, and cavernous limestone; mainly silicified Silver................................................................................................................ Lead................................................................................................................. Copper............................................................................................................ Asbestos; chrysotile....................................................................................... Feldspar.......................................................................................................... Mica................................................................................................................. Dolerite dykes with granite xenoliths Muscovite-bearing monzogranite Biotite-bearing monzogranite Hornblende-bearing tonalite to monzogranite Undivided ñgLut ñgLm Fine- to coarse-grained biotite monzogranite Indee Fault Pisolitic limonite deposits, developed along palaeodrainage lines; dissected by present-day drainage 2940 Maì 2940 Maì 2930 Maì 2945 Maì 2945 Maì 2940 Maê 2955 Maê < 2990 Maê 3020 Maä å 3475 Maî 3485 Maè 3515 Maâ Leucocratic and porphyritic biotite monzogranite with quartz and feldspar phenocrysts; massive to weakly foliated; metamorphosed Interleaved monzogranite, granodiorite, gneiss, and pegmatite, with abundant greenstone xenoliths; metamorphosed Fine- to coarse-grained biotite monzogranite, with abundant greenstone xenoliths; metamorphosed ñgImq Leucocratic and porphyritic biotite monzogranite HornblendeÊbiotite diorite and granodiorite ñgId Biotite monzogranite, seriate to porphyritic K-feldspar with greenstone and granitoid inclusions; metamorphosed Biotite monzogranite, seriate to porphyritic K-feldspar, highly leucocratic and locally strongly ghost-banded; metamorphosed Strongly foliated biotite(Êhornblende) monzogranite, and granitic gneiss Monzogranite (includes ñgLmf ñgLmm and Ý ) Ôaa Ôao Ôaoc Ôab Ôw Óag Óaq Óak Ócf Órk Óaf ñDm ñDmhl ñDcs Óc ñgImy ñgIth ñgItt ñgIchi ñgImq ñgIml ñgIms ñgImsl ñgImsx ñgIlw ñgIpr ñgIwa ñgId ñgIdc ñgIdh ñgIdi ñgIch ñgIchd ñgIchm ñgIchn ñgIchp ñgLkd ñgLpo ñgLm ñgLmf ñgLmb ñgLmm ñgLmp ñgLmi ñgLmw ñgLdmf ñgLmx ñD(t) ñgIdl ñGls ñgImy ñgIth ñgItt ñgIpr ñgIm ñgIch ñgIlw ñgIwa ñgId ñgLkd ñgLpo ñgLmw ñgLmp ñgm ñgg ñog ñogs ñD ñDc ñWe ñP ñba ñbm ñbau ñut ñgLut ñD ñD ñD ñP ñP ñD ñurs ñur ñbm ñbm ñgIpe ñgIlw ñgIlw ñgIchn ñD ñP ñbus ñut ñgLmf ñgLmp ñgLmi ñgL ñgIchn ñgIchi ñgI ñgIchn ñgIpr ñbao ñbao ñbau ñut ñgImy ñgIpr ñgI ñgI ñgItt ñgIms ñog ñgId ñgItt ñgLmm ñgL ñgLkd ñgLmp ñgLutx ñut ñgL ñgL ñgLut ñgL ñO ñOt ñOtbc ñubs ñgL ñgLut ñgI ñogsf ñO ñgLmi ñur Ôac ñgL ñP ñgLut ñgLutx ñWeb ñWebk ñWec ñWebc ñs ñfpx ñfs ñog ñogm ñogs ñogsf ñbaoz ñbus ñubs ñud ñus ñur ñurg ñurs ñut ñuts ñod ñba ñb ñbao ñbaog ñbm ñnp ñcq ñcil ñOt ñOtbc Ôc Ôrg ñDmhh ñDmhh ñDmhh ñD(tqc) ñOcb ñOcb ñgLm ñgLpe ñbau 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 W GS84 positions Reference points to align maps based on the previous datum, AGD84, have been placed near the map corners Chert; weakly banded, grey and White; metamorphosed Banded White and grey chert, and quartzite; local minor jaspilite and iron formation; DEPARTMENT OF MINERALS AND ENERGY L.C. RANFORD, DIRECTOR GENERAL 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 GEOLOGICAL SURVEY OF WESTERN AUSTRALIA TIM GRIFFIN, DIRECTOR GOVERNMENT OF WESTERN AUSTRALIA CLIVE BROWN, M.L.A. MINISTER FOR STATE DEVELOPMENT, TOURISM, SMALL BUSINESS, GOLDFIELDS-ESPERANCE PRODUCT OF THE NATIONAL GEOSCIENCE MAPPING ACCORD W.A. N.T. S.A. N.S.W. Vic. Qld Tas. A.C.T.
![p oó pTp pHpPp p pEp=pb - RS Components Internationaldocs-asia.electrocomponents.com/webdocs/14bb/... · 2 p oópTp pHpPp p pEp=pb % ñp p oópXp=pp p oóp ¶]á ¸ Tp oó c p oó](https://static.documents.pub/doc/80x56/5b09ccc27f8b9a93738e7001/p-o-ptp-phppp-p-peppb-rs-components-internationaldocs-asia-p-optp-phppp-p-peppb.jpg)
![Untitled-1 [] · 9482 —3—0 TPlJ74JVL 9482 aliphatic*ñU 1.7 E 9482 —77 (TPU) 9482 150 ADHESIVE PVC FILMS SEG (TPU)](https://static.documents.pub/doc/80x56/603b46ceda3c6051d563eb56/untitled-1-9482-a3a0-tplj74jvl-9482-aliphaticu-17-e-9482-a77-tpu.jpg)
![M.A Tamil - PR...í ñd DW ì ï í ñ &OIWSD\ D i } o ] À í ñd DW ì ï y D } µ o } µ í ñd DW ì ïDy sWW í ñ yEW ì ïs í s ] o o P W o u v W } P u u } u µ o } Ç E }](https://static.documents.pub/doc/80x56/6118ac2d5939af45926d4d60/ma-tamil-pr-d-dw-oiwsd-d-i-o-d-dw-.jpg)
