AUSTRALIA 1:250 000 SA GEOLOGICAL ATLAS SERIES SHEET … · k op ir n, fe mc donal s, sa nd rifl...

1
! " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ( ! ( ! ( ! ( ! ( " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ( ! ( ! ( ! ( ! ( " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ( ! ( ! ( ! ( ! ( ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " Ì G Ç Ç Ì G Ì G Ì Ì Ì Ç Ç Ì Ç Ç G Ì Ì Ç Ç Ç Ç Ç Ì Ì Ç Ì Ç Ì ALdk ALdk Qhck 8 Qhcks _______ Qpcb ALdk Qhck 8 Qhck 5 Qpr 4 _____ Qpcb Qpcb Qhcks Qhck 9 ALdk ALsw ALdk Qhck 8 ALsw Qhcks Qhck 8 Qhck 9 Qpr 4 _____ ?Lhw Qpcg Qhem Qpr 4 _____ Qpcb Qpr 4 Qhem ?Qpcg Qpcb Qpr 4 _____ Qp ca Qpcg ALs Ql 1 Qpew Qhem ?Lzoy Qe 3 ALsc Qpr 4 Qe 3 Qpr 4 _____ T fe T fe _____ Lic Qpcb ______ T fe Lz Qpr 4 _____ Qp ca T fe _____ Lz Qp ca Qpr 4 _____ T fe _____ Lhw T fe Qpr 4 _____ T fe Ldw T fe _____ Lhw qz Qpr 4 _____ Qp ca Qhck 9 L 10 Qe 3 Lik ?T fe _____ Lz Qpr 4 Lzoh Qhcks _______ Qpcb Qhck 9 Ld Ld Ldw+Ldj+L-u Qpcb Ql 1 L-m Ld 1 +L-u ?Ld ?T fe Ldw+Ldj+L-u Ldw Qp ca _____ T fe _____ ?Lic Ldw Qpr 4 T fe _____ T si Lik Mcb Qhck 8 Lz Qhck 9 Ld Qp ca _____ Lz Qpr 4 Lz Ldc Qpr 4 _____ Ld Qhem T fe _____ T si Ms 1 Ldw+Ldm+Ldj Qpcb ?Ld Qhem Qhck 8 Qhck 9 ALdk ?Qpcb Qhcks _______ Qpcb Qpcb Qpr 4 _____ ?Lhw Ql 1 Ql 1 _____ Qpcg Qhck 8 Qha 1 ALdk Qpr 4 _____ ALdk Qpcb Qe 3 Qpr 4 _____ Qp ca ALdk Qpr 4 _____ ?ALdk Qha 1 Qpr 4 _____ T fe Qpr 4 _____ Qpcb ______ T fe Qhe 3 Lh T fe _____ Lil Qpr 4 _____ ?Li 1 Li 1 T fe _____ Lil Qpr 4 _____ T fe T fe _____ Lz Ldw+Ldj+L-u Lir T fe _____ Lhw+Lz Ql 1 Ldw+Ldj+L-u T fe Lzou Ld T fe _____ Lic Qpr 4 _____ T fe _____ T si Qpcb T fe _____ ?Lz Lz+Lir+ALs T fe _____ ?Lz T fe _____ Lh Lzo Ldc T fe Liu Lzo Qhck 9 ?Ld Ld Li 1 Ld+L-u+Ldj LM-n Li 1 Lz T fe _____ Lzoy Qpr 4 Ld+Ldj T fe _____ Lic Ld 2 T fe _____ ?Ld Lzoy Ldm Lik Lz+Lic Qpr 4 _____ Lir Qhl 3 Qhem Ld Ldc Ld Ms 1 + 2 + 3 Qpap Ldw+Ms 2 Ms 1 Ld Qhem Qpr 4 _____ ?Lil ALsc Qpcb ?Qpcg Qhck 8 ALsw Qhcks ?Qpcg Qpcg Qpcb Qhem Qhem ______ Qpcb Qhem Qe 3 Qe 3 Lhw Qhcks ALsc Qhck 8 Qpr 4 ALdk Qpr 4 Qe 3 ?Qpcg Qpew Qhcks Qpcb ?Qpcg Qhem T fe _____ ?ALsc T fe _____ ALs Qhl 3 Qha 1 Qhem Qhem ALsc Lic T fe _____ Lz Qpcg Qpr 4 _____ T fe _____ ?Lhw Lik Qhl 3 Li 1 T fe _____ Lic+Lz Lhw+Lz Qpr 4 _____ Qp ca qz Qhck 8 T fe _____ Lhw _____ Lz Ldm+Ldc+Ldj+L-u Qe 3 Ldw+L-u+Ldj Qhck 8 Lik Ql 1 Lhw Ldw+L-u+Ldj Lz Ldw Qhcks L 10 Ld T fe _____ T si T fe Qpcb Qhl 3 T fe _____ T si Qpr 4 Qpr 4 Lil Qpr 4 _____ Lhw Qpr 4 _____ Lic Qp ca _____ Lz Lhw Ld Qpr 4 _____ Ld Lhw Qpr 4 _____ Lz Qp ca _____ Lhw Ms 1 Ldc Qha 1 Ms 1 + 2 Lik Ms 1 Ms 1 +Ld Qhcks _______ Qpcb Qhck 9 ALdk Qhck 9 ALdc ALsw Qpcb Qhe 3 Qhck 9 Qpcb ALsw Qpcb Ql 1 Qhe 3 _____ Qhem Qhem Qpr 4 ?Qpcg Ql 1 ALsw Qpr 4 _____ T fe Ql 1 Qe 3 Qpr 4 Qhl 3 Qpr 4 _____ Qp ca _____ Lzo Lz Qpr 4 _____ T fe _____ Lhw Qpr 4 Qpr 4 _____ T fe _____ Lil Lir Ldw ?Lhw T fe Ql 1 Qhcks Ldw+Ldj+L-u Qpew ______ Qpcb Ldw Lic Lz Qhcks Qhcks T fe _____ Ld Qe 3 ?Ld Li 1 Qpr 4 _____ T si Qha 1 Ldc T fe _____ Lzo Qhe 3 _____ Qpew Qha 1 ?Ld Qpr 4 L 10 Qpap ______ Tbw Qpr 4 _____ T fe _____ Lic Ql 1 _____ Qhck 5 Lic Qpr 4 _____ Lil Ql 1 Qpr 4 _____ ?Lhw Qhck 8 Qhcks ALsm Ql 1 Qpr 4 _____ Ld L 10 Lic Lz qz Lhw Qpr 4 _____ Lz ?Lhw Qpr 4 _____ Lz Ld+Ms 1 + 3 Qhcks ______ Ld Ld Qpr 4 _____ ?Lz Ms 1 + 3 Lz Qp ca _____ Lik Ld+Ldj Ldc Ldm+Ldj+L-u Qhck 9 Qhl 3 Qp ca _____ Lz ?ALs Qhck 9 ALdw ALsw Qhcks _______ Qpcg ALdc ?ALs ALdc Ql 1 Qpr 4 _____ Qpcb Qhcks _______ Qpcb Qpr 4 _____ Lhw ALsw Lhw Qpr 4 Qpcb Qhck 9 Qpcb Qe 3 _____ Ql 1 Qha 1 Ql 1 T fe _____ Lhw Qhe 3 Qe 3 Qhl 3 ALsc 2 Qhem ______ Qpcb ______ T fe T fe _____ Lh Ql 1 T fe _____ ALsc Qpr 4 _____ L-m T fe _____ ?Lhw Qpr 4 Qhcks Lz Ldc T fe _____ Lz Ldj Lzo T fe _____ Li 1 Qpr 4 _____ ?Qpew Qpr 4 T fe _____ Lz Ql 1 T fe _____ ?Lh Qpcb Ql 1 Lzom Ldc T fe Li 1 Lhw Qpcb Ldw+L-u T fe _____ Lz my Lir Li 1 Lzom Ldm+Ldj Lzoy Lzo T fe _____ Lzoy Qpr 4 Ldw+Ldj+L-u Qp ca ?Lir Qpr 4 _____ ?Ld Qpr 4 _____ Ld Ldm T fe _____ Lic Ldm Qhcks Qpr 4 Qpcb Qhcks Qpr 4 _____ Lil Lz ?Ld Qhcks Ld ?ALs Qhck 8 Qpcb ALdk ALsw Qhck 8 Qhcks _______ Qpcb ?ALs ?ALs Qe 3 Ql 1 _____ Qpcb Qhck 9 Lhw Qhck 8 Qpr 4 ALsw Qhem ______ Qpcb Qhcks ALdk Qhl 3 Qpr 4 _____ T fe _____ ?Lhw Qpcg ?Qpcg Qha 1 Qhl 3 T fe Ql 1 Qpr 4 _____ ?Lhw Lhw ALsc ALsc 1 +ALsc 2 Qpcb Lz T fe Qhem+Qhe 3 Tp 6 ____ To 4 ALsc Lz T fe _____ Lzo Lil L 10 +Ldc Qpr 4 _____ T fe _____ Lhw Lz Lz T fe Lz L 10 T fe T fe _____ Lzo Qpr 4 _____ T fe Liu Qhck 8 my Ldm Lzo Qpr 4 _____ Lzoh Ldj Ldw ?Ld Lzo Qhcks LM-n 2 Qp ca _____ Qpew ?Ld Lz LM-n 1 Lzoy Ld Ql 1 Ld T fe _____ T si _____ ?Lzoy Qpr 4 _____ Qpcb Lir Ld+Ldj Lic Qpcb ALsm Ld Lir Lil Lz ?Ld Qp ca _____ Lz+Lir Ms 1 +Ld+Ms 3 Qpcb Ld Qhcks Ms 1 + 2 + 3 +Ld Qhck 8 Qp ca _____ Lz Qhcks ALsw ALdk Qhck 8 ALdk Qhcks _______ Qpcb L-p Qpcb Lhw ALsw Qhcks Qpr 4 _____ Qpcb Qpcb ALdk Qhck 5 Lhw T fe Qpr 4 _____ Lhw Qe 3 Qhem ______ Qpr 4 Qha 1 Ql 1 Qhcks Qpr 4 _____ Qp ca Qpcb Qpr 4 _____ Qpcb Ql 1 Qpr 4 _____ Lik Lz Lhw T fe _____ Lil T fe _____ Li 1 T fe _____ ?Lh T fe _____ Lzo Ldw+Ldc+L-u+Ldj Lir+Li 1 Ld Qpr 4 _____ Lhw Lik T fe _____ Li 1 T fe _____ ?Lic T fe _____ Lhw Lil T fe _____ Lz T fe L-m Lz Li 1 Ld T fe _____ Li 1 Qpr 4 _____ T fe Ld Qpcb Ld Ld+Ldj+L-u Ldm+L-u T fe _____ Li 1 Qhck 9 Ld qz Ldw Ld Ldm+Ldj Liu Ldc Ldw Qpr 4 Qhck 9 Qhck 5 _____ Ld Lzoy T fe _____ Lil Qpr 4 _____ T fe _____ T si ?Qp ca _____ T fe Qhck 8 Ld+Ldj+Ms 1 Qpr 4 _____ Ld Lik Lz Ld+Ldj Lil Lz Qhck 8 Qpr 4 Qpr 4 _____ ?ALs Qpr 4 _____ ?Ld Qhck 8 Qpcb ALdw Qpcb ALdk Qpcg Qhcks _______ Qpcb Qhck 9 ALdw Qhck 8 Ql 1 Ql 1 Qhcks _______ Qpcb Qhck 8 ALdk Qhck 9 Qhcks _______ Qpcb Qe 3 Qhem ______ Qpcb ALsc Qhck 9 Qha 1 Ql 1 Qe 3 Qhe 3 _____ Qpew Qhem T fe Qpr 4 _____ Lz Qpr 4 Qha 1 T fe _____ Lz Qpr 4 _____ Lz Qpr 4 Qpr 4 _____ Qpcb Qpr 4 _____ Lzo Qhck 9 Lil Lic T fe _____ Lic Qhck 8 Ldw Ldc Lhw Ldc T fe _____ Ld ?Ldc Ldc+Ldw+Ldj+L-u my Lir Lzo Ld+Ldj+L-u Lic Li 1 +Lz Ldw T fe _____ Lic Lic Ldm Lz T fe Qpcb Ldm+Ldj Qpcb Ldw Lil Lzoh ?Qhem _______ Qpcb Ldw Ld Ld Qpr 4 _____ Lzoy Ld Ld Lir Qpr 4 _____ Lzoy T fe _____ Liu Qhcks Ldw Ld+L-u+Ms Qp ca _____ ?Lil Qpr 4 _____ Mcb Lz Ldw+Ldj Qpcb Lic Ldw+Ldj+Ms 1 + 2 Qpr 4 _____ Lz+Lhw Qp ca _____ T fe _____ T si Qhcks Ldw+Ms 1 +L-u Qp ca _____ T fe _____ T si Qpcb Ms 1 + 2 + 3 Ms 1 + 2 BARNS, Fe ULEY, GRPH CARROW, Fe KAPPERNA, Fe URANNO, GRNT KOPPIO, GRPH BEECROFT, GNSS GREENPATCH, Fe KOPPIO IRON, Fe MCDONALDS, SAND RIFLE RANGE, Fe TUMBY BAY, TALC LOUTH BAY, SAND COFFIN BAY, LSND NORTH BLOCK, KAO GLEN PARK 1, CALI LAKE MALATA, GYPS LAKE GREENLY, GYPS LAKE WANGARY, SAND CHARLTON GULLY, Fe ALLERTON HILLS, KAO POONINDIE EAST, SAND WHITE LAKES NO.3, GYPS DK QUARRIES, GNSS, GRNT IRON MOUNT, Fe, FEORE, FEST STRAWBERRY HILL NORTH, SAND, GRVL 60 80 52 42 86 86 78 74 70 82 60 86 50 70 70 16 80 66 75 80 46 60 70 82 18 82 30 46 22 25 60 35 70 74 50 79 33 37 60 88 36 82 70 62 70 83 28 84 85 82 88 54 50 85 85 24 60 84 85 80 47 82 81 64 75 72 79 Gawler Pond Hall Bay Avoid Bay Tumby Bay Peake Bay Shag Cove Coffin Bay Dutton Bay Boston Bay Yangie Bay Misery Bay Massena Bay Lipson Cove Jussieu Bay Fishery Bay Port Douglas Sleaford Bay Spalding Cove D'anville Bay Tapley Channel Douglas Channel Mount Dutton Bay Port Lincoln Proper RED CLIFF BALD HILL CAPE BURR CAPE EULER FARM BEACH CAPE HARDY REEF POINT NOSE POINT POINT AVOID CAPE CARNOT SHOAL POINT PEAKE POINT NYLLOW HILL POINT MARIA MOUNT GAWLER POINT BOSTON MURRAY POINT COBBLER HILL PICNIC BEACH GUNYAH BEACH POINT LONGNOSE SURFLEET POINT MOUNT DRUMMOND MOUNT DRUMMOND THREE BROTHERS CAPE DONINGTON MACLAREN POINT DRUMMOND POINT TREVALLEY POINT PILLAWORTA HILL CAPE TOURNEFORT STRAWBERRY HILL CAPE CATASTROPHE POINT HASELGROVE OBSERVATORY POINT POINT BOLINGBROKE JESSIEU PENINSULA Kunari Lynfield Koodinga Moorlands Midway Glen Woolawae Downs Wanna Tulka Kiana Moody Coulta Kaldow Karkoo Warrow Uranno Lipson Butler Koppio Uranno Brooker Wanilla Ningana Wangary Pillana Warunda Pearlah Ungarra Coomapoo Yeltukka Yeelanna Grantham Yeltukka Kapinnie Moreenia Gum Flat Wildeloo Edillilie Poonindie Mena Flat Mount Hill Mount Hill Cowieninta Mount Hope White Flat Duck Ponds Mungerowie The Fountain Butler Tanks Cockaleechie Warratta Vale Yallunda Flat Brimpton Lake North Shields Cummins Tumby Bay Coffin Bay Port Neill Port Lincoln Lake Malata Lake Greenly Lake Hamilton Sleaford Mere Lake Wangary Little Swamp Lake Baird Pillana Lagoon Salt Swamp Pillie Lake Curta Willa Waterhole 63 70 75 50 22 46 56 60 70 80 70 85 75 80 70 45 52 50 Coomunga Louth Bay Green Patch 500000 500000 510000 510000 520000 520000 530000 530000 540000 540000 550000 550000 560000 560000 570000 570000 580000 580000 590000 590000 600000 600000 610000 610000 620000 620000 630000 630000 613 0000 613 0000 614 0000 614 0000 615 0000 615 0000 616 0000 616 0000 617 0000 617 0000 618 0000 618 0000 619 0000 619 0000 620 0000 620 0000 621 0000 621 0000 622 0000 622 0000 623 0000 623 0000 Ld ALs Lh Ms Lo L-p Lo Lh Lo Lo The Total Magnetic Intensity Image has been compiled using aeromagnetic data from the Department of State Development, South Australia. Aeromagnetic data has been merged, gridded and image processed by the Geological Survey of South Australia, DSD Resources and Energy Group. SCALE 1:1000000 SCALE 1:1000000 Modified from Interpreted Crystalline Basement Geology Of The Gawler Craton (Fairclough et al. 2003) Interpreted Solid Geology Of The Curnamona Province (Burtt and Betts, 2003), Musgrave Block, Central Australia: regional geology from interpretation of aeromagnetic data (Rankin and Newton, 2002), Solid Geology South Australia (Cowley, 2006). 5 0 5 10 15 20 25 KILOMETRES KILOMETRES SA GEOLOGICAL ATLAS SERIES SHEET GEOLOGICAL SURVEY OF SOUTH AUSTRALIA DEPARTMENT OF STATE DEVELOPMENT SOLID GEOLOGY INTERPRETATION TOTAL MAGNETIC INTENSITY IMAGE AUSTRALIA 1:250 000 +7.50°E +7.25°E +7.00°E +6.75°E +6.50°E +6.25°E +7.75°E KIMBA LINCOLN WHYALLA ELLISTON MAITLAND KINGSCOTE Coulta 5929 Tumby 6129 Lincoln 6028 Spilsby 6128 Wangary 5928 Cummins 6029 WA NT QLD SA NSW VIC TAS INDEX TO 1:100 000 SHEETS INDEX TO ADJOINING 1: 250 000 SHEETS Magnetic Declination 2000 (Annual variation +1.4 minutes) SCALE 1:250,000 DIGITAL EDITION SUBJECT TO AMENDMENT See published printed map for further information A two standard deviation contrast stretch has been applied to the raster image above. 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' 35° 00' 34° 30' 34° 00' 135° 00' 135° 30' 136° 00' 136° 30' COMMODITIES CALI Calcrete Fe Iron FEORE Iron Ore FEST Ironstone - construction materials GNSS Gneiss GRNT Granite GRPH Graphite GRVL Gravel GYPS Gypsum KAO Kaolin LSND Lime sand QTZE Quartzite SAND Sand TALC Talc LINEAR STRUCTURE ............................................. FAULT POSITION ACCURATE ..................................... FAULT POSITION APPROXIMATE ................................................................................ TREND-LINE GEOLOGICAL BOUNDARY .................................................................................. COASTLINE ... GEOLOGICAL BOUNDARY POSITION ACCURATE ........................................................................... GEOLOGICAL BOUNDARY POSITION APPROXIMATE Solid Geology - Linear Structure ......................................................................... Fault position accurate .......................................................................................... Mylonite zone LINCOLN SI5311 Solid Geology Donington Suite Ld Dutton Suite ALd Hall Bay Volcanics ALsh Hutchison Group Lh Miltalie Gneiss L-m Moody Suite Lo Price Metasediments L-p Sleaford Complex ALs Spilsby Suite Ms Unnamed GIS Unit - see description Mc Unnamed GIS Unit - see description Li1 Unnamed GIS Unit - see description L36 nTesla -1442.36 10179.21 -911.8 -323.64 264.52 SI5311 LINCOLN GEOMORPHIC FEATURES ................................................................................................ LAKE ............................................................. INTERMITTENT LAKE ........................................................ MINOR WATERCOURSE .......................................................................................... SWAMP ............................................................................... SAND RIDGE ............................................................................... ! WATERHOLE MINING ........................................................................... G PIT/CUT - CONSTRUCTION MATERIALS (SAND AND/OR CLAY) ............................................................................................. Ì QUARRY - CONSTRUCTION MATERIALS (HARD ROCK) ........... Ì MINE - METALS AND INDUSTRIAL MINERALS ........................................................... Ç DEPOSIT - NO MINING CULTURAL FEATURES ..................................................................... PRINCIPAL ROAD ................................................................ SECONDARY ROAD ........................................................................... MINOR ROADS .............................................................. VEHICULAR TRACKS ....................................................... OPERATIONAL RAILWAY .......................................................... ABANDONED RAILWAY ...................................................................... WATER PIPELINE ................................................................... ! IDENTIFIED POINT ...................................................................................... " BUILDING .................................................................. LANDING GROUND .............................................................. ! ( TOWN OR LOCALITY STRUCTURAL FEATURES ........................................................... TECTONIC FOLIATION ................................. TECTONIC FOLIATION - VERTICAL ....................... HORIZONTAL SEDIMENTARY BEDDING ..................................................................................... HORIZONTAL SEDIMENTARY BEDDING - VERTICAL .............................................................................. HORIZONTAL SEDIMENTARY BEDDING - HORIZONTAL Any person purchasing this map may reproduce it for their own use or that of their staff, but not for any other purpose except with the written permission of the Chief Executive, Department of State Development SA, GPO Box 320, Adelaide, South Australia, 5001. CROWN COPYRIGHT RESERVED Department of State Development SA. Topographic detail based on TOPO-250K GEODATA (source scale 1:250 000) supplied by Geoscience Australia - National Mapping Division, ACT. The relationship between this data and DSD data is not guaranteed. Computer generated from SA_GEOLOGY database (Digital data available upon request) Product of Spatial Information Services. Published by, and with the authority of, the Department of State Development SA. Grey numbered lines indicate the 10000 metre Map Grid Transverse Mercator Projection, Geocentric Datum Australia, 1994. The lake boundaries displayed on this map may have been derived from geological interpretation and may not match lakes interpreted by topographic mapping authorities. Not all structures are represented on this particular map. Mapping and Compilation by M.P. Schwarz, B.Sc.(Hons), and L.R. Rankin, B.Sc.(Hons) with contributions by A.R. Martin, B.Sc.(Hons), A.J. Parker, Ph.D., W.M. Cowley, B.Sc.(Hons), S.O. McAvaney, B.Sc.(Hons), and C.E. Wade, B.Sc.(Hons) S.M. Hill, Ph.D., Director, Geological Survey of South Australia. Geological boundaries displayed on this map have been Derived from geological interpretation and are not intended to be used for navigational purposes. Copies of this map can be obtained from the Department of State Development SA, Adelaide. 9/2/2017 2017 Current version 2016.2 UNITS ARE NOT LISTED IN STRICT STRATIGRAPHIC ORDER BELOW AGE LEVEL R E F E R E N C E HOLOCENE PLEISTOCENE-HOLOCENE PLEISTOCENE PLIOCENE OLIGOCENE EOCENE-PLEISTOCENE TERTIARY MESOPROTEROZOIC PALAEO-MESOPROTEROZOIC PALAEOPROTEROZOIC ARCHAEAN-PALAEOPROTEROZOIC MISCELLANEOUS CHINMINA SYENITE: Monzonite, massive, to weakly foliated, medium to coarse-grained, dark grey-black, phenocrysts of plagioclase, microcline and hornblende. LINCOLN sheet. Lzoh MOODY SUITE: Adamellite, medium-grained; garnetiferous; granite. U-Pb ages 1709-1701Ma. Lzo TOURNEFORT METADOLERITE: Gabbro and dolerite, fine to coarse-grained, massive, black dykes. Chilled margins, variably recrystallised to amphibolite and hornblende granulite. Age ~1800Ma. L-u MILTALIE GNEISS: Gneiss, migmatitic grey granitic, coarse-grained equigranular foliated, quartz, perthitic microcline, plagioclase, biotitic. L-m PRICE METASEDIMENTS: Schist, fine grained, pelitic, magnetite-rich. L-p Mylonitic Donington Suite and/or Miltalie Gneiss. L 10 Peridotite, massive, coarse grained, dark green to black; biotitite, pyroxenite, hornblendite. LM-n 2 Diorite, massive, medium to coarse grained, dark green. LM-n 1 COONTA GABBRO: Gabbro, massive, coarse grained, dark green; diorite, massive, medium to coarse grained, dark green; peridotite, massive, coarse grained, dark green to black. LM-n Quartz veins/bodies, undifferentiated. qz Mylonitised rocks, undifferentiated. my BLUE RANGE BEDS: Sandstone, minor grit and pebble beds, white, massive to crossbedded, rare haematite veins. Mcb Granodiorite, fine-medium grey. Ms 3 Í Í Í Í Í Í Í Í Í Í Fine-grained granite, aplite. Ms 2 Í Í Í Í Í Í Í Granite, medium-coarse tabular-feldspar. Ms 1 SPILSBY SUITE: Granite, grey, coarse-grained porphyritic (Adamellite to granodiorite), Massive, weakly foliated. Age 1576+/-198 Mapooled Rb-Sr Webb 1978, 1475-1410 Ma (K-Ar) Webb et al. 1986. Ms Quaternary playa sediments. Ql 1 YAMBA FORMATION: Clay, lacustrine, gypsiferous; gypsum-quartz sand . Dunes, playa lakes. Qly Undifferentiated Pleistocene calcrete. Qp\ca POORAKA FORMATION: Clay, sand and carbonate earth, silty, with gravel lenses. Qpap BRIDGEWATER FORMATION: Bioclastic barrier shoreline deposits, silica rich, with heavy minerals, shallow sub-tidal. Coastal, cross-bedded aeolian calcarenite with palaeosol horizons and capped by calcrete. Qpcb GLANVILLE FORMATION: Clay, mottled, shelly; calcarenite, skeletal, coquina. Geochron age 132 000+/-6 000 years Bp on TL. Qpcg Pleistocene dune core sand. Qpe 1 WIABUNA FORMATION: Silt to fine-grained sand, orange-brown, calcareous , conglomeratic in part. Aeolian. Qpew Pleistocene gravel, clay, silt and sand with soft carbonate, overlying nodular/tabular calcrete. Based on Qp1 on GAIRDNER, YARDEA, STREAKY BAY, WHYALLA, Qp on CHILDARA. Qpr 4 Limestone, sandy and pebbly, molluscan fauna. Fishery Bay. Tp 6 Limestone, brown and pink, bryozoal, gritty and pebbly at base, latest Oligocene fauna. Fishery Bay. To 4 WANILLA FORMATION: Sand, micaceous, carbonaceous; interbeds of lignite. Tbw Undifferentiated Tertiary ferricrete. T\fe Undifferentiated Tertiary silcrete. T\si Lower and/or Upper Middleback Jaspilite: amphibole-magnetite schist and quartzite. Based on Prot-hm1 on YARDEA. Li 1 COOK GAP SCHIST: Schist, medium-grained,, biotite-garnet-sillimanite quartzo-feldspathic, grading to gneiss, migmatised in high-grade area, locally graphitic. Lic KATUNGA DOLOMITE: Marble, white to pale grey, dolomitic, layered with serpentine, with calcite-diopside-tremolite banding. Lik LOWER MIDDLEBACK JASPILITE: Haematite, banded, with quartzite+magnetite, carbonate, schist and chert. Grades into jaspilite in places. Lil BURRAWING AMPHIBOLITE: Amphibolite, fine to medium-grained, interbedded gradationally with banded diopside-hornblende-rich calcsilicate gneiss. LINCOLN sheet. Lir UPPER MIDDLEBACK JASPILITE: Jaspilite. Liu COULTA GRANODIORITE: Granite; granodiorite; with abundant mafic xenoliths. Foliated. ALdc Í Í Í Í Í Í Í Í KIANA GRANITE: Granite, porphyritic, gneissic. Weak to strong alignment of tabular feldspars. ALdk Í Í Í Í Í Í Í Í WHIDBEY GRANITE: Granite, massive, even grained. Weakly foliated. Age 2337+/-71 Ma. ALdw SLEAFORD COMPLEX: Metasediment; metabasalt, sills, dykes; augen gneiss. Granulite facies, amphibolite facies. ALs CARNOT GNEISSES: Garnet gneiss; porphyroblastic gneiss; paragneiss; basic granulite; layered garnet gneiss; felsic gneiss. Interpreted as metasediments, tholeiitic basalt and synorogenic intrusives. ALsc Paragneiss, banded; garnet-biotite quartz feldspar gneiss; porphyroblastic cordierite-sillimanite quartz feldspar gneiss. Age: 2412+/-72 Ma. LINCOLN sheet. ALsc 1 Orthogneiss; foliated K feldspar granite to augen gneiss. Age: 2436+/-137 Ma (Rb-Sr whole rock); massive to compositionally banded felsic gneiss. Age: 2637+/-21 Ma. LINCOLN sheet. ALsc 2 MASSENA BAY GNEISSES: Gneiss, banded, quartz-feldspar-biotite; quartzofeldspathic orthogneiss with rounded mafic inclusions, migmatitic leucosomes, LINCOLN sheet. ALsm P P P P P P P P P P P P P P P P P P P P P WANGARY GNEISS: Gneiss, microcline-plagioclase-quartz-biotite-muscovite. Age 2380+/-60 Ma (Rb-Sr); 2445+/-32 Ma (U-Pb). ALsw Present day Holocene alluvium; current bedload. Qha 1 SAINT KILDA FORMATION: Undifferentiated Holocene coastal marine sediment. Qhck Supratidal sand/mud flats: gypseous clay. Based on Qhk2 on Vincent 1:50 000. Qhck 5 Shelly/quartz muddy sand of intertidal flats; bare or Zostera-colonised. Based on Qhk6 on Vincent 1:50 000. Veneered by cobbles and gravel in western upper Spencer Gulf. Qhck 8 P P P P P P P P P P P P P Organic/shelly sand/mud of mangrove woodland and samphire-algal marsh. Based on Qhk4 and 5 on Vincent 1:50 000. Qhck 9 SEMAPHORE SAND MEMBER: Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields. Qhcks Holocene sand spread. Qhe 3 MOORNABA SAND: Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes. Qhem Undifferentiated Holocene lacustrine/playa sediments. Qhl Holocene playa sediments. Example: Qhl on CURDIMURKA. Qhl 1 Holocene claypan and lagoonal sediments. Based on Qhl on CHOWILLA. Qhl 3 Quaternary gypsiferous dunes/lunettes. Qe 3 MOREENIA ADAMELLITE: Adamellite, grey, coarse-grained; biotite adamellite, minor garnet, probably grades to granite at Ungarra. LINCOLN sheet. Lzom URANNO MICROGRANITE: Microgranite, grey, equigranular, fine to medium-grained, local weak foliation. Lzou YUNTA WELL LEUCOGRANITE: Granite and pegmatite, medium to coarse-grained muscovite. Variably foliated. Lzoy PETER PAN SUPERSUITE: Magmatic rocks, felsic and lesser mafic. Intruded during the Kimban Orogeny and dated ~1750-1700Ma. Lz DONINGTON SUITE: Quartz gabbronorite, hypersthene gneissic granite, megacrystic intermediate granite gneiss, alkali feldspar granitic gneiss, orbicular granodiorite, metadolerite. 1855-1845Ma. Ld Quartz gabbronorite. Ld 1 Í Í Í Í Í Í Í Í Í Í Orbicular granodiorite. Ld 2 COLBERT GRANITE: Granite-gneiss, massive, foliated, medium-grained equigranular. Ldc JUSSIEU METADOLERITE: Metadolerite dykes and enclaves. Ldj Í Í Í Í Í Í Í Í Í Í MEMORY COVE CHARNOCKITE: Granite gneiss, medium to coarse-grained, felsic hypersthene. Foliated in places, locally porphyritic. Ldm Í Í Í Í Í Í Í Í Í Í Í Í WANNA MEGACRYSTIC GRANITE GNEISS: Granite-gneiss, weakly to strongly foliated, mafic rich, coarse-grained, meagcrystic; granite-granodiorite augen gneiss, ovoid zoned plagioclase and K-fspar to 40 mm diam. Local mafic xenoliths. Ldw HUTCHISON GROUP: Quartzite, pelitic and chemical metasediments, jaspilite. Lh WARROW QUARTZITE: Quartzite, massive, rarely cross-bedded, conglomeratic, pelitic; gneiss; nephrite. Lhw

Transcript of AUSTRALIA 1:250 000 SA GEOLOGICAL ATLAS SERIES SHEET … · k op ir n, fe mc donal s, sa nd rifl...

!!!!!!!!

"

"

"

"

"

"

"

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!(

!(

!(

!(

!(

"

"

"

"

"

"

"

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!(

!(

!(

!(

!(

"

"

"

"

"

"

"

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!

!(

!(

!(

!(

!(

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

)

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"" "

"

""

"

"

"

"

"

"

"

"

"

""

"

""

"

""

""

"

"

"

"

"

" "

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

""

"

""

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

"

" "

"

"

""

"

"

"

"

"

""

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

"

"

""

" "

"

"

"

"

"

"

""

"

"

" "

"

""

"" "

"

"

"

"

"

"

"

"

"

""

"

" "

"

"

"

"

"

"

"

"

"

"

"

""

"

" "

""

"

"

"

"

"

"

"

"

"

" "

""

"

"

"

"

"

"

"

"

"

"

"

" " "

"

"

"

"

"

"

"

""

"

"

" "

"

"

"

"

"

"

"

""

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

""

"

"

""

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

""

""

"

"

"

"

"

"

"

"

"

"

"

"

" "

""

"

"

"

"

"

""

"

"

"

"

" "

"

"

"

"

"

""

"

""

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""

"

""

"

"

"

" "

"

"

"

" "

"

""

""

"

"

"

""" "

"

"

"

""

"

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

""

"

"

""

"

" "

""

"

"

"

"""

"

"

"

"

""

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

" ""

"

""

"

" " "

"

"

""

""

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""""

""

"

"

"

"

"

"

"

"

""

"

"

"

"

"

""

"

"

"

"

"

"

"

"

" "

"

"""

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

" "

"

"

" "

" "

"

"

"

"

"

""

"

"

"

"

"

"

"

""

"

"

"

"

"

"

" ""

"

" "

"

"

"

"

"

"

" "

"

"

" "

"

" "

"

"

"

""

"

"

""

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"" "

""

"

"

"

"

"

"

"

"

"

"

"

""

" "

"

"

"

"

"

"

"

"

"

" "

"

"

""

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

" " "

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

""

"

""

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

""

"

"

"

"

"

"

"

" "

"""

""

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

""

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

""

"

"

" "

"

"

"

"

" " "

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

" "

"

"

"

"

"

"

"

"

""

"

"

"

""

"

"

" "

"

"

"

"

"

"

"

"

"

""

"

"

"

"

"

""

"

""

"

""

"

"""

"

"

"

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

""

" "

"

""

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

""

" ""

"

"

"

"

""

"

"

"

"

"" "

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

" "

"

"

""

"

"

""

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

""

"

"

"

"

"

"

"

"

"

"

"

" ""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"" "

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

" "

"

"

" "

"

"

"

"

"

"

""

""

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

"

" "" "

"

"

"

"

" ""

"

"

"

"

"

"

"

"

"

"

""

"

Ì

G

Ç

Ç

Ì

G

Ì

G

Ì

Ì

Ì

Ç

Ç

Ì

Ç

Ç

G

Ì

Ì

Ç

Ç

Ç

Ç

Ç

Ì

Ì

Ç

Ì

Ç

Ì

ALdk

ALdk

Qhck8

Qhcks_______Qpcb

ALdk

Qhck8

Qhck5

Qpr4_____Qpcb

Qpcb

Qhcks

Qhck9

ALdk

ALsw

ALdk

Qhck8

ALsw

Qhcks

Qhck8

Qhck9

Qpr4_____?Lhw

Qpcg

Qhem

Qpr4_____Qpcb

Qpr4

Qhem

?Qpcg

Qpcb

Qpr4_____Qpca

Qpcg

ALs

Ql1Qpew

Qhem

?Lzoy

Qe3

ALsc

Qpr4

Qe3

Qpr4_____TfeTfe_____Lic

Qpcb______Tfe

Lz

Qpr4_____Qpca

Tfe_____Lz

Qpca

Qpr4_____Tfe_____Lhw

Tfe

Qpr4_____Tfe

Ldw

Tfe_____Lhw

qz

Qpr4_____Qpca

Qhck9

L10

Qe3

Lik

?Tfe_____Lz

Qpr4

Lzoh

Qhcks_______Qpcb

Qhck9

Ld

Ld

Ldw+Ldj+L-u

Qpcb

Ql1

L-m

Ld1+L-u

?Ld

?Tfe

Ldw+Ldj+L-u

Ldw

Qpca_____Tfe_____?Lic

Ldw

Qpr4

Tfe_____Tsi

Lik

Mcb

Qhck8

Lz

Qhck9

Ld

Qpca_____Lz

Qpr4

Lz

Ldc

Qpr4_____Ld

Qhem

Tfe_____Tsi

Ms1

Ldw+Ldm+Ldj

Qpcb

?Ld

Qhem

Qhck8

Qhck9

ALdk

?Qpcb

Qhcks_______Qpcb

Qpcb

Qpr4_____?Lhw

Ql1

Ql1_____Qpcg

Qhck8

Qha1

ALdk

Qpr4_____ALdk

Qpcb

Qe3

Qpr4_____QpcaALdk

Qpr4_____?ALdk

Qha1

Qpr4_____Tfe

Qpr4_____Qpcb______Tfe

Qhe3

Lh

Tfe_____Lil

Qpr4_____?Li1

Li1

Tfe_____Lil

Qpr4_____Tfe

Tfe_____Lz

Ldw+Ldj+L-u

Lir

Tfe_____Lhw+Lz

Ql1

Ldw+Ldj+L-u

Tfe

Lzou

Ld

Tfe_____Lic

Qpr4_____Tfe_____Tsi

Qpcb

Tfe_____?Lz

Lz+Lir+ALs

Tfe_____?Lz

Tfe_____Lh

Lzo

Ldc

Tfe

Liu

Lzo

Qhck9

?Ld

Ld

Li1

Ld+L-u+Ldj

LM-n

Li1Lz

Tfe_____Lzoy

Qpr4

Ld+Ldj

Tfe_____Lic

Ld2

Tfe_____?Ld

Lzoy

Ldm

Lik

Lz+Lic

Qpr4_____LirQhl3

Qhem

Ld

Ldc

Ld

Ms1+2+3

Qpap

Ldw+Ms2

Ms1

Ld

Qhem

Qpr4_____?Lil

ALscQpcb

?Qpcg

Qhck8

ALsw

Qhcks?Qpcg

Qpcg

Qpcb

Qhem

Qhem______Qpcb

Qhem

Qe3

Qe3

Lhw

Qhcks

ALsc

Qhck8

Qpr4

ALdk

Qpr4

Qe3

?Qpcg

Qpew

Qhcks

Qpcb?Qpcg

Qhem

Tfe_____?ALsc

Tfe_____ALs

Qhl3

Qha1

Qhem

Qhem

ALsc

Lic

Tfe_____Lz

Qpcg

Qpr4_____Tfe_____?Lhw

Lik

Qhl3

Li1

Tfe_____Lic+LzLhw+Lz

Qpr4_____Qpca

qz

Qhck8

Tfe_____Lhw_____Lz

Ldm+Ldc+Ldj+L-u

Qe3

Ldw+L-u+Ldj

Qhck8

Lik

Ql1

Lhw

Ldw+L-u+Ldj

Lz

Ldw

Qhcks

L10

Ld

Tfe_____Tsi Tfe

Qpcb

Qhl3Tfe_____Tsi

Qpr4

Qpr4

Lil

Qhem______Mcb1

Qpr4_____Lhw

Qpr4_____Lic

Qpca_____Lz Lhw

Ld

Qpr4_____Ld

Lhw

Qpr4_____Lz

Qpca_____Lhw

Ms1

Ldc

Qha1

Ms1+2

Lik

Ms1 Ms1+Ld

Qhcks_______Qpcb

Qhck9

ALdk

Qhck9

ALdc

ALsw

Qpcb

Qhe3

Qhck9

Qpcb

ALsw

Qpcb

Ql1

Qhe3_____Qhem

Qhem

Qpr4

?Qpcg

Ql1

ALsw

Qpr4_____Tfe

Ql1

Qe3

Qpr4

Qhl3

Qpr4_____Qpca_____Lzo

Lz

Qpr4_____Tfe_____Lhw

Qpr4

Qpr4_____Tfe_____Lil

Lir

Ldw

?Lhw

TfeQl1

Qhcks

Ldw+Ldj+L-u

Qpew______Qpcb

Ldw

LicLz

QhcksQhcks

Tfe_____Ld

Qe3

?LdLi1

Qpr4_____Tsi

Qha1

Ldc

Tfe_____Lzo

Qhe3_____Qpew

Qha1

?Ld

Qpr4

L10

Qpap______Tbw

Qpr4_____Tfe_____Lic

Ql1_____Qhck5

Lic

Qpr4_____Lil

Ql1

Qpr4_____?Lhw

Qhck8

Qhcks

ALsm

Ql1Qpr4_____Ld

L10

Lic

Lz

qz

Lhw

Qpr4_____Lz

?Lhw

Qpr4_____Lz

Ld+Ms1+3

Qhcks______Ld

Ld

Qpr4_____?Lz

Ms1+3

Lz

Qpca_____Lik

Ld+Ldj

Ldc

Ldm+Ldj+L-u

Qhck9

Qhl3

Qpca_____Lz?ALs

Qhck9

ALdw

ALsw Qhcks_______Qpcg

ALdc

?ALs

ALdc

Ql1

Qpr4_____Qpcb

Qhcks_______Qpcb

Qpr4_____LhwALsw

Lhw

Qpr4

Qpcb

Qhck9

Qpcb

Qe3_____Ql1

Qha1

Ql1

Tfe_____Lhw

Qhe3

Qe3

Qhl3

ALsc2

Qhem______Qpcb______Tfe

Tfe_____Lh

Ql1

Tfe_____ALsc

Qpr4_____L-m Tfe_____?Lhw

Qpr4

Qhcks

Lz

Ldc

Tfe_____Lz

Ldj

Lzo

Tfe_____Li1

Qpr4_____?Qpew

Qpr4

Tfe_____Lz

Ql1

Tfe_____?Lh

Qpcb

Ql1

Lzom

Ldc Tfe

Li1

Lhw

Qpcb

Ldw+L-u

Tfe_____Lz

my

Lir

Li1

Lzom

Ldm+Ldj

LzoyLzo

Tfe_____Lzoy

Qpr4

Ldw+Ldj+L-u

Qpca

?Lir Qpr4_____?LdQpr4_____Ld

Ldm

Tfe_____Lic

Ldm

Qhcks

Qpr4Qpcb

Qhcks

Qpr4_____LilLz

?Ld

Qhcks

Ld

?ALs

Qhck8

Qpcb

ALdkALsw

Qhck8

Qhcks_______Qpcb

?ALs

?ALs

Qe3

Ql1_____Qpcb

Qhck9

Lhw

Qhck8

Qpr4

ALsw

Qhem______Qpcb

Qhcks

ALdkQhl3

Qpr4_____Tfe_____?Lhw

Qpcg?Qpcg

Qha1

Qhl3Tfe

Ql1

Qpr4_____?Lhw

Lhw

ALsc

ALsc1+ALsc2Qpcb

Lz

Tfe

Qhem+Qhe3

Tp6____To4

ALsc

Lz

Tfe_____Lzo

Lil

L10+Ldc

Qpr4_____Tfe_____Lhw

Lz

Lz

Tfe

Lz

L10

Tfe

Tfe_____Lzo

Qpr4_____Tfe

Liu

Qhck8

my

Ldm

Lzo

Qpr4_____Lzoh

Ldj

Ldw

?Ld

Lzo

Qhcks_______Qpcb

LM-n2

Qpca_____Qpew

?Ld

Lz

LM-n1

Lzoy

Ld

Ql1

Ld

Tfe_____Tsi_____?Lzoy

Qpr4_____Qpcb

Lir

Ld+Ldj

Lic

Qpcb

ALsm

Ld

LirLil

Lz

?Ld

Qpca_____Lz+Lir

Ms1+Ld+Ms3

Qpcb

Ld

Lz

Qhcks

Ms1+2+3+Ld

Qhck8

Qpca_____LzQhcks

ALsw

ALdkQhck8ALdk

Qhcks_______Qpcb

L-p

Qpcb

LhwALsw

Qhcks

Qpr4_____Qpcb

Qpcb

ALdkQhck5

Lhw

Tfe

Qpr4_____Lhw

Qe3

Qhem______Qpr4

Qha1

Ql1

Qhcks

Qpr4_____Qpca

Qpcb

Qpr4_____QpcbQl1

Qpr4_____Lik

Lz LhwTfe_____Lil

Tfe_____Li1

Tfe_____?Lh

Tfe_____Lzo

Ldw+Ldc+L-u+Ldj

Lir+Li1

Ld

Qpr4_____Lhw

Lik

Tfe_____Li1Tfe_____?Lic

Tfe_____LhwLil

Tfe_____Lz

Tfe

L-mLz

Li1

Ld

Tfe_____Li1

Qpr4_____Tfe

LdQpcb

Ld

Ld+Ldj+L-u

Ldm+L-u

Tfe_____Li1

Qhck9

Ld

qz

Ldw

Ld

Ldm+Ldj

Liu

Ldc

Ldw

Qpr4

Qhck9

Qhck5_____Ld

Lzoy

Tfe_____Lil

Qpr4_____Tfe_____Tsi

?Qpca_____Tfe

Qhck8

Ld+Ldj+Ms1

Qpr4_____Ld

LikLz

Ld+Ldj

LilLz

Qhck8

Qpr4 Qpr4_____?ALs

Qpr4_____?Ld Qhck8

QpcbALdw

Qpcb

ALdk

QpcgQhcks_______Qpcb

Qhck9

ALdw

Qhck8

Ql1

Ql1

Qhcks_______Qpcb

Qhck8

ALdk

Qhck9

Qhcks_______Qpcb

Qe3

Qhem______Qpcb

ALsc

Qhck9

Qha1

Ql1

Qe3

Qhe3_____Qpew

Qhem

Tfe

Qpr4_____Lz

Qpr4

Qha1

Tfe_____Lz

Qpr4_____Lz

Qpr4

Qpr4_____Qpcb

Qpr4_____Lzo

Qhck9

LilLic Tfe_____Lic

Qhck8

Ldw

Ldc

Lhw

LdcTfe_____Ld

?LdcLdc+Ldw+Ldj+L-u

my

LirLzo

Ld+Ldj+L-u

Lic

Li1+Lz

Ldw

Tfe_____LicLic

Ldm

LzTfe

Qpcb

Ldm+Ldj

Qpcb

Ldw

Lil

Lzoh

?Qhem_______Qpcb

Ldw

Ld

Ld

Qpr4_____Lzoy

Ld

Ld

Lir

Qpr4_____Lzoy

Tfe_____Liu

Qhcks

Ldw

Ld+L-u+Ms

Qpca_____?Lil

Qpr4_____Mcb

Lz

Ldw+Ldj

Qpcb

Lic

Ldw+Ldj+Ms1+2

Qpr4_____Lz+LhwQpca_____Tfe_____Tsi

Qhcks

Ldw+Ms1+L-u

Qpca_____Tfe_____Tsi

QpcbMs1+2+3Ms1+2

BARNS, Fe

ULEY, GRPH

CARROW, Fe

KAPPERNA, Fe

URANNO, GRNT

KOPPIO, GRPH

BEECROFT, GNSS

GREENPATCH, Fe

KOPPIO IRON, Fe

MCDONALDS, SAND

RIFLE RANGE, Fe

TUMBY BAY, TALC

LOUTH BAY, SAND

COFFIN BAY, LSND

NORTH BLOCK, KAO

GLEN PARK 1, CALI

LAKE MALATA, GYPS

LAKE GREENLY, GYPS

LAKE WANGARY, SAND

CHARLTON GULLY, Fe

ALLERTON HILLS, KAO

POONINDIE EAST, SAND

WHITE LAKES NO.3, GYPS

DK QUARRIES, GNSS, GRNT

IRON MOUNT, Fe, FEORE, FEST

STRAWBERRY HILL NORTH, SAND, GRVL

60

80

52

42

86

86

78

7470

82

60

86

50

70

70

16

80

66

75

80

46

60

70

82

18

82

30

46

22

25

60

35

70

74

50

79

33

37

60

88

3682

70

62

70

83

28

84

85

82

88

54

50

85

85

24

60

84

85

80

47

82

81

64

75

72

79

Gawler Pond

Hall Bay

Avoid Bay

Tumby Bay

Peake Bay

Shag Cove

Coffin Bay

Dutton Bay

Boston Bay

Yangie Bay

Misery Bay

Massena Bay

Lipson Cove

Jussieu Bay

Fishery Bay

Port Douglas

Sleaford Bay

Spalding Cove

D'anville Bay

Tapley Channel

Douglas Channel

Mount Dutton Bay

Port Lincoln Proper

RED CLIFF

BALD HILL

CAPE BURR

CAPE EULER

FARM BEACH

CAPE HARDY

REEF POINT

NOSE POINT

POINT AVOID

CAPE CARNOT

SHOAL POINT

PEAKE POINT

NYLLOW HILL

POINT MARIA

MOUNT GAWLER

POINT BOSTON

MURRAY POINT

COBBLER HILL

PICNIC BEACH

GUNYAH BEACH

POINT LONGNOSE

SURFLEET POINT

MOUNT DRUMMONDMOUNT DRUMMOND

THREE BROTHERS

CAPE DONINGTON

MACLAREN POINT

DRUMMOND POINT

TREVALLEY POINT

PILLAWORTA HILL

CAPE TOURNEFORT

STRAWBERRY HILL

CAPE CATASTROPHE

POINT HASELGROVE

OBSERVATORY POINT

POINT BOLINGBROKE

JESSIEU PENINSULA

Kunari

Lynfield

Koodinga

Moorlands

Midway Glen

Woolawae Downs

Wanna

Tulka

Kiana

Moody

Coulta

Kaldow

Karkoo

Warrow

Uranno

Lipson

Butler

Koppio

Uranno

Brooker

Wanilla

Ningana

Wangary

Pillana

Warunda

Pearlah

Ungarra

Coomapoo

Yeltukka

Yeelanna

Grantham

Yeltukka

Kapinnie

Moreenia

Gum Flat

Wildeloo

Edillilie

Poonindie

Mena Flat

Mount HillMount Hill

Cowieninta

Mount Hope

White Flat

Duck Ponds

Mungerowie

The Fountain

Butler Tanks

Cockaleechie

Warratta Vale

Yallunda Flat

Brimpton Lake

North Shields

Cummins

Tumby Bay

Coffin Bay

Port Neill

Port Lincoln

Lake Malata

Lake Greenly

Lake Hamilton

Sleaford Mere

Lake Wangary

Little Swamp

Lake Baird

Pillana Lagoon

Salt Swamp

Pillie Lake

Curta Willa Waterhole

63

70

75

50

22

46

56

60

70

80

7085

75

80

70

45

52

50

Coomunga

Louth Bay

Green Patch

500000

500000

510000

510000

520000

520000

530000

530000

540000

540000

550000

550000

560000

560000

570000

570000

580000

580000

590000

590000

600000

600000

610000

610000

620000

620000

630000

630000

6130

000

6130

000

6140

000

6140

000

6150

000

6150

000

6160

000

6160

000

6170

000

6170

000

6180

000

6180

000

6190

000

6190

000

6200

000

6200

000

6210

000

6210

000

6220

000

6220

000

6230

000

6230

000

Ld

ALs

Lh

Ms

Lo

L-p

Lo

Lh

LoLo

The Total Magnetic Intensity Image has been compiled usingaeromagnetic data from the

Department of State Development, South Australia.Aeromagnetic data has been merged, gridded and imageprocessed by the Geological Survey of South Australia,

DSD Resources and Energy Group.

SCALE 1:1000000 SCALE 1:1000000 Modified from Interpreted Crystalline Basement Geology Of The Gawler Craton (Fairclough et al. 2003)Interpreted Solid Geology Of The Curnamona Province (Burtt and Betts, 2003),

Musgrave Block, Central Australia: regional geology from interpretation ofaeromagnetic data (Rankin and Newton, 2002), Solid Geology South Australia (Cowley, 2006).

5 0 5 10 15 20 25KILOMETRES KILOMETRES

SA GEOLOGICAL ATLAS SERIES SHEET

GEOLOGICAL SURVEY OF SOUTH AUSTRALIADEPARTMENT OF STATE DEVELOPMENT

SOLID GEOLOGY INTERPRETATIONTOTAL MAGNETIC INTENSITY IMAGE

AUSTRALIA 1:250 000

+7.50

°E

+7.25

°E

+7.00

°E

+6.75

°E

+6.50

°E

+6.25

°E

+7.75

°E

KIMBA

LINCOLN

WHYALLAELLISTON

MAITLAND

KINGSCOTE

Coulta5929

Tumby6129

Lincoln6028

Spilsby6128

Wangary5928

Cummins6029

WA

NTQLD

SANSW

VIC

TAS

INDEX TO 1:100 000 SHEETS

INDEX TO ADJOINING 1: 250 000 SHEETSMagnetic Declination 2000

(Annual variation +1.4 minutes)

SCALE 1:250,000

DIGITAL EDITIONSUBJECT TO AMENDMENT

See published printed map for further information

A two standard deviation contrast stretch has been applied to the raster image above.

35° 0

0'34

° 30'

34° 0

0'

135° 00' 135° 30' 136° 00' 136° 30'

35° 00'34° 30'

34° 00'

135° 00' 135° 30' 136° 00' 136° 30'

35° 0

0'34

° 30'

34° 0

0'

135° 00' 135° 30' 136° 00' 136° 30'

35° 00'34° 30'

34° 00'

135° 00' 135° 30' 136° 00' 136° 30'

35° 0

0'34

° 30'

34° 0

0'

135° 00' 135° 30' 136° 00' 136° 30'

35° 00'34° 30'

34° 00'

135° 00' 135° 30' 136° 00' 136° 30'

COMMODITIESCALI CalcreteFe IronFEORE Iron OreFEST Ironstone -

constructionmaterials

GNSS GneissGRNT GraniteGRPH GraphiteGRVL GravelGYPS GypsumKAO KaolinLSND Lime sandQTZE QuartziteSAND SandTALC Talc

LINEAR STRUCTURE

.............................................FAULT POSITION ACCURATE.....................................FAULT POSITION APPROXIMATE

................................................................................TREND-LINE

GEOLOGICAL BOUNDARY

..................................................................................COASTLINE...GEOLOGICAL BOUNDARY POSITION ACCURATE

...........................................................................GEOLOGICAL BOUNDARY POSITIONAPPROXIMATE

Solid Geology - Linear Structure

.........................................................................Fault position accurate..........................................................................................Mylonite zone LINCOLN

SI5311

Solid Geology

Donington SuiteLd

Dutton SuiteALd

Hall Bay VolcanicsALsh

Hutchison GroupLh

Miltalie GneissL-m

Moody SuiteLo

Price MetasedimentsL-p

Sleaford ComplexALs

Spilsby SuiteMs

Unnamed GIS Unit - see descriptionMc

Unnamed GIS Unit - see descriptionLi1

Unnamed GIS Unit - see descriptionL36

nTesla

-1442.36 10179.21

-911.8 -323.64 264.52

SI5311

LINCOLN

GEOMORPHIC FEATURES

................................................................................................LAKE.............................................................INTERMITTENT LAKE

........................................................MINOR WATERCOURSE..........................................................................................SWAMP

...............................................................................SAND RIDGE

............................................................................... !WATERHOLE

MINING

........................................................................... GPIT/CUT - CONSTRUCTION MATERIALS (SANDAND/OR CLAY)

............................................................................................. ÌQUARRY - CONSTRUCTION MATERIALS (HARDROCK)

........... ÌMINE - METALS AND INDUSTRIAL MINERALS........................................................... ÇDEPOSIT - NO MINING

CULTURAL FEATURES

.....................................................................PRINCIPAL ROAD................................................................SECONDARY ROAD

...........................................................................MINOR ROADS..............................................................VEHICULAR TRACKS

.......................................................OPERATIONAL RAILWAY..........................................................ABANDONED RAILWAY

......................................................................WATER PIPELINE................................................................... !IDENTIFIED POINT

...................................................................................... "BUILDING..................................................................LANDING GROUND

.............................................................. !(TOWN OR LOCALITY

STRUCTURAL FEATURES

...........................................................TECTONIC FOLIATION.................................TECTONIC FOLIATION - VERTICAL

.......................HORIZONTAL SEDIMENTARY BEDDING.....................................................................................HORIZONTAL SEDIMENTARY BEDDING -

VERTICAL

..............................................................................HORIZONTAL SEDIMENTARY BEDDING -HORIZONTAL

Any person purchasing this map may reproduce it for their own useor that of their staff, but not for any other purpose except with the written

permission of the Chief Executive, Department of State Development SA, GPO Box 320, Adelaide, South Australia, 5001.

CROWN COPYRIGHT RESERVEDDepartment of

State Development SA.

Topographic detail based on TOPO-250K GEODATA (source scale 1:250 000)supplied by Geoscience Australia - National Mapping Division, ACT.The relationship between this data and DSD data is not guaranteed.

Computer generated from SA_GEOLOGY database(Digital data available upon request)

Product of Spatial Information Services.Published by, and with the authority of, the

Department of State Development SA.Grey numbered lines indicate the 10000 metre Map Grid

Transverse Mercator Projection, Geocentric Datum Australia, 1994.The lake boundaries displayed on this map may have been derived from geological interpretation

and may not match lakes interpreted by topographic mapping authorities.Not all structures are represented on this particular map.

Mapping and Compilation by M.P. Schwarz, B.Sc.(Hons), and L.R. Rankin, B.Sc.(Hons) withcontributions by A.R. Martin, B.Sc.(Hons), A.J. Parker, Ph.D., W.M. Cowley, B.Sc.(Hons), S.O.

McAvaney, B.Sc.(Hons), and C.E. Wade, B.Sc.(Hons)S.M. Hill, Ph.D., Director, Geological Survey of South Australia.

Geological boundaries displayed on this map have beenDerived from geological interpretation and are not

intended to be used for navigational purposes.Copies of this map can be obtained from the

Department of State Development SA, Adelaide.9/2/2017

2017

Current version 2016.2

UNITS ARE NOT LISTED IN STRICT STRATIGRAPHIC ORDER BELOW AGE LEVEL

R E F E R E N C EHOLOCENE

PLEISTOCENE-HOLOCENE

PLEISTOCENE

PLIOCENE

OLIGOCENE

EOCENE-PLEISTOCENE

TERTIARY

MESOPROTEROZOIC

PALAEO-MESOPROTEROZOIC

PALAEOPROTEROZOIC

ARCHAEAN-PALAEOPROTEROZOIC

MISCELLANEOUS

CHINMINA SYENITE: Monzonite, massive, to weaklyfoliated, medium to coarse-grained, dark grey-black,phenocrysts of plagioclase, microcline and hornblende.LINCOLN sheet.

Lzoh

MOODY SUITE: Adamellite, medium-grained;garnetiferous; granite. U-Pb ages 1709-1701Ma.Lzo

TOURNEFORT METADOLERITE: Gabbro and dolerite,fine to coarse-grained, massive, black dykes. Chilledmargins, variably recrystallised to amphibolite andhornblende granulite. Age ~1800Ma.

L-u

MILTALIE GNEISS: Gneiss, migmatitic grey granitic,coarse-grained equigranular foliated, quartz, perthiticmicrocline, plagioclase, biotitic.

L-mPRICE METASEDIMENTS: Schist, fine grained, pelitic,magnetite-rich.L-p

Mylonitic Donington Suite and/or Miltalie Gneiss.L10

Peridotite, massive, coarse grained, dark green to black;biotitite, pyroxenite, hornblendite.LM-n2

Diorite, massive, medium to coarse grained, dark green.LM-n1

COONTA GABBRO: Gabbro, massive, coarse grained,dark green; diorite, massive, medium to coarse grained,dark green; peridotite, massive, coarse grained, dark greento black.

LM-n

Quartz veins/bodies, undifferentiated.qzMylonitised rocks, undifferentiated.my

BLUE RANGE BEDS: Sandstone, minor grit and pebblebeds, white, massive to crossbedded, rare haematiteveins.

McbGranodiorite, fine-medium grey.Ms3

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Fine-grained granite, aplite.Ms2

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Granite, medium-coarse tabular-feldspar.Ms1

SPILSBY SUITE: Granite, grey, coarse-grained porphyritic(Adamellite to granodiorite), Massive, weakly foliated. Age1576+/-198 Mapooled Rb-Sr Webb 1978, 1475-1410 Ma(K-Ar) Webb et al. 1986.

Ms

Quaternary playa sediments.Ql1YAMBA FORMATION: Clay, lacustrine, gypsiferous;gypsum-quartz sand . Dunes, playa lakes.Qly

Undifferentiated Pleistocene calcrete.Qp\caPOORAKA FORMATION: Clay, sand and carbonate earth,silty, with gravel lenses.QpapBRIDGEWATER FORMATION: Bioclastic barrier shorelinedeposits, silica rich, with heavy minerals, shallow sub-tidal.Coastal, cross-bedded aeolian calcarenite with palaeosolhorizons and capped by calcrete.

QpcbGLANVILLE FORMATION: Clay, mottled, shelly;calcarenite, skeletal, coquina. Geochron age 132 000+/-6000 years Bp on TL.

QpcgPleistocene dune core sand.Qpe1WIABUNA FORMATION: Silt to fine-grained sand,orange-brown, calcareous , conglomeratic in part. Aeolian.QpewPleistocene gravel, clay, silt and sand with soft carbonate,overlying nodular/tabular calcrete. Based on Qp1 onGAIRDNER, YARDEA, STREAKY BAY, WHYALLA, Qp onCHILDARA.

Qpr4

Limestone, sandy and pebbly, molluscan fauna. FisheryBay.Tp6

Limestone, brown and pink, bryozoal, gritty and pebbly atbase, latest Oligocene fauna. Fishery Bay.To4

WANILLA FORMATION: Sand, micaceous, carbonaceous;interbeds of lignite.Tbw

Undifferentiated Tertiary ferricrete.T\feUndifferentiated Tertiary silcrete.T\si

Lower and/or Upper Middleback Jaspilite:amphibole-magnetite schist and quartzite. Based onProt-hm1 on YARDEA.

Li1COOK GAP SCHIST: Schist, medium-grained,,biotite-garnet-sillimanite quartzo-feldspathic, grading togneiss, migmatised in high-grade area, locally graphitic.

LicKATUNGA DOLOMITE: Marble, white to pale grey,dolomitic, layered with serpentine, withcalcite-diopside-tremolite banding.

LikLOWER MIDDLEBACK JASPILITE: Haematite, banded,with quartzite+magnetite, carbonate, schist and chert.Grades into jaspilite in places.

LilBURRAWING AMPHIBOLITE: Amphibolite, fine tomedium-grained, interbedded gradationally with bandeddiopside-hornblende-rich calcsilicate gneiss. LINCOLNsheet.

LirUPPER MIDDLEBACK JASPILITE: Jaspilite.Liu

COULTA GRANODIORITE: Granite; granodiorite; withabundant mafic xenoliths. Foliated.ALdc

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

KIANA GRANITE: Granite, porphyritic, gneissic. Weak tostrong alignment of tabular feldspars.ALdk

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

WHIDBEY GRANITE: Granite, massive, even grained.Weakly foliated. Age 2337+/-71 Ma.ALdwSLEAFORD COMPLEX: Metasediment; metabasalt, sills,dykes; augen gneiss. Granulite facies, amphibolite facies.ALsCARNOT GNEISSES: Garnet gneiss; porphyroblasticgneiss; paragneiss; basic granulite; layered garnet gneiss;felsic gneiss. Interpreted as metasediments, tholeiiticbasalt and synorogenic intrusives.

ALscParagneiss, banded; garnet-biotite quartz feldspar gneiss;porphyroblastic cordierite-sillimanite quartz feldspargneiss. Age: 2412+/-72 Ma. LINCOLN sheet.

ALsc1Orthogneiss; foliated K feldspar granite to augen gneiss.Age: 2436+/-137 Ma (Rb-Sr whole rock); massive tocompositionally banded felsic gneiss. Age: 2637+/-21 Ma.LINCOLN sheet.

ALsc2MASSENA BAY GNEISSES: Gneiss, banded,quartz-feldspar-biotite; quartzofeldspathic orthogneiss withrounded mafic inclusions, migmatitic leucosomes,LINCOLN sheet.

ALsm

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

WANGARY GNEISS: Gneiss,microcline-plagioclase-quartz-biotite-muscovite. Age2380+/-60 Ma (Rb-Sr); 2445+/-32 Ma (U-Pb).

ALsw

Present day Holocene alluvium; current bedload.Qha1SAINT KILDA FORMATION: Undifferentiated Holocenecoastal marine sediment.QhckSupratidal sand/mud flats: gypseous clay. Based on Qhk2on Vincent 1:50 000.Qhck5Shelly/quartz muddy sand of intertidal flats; bare orZostera-colonised. Based on Qhk6 on Vincent 1:50 000.Veneered by cobbles and gravel in western upper SpencerGulf.

Qhck8

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P P

P P P P POrganic/shelly sand/mud of mangrove woodland andsamphire-algal marsh. Based on Qhk4 and 5 on Vincent1:50 000.

Qhck9SEMAPHORE SAND MEMBER: Unconsolidated whitebioclastic quartz-carbonate sand of modern beaches andtransgressive dune fields.

QhcksHolocene sand spread.Qhe3MOORNABA SAND: Sand, aeolian, off-white and paleyellow, quartz-rich with carbonate pipes.QhemUndifferentiated Holocene lacustrine/playa sediments.QhlHolocene playa sediments. Example: Qhl onCURDIMURKA.Qhl1Holocene claypan and lagoonal sediments. Based on Qhlon CHOWILLA.Qhl3

Quaternary gypsiferous dunes/lunettes.Qe3

MOREENIA ADAMELLITE: Adamellite, grey,coarse-grained; biotite adamellite, minor garnet, probablygrades to granite at Ungarra. LINCOLN sheet.

LzomURANNO MICROGRANITE: Microgranite, grey,equigranular, fine to medium-grained, local weak foliation.LzouYUNTA WELL LEUCOGRANITE: Granite and pegmatite,medium to coarse-grained muscovite. Variably foliated.LzoyPETER PAN SUPERSUITE: Magmatic rocks, felsic andlesser mafic. Intruded during the Kimban Orogeny anddated ~1750-1700Ma.

LzDONINGTON SUITE: Quartz gabbronorite, hypersthenegneissic granite, megacrystic intermediate granite gneiss,alkali feldspar granitic gneiss, orbicular granodiorite,metadolerite. 1855-1845Ma.

LdQuartz gabbronorite.Ld1

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Orbicular granodiorite.Ld2COLBERT GRANITE: Granite-gneiss, massive, foliated,medium-grained equigranular.LdcJUSSIEU METADOLERITE: Metadolerite dykes andenclaves.Ldj

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

MEMORY COVE CHARNOCKITE: Granite gneiss,medium to coarse-grained, felsic hypersthene. Foliated inplaces, locally porphyritic.

Ldm

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

Í Í Í Í Í Í Í

WANNA MEGACRYSTIC GRANITE GNEISS:Granite-gneiss, weakly to strongly foliated, mafic rich,coarse-grained, meagcrystic; granite-granodiorite augengneiss, ovoid zoned plagioclase and K-fspar to 40 mmdiam. Local mafic xenoliths.

LdwHUTCHISON GROUP: Quartzite, pelitic and chemicalmetasediments, jaspilite.LhWARROW QUARTZITE: Quartzite, massive, rarelycross-bedded, conglomeratic, pelitic; gneiss; nephrite.Lhw