Musgrave Block Special, Df

Musgrave Block Special, Df

EROMANGA Cz Cz Cenozoic and Quaternary surficial deposits - sand, silt, clay, gravel, loose rock; deposited in colluvial, eluvial, alluvial GEOLOGICAL SYMBOLS U-Pb zircon geochronology sample locations AMADEUS BASIN BASIN and aeolian environments Ref No Sample No Lat Long MUSGRAVE BLOCK Geological boundary Mz Mz Mesozoic Eromanga Basin - friable white kaolinitic quartz sandstone; minor quartz conglomerate and very fine siltstone 1 BR98DFC550 24°57' 129°04' TO Fault; mapped, approximate 2 PR96IRS623 25°07' 129°04' ALICE SPRINGS OROGENY 400 - 300 Ma 3 PR96IRS549 25°37' 129°20' CENOZOIC 4 BR98DFC491 24°50' 129°21' MESOZOIC ? Fault; concealed, inferred Finke Group Df Df Finke Group - fine to medium quartz sandstone; minor siltstone and shale; pebble and boulder conglomerate 5 BR97CJE153 24°38' 129°24' MUSGRAVE BLOCK DEVONIAN TOPOGRAPHICAL SYMBOLS Thrust (WT - Woodroffe Thrust) 6 PR95IRS420 25°57' 129°25' 7 BR97CJE73 24°42' 129°27' Larapinta Group Ol Ol Larapinta Group - white sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone Syncline 8 BR98DFC429 24°46' 129°31' Sand ridges 9 P89/433 25°15' 129°39' ORDOVICIAN Mafic dyke 10 PR96IRS526 25°36' 129°50' Sealed road 11 P88/34 25°08' 129°52' Mount Currie Cmc Mount Currie Conglomerate - conglomerate containing clasts of sandstone, quartzite, felsic and mafic volcanics, granite, q Quartz vein Conglomerate Cmc AUSTRALIA 1:500 000 GEOLOGICAL SPECIAL NORTHERN TERRITORY 12 PR95DFC439 25°56' 129°54' gneiss, mafic intrusives Unsealed road AMADEUS BASIN 13 PR96IRS529 25°43' 129°57' Fault; concealed, thrust (interpreted from PALAEOZOIC Vehicle track magnetic, gravity and geological data) 14 PR95IRS396 25°59' 130°02' PETERMANN OROGENY 570 - 530 Ma 15 PR95IRS361 25°59' 130°11' CAMBRIAN Railway Fault; concealed, showing relative displacement 16 PR96DFC535 25°58' 130°11' 130°30' PLwi Winnall beds - brown to pale quartz sandstone, often micaceous, dominantly tabular but massive in upper part; 130°00' (interpreted from magnetic data) 17 PR96IRS592 25°59' 130°16' Winnall beds PLwi 129°30' Building 18 PR96IRS747 25°44' 130°20' minor red-purple fine sandstone to siltstone 129°00' Pin 45 Strike and dip of strata 19 PR96IRS741 25°45' 130°21' 24°30' PLwi Landing ground 20 A94/1402 25°44' 130°34' PLin Inindia Beds - quartz sandstone, medium to coarse, may be massive or well bedded, often ferruginised, Hull MT COWLE 60 Strike and dip of Petermann Orogeny foliation 21 O94/57F 25°14' 130°35' sometimes quartzitic; siltstone, red, yellow or pale, often strongly ferruginised; chert and jasper PLwi River, creek 22 A94/1378 25°45' 130°36' Inindia beds PL in layers, often structureless, sometimes breccias; conglomerate PLwi ZONE Strike and dip of foliation, plunge of mineral River Lake 75 23 A93/63 25°52' 130°47' PLd Amata Dykes - dolerite dykes elongation and plunge of intersection lineation PLd Amata PL d dolerite PLd Amadeus 24 A92/10A 25°51' 130°53' PLpi Pinyinna beds - grey quartz-muscovite phyllite, crystalline dolostone, fine grained sandstone, red, green and 25 BJ96/277A 25°39' 131°22' BLOODS 65 Strike and dip of strata parallel to foliation pale grey fissile siltstone, dolomitic siltstone BACKTHRUST 26 BJ96/280 25°41' 131°24' 55 PLde Dean Quartzite - crystalline quartz sandstone, rare vein quartz pebble conglomerate, quartz-kyanite-muscovite layers, 27 BJ75 25°56' 131°25' 50 45 BLOODS 75 Strike and dip of inverted strata red/purple crystalline quartz sandstone, feldspathic sandstone 65 28 BJ96/220 25°50' 131°26' Pinyinna beds PLpi 15 65 85 60 30 5 50 PINYINNA PLku Kulail Sandstone - red/purple crystalline quartz sandstone, abundant trough cross-beds, local heavy mineral layers of 35 65 R 45 70 Strike and dip of gneissic foliation Musgravian Event 29 MP94/503 25°52' 131°38' 30 40 OWLEY ANGE 70 RANGE 70 70 R NEOPROTEROZOIC 20 65 10 70 30 MP-98 25°57' 131°38' hematite and magnetite 80 40 20 25 30 MT PLvp ? 20 80 20 5 25 35 30 PLvh 60 ? DATA SOURCE 70 Strike and dip of second gneissic foliation Musgravian Event 31 MP-1 26°00' 131°44' Giles Event 1080 - 1040 Ma PLde 45 RANGE 50 HARRIS MOUNT ? 20 45 Granite 30 60 CARRUTHERS 32 MP-21 26°00' 131°45' Dean Quartzite PLde PLgb 40 20 PL vp 30 RANGE PLku 15 ? 45 Mineral occurrence 33 MP-5 25°57' 131°47' PL gb Angatja Suite - porphyritic orthopyroxene-clinopyroxene granite, charnockite, and hornblende-biotite granite, BLOODS85 35 Bloods Range 35 PLvh 50 Ol 1 3030 35 20 (Puntitjata) 35 45 PLde 10 NTGS 34 MP-43 25°59' 131°49' variably mylonitised and recrystallised to garnet-clinopyroxene-biotite-bearing assemblages 85 85 55 45 q 70 50 30 35 PLvh 7 45 Cu Prospect 35 S-12 25°54' 133°09' PLgb Hull Suite - biotite-muscovite granite, weakly foliated; coarsely porphyritic biotite-muscovite-epidote-garnet granite 25 Ag,Cu,Pb,Au McNICHOLS 40 55 FREGON DOMAIN MULGA PARK DOMAIN 2 40 25 PLbl 5 36 S-5 25°56' 133°14' PLgb Michell Nob Granite - coarse, porphyritic biotite-hornblende granite, variably mylonitised. Locally garnet-bearing 30 40 RANGE 3 ? 65 q PLbl Geochronology sample location and reference number 4555 PLgb2 NTGS-GA NGMA 29 37 S-556 25°50' 133°18' PL gb4 Nulchara Charnockite - coarse, porphyritic charnockite with clinopyroxene-orthopyroxene-hornblende-biotite 25 55 D 25 20 38 FI00CJE44 25°54' 133°50' GILES EVENT GILES EVENT and common rapakivi texture 20 Walu o 25 PLku 50 PL 50 c vp PLd Alcurra Dykes -amphibolite and dolerite dykes, sills and plugs; minor gabbro k 45 PL vp 1080 - 1040 Ma granite 1080 - 1040 Ma granite e 8 r 45 TJAUWATA GROUP PLug Giles Complex - pyroxenite and norite 50 55 PLgb R 60 PLtjb METAMORPHIC FACIES DIAGRAM PLgb i PLtj 40 55 Tjauwata Group v 50 c e 45 PLtj 45 55 r ? a 60 PLvw Wankari Volcanics - porphyritic rhyolite with rare epidotised and amygdeloidal mafic volcanics 50 Cu 40 129°00' 130°00' 130°30' Bloods Range Formation PLbl 50 PLtjb 24°30' PETERMANN OROGENY MUSGRAVE OROGENY 60 60 PLtja Ol 24°30' MT COWLE 1 243 Bloods Range Formation - red shales, polymictic conglomerate, volcaniclastics, tuffaceous horizons MOUNT40 35 65 Cu PLbl 35 SKENE 60 45 35 50 65 Cu Greenschist facies (UG = upper greenschist) Upper amphibolite facies ? 50 Cu 30 60 BLOODS and local lensoidal quartz sandstone beds 30 50 4 RANGE Wankari 50 70 35 Ag,Cu,Ni,Zn 25 Lower-mid amphibolite facies (E = epidote amphibolite) Granulite facies PL vw Puntitjata Rhyolite ~ 1075 Ma PLvp 50 50 40 Docker River Volcanics PLvp Puntitjata Rhyolite - porphyritic rhyolite 20 (Kaltukatjara) 25 ? 70 Medium-pressure upper amphibolite facies 40 15 70 MT 35 UG PL vh Mount Harris Basalt - variably silicified and epidotised, amygdaloidal basalt ILYARALONA60 45 PLde UG 6 - Pressure estimate in kbar Docker River Tjuninanta 35 70 PETERMANN E 131°00' HASTIE 30 25°00' High-pressure garnet amphibolite facies (Petermann Orogeny only) PLd PLd 25 (Kaltukatjara) 50 25 E Alcurra dolerite Mount Harris Basalt PLvh PLtj(a-c) Tjuninanta Formation 35 40 25 E 20 25 RANGE 30 Garnet granulite facies PLug 30 35 55 35 30 25 30 5-6 PLtj Interlensed, silicified, epidotised amygdaloidal basalt 65 40 40 q 55 ? >4 a PLtja PLga1 m Yulara 40 igm RANGES 40 35 30 ? at PLtj b Quartzite, quartz-muscovite schist and dark grey phyllitic schist 45 55 55 35 PLgb ite MT OLGA 0 50 100 km Giles W.A. Karukaki PIULTARANA 30 5 N.T. iso 20 40 35 gr KATAMALA PLtj c Volcaniclastics Livingstone 45 q T ad 35 HRUS CONE Complex 20 PETERMANN PLtjb FE T Pass MANNANANA 35 OF 132°00' 133°00' 134°00' Tjuninanta Formation PLka Karukali Quartzite - white crystalline quartz sandstone; rounded quartz pebble conglomerate beds; local heavy mineral layers of 40 35 25 DR 6-7 25°30' 40 OO Amputjutu 25 PETERMANN ABORIGINAL LAND TRUST W hematite and magnetite RANGE 10 6 PLtja Hull PLga 9 10 BUTLER STU RANGE 40 1 MT JENKINS H 20 60 20 PLpi DOME WY ART PLtjc MUSGRAVE BLOCK PLga Pitjantjatjara Supersuite 1190 - 1120 Ma 85 40 Umbeara 1 PLga 9 T 1a US PROTEROZOIC ga 131°00' THR Kulgera PLtjb PL 1 Pottoyu Suite - coarsely porphyritic foliated biotite granite, typically with rapakivi texture, locally migmatitic with 20 PLwa E PLde 30 45 MT ROBERT WOODROF F DEAN RGE Chirnside 25°00' Mount coarse hornblende; less abundant equigranular leucogranite 40 20 Mulga Park Victory Cavenagh PITJANTJATJARA SUPERSUITE PITJANTJATJARA SUPERSUITE RANGES PLpi MT SAMUEL MT FRASER Downs River 55 45 12 13 N.T. 26°00' PLga Amputjuta Dacite - finely porphyritic hypabyssal dacite 85 12 13 1a 30 Creek 30 132°00' 134°00' -- 26°00' 131°00' S.A. 1190 - 1120 Ma granite 1190 - 1120 Ma granite PLga 65 50 PLga 129°00' 130°00' PLga Mantarrur Suite - dominantly porphyritic granite, with biotite-rich matrix, varies from megacrystic to fine- or meduim-grained, 1a 30 1 Cmc 2 25°00' 45 PILTARDI mostly foliated; minor leucogranite; minor muscovite-bearing granite 60 60 20 Tjunti 60 50 PLga PLga 50 Lasseters Cave PLga3 Umutju Suite - foliated to undeformed clinopyroxene- and/or hornblende-bearing porphyritic granite with rounded blue-grey 20 Ck 45 Karukali Quartzite PLka 15 65 45 25 INDEX TO ADJOINING MAPS MAP LOCALITY phenocrysts of K-feldspar. Less commonly equigranular and medium-grained. Localised biotite-hornblende-garnet migmatite MOUNT Shaw CURDIE 50 127°30' 135°00' PLd 40 50 PLga4 Walal Granite - porphyritic hornblende-biotite granite and granodiorite, with less abundant equigranular leucogranite; 40 PLpi 30 45 24°00' 24°00' 35 PLga1 20 PLwi variably deformed and recrystallised to garnet-bearing assemblages 25 35 NT 60 KATITI ABORIGINAL LAND WA DARWIN 3 4 768 125 9 Creek SG 52-11 SG 52-16 SG 53-13 SG 53-14 PLga5 Kulpitjata Suite - variably deformed porphyritic biotite granite,

View Full Text

Details

  • File Type
    pdf
  • Upload Time
    -
  • Content Languages
    English
  • Upload User
    Anonymous/Not logged-in
  • File Pages
    1 Page
  • File Size
    -

Download

Channel Download Status
Express Download Enable

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

  • Not to be reproduced or distributed without explicit permission.
  • Not used for commercial purposes outside of approved use cases.
  • Not used to infringe on the rights of the original creators.
  • If you believe any content infringes your copyright, please contact us immediately.

Support

For help with questions, suggestions, or problems, please contact us