Last edited by Vuran
Tuesday, July 21, 2020 | History

2 edition of Geology of the Granites-Tanami Region, Northern Territory and Western Australia found in the catalog.

Geology of the Granites-Tanami Region, Northern Territory and Western Australia

D. H. Blake

Geology of the Granites-Tanami Region, Northern Territory and Western Australia

by D. H. Blake

  • 22 Want to read
  • 15 Currently reading

Published by Australian Govt. Pub. Service in Canberra .
Written in English

    Places:
  • Australia,
  • Northern Territory.,
  • Western Australia.
    • Subjects:
    • Geology -- Australia -- Northern Territory.,
    • Geology -- Australia -- Western Australia.,
    • Mines and mineral resources -- Australia -- Northern Territory.,
    • Mines and mineral resources -- Australia -- Western Australia.

    • Edition Notes

      Other titlesGranites-Tanami Region, Northern Territory and Western Australia.
      StatementD.H. Blake, I.M. Hodgson & P.C. Muhling.
      SeriesBulletin ;, 197, Bulletin (Australia. Bureau of Mineral Resources, Geology and Geophysics) ;, 197.
      ContributionsHodgson, I. M., Muhling, P. C. 1944-, Australia. Bureau of Mineral Resources, Geology and Geophysics.
      Classifications
      LC ClassificationsQE340 .A39 no. 197, QE343 .A39 no. 197
      The Physical Object
      Paginationvi, 91 p. :
      Number of Pages91
      ID Numbers
      Open LibraryOL1923698M
      ISBN 100642037299, 0642044465
      LC Control Number90135722

      Barkly Region Attractions: Karlu Karlu / Devils Marbles Conservation Reserve • One of the unique geological attractions in the Barkly Region is located in the Devils Marbles Conservation Reserve, approximately km north of Alice unique formation are known by the Indigenous name of Karlu Karlu (the Kaytetye name), or Karlwe Karlwe (the Warrumungu name). The Nabarlek uranium deposit, Northern Territory, Australia; some petrologic and geochemical constraints on genesis.

      of northern Australia. Conclusions The new zircon U-Pb ages, together with Nd• isotope model ages and whole-rock geochemistry, demonstrate the existence in The Granites• Tanami region of largely concealed late Archaean complexes. The exposed Archaean rocks are ves• tiges of basement terranes on which subsequent. Climbing Uluru. Uluru (Ayers Rock) is a deeply sacred place to the Indigenous Anangu climb was permanently closed on 26 October Rather than climbing Uluru, you can take the fascinating Ulu r u base walk instead. Start from Mala carpark in the morning while it's cool, take plenty of water and discover the diverse plants, and animals and geological features.

      The Tanami Desert, one of the most isolated and arid areas on earth, was not truly explored until well into the twentieth-Century. It is as far from the beaten track as you are likely to get and strictly the domain of the adventurous and well equipped four-wheel-driver. This accompanied geotour delivers a unifying interpretation of geology and landscape of Australia's Red Centre, highlighting as well a comprehensive overview of the region's natural and cultural led by a geologist or a self-guided option of a geotour in Central Australia: Outstanding geology and geomorphology highlights including Uluru, Kata Tjuta, Kings Canyon, and the.


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Geology of the Granites-Tanami Region, Northern Territory and Western Australia by D. H. Blake Download PDF EPUB FB2

Additional Physical Format: Online version: Blake, D.H., active Geology of the Granites-Tanami Region, Northern Territory and Western Australia. Geology of The Granites - Tanami region, Northern Territory and Western Australia / D.H.

Blake, I.M. Hodgson & P.C. Muhling Australian Government Publishing Service Canberra Wikipedia Citation Please see Wikipedia's template documentation for further citation fields that may be required.

Granites-Tanami region, Western Australia and Northern Territory and interregional correlations. BMR Journal of Australian Geology and Geophysics, 3: Blake, D.H., Hodgson, I.M. and Muhling, P.C, Geology of the Granites-Tanami region, Northern Territory and Western Australia.

Bureau of Mineral Resources (Geoscience Australia), Size: 2MB. Blake DH, Hodgson IM, Muhling PC () Geology of The Granites-Tanami Region, Northern Territory and Western Australia. Bureau of Mineral Resources Geology and Geophysics Bulletin Google ScholarCited by: Components.

Australia's geology can be divided into several main sections: the Archaean cratonic shields, Proterozoic fold belts and sedimentary basins, Phanerozoic sedimentary basins, and Phanerozoic metamorphic and igneous rocks. Australia as a separate continent began to form after the breakup of Gondwana in the Permian, with the separation of the continental landmass from the African.

The age peak of Ga in the Ranford Formation can be correlated with the Hooper Orogeny ( Ma) and Halls Creek Orogeny ( Ma) that induced multiple periods of deformation and.

Geology of The Granites-Tanami region, Northern Territory and Western Australia: Evaporites in Australia: The Exmouth Plateau: stratigraphy, structure and petroleum potential: The geology of the Fairfield Group, Canning Basin, Western Australia: A geological synthesis of Papua New Guinea: The Proterozoic and Palaeozoic rocks of The Granites-Tanami region, Western Australia and Northern Territory, and interregional correlations: Lithological correlations of Adelaidean glaciogenic rocks in parts of the Amadeus, Ngalia, and Georgina Basins: Neoproterozoic glaciogenic formations are preserved in the Kimberley region and northwestern Northern Territory of northern Australia.

They are distributed in the west Kimberley adjacent to the northern margins of the King Leopold Orogen, the Mt Ramsay area at the junction of the King Leopold and Halls Creek orogens, and east Kimberley, adjacent to the eastern margin of the Halls Creek Orogen.

ABM’s exploration projects are located in the broader Tanami Desert region of the Northern Territory. The Tanami project area is located in an area bounded on the western margin by the Northern Territory / West Australian border, north to Birrindudu and south to.

into this map. The main map available in W A side is the Geology of The Granites - Tanami Region ( ), which was published in by BMR and GSW. In the Northern Territory area, published 1: regional geological maps were used as references, however my own work in the region during to over rides the survey map.

In the present study involving Random Forest (RF)-based gold prospectivity modelling of the Tanami region, a greenfields terrain in Western Australia, we apply the Synthetic Minority Over-sampling. The Tanami Operations are located approximately km to the NW of Alice Springs in the Tanami Desert of the Northern Territory, Australia.

Gold was first discovered in the Tanami region inalthough the first significant deposit was not delineated until. 3 GEOLOGY The Granites-Tanami Goldfields lie in the eastern part of the Early Proterozoic Granites-Tanami Inlier, which is part of the Northern Australian Orogenic Province (Plumb, ).

The Inlier abuts the Arunta Complex to the south and east and is probably a continuation of the Halls Creek Orogen in Western Australia (Hendrickx, et al, ).

Western Australia (abbreviated as WA) is a state occupying the western per cent of the land area of Australia excluding external territories. It is bounded by the Indian Ocean to the north and west, and the Southern Ocean to the south, the Northern Territory to the north-east, and South Australia to the south-east.

Western Australia is Australia's largest state, with a total land area of. Plate 8, The Granites - Tanami [cartographic material] Australian/Harvard Citation.

Aerial, Geological and Geophysical Survey of Northern Australia.Map of western portion Central Australia showing topographical features. Plate 8, The Granites - Tanami [cartographic material] Wikipedia Citation. Stratabound, uraniferous diagenetic xenotime cements provide a minimum depositional age of 1,±3 Ma for the sedimentary Birrindudu Group in the Killi Killi Hills, Tanami Region in northern Australia.

The age of xenotime formation is broadly coeval with that recently proposed (1,–1, Ma) for uranium mineralisation in the unconformity-associated deposits of the Pine Creek Inlier.

Granites-Tanami Block: Northern Territory(8 Mb) Available from the Northern Territory Geological Survey: Oonagalabi( Mb) E S: Arunta Province: Maps from the Geological Survey of Western Australia. Australia - Australia - Geologic history: The earliest known manifestations of the geologic record of the Australian continent are billion-year-old detrital grains of zircon in metasedimentary rocks that were deposited from to billion years ago.

Based on that and other findings, the Precambrian rocks in Australia have been determined to range in age from about billion to Royalties Online System for Western Australian mineral and petroleum producers to electronically prepare, lodge and view royalty returns and production reports.

About Access; Interactive geological map () An interactive, GIS-based mapping system. Construct your own geological map and incorporate other mineral and petroleum exploration datasets including mines and mineral. The Musgrave Province covers an area of approximately km2, straddling the border between South Australia, the Northern Territory and Western Australia.

The oldest exposed rocks belong to the undifferentiated Birksgate Complex and consist of amphibolite to granulite facies, felsic and minor mafic gneisses with igneous intrusive, volcanic.Neoproterozoic glacigenic formations are preserved in the Kimberley region and northwestern Northern Territory of northern Australia.

They are distributed in the west Kimberley adjacent to the northern margins of the King Leopold Orogen, the Mt Ramsay area at the junction of the King Leopold and Halls Creek Orogens, and the east Kimberley, adjacent to the eastern margin of the Halls Creek Orogen.

The Tanami Gold Province encompasses nearlykm 2 from the central west of the Northern Territory and into north-eastern Western Australia (Huston et al., ). The region is highly prospective for Au mineralisation and hosts the Moz Callie Au-deposit (Cross et al., ) and other smaller deposits and prospects.