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The mesac Open Data Portal datasets contain detailed records of seismic surveys and geochemical data, and they are made available here to industry, researchers and the public.
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TYPE OF RECORD

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CATEGORY TYPE

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  • Mineral Resources (Excl. Energy Resources) - (2)
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    • Primary Mining And Extraction Of Mineral Resources - (1)
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DOCUMENT TYPE

  • Departmental Publication - (1)
    • Geological Survey Geoscience Publication - (1)
  • Mineral Company Report - (1)
    • Mineral Exploration - (1)

COMMODITY

  • uranium - (2)
  • base metal - (1)
  • coal - (1)
  • Critical minerals - (1)
  • diamond - (1)
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  • iron - (1)
  • iron ore - (1)
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  • precious metal - (1)

GEOLOGICAL PROVINCE

  • Murray Basin - (2)
  • Eromanga Basin - (1)
  • Frome Embayment - (1)
  • Renmark Trough - (1)

STRATIGRAPHY

  • Blanchetown Clay - (1)
  • Bookpurnong Formation - (1)
  • Buccleuch Formation - (1)
  • Ettrick Formation - (1)
  • Finniss Formation - (1)
  • Loxton Sand - (1)
  • Mannum Formation - (1)
  • Murray Group - (1)
  • Parilla Sand Member - (1)
  • Renmark Group - (1)
  • Winnambool Formation - (1)

FORMAT

  • PDF - (1)

UPDATE FREQUENCY

There are no UPDATE FREQUENCY that match this search

PUBLICATION DATE

Specific date: 1980, 20/04/1980, 04/1980

Date range: 1980-2022, 04/1980-08/1990

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2 records found

Category type: Seismology And Seismic Exploration Commodity: Uranium Geological province: Murray Basin

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  • Cronje Dam and Oak Bank Outstation (the Cronje Dam Sedimentary Uranium Project). Annual and joint annual reports, plus final report at remaining licence's expiry/full surrender, for the period 20/10/2005 to 1/11/2014.

    An area comprised of three separate sub-blocks generally located ~60 km south of Manna Hill and ~70 km south-southeast of Olary has been explored for Tertiary sedimentary uranium which may have formed in buried north to south trending palaeochannels...
      Document
    • PDF
  • RB 2003/00013 North-western Murray Basin geological synthesis, South Australia.

    The Murray Basin is an intracratonic basin filled with Cainozoic fluvial to shallow marine sediments. Deposition in the Eocene and early Oligocene was characterised by floodplain and swamp deposits, emplaced with occasional interbeds of shelly clays...
      Document Published: 01 Aug 2003
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