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Geophysical interpretation of the central Olympic Cu-Au province 1:500 000 map

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Created 13/01/2025

Updated 13/01/2025

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The Olympic Cu-Au Province, of the eastern Gawler Craton, lies beneath the sedimentary sequences of the Stuart Shelf. Rocks of the basement are Late Archaean metamorphics, and the Proterozoic Donington Suite, Hutchison Group, Wallaroo Group, Hiltaba Suite granitoids and mafic intrusives, and the Gawler Range Volcanics. Except for parts of the Gawler Range Volcanics, none of the basement crops out and is covered by sequences exceeding 3 km thickness, in places. Interpretation of units and structures was via gravity and airborne magnetic data. Some geological calibration was done by checking exploration drill logs or by examining the core. When core was examined, petrophysical properties were measured and used to constrain the interpretation. Related products Geophysical interpretation of the central Olympic Cu-Au province - GIS Dataset

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Title Geophysical interpretation of the central Olympic Cu-Au province 1:500 000 map
Language eng
Licence Not Specified
Landing Page https://devweb.dga.links.com.au/data/dataset/b5f388e7-16cb-4b01-a13e-e7fa6fa9a996
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
Data Portal Data.gov.au