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RB 2006/00001 Guide to the sedimentary cover of the central Gawler Craton, South Australia
The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...-
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Published: 01 Jan 2006
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RB 2007/00008 CHILDARA, South Australia, [geological map] sheet SH53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The CHILDARA 1:250 000 map area is located on the western Gawler Craton, an ancient crystalline shield comprising Archaean, Palaeoproterozoic and Mesoproterozoic metasediments, volcanics and granites that has been tectonically stable since 1450 Ma...-
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Published: 01 May 2007
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ExpNotes BARTON: Explanatory Notes BARTON
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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RB 2022/00011 Eucla Basin and peripheral paleovalleys.
The Cenozoic Eucla Basin is located on the southern margin of the Australian continent, with a present-day basin onshore edge which extends for over 2,000 km from Western Australia into South Australia. The basin’s sediment fill comprises a thin...-
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Published: 01 Nov 2022
