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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
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RB 2018/00036 Regional geochemistry of the Coompana area.
The Coompana area is characterised by several thick basin cover sequences dominantly composed of limestone, and forms the topographically flat Nullarbor Plain. Consequently, this region was previously considered too challenging for mineral...-
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Published: 01 Oct 2018
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RB 2015/00029 What lies beneath the western Gawler Craton? [Eucla-Gawler Seismic Survey line] 13GA-EG1E Seismic and Magnetotelluric Workshop 2015. Extended abstracts [of technical presentations].
This compilation of written and associated oral papers that were presented for the “What lies beneath the western Gawler Craton? 13GA-EG1E Seismic and Magnetotelluric Workshop 2015” is an important step in building our geological understanding of one...-
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Published: 01 Dec 2015
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RB 2023/00043 Remapping the paleovalley systems of the central-western Gawler Craton, South Australia.
The Geological Survey of South Australia’s (GSSA) Gawler Challenge Phase 2: next generation mineral systems mapping (GP2) program allowed the authors of this report to revisits some ground-breaking landscape evolution studies with new geophysical data...-
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Published: 01 Dec 2023
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Bull 055 A geochronological framework for the Gawler Craton, South Australia
This bulletin contains geochronological data and interpretations from the Gawler Craton of South Australia that have been completed by Mark Fanning of The Australian National University, by Geological Survey of South Australia personnel, and by...-
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