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RB 2020/00008 Gawler Craton Airborne Geophysical Survey Region 1A, Tallaringa North – Enhanced geophysical imagery and magnetic source depth models.
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
Document
Published: 01 Mar 2020
- ZIP,
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Geology of the Innamincka Dome with preliminary notes to accompany a geological 4-mile plan.
Discusses previous work (particularly of Jack in Geol Surv. of S.Aust. Bulletins, 11 and 14). Geology: Stratigraphy; the dome is capped by a few tens of feet of Tertiary. The Patchawarra Bore penetrated about 4,000 feet of Winton Formation and was...-
Document
Published: 01 Jan 1958
- ZIP
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RB 2020/00011 Gawler Craton Airborne Geophysical Survey Region 1B, Tallaringa South – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
Document
Published: 01 Apr 2020
- ZIP,
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Northern Gawler Province regional geology 3D Model (GOCAD version 1).
Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...-
Model
- ZIP,
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Northern Gawler Province regional geology 3D Model (3D pdf version 1)
Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...-
Model
- ZIP,
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (3D pdf version 1)
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (GOCAD version 1).
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
