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RB 95/00021 Neoproterozoic depositional sequences and tectonics, eastern Officer Basin, South Australia.
The Officer Basin probably formed when the Gawler Craton collided westerly with the Yilgarn Craton during 1300-1000 Ma; the collision-faulted belt of the Fraser-Musgrave Orogen might form the basement of the Munyarai Trough in the eastern part of the...-
Document
Published: 01 Jun 1995
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Mount Chandler (Musgrave Ranges Project). Annual and final reports for the period 11/11/1996 to 10/11/1999.
Cu-Au-U prospects associated with shear zones and Kulgeran age granites have been identified in an area approximately 60 km north-west of Marla. Best assay results were obtained from the Indulkana Shear Zone, where rock chip sampling returned up to...-
Document
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Lineaments and circular structures, disrupted palaeodrainage, and Cainozoic reactivation of diapiric salt walls in the eastern Officer Basin.
There is no abstract created for this record-
Document
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Mount Mystery, Mount Alberga and Mount Gordon, eastern Officer Basin. Joint progress and final reports for the period 12/1/81 to 11/1/82.
TARGET: Base metal sulphides associated with evaporitic carbonates of the Cambrian Observatory Hill Formation, and sodium carbonate evaporite minerals (i.e. trona, natrite, etc.) in lacustrine sediments. EXPLORATION: Analysis of available drill core...-
Document
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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,
