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RB 92/00006 Southeastern margin of the Gawler Craton.
The Cygnet-Snelling Fault Zone on Kangaroo Island is a fundamental structure that both influenced sedimentation during the Cambrian, and refined the boundary between major tectonic provinces during the Delamerian Orogeny. It is coincident with the...-
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Published: 01 Jan 1992
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RB 92/00001 Geological and geomorphological framework of Kangaroo Island.
The framework of Kangaroo Island was largely established during the Cambrian, when widespread marine sedimentation resulted in thick accumulations of shallow shelf to deep marine terrigenous sediments. Orogenesis has deformed the strata into an...-
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Published: 01 Jan 1992
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RB 92/00002 Geophysical appraisal of northern Kangaroo Island.
Crystalline basement of the Gawler Craton continues further southwards than previously interpreted, extending under northern Kangaroo Island. Depths to basement range from 200 metres near Emu Bay, and approximately 250-750 metres inland from Cape...-
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Published: 01 Jan 1992
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Interim report on the lower Cambrian stratigraphy of Kangaroo Island, SA.
There is no abstract created for this record-
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Published: 01 Jan 1966
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Cambrian source rock geochemistry, Stansbury Basin, part 3. Thermal maturity of Early Cambrian Mount McDonnell Formation in Investigator 2, northern Kangaroo Island.
5 drillcore samples of Early Cambrian Mount McDonnell Formation shallow marine mudstone intersected by SADME stratigraphic drillhole Investigator 2 on Kangaroo Island between 139 and 505 metres depth KB were analysed geochemically to determine their...-
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Cambrian source rock geochemistry, Stansbury Basin, part 1. Preliminary evaluation of Mount McDonnell Formation in coastal exposures on northern Kangaroo Island.
17 samples of Early Cambrian Mount McDonnell Formation shallow marine mudstone outcropping on the northern coastline of Kangaroo Island near Hummocky Point were analysed geochemically to determine their source rock richness and thermal maturity, and...-
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