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RB 2018/00026 Sedimentology of the late Palaeozoic Cape Jervis Formation, Troubridge Basin, South Australia.
The late Palaeozoic Cape Jervis Formation of the Troubridge Basin in southern South Australia provides a sedimentological record of the glacial environment during the Permo-Carboniferous glaciation. The sedimentary sequence is divided into five...-
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Published: 01 Nov 2018
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RB 64/00041 Permian deposits of South Australia and their fauna.
Lower Permian sediments occur in all the main sedimentary basins of South Australia. The Cape Jervis Beds are described, and the Lake Phillipson Beds and Stuart Range Beds formally named. In general, the formations follow a sequence of boulder clay...-
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Published: 01 Jan 1967
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RB 71/00120 Permian and reworked Devonian microfossils from the Troubridge Basin.
Data, on numerous Permian samples from the Troubridge Basin, prepared for foraminifera and acid-resistant microfossils, are listed. By far the most important is a dark grey clay from Waterloo Bay, Yorke Peninsula, in which were found foraminifera...-
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Published: 29 Jul 1971
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RB 2004/00021 Palynostratigraphy of the sediments from Meadows Bore 1, Meadows Basin, and other diamond exploration sites from Adelaide Hills, South Australia.
Palynological analyses of samples from Meadows Bore 1 indicate the presence of Late Miocene to Early Pliocene sediments, correlated with the Monotocidites galeatus Zone. At the base of the Tertiary interval examined it appears that a wet rainforest...-
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Published: 01 Oct 2004
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RB 2001/00017 TER 001, Yorke Peninsula. Well completion report.
Drillhole TER 1, funded by the TEISA program, was drilled to test basement depth and stratigraphy to the west of Minlaton, Yorke Peninsula. This drilling project followed TEISA aeromagnetic and geological surveys of the Peninsula in 1999, which had...-
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Published: 01 Nov 2001
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A new geological map of Hallett Cove.
Hallett Cove is one of South Australia’s foremost natural science treasures. Exposed examples for prime geological concepts of superposition of strata, depositional unconformities (representing time breaks), and folding and faulting of sedimentary...-
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