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Brief petrology of bottomhole rock samples from Apollo no. 1 and Gemini no. 1 offshore wells, Great Australian Bight, and comparison with outcropping rocks from onshore Eyre Peninsula.
Two drill cuttings samples from 2842 and 2860 feet depth KB in Apollo 1 (economic basement) were examined for their heavy mineral composition as an aid to stratigraphic correlation with Precambrian sediments found in the adjacent onshore. The well...-
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Published: 23 Dec 1975
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RB 2002/00007 The Palaeo-Mesoproterozoic geology of northern Yorke Peninsula, South Australia. Hiltaba Suite - related alteration and mineralisation of the Moonta - Wallaroo Cu-Au district (Resources '96 Convention, Adelaide, geological field excursion
Returns from copper and gold won from the Moonta-Wallaroo district supported the South Australian economy from 1860-1920. During those 60 years some 355,000 t of copper and 2 t of gold were extracted from the twin mining fields of Wallaroo and Moonta:...-
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Published: 01 Nov 1996
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RB 90/00001 Explanatory Notes for the KIMBA 1:250 000 geological map.
The KIMBA 1:250 000 geological map sheet (hereafter referred to as KIMBA) lies in central Eyre Peninsula, extending between latitudes 33° to 34° S and longitudes 135° to 136°30'E (Fig 1). The principal towns are Kimba and Cleve, with smaller towns at...-
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Published: 01 Dec 1989
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RB 2008/00003 The Corunna Conglomerate, Gawler Craton: a review of the sedimentology and new U-Pb zircon geochronology.
The Corunna Conglomerate is a sequence of unmetamorphosed fluvial to shallow marine sediments, comprising conglomerates, sandstones and siltstones, which were deposited in active fault grabens in the eastern Gawler Craton. It is found on the...-
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Published: 01 Apr 2008
