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Bull 047 The Sedimentology of the Cambrian Wirrealpa and Aroona Creek Limestones
The Wirrealpa and Aroona Creek Limestones are early Middle Cambrian formations which crop out in the Flinders Ranges of eastern South Australia. They are up to 140 m thick and are underlain and overlain conformably by thick red bed sequences. This...-
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RB 2002/00024 Sequence analysis and petroleum potential in the Arrowie Basin, South Australia.
Cambrian sediments in the Arrowie Basin were deposited on a rifted continental margin. Four distinct depositional regimes, ranging from a western, tectonically stable shelf, through platform-ramp to eastern slope and trough-synclines, can be...-
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Published: 01 Feb 2003
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Curnamona Homestead. Progress and technical reports to licence expiry/renewal, for the period 1/1/1969 to 31/12/1970.
Reconnaissance shallow stratigraphic drilling with subsequent borehole geophysical electric and radioactivity logging in the south-western Frome Embayment (21 rotary mud partly cored holes, total 8841 feet), over areas lying adjacent to outcropping...-
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Published: 31 Dec 1970
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RB 2002/00033 Correlation within Early Palaeozoic basins of eastern South Australia.
The great majority of lower Palaeozoic rocks in the Stansbury, Arrowie and Warburton Basins are of Cambrian age, although a few Early Ordovician fossils have been reported from drillholes in the sub-surface Warburton Basin. The Cambrian is the only...-
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Published: 01 Dec 2002
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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