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RB 60/00051 Stratigraphy and micropalaeontology of three deep bores, Hd Port Gawler.
Three relatively deep bores, drilled recently on the northern Adelaide Plains in the Hundred of Port Gawler, about 20 miles north of Adelaide, have intersected useful complementary sections of the Cainozoic succession, ranging from 560 feet to 1148...-
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Published: 15 Mar 1965
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RB 94/00009 Soils, stratigraphy and engineering geology of near surface materials of the Adelaide Plains.
Metropolitan Adelaide is founded on a wide variety of soils that overlie sediments and rocks. Some of the soils and sediments react to seasonal and human-induced changes in water content with marked changes in volume. The black earths and...-
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Published: 01 Jul 1996
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RB 66/00999 Palaeontological examination of material collected from three sand-producing water wells situated between Angle Vale and Gawler.
There is no abstract created for this record-
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Published: 29 Feb 1972
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RB 64/00073 Foraminifera and stratigraphy of the type section of Port Willunga Beds, Aldinga Bay.
The type section 20 miles (32 km) south of Adelaide has been re-examined. Comprising about 107 feet (32½ m) of bryozoal calcarenitic impure limestones, sands, silts, and clays, it is informally subdivided into three apparently conformable successions...-
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Published: 01 Jan 1967
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RB 70/00192 Port Willunga Beds in the Port Noarlunga-Seaford area.
A thickness of approximately 112 feet of Port Willunga Beds is exposed in coastal outcrops and is comparable with the type-section at Port Willunga. The age as determined by planktonic foraminifera, ranges from Upper Eocene to middle Oligocene. An...-
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Published: 07 Dec 1970
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RB 72/00190 Two Cainozoic fossiliferous sands from Waterloo Bay, Yorke Peninsula, SA, Hd Melville, Co. Fergusson.
One sand has benthonic foraminifera of Upper Eocene age, and is referred to Rogue Formation, correlating also with basal Port Willunga Beds. The other sand is from a Pleistocene "aeolianite" sequence, Bridgewater formation. Its microfauna, mostly...-
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Published: 02 Oct 1972