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RB 49/00102 Stratigraphy of the Murray Basin in South Australia.
The Murray Basin is an area of Mesozoic and Tertiary sedimentation divided into two main units the Murray Basin proper separated by structural highs, the Padthaway “Horst”, from the Gambier Sunklands. Knowledge of the Mesozoic in the Murray Basin...-
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Published: 05 Oct 1959
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RB 91/00054 Early Oligocene and Late Eocene age determined for core samples from a borehole near Mundulla.
4 samples of drill core from a groundwater investigation well located approximately 6.5 km north-west of Mundulla were examined palaentologically to evaluate whether the Tertiary Murray Basin sediments that were cored can be correlated with similar...-
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Published: 10 May 1991
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Bull 036 Stratigraphy of the Murray Basin in South Australia
This publication details the stratigraphy of the Murray Basin Province of South Australia. The work leading up to this report has played a major part in the understanding of the sedimentary succession of this important basin-area of the State. The...-
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RB 00713 Donna 1. Subsurface stratigraphy and micropalaeontological study.
Donna 1 well intersected 500 feet of Tertiary sediments and 1800 feet of Permian sands before drilling was suspended at 2300 feet. The formation at this level is presumed to be of Permian age, while the siliceous limestone cored between 2073 and 2078...-
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Published: 31 Jan 1900
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RB 66/00047 Groundwater supplies at Keith and its surroundings. Progress report no. 6, micropalaeontological examination of bores, Hds Stirling and Laffer.
Foraminifera and stratigraphy of four water bores in the Hundred of Stirling and one bore in the Hundred of Laffer have been examined. The total thickness of the Cainozoic sequence to bedrock, proved in two bores, varies from 398 feet near Emu Flat, 4...-
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Published: 01 Jan 1968
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RB 76/00006 Foraminiferal biostratigraphy of Department of Mines borehole STR-2, Keith area.
STR-2, on the Padthaway Ridge, near Monster Mount, Keith district, penetrated a Cainozoic sequence approximately 88 m thick resting on bed-rock of weathered quartz-feldspar porphyry. ?Coomandook Formation (8-28 m, ?Early Pleistocene) 1s distinguished...-
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Published: 27 Jan 1976
