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RB 80/00079 Lithologies and interpretations of the Observatory Hill Beds, Marla 1A and 1B.
A detailed description and interpretation of the carbonate lithologies present in drill cores recovered from two recently completed SADME stratigraphic wells have revealed that the Observatory Hill Beds in the Marla area were deposited in a shallow...-
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Published: 01 May 1980
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RB 99/00031 Assessment of zinc-lead prospectivity on the Murnaroo Platform and in the Manya Trough, eastern Officer Basin, South Australia.
The Neoproterozoic to Palaeozoic Officer Basin is located on and adjacent to the northwestern margin of the Gawler Craton. Deposition of the basin began in Adelaidean time, before and during the breakup of the supercontinent Rodinia. The...-
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Published: 01 Dec 1999
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Sedimentology and petroleum geochemistry of the Ouldburra Formation, eastern Officer Basin, Australia.
Deposition of the Early Cambrian Ouldburra Formation, a mixed siliciclastic/carbonate, marine carbonate and evaporite succession, occurred in the shallow marine setting of the Manya Trough. The observed variations between the facies are interpreted...-
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Sedimentology of the Ouldburra Formation (Early Cambrian), northeastern Officer Basin.
The Ouldburra Formation (Early Cambrian) is a newly defined sequence of carbonates, mixed carbonate/siliciclastics and evaporites in the northeastern Officer Basin, northern South Australia. Deposition took place during the late stages of...-
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North-eastern Officer Basin area. Progress reports and final report to licences' joint full surrender, for the period 20/8/1980 to 8/11/1986.
Exploration for trona and base metals was centred on the Marla region. Work included regional gravity and magnetic studies, acquisition of airborne magnetic and multi-channel radiometric data, with follow-up ground magnetic and gravity surveys,...-
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RB 2004/00012 Deposition and chemical composition of Early Cambrian salt in the eastern Officer Basin, South Australia
In South Australia, Cambrian massive salt deposits of the eastern Officer Basin occur in troughs lying along the western and north-western margins of the Gawler Craton, and are considered to have been deposited in marginal to open marine environments....-
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Published: 01 Jul 2004
