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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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Source rock evaluation of 2 Cambrian drillhole samples from wells (Amoco-Duval) KD-2A and (Getty) Yarle Lakes 1, Officer Basin, South Australia.
There is no abstract created for this record-
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Published: 28 Apr 1986
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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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Guide to the lithofacies of the Ouldburra Formation.
The Ouldburra Formation is the lower of 2 major carbonate units in the NE Officer Basin. It is essentially an Early Cambrian shallow marine / epeiric sea sequence, underlain by the Murnaroo Formation and overlain by the Observatory Hill Formation....-
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Petrographic study of the Ouldburra Formation.
This report presents over 500 thin section descriptions from cored Ouldburra Formation rocks lying within the PEL 23 area. The work forms an integral part of an on-going study of the sedimentology of the Ouldburra Formation and its possible...-
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Results of base metal analyses on 8 selected drill core samples taken from the Cambrian Ouldburra Formation in wells Wilkinson 1 and Marla 1b.
There is no abstract created for this record-
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Published: 19 Mar 1980
