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RB 82/00001 Supergroup classification in the Adelaide Geosyncline.
The term Adelaide Geosyncline is still appropriate and does not prejudice its interpretation in terms of modern tectonic theory. 3 new supergroups are proposed. The early Adelaidean Warrina Supergroup combines the Callanna Group and Burra Group, while...-
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Published: 01 Feb 1982
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RB 99/00006 Adelaide Geosyncline of South Australia and its significance in Neoproterozoic continental reconstruction.
The Adelaide Geosyncline is a deeply subsident Neoproterozoic to Middle Cambrian basin complex in South Australia with a record of at least five major successive rift cycles. Each rift system has its own locus and orientation. Although the rift...-
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Published: 01 Mar 1999
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AMIRA Project P544: Proterozoic sediment-hosted copper deposits. Quarterly progress reports and final report for the period July 2000 to October 2003.
The original objectives of this project were: 1) To understand the processes responsible for transporting, concentrating and fixing copper and other ore constituents during sedimentary basin evolution 2) To document the various stages and paragenesis...-
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Data release - as updated : Willouran Ranges. Annual reports to licence expiry/full surrender, for the period 17/1/2012 to 16/1/2022.
An area covering most of the Willouran Ranges has been explored for possible economic buried epigenetic or sediment-hosted copper mineralisation that may have formed within the Proterozoic bedrock. Both primary and secondary copper targets were...-
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Published: 23 Mar 1922
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Bull 053 The Adelaide Geosyncline: Later Proterozoic Stratigraphy, Sedimentation, Pataeontology and Tectonics
The extremely thick succession provides one of the most complete sedimentary records for the Late Proterozoic. The term geosyncline is used in a non-genetic sense for the basin in which deposition occurred during the Adelaidean and Cambrian. Only the...-
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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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