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The Flinders Ranges breccias of South Australia diapirs or décollement?
Division of Mineral Physics, C.S.I.R.O.
Geology Department, La Trobe University, Bundoora.
1977 (English)In: Journal of the Geological Society, ISSN 0016-7649, E-ISSN 2041-479X, Vol. 134, no 3, p. 363-384Article in journal (Refereed) Published
Abstract [en]

Breccia-cored domes in the Northern Flinders Ranges, South Australia, have been regarded as diapirs analogous to diapiric salt structures in northwestern Germany and the Gulf Coast. It is shown that the core of the Blinman Dome is not intrusive and is not composed of less dense rocks; hence a diapiric process cannot apply. It is suggested that much of the breccia of the core is formed by deformation of a stratigraphic unit composed of interbedded competent and incompetent beds at a Flinders Ranges dgcollernent and results from folding. If this model is correct, the Flinders Ranges structures should occur at ddcollements in other parts of the world.

Place, publisher, year, edition, pages
1977. Vol. 134, no 3, p. 363-384
National Category
Other Civil Engineering
Research subject
Mining and Rock Engineering
Identifiers
URN: urn:nbn:se:ltu:diva-4034DOI: 10.1144/gsjgs.134.3.0363Local ID: 1e514569-75f8-46e7-a3fd-8fa1c4ddfb34OAI: oai:DiVA.org:ltu-4034DiVA, id: diva2:976896
Note
Godkänd; 1977; 20120104 (andbra)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2017-11-21Bibliographically approved

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