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The Cottons Breccia (Ediacaran) and its tectonostratigraphic context within the Grassy Group, King Island, Australia: A rift-related gravity slump deposit
Direen, NG and Jago, JB (2008) The Cottons Breccia (Ediacaran) and its tectonostratigraphic context within the Grassy Group, King Island, Australia: A rift-related gravity slump deposit. Precambrian Research, 165 (1-2). pp. 1-14. ISSN 0301-9268
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The Cottons Breccia is part of the upper Neoproterozoic (Ediacaran: 586–572 Ma) Grassy Group, exposed
on King Island, Tasmania. This formation has been widely interpreted as an unambiguous tillite, in support
of tectono-climatic models that invoke catastrophic latest Neoproterozoic global glaciation. However,
dissenting opinions interpret the Cottons Breccia as a tectonic breccia.
In this paper,we reviewthe tectonostratigraphy of the Cottons Breccia, and the enclosing Grassy Group.
We find no unambiguous evidence for a direct glacial origin, as postulated by some early workers. An
interpretation of the Cottons Breccia as a deposit within half-graben in the shoulder regions of an actively
developing latest Neoproterozoic volcanic rifted margin is consistent with all the available sedimentological,
structural, geochronological, and tectonic evidence.
|Keywords:||Neoproterozoic glaciations Palaeogeography Tasmania Tectonostratigraphy Volcanic rifted margins|
|Journal or Publication Title:||Precambrian Research|
|Page Range:||pp. 1-14|
|Identification Number - DOI:||10.1016/j.precamres.2008.05.008|
The definitive version is available at http://www.sciencedirect.com
|Date Deposited:||07 Sep 2010 02:54|
|Last Modified:||18 Nov 2014 04:12|
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