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
|PDF - Full text restricted - Requires a PDF viewer|
Official URL: http://dx.doi.org/10.1016/j.precamres.2008.05.008
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.
|Additional Information:||The definitive version is available at http://www.sciencedirect.com|
Volcanic rifted margins|
|Deposited By:||Ms June Pongratz|
|Deposited On:||07 Sep 2010 12:54|
|Last Modified:||07 Sep 2010 12:54|
|ePrint Statistics:||View statistics for this ePrint|
Repository Staff Only: item control page