Article ID Journal Published Year Pages File Type
4724251 Precambrian Research 2008 14 Pages PDF
Abstract
In this paper, we review the 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.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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