Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4724251 | Precambrian Research | 2008 | 14 Pages |
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
Authors
N.G. Direen, J.B. Jago,