Cyclic late Katian through Hirnantian glacioeustasy and its control of the development of the organic-rich Wufeng and Longmaxi shales, South China
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DOI: 10.1016/j.palaeo.2019.04.012
Abstract: Abstract Deposition of the organic-rich shales of the Wufeng and lowermost Longmaxi formations (late Katian through Hirnantian) occurred in a relatively stable tectonic setting and commenced at approximately 4.5 Myr prior to the end-Ordovician glacial maximum.… read more here.
Keywords: katian hirnantian; wufeng; rich shales; organic rich ... See more keywords