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Zitai Formation

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This is an old revision of this page, as edited by Yobot (talk | contribs) at 19:05, 29 July 2011 (WP:CHECKWIKI error 22 fixes (category with space) + general fixes (BRFA 16) using AWB (7799)). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The Zitai Formation is a geological sequence of Middle Ordovician origin, that occurs along the southeastern edge of the Yangtze Platform in southern China. It is a purple-red limestone with a few interspersed yellow-green shale beds. It contains a fossil fauna dominated by trilobites and nautiloids.


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