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《Sedimentary Facies and Palaeogeography》 1997-01
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Peng Huaming East China College of Geology  
The Cambrian strata referred to as a succession of dark marine carbonate sediments in Jiangshan,Zhejiang,consist of a transgressive facies sequence including the lagoon facies and shallow-marine platform facies.The present paper discusses the evolution and tectonic implications for regional palaeogeographic framework of the southeastern margin of the Zhejiang-Anhui Sea Basin on the basis of sedimentary facies in combination with regional geological data in the working area.
【CateGory Index】: P512.2
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