Amalgamation between the Yangtze and Cathaysia Blocks in South China: Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks

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Amalgamation between the Yangtze and Cathaysia Blocks in South China: Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks

South China was formed through the amalgamation of the Yangtze Block with the Cathaysia Block, but the timing of this amalgamation is controversial, ranging from Mesoproterozoic to Mesozoic. We report here SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu Group volcanic rock...

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Bibliographic Details
Main Authors:	Li, X., Li, W., Li, Zheng-Xiang, Lo, C., Wang, J., Ye, M., Yang , Y.
Format:	Journal Article
Published:	Elsevier Science BV 2009
Subjects:	U-Pb zircon age Geochemistry South China Nd-Hf isotopes Volcanic arc Neoproterozoic
Online Access:	http://hdl.handle.net/20.500.11937/7922

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