SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block

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SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block

It has been generally accepted that the South China Block was formed through amalgamation of the Yangtze and Cathaysia Blocks during the Proterozoic Sibaoan orogenesis, but the timing and kinematics of the Sibao orogeny are still not well constrained. We report here SHRIMP U–Pb zircon geochronologic...

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Bibliographic Details
Main Authors:	Ye, M., Li, X., Li, W., Liu, Y., Li, Zheng-Xiang
Format:	Journal Article
Published:	International Association for Gondwana Research 2007
Subjects:	Magmatic arc Geochemistry Rodinia Granitoids South China SHRIMP U–Pb zircon age Neoproterozoic
Online Access:	http://hdl.handle.net/20.500.11937/15529

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