Age and origin of high Ba-Sr appinite-granites at the northwestern margin of the Tibet Plateau: implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt

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Age and origin of high Ba-Sr appinite-granites at the northwestern margin of the Tibet Plateau: implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt

The Buya appinite-granite is a typical high Ba-Sr granite emplaced at the northern West Kunlun orogenic belt along the northwestern margin of the Tibetan Plateau. The granite is dated at ca. 430 Ma using the SHRIMP U-Pb zircon method. It consists of alkaline feldspar granites with coeval appinite en...

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Bibliographic Details
Main Authors:	Ye, H-M., Li, X-H., Li, Zheng-Xiang, Zhang, C-L.
Format:	Journal Article
Published:	Elsevier Science BV 2008
Subjects:	Tectonic implications Petrogenesis Geochemistry Buya high Ba-Sr appinite-granite West Kunlun orogenic belt Geochronology
Online Access:	http://hdl.handle.net/20.500.11937/45509

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