Partial melting of thickened continental crust in central Tibet: Evidence from geochemistry and geochronology of Eocene adakitic rhyolites in the northern Qiangtang Terrane

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Partial melting of thickened continental crust in central Tibet: Evidence from geochemistry and geochronology of Eocene adakitic rhyolites in the northern Qiangtang Terrane

The composition of the deep crust is a key to understanding the formation of the low-velocity zone in the middle to lower crust of the Tibetan Plateau. The Suyingdi rhyolites exposed in the northern Qiangtang Terrane have high Sr (296–384 ppm) and low Y (5.81–7.93 ppm), with therefore high Sr/Y rati...

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Bibliographic Details
Main Authors:	Long, X., Wilde, Simon, Wang, Q., Yuan, C., Wang, Xuan-Ce, Li, J., Jiang, Z., Dan, W.
Format:	Journal Article
Published:	Elsevier 2015
Online Access:	http://hdl.handle.net/20.500.11937/11384

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