Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow

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Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow

There is considerable controversy over the nature of geophysically recognized low-velocity-high-conductivity zones (LV-HCZs) within the Tibetan crust, and their role in models for the development of the Tibetan Plateau. Here we report petrological and geochemical data on magmas erupted 4.7-0.3 Myr a...

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Bibliographic Details
Main Authors:	Wang, Q., Hawkesworth, C., Wyman, D., Chung, S., Wu, F., Li, X., Li, Zheng-Xiang, Gou, G., Zhang, X., Tang, G., Dan, W., Ma, L., Dong, Y.
Format:	Journal Article
Published:	Macmillan Publishers Limited 2016
Online Access:	http://hdl.handle.net/20.500.11937/30504

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