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...
| Main Authors: | , , , , , , , , , , , , |
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| Format: | Journal Article |
| Published: |
Macmillan Publishers Limited
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/30504 |