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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Gepubliceerd in:Nat Commun
Hoofdauteurs: Wang, Qiang, Hawkesworth, Chris J., Wyman, Derek, Chung, Sun-Lin, Wu, Fu-Yuan, Li, Xian-Hua, Li, Zheng-Xiang, Gou, Guo-Ning, Zhang, Xiu-Zheng, Tang, Gong-Jian, Dan, Wei, Ma, Lin, Dong, Yan-Hui
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Nature Publishing Group 2016
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Article
Online toegang:https://ncbi.nlm.nih.gov/pmc/articles/PMC4912662/
https://ncbi.nlm.nih.gov/pubmed/27307135
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms11888
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