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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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: 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
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2016
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Article
Acesso em linha: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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