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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Enregistré dans:
Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: 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
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group 2016
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Article
Accès en ligne: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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