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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4912662/
https://www.ncbi.nlm.nih.gov/pubmed/27307135
http://dx.doi.org/10.1038/ncomms11888

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4912662/
https://www.ncbi.nlm.nih.gov/pubmed/27307135
http://dx.doi.org/10.1038/ncomms11888

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