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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Detaylı Bibliyografya
Yayımlandı:Nat Commun
Asıl Yazarlar: 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
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group 2016
Konular:
Article
Online Erişim: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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