Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite

Southern Tibet is the most active orogenic region on Earth where the Indian Plate thrusts under Eurasia, pushing the seismic discontinuity between the crust and the mantle to an unusual depth of ~80 km. Numerous earthquakes occur in the lower portion of this thickened continental crust, but the trig...

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Detalles Bibliográficos
Autores principales: Shi, Feng, Wang, Yanbin, Yu, Tony, Zhu, Lupei, Zhang, Junfeng, Wen, Jianguo, Gasc, Julien, Incel, Sarah, Schubnel, Alexandre, Li, Ziyu, Chen, Tao, Liu, Wenlong, Prakapenka, Vitali, Jin, Zhenmin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6113232/
https://www.ncbi.nlm.nih.gov/pubmed/30154406
http://dx.doi.org/10.1038/s41467-018-05964-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6113232/
https://www.ncbi.nlm.nih.gov/pubmed/30154406
http://dx.doi.org/10.1038/s41467-018-05964-1

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