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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...
| Autores principales: | , , , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| 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 |