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Rayleigh-wave dispersion reveals crust-mantle decoupling beneath eastern Tibet

The Tibetan Plateau results from the collision of the Indian and Eurasian Plates during the Cenozoic, which produced at least 2,000 km of convergence. Its tectonics is dominated by an eastward extrusion of crustal material that has been explained by models implying either a mechanical decoupling bet...

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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Legendre, Cédric P., Deschamps, Frédéric, Zhao, Li, Chen, Qi-Fu
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2015
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC4637932/
https://ncbi.nlm.nih.gov/pubmed/26548657
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep16644
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