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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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Detalles Bibliográficos
Publicado en:Sci Rep
Autores principales: Legendre, Cédric P., Deschamps, Frédéric, Zhao, Li, Chen, Qi-Fu
Formato: Artigo
Lenguaje:Inglês
Publicado: Nature Publishing Group 2015
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Acceso en línea: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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