Mantle-flow diversion beneath the Iranian plateau induced by Zagros’ lithospheric keel

Previous investigation of seismic anisotropy indicates the presence of a simple mantle flow regime beneath the Turkish-Anatolian Plateau and Arabian Plate. Numerical modeling suggests that this simple flow is a component of a large-scale global mantle flow associated with the African superplume, whi...

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Detalles Bibliográficos
Autores principales: Kaviani, Ayoub, Mahmoodabadi, Meysam, Rümpker, Georg, Pilia, Simone, Tatar, Mohammad, Nilfouroushan, Faramarz, Yamini-Fard, Farzam, Moradi, Ali, Ali, Mohammed Y.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7854601/
https://www.ncbi.nlm.nih.gov/pubmed/33531534
http://dx.doi.org/10.1038/s41598-021-81541-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7854601/
https://www.ncbi.nlm.nih.gov/pubmed/33531534
http://dx.doi.org/10.1038/s41598-021-81541-9

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