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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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| Publicado no: | Sci Rep |
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| Main Authors: | , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2021
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7854601/ https://ncbi.nlm.nih.gov/pubmed/33531534 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-021-81541-9 |
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