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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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| Yayımlandı: | Sci Rep |
|---|---|
| Asıl Yazarlar: | , , , , , , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Publishing Group UK
2021
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| Konular: | |
| Online Erişim: | 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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