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No mafic layer in 80 km thick Tibetan crust
All models of the magmatic and plate tectonic processes that create continental crust predict the presence of a mafic lower crust. Earlier proposed crustal doubling in Tibet and the Himalayas by underthrusting of the Indian plate requires the presence of a mafic layer with high seismic P-wave veloci...
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| Izdano u: | Nat Commun |
|---|---|
| Glavni autori: | , , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Nature Publishing Group UK
2021
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| Teme: | |
| Online pristup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7886915/ https://ncbi.nlm.nih.gov/pubmed/33594060 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-021-21420-z |
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