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Localized foundering of Indian lower crust in the India–Tibet collision zone
The deep structure of the continental collision between India and Asia and whether India’s lower crust is underplated beneath Tibet or subducted into the mantle remain controversial. It is also unknown whether the active normal faults that facilitate orogen-parallel extension of Tibetan upper crust...
Uloženo v:
| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2020
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7547243/ https://ncbi.nlm.nih.gov/pubmed/32958679 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2000015117 |
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