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Southern Tibetan rifting since late Miocene enabled by basal shear of the underthrusting Indian lithosphere
Syncontractional extension is prominent in present-day Tibet, but its origin remains vigorously debated. Several deep-seated geodynamic processes (e.g., Indian underthrusting, horizontal flow, and mantle upwelling) have been linked to Tibetan rifting. Indian underthrusting is a good candidate becaus...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10160080/ https://www.ncbi.nlm.nih.gov/pubmed/37142610 http://dx.doi.org/10.1038/s41467-023-38296-w |