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Oblique convergence and strain partitioning in the outer deformation front of NE Himalaya
Himalayan-Tibetan orogeny has considered as a natural black box in the context of geodynamic evolution and tectonic complexity. The eastward extrusion model of Tibetan crust contradicts with the oblique convergence model in the NE-Himalaya (Bhutan/Arunachal region), where the overall convergence rat...
Autores principales: | Panda, Dibyashakti, Kundu, Bhaskar, Santosh, M. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6043504/ https://www.ncbi.nlm.nih.gov/pubmed/30002418 http://dx.doi.org/10.1038/s41598-018-28774-3 |
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