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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...

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Detalles Bibliográficos
Autores principales: Panda, Dibyashakti, Kundu, Bhaskar, Santosh, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
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