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- W4386329632 abstract "Although the Himalayan-Tibetan orogen is a result of compressional tectonics, the orogen also hosts active rifts accommodating east-west extension orthogonal to the north-south India-Asia convergence. In this study we address the question of how the north-trending rifts were formed by conducting high-resolution seismic imaging survey across southeastern Tibet where the Cona rift is exposed. Our work shows that the crustal structures of this youngest rift in southern Tibet was constructed by multiple-scale structures that are decoupled with depth and long rift trend. We suggest this deformation style to have resulted from eastward extrusion of the middle and upper crust with increasing speeds to the north towards the Yarlunbg-Zangpo suture. The differential eastward extrusion in turn may have contributed to the formation and evolution of the eastern Himalayan syntaxis." @default.
- W4386329632 created "2023-09-01" @default.
- W4386329632 creator A5008395330 @default.
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- W4386329632 creator A5053456065 @default.
- W4386329632 creator A5070606956 @default.
- W4386329632 creator A5083280670 @default.
- W4386329632 date "2023-08-30" @default.
- W4386329632 modified "2023-09-28" @default.
- W4386329632 title "Lithospheric structures of the eastern Himalayas as revealed by receiver function analysis" @default.
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