Miocene Subsidence and Surface Uplift of Southernmost Tibet Induced by Indian Subduction Dynamics

Abstract The Indus‐Yarlung suture of southernmost Tibet marks the initial collisional zone, the ongoing India‐Asia collision, and yet more than ~30 million years after the onset of collision, a thick detrital sedimentary unit was deposited just north of the suture: the Kailas Formation. The mechanis...

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Xehetasun bibliografikoak

Egile Nagusiak:	T. Shen, G. Wang, A. Replumaz, L. Husson, A. A. G. Webb, M. Bernet, P. H. Leloup, P. Zhang, G. Mahéo, K. Zhang
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Wiley 2020-10-01
Saila:	Geochemistry, Geophysics, Geosystems
Gaiak:	dynamic topography Tibetan Plateau Kailas basin thermochronology surface uplift basin subsidence
Sarrera elektronikoa:	https://doi.org/10.1029/2020GC009078
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