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...

Descrizione completa

Dettagli Bibliografici

Autori principali:	T. Shen, G. Wang, A. Replumaz, L. Husson, A. A. G. Webb, M. Bernet, P. H. Leloup, P. Zhang, G. Mahéo, K. Zhang
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	Wiley 2020-10-01
Serie:	Geochemistry, Geophysics, Geosystems
Soggetti:	dynamic topography Tibetan Plateau Kailas basin thermochronology surface uplift basin subsidence
Accesso online:	https://doi.org/10.1029/2020GC009078
Tags:	Aggiungi Tag Nessun Tag, puoi essere il primo ad aggiungerne!!