The Cenozoic Multiple-Stage Uplift of the Qiangtang Terrane, Tibetan Plateau

The Cenozoic Multiple-Stage Uplift of the Qiangtang Terrane, Tibetan Plateau

Cenozoic collision between the Indian and Asian continents is generally considered as the main driver forming the high Tibetan Plateau (TP). However, it remains hotly debated when and how the relatively flat and highly elevated TP was formed. Here, we present combined analyses of the apatite fission...

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Bibliographic Details
Main Authors: Zhongbao Zhao, Haijian Lu, Shiguang Wang, Haibing Li, Chao Li, Dongliang Liu, Jiawei Pan, Yong Zheng, Minkun Bai
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-06-01
Series:Frontiers in Earth Science
Subjects:
low-temperature thermochronology
crustal shortening deformation
mantle delamination
isostatic rebound
thermal expansion
Tibetan Plateau
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.818079/full

Internet

https://www.frontiersin.org/articles/10.3389/feart.2022.818079/full

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