The Tibetan plateau is bounded in part by cratonic blocks, and in part by tectonothermally younger and weaker crust. How the Tibetan plateau interacts with bordering non-cratonic …
Key in understanding the geodynamics governing subduction and orogeny is reconstructing the paleogeography of 'Greater India', the Indian plate lithosphere that subducted since …
Considerable debate exists regarding how the East Asian summer monsoon (EASM) varied over the late Miocene, limiting our ability to understand the long-term evolution and forcing …
J Yu, D Zheng, W Wang, J Pang, C Li, Y Wang… - Global and Planetary …, 2023 - Elsevier
Abstract The northeastern Tibetan Plateau occupies the northernmost portion of the plateau, whose timing and pattern of deformation during its Cenozoic tectonic development provide …
P He, C Song, Y Wang, L Chen… - Journal of …, 2017 - Wiley Online Library
Abstract The India‐Asia collision resulted in the Cenozoic framework of faults, ranges, and tectonic basins and the high topography of the northeastern Tibetan Plateau, but how and …
J Xiong, Y Liu, P Zhang, C Deng, V Picotti, W Wang… - Geomorphology, 2022 - Elsevier
The distinctive right-angled bend of the Yellow River around the Ordos Block, a large Permo- Mesozoic continental block in East Asia, has attracted much attention from …
W Wang, P Zhang, C Liu, D Zheng, J Yu… - Journal of …, 2016 - Wiley Online Library
The development of Cenozoic basins in the northeast margin of the Tibetan Plateau is central to understanding the dynamics of plateau growth. Here we present a …
L Sun, C Deng, T Deng, Y Kong, B Wu, S Liu… - Palaeogeography …, 2023 - Elsevier
The Cenozoic biochronology framework for northern China has been based on few vertebrate fossil localities with unverified age constraints. The Linxia Basin, located on the …