J Lei, D Zhao, X Xu, YG Xu, M Du - Physics of the Earth and Planetary …, 2019 - Elsevier
The big mantle wedge (BMW) model was originally proposed to explain the origin of the intraplate Changbaishan volcano in NE China where the subducting Pacific slab becomes …
X He, LF Zhao, XB Xie, X Tian… - Journal of Geophysical …, 2021 - Wiley Online Library
The continuous convergence between the Indian and Eurasian plates caused massive lithospheric deformation in the Tibetan Plateau and led to excessive crustal material …
The shallow crustal structure of Mars records the evolutionary history of the planet, which is crucial for understanding the early Martian geological environment. Until now, seismic …
Mantle degassing transect across different tectonic units within a plate convergent setting has been well documented for oceanic convergent margins by systematic changes in …
Z Huang, L Wang, M Xu, D Zhao… - Journal of Geophysical …, 2019 - Wiley Online Library
Abstract The SE Tibetan Plateau is located between the eastern Himalayan syntaxis and the stable Yangtze craton; its tectonic evolution is important for understanding the plateau …
The structure and dynamics of the upper mantle control tectonics, seismicity, magmatism, and the development of mineral deposits. Seismic tomography maps spatial variations in …
X Yang, Y Luo, C Jiang, Y Yang… - Journal of Geophysical …, 2023 - Wiley Online Library
Since the continental collision between the Indian and Eurasian plates began about 50 Ma ago, southeastern Tibet (SET) has undergone complex tectonic deformation. In this study …
M Xu, Z Huang, L Wang, M Xu, Y Zhang… - Journal of …, 2020 - Wiley Online Library
The tectonic uplift of the Tibetan Plateau is a focus in the geosciences. Middle‐lower crustal flow is a popular model to interpret the geodynamic mechanism on the margin of the Tibetan …