As the western boundary of the Sichuan-Yunnan block (SYB), the Red River fault (RRF) is a
major fault that controls deep crustal movement and deformation in the southeast margin of …

Mechanisms for uplift and deformation of the Tibetan Plateau remain vigorously debated;
hypotheses include stepwise growth, distributed thickening, and crustal channel flow, each …

Tectonic research of the Tibetan Plateau has long focused on its deformation style and
mechanisms. The 2008 Mw7. 9 Wenchuan earthquake ruptured the Longmen Shan fault …

Azimuthal anisotropy retrieved from surface waves is important for constraining depth‐
varying deformation patterns in the crust and upper mantle. We present a direct inversion …

Based on a new seismic surface wave data set, we present a model of Alaskan crustal
seismic anisotropy that provides new insight into Alaska's geographically diverse …

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 …

Constraining variations of lithospheric structure and deformation across southeastern Tibet
and the surrounding region are crucial for understanding the lateral growth of the plateau …

The uplift of the Tibetan Plateau in the Cenozoic has greatly affected the tectonics in Asia.
But the evolution of the plateau is still unclear. The northeastern Tibetan Plateau is under …

In this study, we obtain a three‐dimensional (3‐D) high resolution seismic anisotropy model
of NE Tibet using ambient noise double beamforming (DBF) tomography with ChinArray …