The eastern margin of the Tibetan Plateau is covered by dense faults, with actively
destructive earthquakes, which makes it a natural laboratory to study lateral extrusion …

Abstract The Anninghe and Longmenshan fault zones are the eastern boundary of the
Tibetan Plateau, and they are also important strong earthquake active zones. The study of …

We assemble the local earthquake data recorded by 71 permanent stations and 418
portable stations around the northeastern margin of the Tibetan plateau, and then utilize the …

We applied the double difference tomography method to relocate seismic events and invert
crustal velocity structure of the northeastern Tibetan plateau using seismic data from …

The Longmenshan area in the eastern Tibetan Plateau experienced strong crustal
deformation and faulting during Mesozoic and late Cenozoic epochs resulting in significant …

We applied the double-difference tomography to relocate seismic events and deter-mined
the crustal structure of the southeastern Tibetan Plateau from the inversion of the local …

Due to the heavy damages caused by the 2017 M s 7.0 Jiuzhaigou earthquake that occurred
in a complex tectonic environment, investigations on the seismogenic structure and tectonic …

As the southeastern margin of the Tibetan Plateau, the Xiaojiang fault zone plays an
important role in the lateral escape of Tibetan Plateau materials. In this work, the 3‐DP …

The deep velocity structure underneath the southeastern margin of the Tibetan Plateau is
the key to understand the tectonic evolution of the Tibetan Plateau. In this study, 145,254 …

In order to investigate the deep structure and dynamics of the triangular colliding system of
the eastern Tibetan Plateau (TP), as well as the Yangtze Platform and the Qinling-Dabie …