Our seismic study together with the MT analysis reveal a “R‐shape” flow existing in both the
lower crust and uppermost mantle, which suggests the crustal deformation along the deep …

The continental convergence between the Indian and Eurasian plates in the Cenozoic not
only caused the formation of the Tibetan Plateau (TP) but also pushed a large volume of …

Southeastern Tibet marks the site of presumed clockwise rotation of the crust due to the
India–Eurasian collision and abutment against the stable Sichuan basin and South China …

We applied the double difference tomography method to simultaneously invert the seismic
event locations and the crustal structure of the northeastern Tibetan Plateau with the …

Abstract A 180-km-long, high-resolution seismic-reflection survey that imaged the entire
crust and the uppermost mantle lithosphere was conducted across the northeastern Tibetan …

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 …

A dense linear array of 38 broadband seismograph stations was deployed to traverse the
northeastern margin of Tibetan plateau (NE Tibet). Shear wave splitting measurements …

In the past ten years, three major earthquakes with devastating impacts have taken place
along the margins of the Bayan Har Terrane in NE Tibetan Plateau, China. To understand …

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

The Qilian Orogen Zone (QOZ), located in the north margin of the Tibetan Plateau, is the key
area for understanding the deformation and dynamics process of Tibet. Numerous …