Using a topography-dependent tomographic scheme, the seismic velocity structure of the
Eastern Tibetan Plateau, including the uplifted Longmenshan (LMS) orogenic belt, is …

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

SUMMARY A new crustal 3-DP-wave velocity model beneath NE Tibet is determined by
jointly inverting 62 339 high-quality first P wave and later PmP-wave arrival-time data from …

Northeastern Tibet is still in the primary stage of tectonic deformation and is the key area for
studying the lateral expansion of the Tibetan plateau. In particular, the existence of lower …

The uplift and expansion of Tibetan Plateau has dramatically changed the tectonics, climate
and environment of Asia, and has caused high seismic hazards at its southeastern margin …

An east–west trending, high-density seismic array was deployed along the eastern margin of
the Tibetan Plateau to investigate its eastward expansion. The 160 km long array spans the …

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 …

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 …

The northeastern margin of Tibet is of key importance in understanding the uplift and
expansion of Tibetan Plateau. In this research, we perform Rayleigh wave tomography from …

A high‐resolution image of the deep structures in the southeastern Tibetan plateau and
Yangtze block was revealed by teleseismic inversion based on the dense teleseismic data …