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 …

We used 71670 P-wave arrival times from 3594 earthquakes recorded by the Sichuan and
Yunnan seismic networks to determine the three-dimensional P-wave velocity structure in …

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

The lower crustal flow model is one of several competing models considered to interpret the
growth and expansion of southeastern Tibet. However, the dynamic processes involved in …

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 …

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 …

The southeast margin of the Tibetan Plateau lies between the heartland of the plateau to the
west and the stable south China block to the east, spanning from western Sichuan to central …

The special seismic tectonic environment and frequent seismicity in the southeastern margin
of the Qinghai–Tibet Plateau show that this area is an ideal location to study the present …

Teleseismic events used in this study were recorded by 35 seismic stations that operated by
China Earthquake Administration in the Ludian epicenter and surrounding region. We used …

High-resolution 3-DP and S wave velocity (Vp and Vs) models of the crust and uppermost
mantle beneath the northeastern (NE) Tibetan Plateau and the surrounding areas were …