The mechanism of present-day crustal deformation in southeast Tibet remains controversial.
3-D high-precision geodetic data can provide significant clues to analyse the key driving …

We determined the first 3-D P-wave anisotropy tomography beneath Southeast Tibet and
adjacent regions using 63,773 P-wave arrivals from 2866 local earthquakes and 55,457 …

The Sichuan–Yunnan block is located in the eastern of Tibetan Plateau and exhibits strong
tectonic and earthquake activity. The Maisu fault is an E–W-trending fault within this block …

Abstract The Yecheng-Shiquanhe profile runs over the western Tibetan Plateau from the
south margin of the Tarim Basin, crossing the west Kunlun orogeny, to the east of …

A total of 400 regional earthquakes were located in northern Tibetan Plateau from data
recorded by INDEPTH‐IV and PKU Eastern Kunlun arrays from May 2007 to June 2009. The …

New Pn tomography on Tibetan Plateau (TP) and neighboring region is conducted with data
assembled from various sources. The improved Pn tomographic image delineates several …

Signals from 11 shots and 8 earthquakes, and numerous teleseismic events were recorded
along the 400-km seismic line INDEPTH III in central Tibet and interpreted together with …

Abstract The Tibetan Plateau is produced by the continental-continental collision between
the India and Eurasian plates as well as the subsequent convergence. It has become a …

Because of the complex interaction among the Tibetan Plateau, the Alxa block and the
Ordos block, the deformation mechanisms of the northeastern (NE) Tibetan Plateau have …

We have located a total of 232 local earthquakes using data recorded by the SANDWICH
seismic network from November 2013 to October 2014 in central Tibet across the Bangong …