SUMMARY The Northeastern Tibetan Plateau has thickened crust and is still undergoing
strong active crustal shortening and deformation. Crustal anisotropy can provide clues to …

Constraining variations of lithospheric structure and deformation across southeastern Tibet
and the surrounding region are crucial for understanding the lateral growth of the plateau …

Abstract The Northeastern Tibetan plateau records Caledonian Qilian orogeny and
Cenozoic reactivation by continental collision between the Indian and Asian plates. In order …

The uplift mechanism and geodynamic model of the northeastern (NE) Tibetan Plateau
remain controversial. Two competing models have been proposed for the uplift of the NE …

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 …

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 …

The modern kinematics in and around the Tibetan Plateau have been widely investigated;
however, the deformation distribution pattern describing the crustal kinematics in this region …

We collect precise leveling data observed in the period of 1970 to 2012 around the eastern
margin of the Tibetan Plateau, and process the data to acquire present day crustal vertical …

The ongoing collision between the Indian plate and the Eurasian plate brings up NS crustal
shortening and thickening of the Tibet Plateau, but its dynamic mechanisms remain …

The formation of the Himalayan Range and Tibetan plateau has broad implications for earth
sciences. Yet the exact mechanisms of the mountain-building processes, in particular, the …