The SinoProbe, deep exploration in China, is a multidisciplinary earth science research
program that aims at revealing the composition, structure and evolution of the continental …

Lithospheric deformation of the Tibetan plateau is caused by subduction of the Indian
(northward) and Asian (southward) plates. The effects of this interaction on inner reaches of …

Understanding the geodynamic process of orogeny and cratonization, and their transition is
among the key topics of research in evaluating the link between plate tectonics and …

We present high‐resolution 3D images of the crustal S‐wave velocity structure beneath
northeastern Tibet, via ambient noise imaging techniques. The data come from continuous …

We present a new 3‐D lithospheric V s model for the NE Tibetan Plateau (NETP) and the
western North China Craton (NCC). First, high‐frequency receiver functions (RFs) were …

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 …

GPS measurements indicate rapid lateral extrusion of the NE Tibetan Plateau, which causes
active NE-directed crustal shortening and has initiated oblique shearing along the margins …

The lower crustal flow model has become an interesting proposal to describe the growth and
expansion of eastern Tibet. To date, however, the geophysical results are not definitive due …

The mechanisms that underlie crustal thickening and deformation along the northeastern
margin of the Tibetan Plateau, as well as the interplay among different tectonic blocks and …

Several geodynamic models have been proposed for the deformation mechanism of Tibetan
Plateau (TP), but it remains controversial. Here we applied a method of joint inversion of …