We present a new crustal thickness map of the Chinese mainland and adjacent areas based
on a compilation of previously published data. More than 1900 estimates of crustal thickness …

Competing models that account for the construction of the Tibetan Plateau include
continental subduction, underthrusting, distributed shortening, channel flow, and older …

The Tibetan plateau is bounded in part by cratonic blocks, and in part by tectonothermally
younger and weaker crust. How the Tibetan plateau interacts with bordering non-cratonic …

Continental China consists of a complex amalgamation of geotectonic units and has
experienced strong and widespread tectonic deformation since the Mesozoic. To …

A Mw 6.6 earthquake struck Menyuan, Qinghai, China, on 7 January 2022. To determine the
rupture parameters of this event, the coseismic InSAR deformation fields were mapped and …

We analyze a large amount of receiver function data recorded by regional seismic networks
of the China Earthquake Administration to estimate crustal structure and deformation …

Understanding the Mesozoic–Cenozoic tectonic evolution of the North China Craton (NCC)
and the NE Tibetan Plateau (TP) requires detailed knowledge of the lithospheric structure …

We analysed a large amount of teleseismic receiver function data recorded by 172
broadband stations in the NE Tibetan plateau and its surrounding areas to investigate the …

The sedimentary and crustal thicknesses and Poisson's ratios of the NE Tibetan Plateau and
its adjacent regions are estimated by the h–κ stacking and CCP image of receiver functions …

Abstract The Cenozoic Qilian Shan thrust belt is the northern margin of the Tibetan Plateau,
which developed in part due to progressive India-Asia convergence during Himalayan …