Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on
earth, and become a key region for comprehending the rheology and tectonic evolution of …

Forming the northern margin of the Cenozoic Himalayan–Tibetan orogen, the area
surrounding the Qaidam Basin is a key region to study the mechanisms that govern the long …

Contrasting views exist on timing and mechanisms of Tertiary crustal uplift in the NE Tibetan
Plateau based on different approaches, with many models attributing surface uplift to crustal …

We present an updated joint tomographic method to simultaneously invert receiver function
waveforms and surface wave dispersions for a 3-DS-wave velocity (Vs) model. By applying …

Abstract The Hoh Xil Basin (HXB) was located in the foreland of the proto‐Tibetan Plateau
and has obtained a high elevation and thick crust since the Late Oligocene. However, crust …

Abstract The Hoh Xil Basin (HXB) is a key site for continental sedimentation from the Late
Cretaceous to the Neogene on the northern-central Tibetan Plateau and provides a record …

The uplift mechanism and deep crustal deformation of the northeast of the Tibetan plateau in
response to the Cenozoic India-Asian collision are still poorly constrained. Previous studies …

Receiver function is important for imaging crustal and upper-mantle discontinuities.
However, sparsely scattered stations could introduce imaging artefacts or misinterpretations …

SUMMARY Virtual Deep Seismic Sounding (VDSS) has emerged as a novel method to
image the crust–mantle boundary (CMB) and potentially other lithospheric boundaries. In …

We analyzed P-wave receiver functions from seismic stations covering most of Saudi Arabia
to map the thickness of the crust across the Arabian plate. We present an update of crustal …