The Dabashan orocline is a large thrust belt in central China. Determination of its high-
resolution three-dimensional (3D) crustal shear-wave (S-wave) velocity structure can …

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 …

The traditional H–κ stacking technique is often used to determine the crustal thickness (H)
and V p/V s (κ) using multiple Moho converted P-to-S phases, but weak crustal multiples and …

Virtual deep seismic sounding (VDSS) uses the arrival time of post-critical SsPmp relative to
the direct S wave to infer Moho depth at the Pmp reflection point. Due to the large offset …

Joint inversion for crustal velocity structure using only surface wave dispersion and receiver
function data often suffers the non-unique solution problem due to lack of P wave velocity …

This study proposes a method of constraining compression (P) wave velocity (⁠ VP⁠)
profiles (up to a depth of 1700 m) using P‐wave seismograms recorded on the ground …

Crustal thickness and its variation can provide important insights into the tectonics of a
region. The most popular methodology to determine crustal thickness–receiver function …

Crustal thickness H and v P/v S ratio are two basic parameters for deciphering the crustal
structure. We present an improved technique to constrain crustal thickness, v P/v S ratio and …

Through multi-channel cross-correlation, the differences of arrival time differences of SsPmp
and Ss between adjacent stations in dense broadband seismic array are measured, and …

Earth's interior states, such as its chemical composition, pressure and thermal status, are
reflected in its seismic properties, that is, the P-, S-wave velocities and velocity …