Lithospheric discontinuities, including the lithosphere‐asthenosphere boundary (LAB) and
the enigmatic mid‐lithospheric discontinuities (MLDs), hold important clues about the …

The shallowest intracrustal layer (extending to 8±2 km depth) beneath the Mars InSight
Lander site exhibits low seismic wave velocity, which is likely related to a combination of …

Abstract The Permian Emeishan large igneous province (LIP) in Southwestern China is
recognized as a remnant of mantle plume activity. Its crust composition has a significant …

Ambient noise autocorrelations can be used to reconstruct the seismic reflection response of
the Earth structure beneath single stations using continuous recordings without the need for …

East China has experienced multiple periods of tectonic movements, which have contributed
to the composition and rheological properties of its present crust. Estimating the composition …

The shallowest intracrustal layer (extending to 8±2 km depth) beneath the Mars InSight
Lander site exhibits low seismic wave velocity, which are likely related to a combination of …

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 …

Abstract 11 Lithospheric discontinuities, including the lithosphere-asthenosphere boundary
(LAB) 12 and the enigmatic mid-lithospheric discontinuities (MLDs), hold important clues …

Abstract Virtual Deep Seismic Sounding (VDSS) has recently emerged as a novel method to
image the crust-mantle boundary. However, the nature of post-critical SsPmp, the phase …