We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …

This review presents an account of the variations in crustal and upper mantle structure
beneath the Indian subcontinent and its environs, with emphasis on passive seismic results …

Summary The European Plate has a 4.5 Gy long and complex tectonic history. This is
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …

Southeastern Tibet marks the site of presumed clockwise rotation of the crust due to the
India–Eurasian collision and abutment against the stable Sichuan basin and South China …

We examine the effects on receiver functions of transverse anisotropy and of dip**
isotropic boundaries. Splitting of the Moho Ps phase predicts the anisotropy from a …

P-SH conversion is commonly observed in teleseismic P waves, and is often attributed to
dip** interfaces beneath the receiver. Our modelling suggests an alternative explanation …

A 1000km long passive seismic observation profile consisted of 47 broadband portable
seismometers was deployed from Maqên in northeastern Tibetan Plateau to Yulin in central …

The vertical component P-wave receiver function is an important source of data in studies of
the crust/mantle transfer function for determining Earth structure under isolated receivers or …

The inversion of teleseismic receiver functions for lithospheric structure is difficult due to the
non-linearity of the problem, which is greatly increased in the presence of dip** interfaces …

We estimated crustal structures under 18 broadband stations in southern Korea by
combining receiver functions and surface-wave dispersion with the genetic algorithm (ga) …