We analyze S-receiver functions to investigate variations of lithospheric thickness below the
entire region of Turkey and surrounding areas. The teleseismic data used here have been …

We investigated the crustal structure at 34 stations using the H-κ stacking method and jointly
inverting receiver functions with Rayleigh-wave phase and group velocities. These seismic …

Azimuthal anisotropy derived from multimode Rayleigh wave tomography in China exhibits
depth‐dependent variations in Tibet, which can be explained as induced by the Cenozoic …

Compressional and extensional tectonics following northward plate convergences since the
Miocene have formed the major surface features in Turkey, such as faulting and orogeny …

The northeastern margin of the Tibetan Plateau is a key area for studies of the crustal
thickening and outward expansion of the plateau and its interactions with surrounding …

Of the two debated, end-member models for the late-Cenozoic thickening of Tibetan crust,
one invokes 'channel flow'(rapid viscous flow of the mid-lower crust, driven by topography …

Focal mechanism solutions and their predicted stress pattern can be used to investigate
tectonic deformation in seismically active zones and contribute to understanding and …

The present study investigates azimuthal anisotropy and its relation to the geodynamical
processes beneath the back‐arc of the Hellenic subduction zone in the eastern Aegean and …

SUMMARY The Northeastern Tibetan Plateau has thickened crust and is still undergoing
strong active crustal shortening and deformation. Crustal anisotropy can provide clues to …

We use local and teleseismic earthquakes to analyze shear wave splitting within the Pamir‐
Hindu Kush region, north of the western syntaxis of the India‐Asia collision zone. These two …