The Zagros of Iran form one of the youngest collisional orogenic belts on Earth. At shallow
depths, shortening across the Zagros is accommodated by folding in the sediments, high …

High resolution structures of the lithosphere–asthenosphere system beneath a seismic
profile in Iran are obtained by the simultaneous inversion of data from receiver functions and …

The Iranian plateau is a natural laboratory for deciphering the lithospheric deformation and
deep dynamics in response to the Neo‐Tethyan subduction and subsequent Arabia‐Eurasia …

Hundreds of compositionally diverse volcanoes have erupted on the Turkish–Iranian
Plateau in the last 15 Myr, attributed to one or more of the processes of Middle Miocene …

Previous investigation of seismic anisotropy indicates the presence of a simple mantle flow
regime beneath the Turkish-Anatolian Plateau and Arabian Plate. Numerical modeling …

The geometry of intra-continental lithosphere boundaries along the Zagros orogenic belt in
the Arabia-Eurasia collision is investigated by means of teleseismic data. The data are …

We inverted 3555 regional and teleseismic P-wave relative time residuals to resolve deep
velocity structure beneath the NW part of the Zagros collision zone. The data were gathered …

More accurate crustal structure models will help us to better understand the tectonic
convergence between Arabian and Eurasian plates in the Iran plateau. In this study, the …

We map the lateral variations of P-wave velocity beneath the Zagros collision zone in Iran
down to 800 km depth by regional travel time tomography. We invert 32,293 relative travel …

We compute a 2-D tomogram using the P wave arrival time readings from a temporary
seismic experiment to study the seismic structure of the crust and upper mantle in NW Iran …