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 …

We conducted a tomographic inversion of Rayleigh‐wave dispersion to obtain 2D phase
and group velocity tomographic images in the 10–100 s period range and shear‐wave …

Abstract The Turkish–Iranian Plateau is located on the hinterland of the Bitlis–Zagros suture
zone and contains systematic active strike-slip fault patterns forming several rhomboidal …

In this study, we focus on Northwest Iran and exploit a dataset of Rayleigh-wave group-
velocity measurements obtained from ambient noise cross-correlations and earthquakes …

We present a new approach for understanding the origin and nature of seismic anomalies in
the continental crust of the Northern Middle East. We have created detailed attenuation (Q …

Seismic attenuation measurements, especially those obtained from coda decay analysis,
are becoming a key data source for the characterization of the heterogeneous Earth due to …

The attenuation of seismic waves in the Zagros region (southwestern Iran) was investigated
using seismic waveforms collected from 2006 to 2019. The selected data set consists of …

The Zagros collision zone, located in the southwest of Iran, is experiencing an immoderately
large number of seismic hazards caused by the convergence between the two Arabia and …

We have analyzed more than 2800 local earthquakes recorded by the Iranian National
Seismic Network (INSN) and the Iranian Seismological Center (IRSC) to estimate coda wave …

In this study, spatial variation of coda wave attenuation in the north western (NW) Iranian
Plateau is explored using local earthquakes. Single backscattering method is used to map …