results of velocity structure modeling in the earth's crust using a comparison approach of receiver function analysis and joint inversion of receiver functions with surface wave dispersion data are presented in this paper. seismograms of the teleseismic events that have been recorded on a broadband seismic station in the central alborz were used for data processing. velocity models that we...

In spite of numerous active and passive seismological investigations, the existence continuous or interrupted continental subduction below Western Alps is still open to debate. Many observations focus on Moho deeper part mantle, while reliable information Lithosphere-Asthenosphere Boundary (LAB) Alpine region scarce. Exploiting data from dense, broadband AlpArray Seismic Network we present a se...

We describe and apply an iterative, t ime-domain deconvolution approach to receiver-function estimation and illustrate the reliability and advantages of the technique using syntheticand observation-based examples. The iterative technique is commonly used in earthquake t ime-function studies and offers several advantages in receiver-function analysis such as intuitively stripping the largest rec...

As part of a joint Sino-U.S. research project to study the deep structure of the Tibetan plateau, 11 broadband digital seismic recorders were deployed on the plateau for one year of passive seismic recording. In this report we use teleseimic P waveforms to study the seismic velocity structure of crust and upper mantle under three stations by receiver function inversion. The receiver function is...