We present results of a P-receiver function analysis on a temporary seismic network in
Northwest Iran. The network provides an east-west cross-section of crustal structure from Astara to Lake Urmia. We computed the receiver functions in the time domain as well as the frequency domain. By migrating the receiver functions to depth, a 2D picture of crustal structure, moho depth variations, and other
... [Show full abstract] mid-crustal discontinuities was obtained. Moho depth increases smoothly from 40 km under Lake Urmia in the west to about 45 km east of the Sabalan in the East. Further east, the moho increases sharply to 55 km under the Talesh mountains. In the regions of Sahand and Sabalan volcanic zones, more complex crustal structures are observed. Underneath the west Caspian coast, sedimentary structures with a total thickness of 25 km can be inferred.