Figure 3
From: Crustal Structure of the Collision-Subduction Zone in South of Iran Using Virtual Seismometers
(a) Stations of the IrSC network with the two earthquake pair shown as red stars. (b) cross-correlation (ECC) traces in the period range of 4–26 s for all available stations in the stationary zone, i.e., the station labeled in part (a). (c) Comparison of linear (LIN) and phase weighted (PWS) stacking of ECC with Rayleigh wave excited by an earthquake (2016.12.03; referred in Fig. 1). All traces were normalized to the maximum amplitude of PWS stacking signals.
