This dataset contains P wave receiver functions for seismic stations and interpolated P receiver functions on a 0.5*0.5 degree grid over the Iranian Plateau. For each of the points having a receiver function, a Rayleigh wave dispersion curve derived from the measurements of ambient noise cross-correlations and regional earthquakes is provided.
Steps to reproduce
Fundamental mode Rayleigh wave dispersion curves from both the ambient noise cross-correlations and regional earthquakes were extracted using a multiple-filter analysis. P wave receiver functions were calculated based on using the iterative time-domain deconvolution method.