In response to the Economic development plans in Iranian Makran subduction zone, Department of Earth Sciences of Institute for Advanced Studies in Basic Sciences started its integrated geophysical and geological survey in Makran in spring 2015. The integrated survey is consisted of 1) a broad band seismic network to estimate the geometry of subducting plate, map seismicity of the region and estimate the thickness of sediments in the accretionary prism, 2) a campaign GPS survey to investigate the deformation within the Makran acrretionary prism, 3) neotectonic survey to map active faults, and 4) petrological sampling to reconstruct the geodynamical evolution of the subduction zone in time. The surveys will provide the basic knowledge to prepare a reliable Earthquake and Tsunami map of the region. I will briefly introduce the different aspect of this large experiment and present some of its early outcomes.