Mokhtari, Mohammad; Fard, Iraj Abdollahie; Hessami, Khaled - In: Natural Hazards 47 (2008) 2, pp. 185-199
The character of convergence along the Arabian–Iranian plate boundary changes radically eastward from the Zagros ranges to the Makran region. This appears to be due to collision of continental crust in the west, in contrast to subduction of oceanic crust in the east. The Makran subduction zone...