The Rigan area is located in east central Iran (see Fig. 1), at the southern part of the Lut block and the northern edge of the Jaz Murian depression (Mirzaei, 1998). The study area is surrounded by different active strike‐slip faults, that is, the Bam fault from the west‐northwest, the Kahurak fault from the northeast, and the Nosrat–Abad fault zone from the east (Fig. 1). The region experienced large destructive earthquakes including the 26 December 2003 (Mw 6.6) Bam earthquake.

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Available information on the lateral heterogeneity and the velocity structure of the crust for...

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