Fig. 9From: Complex faulting in the Quetta Syntaxis: fault source modeling of the October 28, 2008 earthquake sequence in Baluchistan, Pakistan, based on ALOS/PALSAR InSAR dataSlip distribution of the seismic sequence. The top of the faults is 300 m below the crust surface. The calculated magnitudes (Mw) for RLF1, RLF2, LLF1, and LLF2 are 6.5, 6.2, 6.3, and 5.9 respectivelyBack to article page