The Mw 6.2 Murmuri earthquake occurred on 18 August 2014, in Ilam province. In this paper we analyze ~3 months of aftershock sequence recorded by a temporary seismic stations. After extracting the arrival times of P- and S-phases from continues waveforms, the aftershock sequence were relocated using the single-event and multiple event techniques. The Murmuri sequence shows a secondary aftershock sequence, which started on October 15, approximately 2 months after the mainshock and represents an activity migration to southeastern part. General pattern of the aftershocks distribution covers two connected active areas with approximately 35×15 km2 and 20×7 km2. In the first fault segment, which caused the mainshock, the rupture probably initiated at the northwestern part of the active zone where the mainshock is located, and propagated to the southeast. In the second fault segment which caused the aftershock Mw 5.8 on 15 October 2014, locating the hypocenter of this aftershock in the northwestern part suggests that similar to the first fault the rupture initiated at the northwestern part of the active zone and propagated to the southeastern part. The sections orthogonal to the aftershocks delineation as fault strikes suggest the northeastward dipping trend in the first fault segment and north-to-northeastward dipping trend in the second fault segment.