The January 25th, 2014 Kebumen earthquake: A normal faulting in subduction zone of Southern Java

Le résumé fourni par la source

Normal faulting mechanism of earthquake in subduction zone is quite interested to study further. We investigated the Kebumen, January 25, 2014 earthquake sequences by retrieving focal mechanisms using full moment tensor inversion. We used BMKG seismic data from stations in the vicinity of Central Java region for these inversions. Then we correlated the static coulomb stress change by the mainshock to the aftershocks. We found that mainshock is a normal faulting earthquake with nodal plane 1; strike 283, dip 22 and rake -100; nodal plane 2 with strike 113, dip 68 and rake -86. Using distribution analysis of high precision aftershocks after relocated; we considered that the reliable fault plane was nodal plane 1 with strike trending SE-NW. The focal mechanisms provide an estimate of the local stress field in the Wadati-Beniof Zone of Southern Java subduction zone. There is also conclution stating that the mainshock may trigger the aftershocks mainly in three zones, i.e. in continental crustal, upper mantle and on the oceanic slab. This is visually showed that the high quality aftershocks located in positive zones of static coulomb stress change.

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