Abstract

We have successfully relocated 74 out of 89 aftershocks until December 19, 2016, by using hypocenter double-difference method. We also have conducted focal mechanism analysis to estimate the type of fault slip. The results indicate improvement in hypocenter location, where the initial earthquakes focus depth at a fixed depth of 10 km have been updated and have described the patterns of active fault in the area trending Northwest-Southeast. The validity through the histogram of travel-time residual shows fairly good data processing where the residual value is close to zero (t.obs - t.cal ~ 0). Based on focal mechanism solutions of mainshock and two selected aftershocks, the type of fault is right lateral strike-slip.

Highlights

  • On December 7th, 2016 an earthquake occurred in Pidie Jaya, Aceh, Indonesia

  • According to Indonesian Agency for Meteorological, Climatological and Geophysics (BMKG), this earthquake occurred at 05:03:36 a.m with a magnitude Mw 6.5, the epicenter is located at 5.29o N, 96.22o E with a depth of 15 km

  • The velocity model of IASPEI91 was used for the hypocenter determination in BMKG catalogue (Kennett and Engdahl, 1991) by using SeisComP3 Program (GFZ)

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Summary

INTRODUCTION

On December 7th, 2016 an earthquake occurred in Pidie Jaya, Aceh, Indonesia. According to Indonesian Agency for Meteorological, Climatological and Geophysics (BMKG), this earthquake occurred at 05:03:36 a.m with a magnitude Mw 6.5, the epicenter is located at 5.29o N, 96.22o E with a depth of 15 km. The authority has been reported at least 102 fatalities and 700 people were injured and thousands of buildings were damaged. About a minute after the mainshock, followed by sequences aftershocks until a few weeks later

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