Fault source investigation of the 6 December 2016 MwMw 6.5 Pidie Jaya, Indonesia, earthquake based on GPS and its implications of the geological survey result
Author:
Gunawan Endra1, Nishimura Takuya2, Susilo Susilo3, Widiyantoro Sri14, Puspito Nanang T.1, Sahara David P.1, Hanifa Nuraini Rahma56, Hidayati Sri7, Omang Amalfi7, Agustan Agustan8
Affiliation:
1. Global Geophysics Research Group, Faculty of Mining and Petroleum Engineering , Bandung Institute of Technology , Bandung , Indonesia 2. Disaster Prevention Research Institute , 12918 Kyoto University , Kyoto , Japan 3. Geospatial Information Agency , Cibinong , Indonesia 4. Faculty of Engineering , Maranatha Christian University Bandung , Bandung , Indonesia 5. Center for Earthquake Science and Technology , Bandung Institute of Technology , Bandung , Indonesia 6. National Center for Earthquake Studies , Bandung , Indonesia 7. Centre for Volcanology and Geological Hazard Mitigation , Geological Agency , Bandung , Indonesia 8. Agency for the Assessment and Application of Technology , Jakarta , Indonesia
Abstract
Abstract
On 6 December 2016 at 22:03 UTC, a devastating magnitude 6-class strike-slip earthquake occurred along an unidentified and unmapped fault in Pidie Jaya, northern Sumatra. We analysed the possible fault using continuous Global Positioning System (GPS) observation available in the region. In our investigation, we searched for the fault source parameters of the north- and south-dipping left-lateral faults and the west- and east-dipping right-lateral faults. We identified that the fault responsible for the earthquake was located offshore, with a southwest-northeast direction. We also computed the Coulomb failure stress and compared the result with the distribution of the aftershocks. In this study, we demonstrated that the result of the geological field survey conducted soon after the mainshock was attributed to the secondary effects of ground shaking and near-surface deformation, and not surface faulting. The newly identified offshore fault proposed by this study calls for further investigation of the corresponding submarine morphological attributes in this particular region.
Funder
Institut Teknologi Bandung
Publisher
Walter de Gruyter GmbH
Subject
Earth and Planetary Sciences (miscellaneous),Engineering (miscellaneous),Modelling and Simulation
Reference36 articles.
1. Sieh, K., Natawidjaja, D. Neotectonics of the Sumatran fault, Indonesia. Journal of Geophysical Research: Solid Earth, 2000, 105(B12), pp. 28295–28326. 2. Ito, T., Gunawan, E., Kimata, F., Tabei, T., Simons, M., Meilano, I., Agustan, A., Ohta, Y., Nurdin, I., Sugiyanto, D. Isolating along-strike variations in the depth extent of shallow creep and fault locking on the northern Great Sumatran Fault. Journal of Geophysical Research: Solid Earth (1978–2012), 2012, 117(B6), doi: 10.1029/2011JB008940. 3. Bradley, K.E., Feng, L., Hill, E.M., Natawidjaja, D.H., Sieh, K. Implications of the diffuse deformation of the Indian Ocean lithosphere for slip partitioning of oblique plate convergence in Sumatra. Journal of Geophysical Research: Solid Earth, 2017, 122(1), pp. 572–591. 4. Natawidjaja, D.H., Bradley, K., Daryono, M.R., Aribowo, S., Herrin, J. Late Quaternary eruption of the Ranau Caldera and new geological slip rates of the Sumatran Fault Zone in Southern Sumatra. Indonesia. Geoscience Letters, 2017, 4(1), p. 21. 5. Gunawan, E., Widiyantoro, S., Rosalia, S., Daryono, M.R., Meilano, I., Supendi, P., Ito, T., Tabei, T., Kimata, F., Ohta, Y., Ismail, N. Coseismic Slip Distribution of the 2 July 2013 Mw 6.1 Aceh, Indonesia, Earthquake and Its Tectonic Implications. Bulletin of the Seismological Society of America, 2018, 108(4), pp. 1918–1928, doi: 10.1785/0120180035.
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