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dc.contributor.authorSupendi, Pepen
dc.contributor.authorNugraha, Andri Dian
dc.contributor.authorWidiyantoro, Sri
dc.contributor.authorAbdullah, Chalid Idham
dc.contributor.authorPuspito, Nanang T.
dc.contributor.authorPalgunadi, Kadek Hendrawan
dc.contributor.authorDaryono, D.
dc.contributor.authorWiyono, Samsul Hadi
dc.date.accessioned2020-01-12T13:47:25Z
dc.date.available2020-01-12T13:47:25Z
dc.date.issued2019-12-16
dc.identifier.citationSupendi, P., Nugraha, A. D., Widiyantoro, S., Abdullah, C. I., Puspito, N. T., Palgunadi, K. H., … Wiyono, S. H. (2019). Hypocenter relocation of the aftershocks of the Mw 7.5 Palu earthquake (September 28, 2018) and swarm earthquakes of Mamasa, Sulawesi, Indonesia, using the BMKG network data. Geoscience Letters, 6(1). doi:10.1186/s40562-019-0148-9
dc.identifier.doi10.1186/s40562-019-0148-9
dc.identifier.urihttp://hdl.handle.net/10754/660977
dc.description.abstractOn September 28, 2018, the Mw 7.5 earthquake occurred in Palu, Central Sulawesi, Indonesia. This earthquake produced strong tremors, landslides, liquefaction and a tsunami and caused thousands of fatalities and damaged houses and infrastructure. We have relocated 386 of the 554 Palu aftershocks by using the double-difference relocation method (hypoDD) from September 28 to November 22, 2018. The aftershock pattern is consistent with the crustal deformation in the area and generally shows that the events have a NW–SE trending of ~ 200 km in length and ~ 50 km in width. Most of the aftershocks are located to the east of the Palu-Koro Fault Line. Since November 2, 2018, there have been hundreds of swarm earthquakes in the area of Mamasa, West Sulawesi, which is about 230 km south of the city of Palu. Some of these earthquakes were felt, and houses were even damaged. We have relocated 535 of the 556 swarm earthquakes having a magnitude of M 2 to M 5.4. Our results show that the seismicity pattern has a dip that becomes shallower to the west (dipping at a ~ 45° angle) and extends from north to south for a length of ~ 50 km. We also conducted a focal mechanism analysis to estimate the type of fault slip for selected events of an M > 4.5 magnitude. Most of the solutions of the focal mechanism analysis show a normal fault type. This swarm earthquake probably corresponds to the activity of the fault in the local area.
dc.description.sponsorshipWe are grateful to the Indonesian Agency for Meteorology, Climatology, and Geophysics (BMKG) for access to their earthquake data which were used in this study. All figures were made using Generic Mapping Tools (Wessel and Smith 1998). We thank James D. P. Moore for constructive comments, which helped us improve the manuscript considerably.
dc.publisherSpringer Nature
dc.relation.urlhttps://geoscienceletters.springeropen.com/articles/10.1186/s40562-019-0148-9
dc.relation.urlhttps://geoscienceletters.springeropen.com/track/pdf/10.1186/s40562-019-0148-9
dc.rightsThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.titleHypocenter relocation of the aftershocks of the Mw 7.5 Palu earthquake (September 28, 2018) and swarm earthquakes of Mamasa, Sulawesi, Indonesia, using the BMKG network data
dc.typeArticle
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalGeoscience Letters
dc.eprint.versionPublisher's Version/PDF
dc.contributor.institutionGeophysical Engineering Study Program, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, 40132, Indonesia
dc.contributor.institutionAgency for Meteorology, Climatology, and Geophysics (BMKG), Bandung, 40161, Indonesia
dc.contributor.institutionCenter for Earthquake Science and Technology, Institut Teknologi Bandung, Bandung, 40132, Indonesia
dc.contributor.institutionGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, 40132, Indonesia
dc.contributor.institutionGeodynamic and Sedimentology Research Group, Faculty of Earth Sciences and Technology, Institut Teknologi Bandung, Bandung, 40132, Indonesia
dc.contributor.institutionAgency for Meteorology, Climatology, and Geophysics (BMKG), Jakarta, 10610, Indonesia
kaust.personPalgunadi, Kadek Hendrawan
dc.relation.issupplementedbyDOI:10.6084/m9.figshare.c.4784517.v1
refterms.dateFOA2020-01-12T13:48:04Z
display.relations<b>Is Supplemented By:</b><br/> <ul><li><i>[Dataset]</i> <br/> Pepen Supendi, Nugraha, A., Widiyantoro, S., Chalid Abdullah, Nanang Puspito, Kadek Palgunadi, D. Daryono, &amp; Samsul Wiyono. (2019). <i>Hypocenter relocation of the aftershocks of the Mw 7.5 Palu earthquake (September 28, 2018) and swarm earthquakes of Mamasa, Sulawesi, Indonesia, using the BMKG network data</i>. figshare. https://doi.org/10.6084/M9.FIGSHARE.C.4784517.V1. DOI: <a href="https://doi.org/10.6084/m9.figshare.c.4784517.v1" >10.6084/m9.figshare.c.4784517.v1</a> Handle: <a href="http://hdl.handle.net/10754/664960" >10754/664960</a></a></li></ul>
dc.date.published-online2019-12-16
dc.date.published-print2019-12


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This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
Except where otherwise noted, this item's license is described as This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.