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Focal Mechanism Analysis of the Earthquakes Beneath the Sunda-Banda Arc Transition, Indonesia, Using the BMKG Data

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dc.contributor.authorSupendi, P
dc.contributor.authorRawlinson, N
dc.contributor.authorNugraha, AD
dc.contributor.authorWidiyantoro, S
dc.contributor.authorAbdullah, CI
dc.contributor.authorDaryono
dc.contributor.authorPrayitno, BS
dc.contributor.authorSadly, M
dc.contributor.authorKarnawati, D
dc.date.accessioned2022-06-07T08:10:47Z
dc.date.available2022-06-07T08:10:47Z
dc.date.issued2022-05-01
dc.date.updated2022-06-07T08:10:46Z
dc.description.abstract<jats:title>Abstract</jats:title> <jats:p>Structural complexity in the Sunda-Banda arc transition is a topic of much debate amongst Earth scientists. We have processed focal mechanism study using moment tensor inversion for 20 events in the region using the Agency for Meteorology, Climatology, and Geophysics (BMKG) data from 2014-2016 for earthquakes of magnitude Mw ≥ 5.0. Our result shows different solutions that depend on the source region of the earthquakes that include subduction zones and collision zones, which host active faults and the back-arc thrusts. Earthquakes that occurred in the subduction zone appear to rupture on thrust faults for shallow and intermediate events, while the deep events have normal fault mechanisms. The shallow events in the collision zone occur on thrust faults with differing strike directions, but generally, there are largely parallel to the Timor trough. We also found normal fault mechanisms at play for deep events below the collision zone. The occurrence of deep earthquakes in this area is consistent with remnant slab activity that persists to the present day. Focal mechanism solutions for shallow events in the north of Sumbawa island indicate a thrust fault with a strike direction that is almost parallel to the back-arc thrust in this area. We also found evidence of strike-slip motion along local-scale active faults in the area.</jats:p>
dc.identifier.doi10.17863/CAM.85151
dc.identifier.eissn1755-1315
dc.identifier.issn1755-1307
dc.identifier.otherees_1031_1_012012
dc.identifier.othere10311012
dc.identifier.urihttps://www.repository.cam.ac.uk/handle/1810/337742
dc.languageen
dc.language.isoeng
dc.publisherIOP Publishing
dc.publisher.urlhttp://dx.doi.org/10.1088/1755-1315/1031/1/012012
dc.subject37 Earth Sciences
dc.subject3705 Geology
dc.subject3706 Geophysics
dc.titleFocal Mechanism Analysis of the Earthquakes Beneath the Sunda-Banda Arc Transition, Indonesia, Using the BMKG Data
dc.typeArticle
prism.issueIdentifier1
prism.publicationNameIOP Conference Series: Earth and Environmental Science
prism.volume1031
rioxxterms.licenseref.urihttp://creativecommons.org/licenses/by/3.0/
rioxxterms.versionVoR
rioxxterms.versionofrecord10.1088/1755-1315/1031/1/012012

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