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Preliminary results of local earthquake tomography around Bali, Lombok, and Sumbawa regions

Conference Paper (PDF Available)  · November 2014with197 Reads
DOI: 10.1063/1.4915027
Conference: Conference: 4th International Symposium on Earthquake and Disaster Mitigation 2014 (ISEDM 2014), At Bandung, Volume: AIP Conference Proceedings 1658
Andri Dian Nugraha at Bandung Institute of Technology
  • 22.21
  • Bandung Institute of Technology
Ridwan Kusnandar at Meteorological Climatological and Geophysical Agency
  • 3.46
  • Meteorological Climatological and Geophysical Agency
Nanang Puspito at Bandung Institute of Technology
  • 17.41
  • Bandung Institute of Technology
Tedi Yudistira at Bandung Institute of Technology
  • 13.56
  • Bandung Institute of Technology
Abstract
Bali, Sumbawa, and Lombok regions are located in active tectonic influence by Indo-Australia plate subducts beneath Sunda plate in southern part and local back-arc thrust in northern part the region. Some active volcanoes also lie from eastern part of Java, Bali, Lombok and Sumbawa regions. Previous studies have conducted subsurface seismic velocity imaging using regional and global earthquake data around the region. In this study, we used P-arrival time from local earthquake networks compiled by MCGA, Indonesia within time periods of 2009 up to 2013 to determine seismic velocity structure and simultaneously hypocenter adjustment by applying seismic tomography inversion method. For the tomographic inversion procedure, we started from 1-D initial velocity structure. We evaluated the resolution of tomography inversion results through checkerboard test and calculating derivative weigh sum. The preliminary results of tomography inversion show fairly clearly high seismic velocity subducting Indo-Australian and low velocity anomaly around volcano regions. The relocated hypocenters seem to cluster around the local fault system such as back-arc thrust fault in northern part of the region and around local fault in Sumbawa regions. Our local earthquake tomography results demonstrated consistent with previous studies and improved the resolution. For future works, we will determine S-wave velocity structure using S-wave arrival time to enhance our understanding of geological processes and for much better interpretation.
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