This study is to characterize the source mechanism of tsunamigenic earthquake based on seismic wave calculation. The source parameter used are the ratio (Θ) between the radiated seismic energy (E) and seismic moment (Mo), moment magnitude (MW), rupture duration (To) and focal mechanism. These determine the types of tsunamigenic earthquake and tsunami earthquake. We calculate the formula using the teleseismic wave signal processing with the initial phase of P wave with bandpass filter 0.001 Hz to 5 Hz. The amount of station is 84 broadband seismometer with far distance of 30° to 90°. The 2 June 1994 Banyuwangi earthquake with MW=7.8 and the 17 July 2006 Pangandaran earthquake with MW=7.7 include the criteria as a tsunami earthquake which distributed about ratio Θ=−6.1, long rupture duration To>100 s and high tsunami H>7 m. The 2 September 2009 Tasikmalaya earthquake with MW=7.2, Θ=−5.1 and To=27 s which characterized as a small tsunamigenic earthquake.
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24 March 2014
4TH INTERNATIONAL CONFERENCE ON MATHEMATICS AND NATURAL SCIENCES (ICMNS 2012): Science for Health, Food and Sustainable Energy
8–9 November 2012
Bandung, Indonesia
Research Article|
March 24 2014
Characterization of tsunamigenic earthquake in Java region based on seismic wave calculation
Sugeng Pribadi;
Sugeng Pribadi
Badan Meteorologi Klimatologi Geofisika, Jl Angkasa I No. 2 Jakarta,
Indonesia
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Afnimar;
Afnimar
Institut Teknologi Bandung, Jl. Ganesha 10, Bandung 40132,
Indonesia
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Nanang T. Puspito;
Nanang T. Puspito
Institut Teknologi Bandung, Jl. Ganesha 10, Bandung 40132,
Indonesia
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Gunawan Ibrahim
Gunawan Ibrahim
Institut Teknologi Bandung, Jl. Ganesha 10, Bandung 40132,
Indonesia
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AIP Conf. Proc. 1589, 129–132 (2014)
Citation
Sugeng Pribadi, Afnimar, Nanang T. Puspito, Gunawan Ibrahim; Characterization of tsunamigenic earthquake in Java region based on seismic wave calculation. AIP Conf. Proc. 24 March 2014; 1589 (1): 129–132. https://doi.org/10.1063/1.4868766
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