2014
DOI: 10.14716/ijtech.v5i3.610
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Lesser Sunda Islands Earthquake Inter-occurrence Times Distribution Modeling

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Cited by 7 publications
(5 citation statements)
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“…Seismic Hazard Analysis is normally performed to predict the risk level of earthquake impact, which includes probabilistic seismic hazard analysis (PSHA) and deterministic seismic hazard analysis (DSHA) (Reiter, 1990). PSHA is a statistical method used to predict a representative earthquake, considering its recurrence in a region (Kinasih et al, 2014), whereas DSHA is a simple deterministic method which determines the most credible earthquake or the controlling earthquake. In DSHA, the most credible earthquake is predicted based on the serious impact on the study area (Mase & Somatri, 2016).…”
Section: Deterministic Seismic Hazard Analysismentioning
confidence: 99%
“…Seismic Hazard Analysis is normally performed to predict the risk level of earthquake impact, which includes probabilistic seismic hazard analysis (PSHA) and deterministic seismic hazard analysis (DSHA) (Reiter, 1990). PSHA is a statistical method used to predict a representative earthquake, considering its recurrence in a region (Kinasih et al, 2014), whereas DSHA is a simple deterministic method which determines the most credible earthquake or the controlling earthquake. In DSHA, the most credible earthquake is predicted based on the serious impact on the study area (Mase & Somatri, 2016).…”
Section: Deterministic Seismic Hazard Analysismentioning
confidence: 99%
“…The PSHA parameters for Kupang were lower than those of Mataram and Bima. As consequences, probability analyses show that medium and weaker earthquakes have a bigger chance of reoccurrence in Lombok and surrounding islands, most probably within 5 years [69].…”
Section: Table 3: Pga Values For Various Cities In the Nusa Tenggara mentioning
confidence: 96%
“…Total kejadian gempa di Lombok dan sekitarnya dari tahun 1900 sampai 2014 adalah 2081 kejadian, yakni amplitudo gempa 4-4.9 SR terdapat 1709 kejadian, 5-5.9 SR terdapat 336 kejadian, dan 6-8 SR terdapat 36 kejadian. Gempa-gempa tersebut merupakan gempa-gempa dangkal (kedalaman < 40 km) yang berpotensi menimbulkan bencana [3].…”
Section: Pendahuluanunclassified