2015
DOI: 10.1016/j.tecto.2015.07.004
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Seismic hazard from instrumentally recorded, historical and simulated earthquakes: Application to the Tibet–Himalayan region

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Cited by 26 publications
(16 citation statements)
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“…A progress in geohazard (earthquakes, volcanoes, landslides, tsunami) assessments is based on in-depth analysis of individual hazards. In seismic hazard analysis, recent advances are associated with neo-deterministic approach to hazard assessment [Panza et al, 2010] and data-enhanced probabilistic SHA [Sokolov and Ismail-Zadeh, 2015]. Particularly, tectonically-realistic earthquake simulators help to generate seismicity for a big interval of time and to employ large synthetic seismic events for hazard assessment.…”
Section: Resultsmentioning
confidence: 99%
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“…A progress in geohazard (earthquakes, volcanoes, landslides, tsunami) assessments is based on in-depth analysis of individual hazards. In seismic hazard analysis, recent advances are associated with neo-deterministic approach to hazard assessment [Panza et al, 2010] and data-enhanced probabilistic SHA [Sokolov and Ismail-Zadeh, 2015]. Particularly, tectonically-realistic earthquake simulators help to generate seismicity for a big interval of time and to employ large synthetic seismic events for hazard assessment.…”
Section: Resultsmentioning
confidence: 99%
“…Using the Monte-Carlo probabilistic SHA, Sokolov and Ismail-Zadeh [2015] developed a new approach to hazard assessment incorporating large magnitude synthetic events obtained by BAFD simulations consistent with the geophysical and geodetic data as well as the observed earthquakes into the ground motion estimation. Earthquake scenarios for hazard assessment are generated stochastically to sample the magnitude and spatial distribution of seismicity, as well as the distribution of ground motion for each seismic event.…”
Section: Earthquake Simulator and Hazard Assessmentmentioning
confidence: 99%
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“…PSHA adalah formulasi matematis yang berasal dari analisis probabilitas hubungan statistik antara besarnya gempabumi, lokasi, dan redaman gerakan tanah (Wang, 2012). PSHA dapat menentukan frekuensi total yang melebihi berbagai tingkat gerakan tanah selama periode waktu tertentu (Sokolov dan Ismail-Zadeh, 2015), sehingga pendekatan ini dapat digunakan untuk menghitung bahaya gempabumi berdasarkan pada kumpulan kejadian gempabumi (McGuire, 1995). Untuk bahaya seismik pendekatan ini diakui lebih baik daripada pendekatan deterministik (Mualchin, 2010).…”
Section: Abstrakunclassified