2012
DOI: 10.1785/0120110219
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Comprehensive Probabilistic Seismic Hazard Analysis of the Andaman-Nicobar Regions

Abstract: An updated catalog of earthquakes has been prepared for the AndamanNicobar and adjoining regions. The catalog was homogenized to a unified magnitude scale, and declustering of the catalog was performed to remove aftershocks and foreshocks. Eleven regional source zones were identified in the study area to account for local variability in seismicity characteristics. The seismicity parameters were estimated for each of these source zones, and the seismic hazard evaluation of the Andaman-Nicobar region has been pe… Show more

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Cited by 29 publications
(6 citation statements)
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“…The spatial variation pattern of the hazard value shows good agreement with the maps of Zhang PZ et al (1999), Ram and Wang GX (2013), and Rahman et al (2018). In addition, the resulting hazard values for the Nepal area are comparable with results for the adjacent regions in India (e.g., Kolathayar and Sitharam, 2012;Nath and Thingbaijam, 2012) and Tibet (Rahman et al, 2018). The rock-site PGA value around the epicenter of the 2015 Gorkha earthquake shown in previous studies (e.g., Chaulagain et al, 2015;Ram and Wang GX, 2013;Zhang PZ et al, 1999) is below 0.4g.…”
Section: Conclusion and Discussionsupporting
confidence: 83%
See 1 more Smart Citation
“…The spatial variation pattern of the hazard value shows good agreement with the maps of Zhang PZ et al (1999), Ram and Wang GX (2013), and Rahman et al (2018). In addition, the resulting hazard values for the Nepal area are comparable with results for the adjacent regions in India (e.g., Kolathayar and Sitharam, 2012;Nath and Thingbaijam, 2012) and Tibet (Rahman et al, 2018). The rock-site PGA value around the epicenter of the 2015 Gorkha earthquake shown in previous studies (e.g., Chaulagain et al, 2015;Ram and Wang GX, 2013;Zhang PZ et al, 1999) is below 0.4g.…”
Section: Conclusion and Discussionsupporting
confidence: 83%
“…The weight assessment and thereby the ranking of different GMPEs are not carried out because of scarcity of strong motion records in the Himalayan‐Tibetan region. Due to insufficient observed data, many seismic hazard studies for Asian countries (e.g., Chaulagain et al, ; Kolathayar and Sitharam, ; Nath and Thingbaijam, ; Ornthammarath et al, ) used equal weight for all models. In this study, therefore, for each of these four models, equal probabilistic weights (1/4) are assigned.…”
Section: Methodsmentioning
confidence: 99%
“…Over the past decades, numerous seismic hazard studies have been conducted with the two methods (e.g., Joshi et al, 2007;Kolathayar and Sitharam, 2012;Moratto et al, 2007;Sitharam and Vipin, 2011;Stirling et al, 2011). The two methods have also been prescribed in various technical references.…”
Section: Dsha Versus Pshamentioning
confidence: 99%
“…PSHA and DSHA are the two representative approaches in assessing earthquake hazards. Over the past decades, numerous seismic hazard studies have been conducted with the two methods (e.g., Joshi et al, 2007;Kolathayar and Sitharam, 2012;Moratto et al, 2007;Sitharam and Vipin, 2011;Stirling et al, 2011 It is worth noting that extensive discussions over the pros and cons of the two methods have been reported in the literature (e.g., Bommer, 2003;Castanos and Lomnitz, 2002;Krinitzsky, 2003;Klugel, 2008). In general, DSHA is a simple approach that earthquake scenarios are considered logically understandably, but the uncertainties in DSHA may not be well quantified.…”
Section: Dsha Versus Pshamentioning
confidence: 99%