2013
DOI: 10.3724/sp.j.1246.2013.02016
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Source rupture process inversion of the 2013 Lushan earthquake, China

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Cited by 5 publications
(4 citation statements)
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“…The linear inversion model carried out using extended dimensions (compared to the non-linear inversion) of the source faults has helped to derive the distributed slip along the fault planes. The seismic moment and magnitude obtained based on linear inversion model is comparable to the values reported by Lifen et al (2013) and Zhao et al (2013), using teleseismic body wave data.…”
Section: Discussionsupporting
confidence: 72%
“…The linear inversion model carried out using extended dimensions (compared to the non-linear inversion) of the source faults has helped to derive the distributed slip along the fault planes. The seismic moment and magnitude obtained based on linear inversion model is comparable to the values reported by Lifen et al (2013) and Zhao et al (2013), using teleseismic body wave data.…”
Section: Discussionsupporting
confidence: 72%
“…According to the results of the seismic stress change analysis, shown in Fig. 4, there are several potential earthquake zones, including along the west coasts of Aceh, Nias, and Bengkulu, in addition to the Mentawai seismic gap zones [37], [38], [41], [42]. In more detail, it shows that the seismic stress zone has consistently increased by the depth of 30-50 kms for the Bengkulu west coast.…”
Section: Resultsmentioning
confidence: 94%
“…3b, highlights a Mentawai seismic gap zone. The pattern of the increased seismic stress in the gap zone will not only trigger major earthquakes in Mentawai islands, but also tsunamis that are assumed to bring about effects upon the densely populated cities and coastal areas around West Sumatra within about 30 minutes [8], [37]- [40].…”
Section: Resultsmentioning
confidence: 99%
“…The P-wave first motion method (Reasenberg and Oppenheimer 1985;Hardebeck and Shearer 2002), the P-wave and S-wave amplitude ratio method (Kisslinger et al 1981;Snoke et al 1984), and the waveform moment tensor inversion (Dreger and Helmberger 1993;Zhu and Rivera 2002) are common methods to solve for focal mechanism solution at present. Focal mechanism solutions have been applied to the source process (Yue and Lay 2013;Zhang et al 2013;Zhang et al 2016) and have become indispensable data for earthquake researchers to carry out study on regional stress fields and seismic hazard assessment (Gephart and Forsyth 1984;Gephart 1990;Arnold and Townend 2007;Martínez et al 2013;Tan et al 2016).…”
Section: Introductionmentioning
confidence: 99%