Simulation of Strong Ground Motion of the 2009 Bhutan Earthquake Using Modified Semi-Empirical Technique
On 21st September 2009 an earthquake of magnitude ( M w 6.1) occurred in the East Bhutan. This earthquake caused serious damage to the residential area and was widely felt in the Bhutan Himalaya and its adjoining area. We estimated the source model of this earthquake using modified semi empirical te...
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| Veröffentlicht in: | Pure and applied geophysics 2017-12, Vol.174 (12), p.4343-4356 |
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| creator | Sandeep Joshi, A. Lal, Sohan Kumar, Parveen Sah, S. K. Vandana Kamal |
| description | On 21st September 2009 an earthquake of magnitude (
M
w
6.1) occurred in the East Bhutan. This earthquake caused serious damage to the residential area and was widely felt in the Bhutan Himalaya and its adjoining area. We estimated the source model of this earthquake using modified semi empirical technique. In the rupture plane, several locations of nucleation point have been considered and finalised based on the minimum root mean square error of waveform comparison. In the present work observed and simulated waveforms has been compared at all the eight stations. Comparison of horizontal components of actual and simulated records at these stations confirms the estimated parameters of final rupture model and efficacy of the modified semi-empirical technique (Joshi et al., Nat Hazards 64:1029–1054,
2012b
) of strong ground motion simulation. |
| doi_str_mv | 10.1007/s00024-017-1663-2 |
| format | Article |
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M
w
6.1) occurred in the East Bhutan. This earthquake caused serious damage to the residential area and was widely felt in the Bhutan Himalaya and its adjoining area. We estimated the source model of this earthquake using modified semi empirical technique. In the rupture plane, several locations of nucleation point have been considered and finalised based on the minimum root mean square error of waveform comparison. In the present work observed and simulated waveforms has been compared at all the eight stations. Comparison of horizontal components of actual and simulated records at these stations confirms the estimated parameters of final rupture model and efficacy of the modified semi-empirical technique (Joshi et al., Nat Hazards 64:1029–1054,
2012b
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M
w
6.1) occurred in the East Bhutan. This earthquake caused serious damage to the residential area and was widely felt in the Bhutan Himalaya and its adjoining area. We estimated the source model of this earthquake using modified semi empirical technique. In the rupture plane, several locations of nucleation point have been considered and finalised based on the minimum root mean square error of waveform comparison. In the present work observed and simulated waveforms has been compared at all the eight stations. Comparison of horizontal components of actual and simulated records at these stations confirms the estimated parameters of final rupture model and efficacy of the modified semi-empirical technique (Joshi et al., Nat Hazards 64:1029–1054,
2012b
) of strong ground motion simulation.</description><subject>Computer simulation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquake damage</subject><subject>Earthquakes</subject><subject>Geophysics/Geodesy</subject><subject>Ground motion</subject><subject>Hazards</subject><subject>Motion simulation</subject><subject>Parameter estimation</subject><subject>Parameter modification</subject><subject>Residential areas</subject><subject>Rupture</subject><subject>Rupturing</subject><subject>Seismic activity</subject><subject>Simulation</subject><subject>Waveforms</subject><issn>0033-4553</issn><issn>1420-9136</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kLFOwzAQhi0EEqXwAGyWmA1nO7GTEapSkFoxtJ0tJ3EalyZu7WTg7XEVkFiYTjr933-6D6F7Co8UQD4FAGAJASoJFYITdoEmNGFAcsrFJZoAcE6SNOXX6CaEPcSgTPMJata2HQ66t67Drsbr3rtuhxfeDV2FV-533zcGM4AcvzRDrzs8175vToP-NHgbbCRWrrK1NRVem9aSeXu03pb6gDembDp7Gswtuqr1IZi7nzlF29f5ZvZGlh-L99nzkmjO854wnaSZzCQFWbIMTCakYFJUJikLwXPGRKGLtDSZSSuqc0OhLsrEsDr-WmYG-BQ9jL1H7-LZ0Ku9G3wXTyqaCyllnopzio6p0rsQvKnV0dtW-y9FQZ2FqlGoip7UWahikWEjE2K22xn_p_lf6BvmWXeS</recordid><startdate>20171201</startdate><enddate>20171201</enddate><creator>Sandeep</creator><creator>Joshi, A.</creator><creator>Lal, Sohan</creator><creator>Kumar, Parveen</creator><creator>Sah, S. 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K.</au><au>Vandana</au><au>Kamal</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Simulation of Strong Ground Motion of the 2009 Bhutan Earthquake Using Modified Semi-Empirical Technique</atitle><jtitle>Pure and applied geophysics</jtitle><stitle>Pure Appl. Geophys</stitle><date>2017-12-01</date><risdate>2017</risdate><volume>174</volume><issue>12</issue><spage>4343</spage><epage>4356</epage><pages>4343-4356</pages><issn>0033-4553</issn><eissn>1420-9136</eissn><abstract>On 21st September 2009 an earthquake of magnitude (
M
w
6.1) occurred in the East Bhutan. This earthquake caused serious damage to the residential area and was widely felt in the Bhutan Himalaya and its adjoining area. We estimated the source model of this earthquake using modified semi empirical technique. In the rupture plane, several locations of nucleation point have been considered and finalised based on the minimum root mean square error of waveform comparison. In the present work observed and simulated waveforms has been compared at all the eight stations. Comparison of horizontal components of actual and simulated records at these stations confirms the estimated parameters of final rupture model and efficacy of the modified semi-empirical technique (Joshi et al., Nat Hazards 64:1029–1054,
2012b
) of strong ground motion simulation.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s00024-017-1663-2</doi><tpages>14</tpages></addata></record> |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Computer simulation Earth and Environmental Science Earth Sciences Earthquake damage Earthquakes Geophysics/Geodesy Ground motion Hazards Motion simulation Parameter estimation Parameter modification Residential areas Rupture Rupturing Seismic activity Simulation Waveforms |
| title | Simulation of Strong Ground Motion of the 2009 Bhutan Earthquake Using Modified Semi-Empirical Technique |
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