Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake
Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times diff...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hu, Xiaogang [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Acta seismologica Sinica - Beijing, 1988, 26(2013), 3-4 vom: Aug., Seite 169-177 |
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| Übergeordnetes Werk: |
volume:26 ; year:2013 ; number:3-4 ; month:08 ; pages:169-177 |
| Links: |
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| DOI / URN: |
10.1007/s11589-013-0029-9 |
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| Katalog-ID: |
SPR020952481 |
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| 520 | |a Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. | ||
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10.1007/s11589-013-0029-9 doi (DE-627)SPR020952481 (SPR)s11589-013-0029-9-e DE-627 ger DE-627 rakwb eng Hu, Xiaogang verfasserin aut Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 Jiang, Ying aut Enthalten in Acta seismologica Sinica Beijing, 1988 26(2013), 3-4 vom: Aug., Seite 169-177 (DE-627)516023276 (DE-600)2245562-0 1993-1344 nnns volume:26 year:2013 number:3-4 month:08 pages:169-177 https://dx.doi.org/10.1007/s11589-013-0029-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 GBV_ILN_2037 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2119 GBV_ILN_2129 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4753 AR 26 2013 3-4 08 169-177 |
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10.1007/s11589-013-0029-9 doi (DE-627)SPR020952481 (SPR)s11589-013-0029-9-e DE-627 ger DE-627 rakwb eng Hu, Xiaogang verfasserin aut Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 Jiang, Ying aut Enthalten in Acta seismologica Sinica Beijing, 1988 26(2013), 3-4 vom: Aug., Seite 169-177 (DE-627)516023276 (DE-600)2245562-0 1993-1344 nnns volume:26 year:2013 number:3-4 month:08 pages:169-177 https://dx.doi.org/10.1007/s11589-013-0029-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 GBV_ILN_2037 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2119 GBV_ILN_2129 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4753 AR 26 2013 3-4 08 169-177 |
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10.1007/s11589-013-0029-9 doi (DE-627)SPR020952481 (SPR)s11589-013-0029-9-e DE-627 ger DE-627 rakwb eng Hu, Xiaogang verfasserin aut Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 Jiang, Ying aut Enthalten in Acta seismologica Sinica Beijing, 1988 26(2013), 3-4 vom: Aug., Seite 169-177 (DE-627)516023276 (DE-600)2245562-0 1993-1344 nnns volume:26 year:2013 number:3-4 month:08 pages:169-177 https://dx.doi.org/10.1007/s11589-013-0029-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 GBV_ILN_2037 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2119 GBV_ILN_2129 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4753 AR 26 2013 3-4 08 169-177 |
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10.1007/s11589-013-0029-9 doi (DE-627)SPR020952481 (SPR)s11589-013-0029-9-e DE-627 ger DE-627 rakwb eng Hu, Xiaogang verfasserin aut Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 Jiang, Ying aut Enthalten in Acta seismologica Sinica Beijing, 1988 26(2013), 3-4 vom: Aug., Seite 169-177 (DE-627)516023276 (DE-600)2245562-0 1993-1344 nnns volume:26 year:2013 number:3-4 month:08 pages:169-177 https://dx.doi.org/10.1007/s11589-013-0029-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 GBV_ILN_2037 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2119 GBV_ILN_2129 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4753 AR 26 2013 3-4 08 169-177 |
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10.1007/s11589-013-0029-9 doi (DE-627)SPR020952481 (SPR)s11589-013-0029-9-e DE-627 ger DE-627 rakwb eng Hu, Xiaogang verfasserin aut Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 Jiang, Ying aut Enthalten in Acta seismologica Sinica Beijing, 1988 26(2013), 3-4 vom: Aug., Seite 169-177 (DE-627)516023276 (DE-600)2245562-0 1993-1344 nnns volume:26 year:2013 number:3-4 month:08 pages:169-177 https://dx.doi.org/10.1007/s11589-013-0029-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 GBV_ILN_2037 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2119 GBV_ILN_2129 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4753 AR 26 2013 3-4 08 169-177 |
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Hu, Xiaogang misc Free oscillations misc Moment tensor solution misc Seismic moment Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake |
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Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake Free oscillations (dpeaa)DE-He213 Moment tensor solution (dpeaa)DE-He213 Seismic moment (dpeaa)DE-He213 |
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evaluation of the seismic moment of the april 20, 2013 lushan earthquake |
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Evaluation of the seismic moment of the April 20, 2013 Lushan earthquake |
| abstract |
Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 |
| abstractGer |
Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 |
| abstract_unstemmed |
Abstract The April 20, 2013 Lushan earthquake which occurred in Sichuan, China had only moderate thrust. However, the computed seismic moments (M0) for the Lushan earthquake calculated by several institutions differ significantly from 0.4 × $ 10^{19} $ to 1.69 × $ 10^{19} $ Nm, up to four times difference. We evaluate ten computed M0s by using normal mode observations from superconducting gravimeters in Mainland China. We compute synthetic normal modes on the basis of moment tensor solutions and fit them to the observed normal modes. Comparison of our results indicates that M0 is the main cause for some large differences between observations and synthetics. We suggest that a moment magnitude of Mw6.6, corresponding to a M0 of 0.97–1.08 × $ 10^{19 } $Nm, characterizes the size and strength of the seismic source of the Lushan earthquake. © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013 |
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