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The Statistical Relationship between the Maximum Amplitude of the Body Strain Record and the Surface-wave Magnitude and Epicenter Distance

The Statistical Relationship between the Maximum Amplitude of the Body Strain Record and the Surface-wave Magnitude and Epicenter Distance
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摘要 Based on the body strain record of Tiantanghe station from 2008 to 2014,we make a statistical analysis of the relationship between the maximum amplitude of the body strain record and the surface-wave magnitude,epicenter distance of the earthquakes,which occurred in the Chinese mainland and its surrounding areas with MS≥6. 0 and the rest of the world with MS≥7. 0. According to statistical results,we propose a statistical formula between the surface-wave magnitude of earthquake and the maximum amplitude of the body strain record,the epicenter distance: M_S~*= 0. 37 ln A_max+ 0. 57 ln D + 0. 07. We can also derive a theoretical estimation formula for the maximum amplitude: A_max=e^(2. 7(M_S^*-0. 07))D^(-1. 54). This demonstrates that the maximum amplitude of the body strain record increases exponentially with the increase of the surface-wave magnitude, and decreases with the increase of the epicenter distance,and shows a negative correlation with their product. We further discuss the necessity of adding instruments with high frequency sampling to earthquake monitoring, and dicuss the prospects for precise earthquake prediction in future. Based on the body strain record of Tiantanghe station from 2008 to 2014, we make a statistical analysis of the relationship between the maximum amplitude of the body strain record and the surface-wave magnitude, epicenter distance of the earthquakes, which occurred in the Chinese mainland and its surrounding areas with Ms≥6. 0 and the rest of the world with Ms ≥7. 0. According to statistical results, we propose a statistical formula between the surface-wave magnitude of earthquake and the maximum amplitude of the body strain record, the epicenter distance : Ms = 0. 371nAmax + 0. 571nD + 0. 07. We can also derive a theoretical estimation formula for the maximum amplitude: Amax = e2.7(Ms^-0.07)D^-1.54. This demonstrates that the maximum amplitude of the body strain record increases exponentially with the increase of the surface-wave magnitude, and decreases with the increase of the epicenter distance, and shows a negative correlation with their product. We further discuss the necessity of adding instruments with high frequency sampling to earthquake monitoring, and dicuss the prospects for precise earthquake prediction in future.
出处 《Earthquake Research in China》 CSCD 2017年第1期107-115,共9页 中国地震研究(英文版)
基金 founded by the Combined Project of Monitoring,Prediction and Research of China Earthquake Administration entitled "Statistical Study on the Earthquake Cases of Imminent Anomaly in Sacks Volume Strain Measurements (154201)" the Operation Maintenance of Shisanling Seismic Station,Institute of Earthquake Science,CEA(40417600105)
关键词 Body strain Seismic wave Statistical analysis High sampling rate Earthquake monitoring Earthquake prediction Body strain Seismic wave Statistical analysis High sampling rate Earthquake monitoring Earthquake prediction
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