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作 者:Zehua Qiu Shunliang Chi Zhenming Wang Seth Carpenter Lei Tang Yanping Guo Guang Yang
机构地区:[1]Institute of Crustal Dynamics, China Earthquake Administration [2]Earthquake Administration of Hebi [3]Kentucky Geological Survey, University of Kentucky [4]Guza Seismic Station, Earthquake Administration of Sichuan Province
出 处:《Earthquake Science》2015年第3期209-214,共6页地震学报(英文版)
基 金:supported by the Special Fund for Earthquake Research in the Public Interest(No.201108009)
摘 要:At a sampling rate of 100 samples per second,the YRY-4 four-gauge borehole strainmeters(FGBS) are capable of recording transient strains caused by seismic waves such as P and S waves or strain seismograms. At such a high sampling rate, data from the YRY-4 strainmeters demonstrate fairly satisfactory self-consistency. The strain tensor seismograms demonstrate the senses of motion of P waves, that is, the type of seismic wave travels in the direction of the maximum normal strain change. The observed strain patterns of S waves significantly differ from those of P waves and should contain information about the source mechanism. Spectrum analysis shows that the strain seismograms are consistent with conventional broadband seismograms from the same site.At a sampling rate of 100 samples per second,the YRY-4 four-gauge borehole strainmeters(FGBS) are capable of recording transient strains caused by seismic waves such as P and S waves or strain seismograms. At such a high sampling rate, data from the YRY-4 strainmeters demonstrate fairly satisfactory self-consistency. The strain tensor seismograms demonstrate the senses of motion of P waves, that is, the type of seismic wave travels in the direction of the maximum normal strain change. The observed strain patterns of S waves significantly differ from those of P waves and should contain information about the source mechanism. Spectrum analysis shows that the strain seismograms are consistent with conventional broadband seismograms from the same site.
关 键 词:Four-gauge borehole strainmeter(FGBS) Strain seismogram P-wave S-wave Self-consistency Spectrum analysis
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