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《Progress in Geophysics》 2007-06
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Discussion on strain tidal factor separation and anisotropy——Analysis of first data of borehole component strain-meter of China's digital seismological observational networks

CHI Shun-liang1,WU Hong-ling2,LUO Ming-jing3(1.Hebi Seismological Bureau,Hebi 458030,China2.China Geological Academy Geological Mechanics Institute,Beijing 100085,China3.Henan Seismological Bureau,Zhengzhou 450000,China)  
The National Digital Seismological Observational Networks plans to install in China's mainland 40 YRY-4 Borehole Strain meters developed by CHI Shun-liang.First set of data has been analysesed,and from the best quality data,relative accuracy of M2 wave factor can reach 0.001,which is better than the best long-base cave strain meters.We also discovered at various borehole strain-meter stations tidal response(tidal factor) are separate and have orderly anisotropy.We believe that fault isolation is the cause of separation and anisotropy.Finite element model of fault block's azimuth response has contingency with measured response,which supports this hypothesis.The anisotropy of tidal response will be helpful at geologic structure research,city fault survey,land block micro activity,earthquake intensity area delimit.And it can also improve tidal displacement revises of GPS data.
【CateGory Index】: P315.7
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