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青岛钻孔体应变短时畸变分析

Study on the short time distortion anomaly of borehole volume strain in Qingdao

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【作者】 冯志军赵金花荆强陈安范殷海涛李杰

【Author】 FENG Zhi-jun1,ZHAO Jin-hua1,JING Qiang1,CHEN An-fan2,YIN Hai-tao1,LI Jie1(1.Earthquake Administration of Shandong Province,Jinan,Shandong 250014,China;2.Agriculture Service Center of Xing’an Street of Shandong Province,Anqiu,Shandong 262100,China)

【机构】 山东省地震局山东安丘市兴安街道农业服务中心

【摘要】 在分析青岛钻孔体应变干扰的基础上,对青岛钻孔体应变出现的短时畸变进行了统计分析。结果表明,青岛钻孔体应变短时畸变可能是钻孔岩壁岩块掉落引起的张性异常,不是地震前兆异常;短时畸变与气压短时突变波动引起的信号均包含有2 m in~5 m in周期信号,比正常时多了5 m in的周期信号,两者的高频信号幅值相同,约为正常的1.5倍;气压的短时突变可引起青岛体应变观测出现固体潮同步波动畸变和曲线加粗变化。

【Abstract】 Statistically analyzes the short time distortion anomalies of borehole volume strain in Qingdao based on analyzing the interference.Results show that these distortion anomalies are probably tensional anomalies caused by dropping rocks from the wellface rather than precursory anomalies.The signal caused by the short time distortion anomaly and pressure fluctuation include 2~5 minutes period,and 5 minutes more than normal signal,and the same high-frequency amplitude of them were about 1.5 times than normal.The short time mutation of pressure cause solid tide synchronal distortion and curve change thicker in Qingdao volume strain observation.

【关键词】 青岛钻孔体应变干扰畸变
【Key words】 Qingdaoborehole volume straininterferencedistortion anomalies
【基金】 “十一五”科技支撑项目(2006BAC01B03—03—04);2007年山东省地震局合同制项目资助
  • 【文献出处】 山西地震 ,Earthquake Research in Shanxi , 编辑部邮箱 ,2009年04期
  • 【分类号】P315.63
  • 【被引频次】1
  • 【下载频次】37
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