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合肥地震台短水准异常与周边地震活动分析

Analysis on short range leveling abnormalities in Hefei Seismic Station and earthquake activities of its surrounding area

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【作者】 葛计划熊瑛孙军陈勇周自强顾乃根杨军

【Author】 Ge Jihua~(1)),XiongYing~(2)),Sun Jun~(1)),Chen Yong~(1)),Zhou Ziqiang~(1)),Gu Naigen~(1))and Yang Jun~(1)) 1)Hefei Seismic Station,Anhui Province 231607,China 2)Earthquake Administration of Anhui Province,Hefei 230031,China

【机构】 合肥地震台安徽省地震局

【摘要】 以合肥地震台跨断层短水准数据,结合地区小震释放能量,分析历史测量资料在地震期间的变化,并研究辅助资料对测量资料的影响,得出:①降水可能造成敏感地块的断层形变异常,但在区域应力作用断层到一定强度时,断层形变异常仍具有一定前兆意义;②安徽地区小震释放能量与合肥地震台断层形变存在一定相关性,断层活动连续几个月持续拉张或挤压,在近区常有地震(或小震群)对应较好,由于资料对应地震的震中方位的差异,说明资料可以反映区域应力场的变化。

【Abstract】 In this paper,the characteristics of fault deformation evolution was analyzed based on the cross-fault leveling data of Hefei Seismic Station during earthquake occurring in its surrounding area,and the cross-fault leveling data influenced by assist observation data also have been studied.The conclusions are as follows:1)though the rainfall can lead to the fault deformation, the fault deformation anomaly still have precursory significance in some degree when the regional stress have intensity effect on the fault.2)the release energy of small earthquake of its surrounding area have relations with the cross-fault deformation,if the fault trend to a direction for several months,small earthquakes(or earthquake)activity in its surrounding area will be enhance.The data can reflect the regulation of regional stress field because of difference between data and the epicentral azimuth.

【基金】 中国地震局“三结合课题”;安徽省地震局合同制课题201021资助
  • 【文献出处】 地震地磁观测与研究 ,Seismological and Geomagnetic Observation and Research , 编辑部邮箱 ,2011年05期
  • 【分类号】P315.5
  • 【被引频次】3
  • 【下载频次】8
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