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作 者:王同利[1] 崔博闻[1] 李然 王丽红[1] 胡毅涛[1] 邢海林 李经山[1] Wang Tongli;Cui Bowen;Li Ran;Wang Lihong;Hu Yitao;Xing Hailin;Li Jingshan(Beijing Earthquake Agency,Beijing 100080,China)
机构地区:[1]北京市地震局,北京100080
出 处:《中国地震》2022年第3期455-463,共9页Earthquake Research in China
基 金:国家星火计划项目(XH20210401);中国地震局冬奥会保障晋冀蒙监测能力提升项目共同资助。
摘 要:基于通州地表地电阻率在1976年唐山 M 7. 8地震前有明显前兆异常以及通州新建井下小极距地电阻率在2020年古冶 M 5. 1地震和2021年滦州 M 4. 3地震前出现的异常变化,从台站周边构造环境 、地震特征等方面进行对比分析,认为通州台地电阻率对唐山地区中强地震的中短期映震能力比较强。同时分析结果也显示在目前观测环境条件下,井下小 极距地电阻率再现了通州台地电阻率对周边地区中强地震具有较强地映震能力。The surface resistivity measured at the Tongzhou station changes before and after the Tangshan M 7. 8 earthquake in 1976,and the similar resistivity changes from small well were also detected before the Tangshan Guye M 5. 1 in 2022 and the Tangshan Luanzhou M 4. 3 in 2021. In this paper we study the change mechanism of resistivity based on the tectonic surrounding the Tongzhou station,measuring ability of resistivity and the characteristics of medium-strong earthquake. The results show that the resistivity changes of Tongzhou is sensitive to the moderate and strong earthquake in Tangshan region,the small well resistivity is more significant changes before and after the earthquake than surface resistivity.
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