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作 者:于海生[1] 陆明勇[1] 杜建国[2] 李宁[1] 张金城[1] 刘天海[1] 寇建新[1] YU Hai-sheng LU Ming-yong DU Jian-guo LINing ZHANG Jin-cheng LIU Tian-hai KOU Jian-xin(National Earthquake Response Support Agency, Beijing 100049 , China Institute of Earthquake Forecasting of China Earthquake Administration, Beijing 100036, China)
机构地区:[1]中国地震应急搜救中心,北京100049 [2]中国地震局地震预测研究所,北京100036
出 处:《内陆地震》2017年第3期290-295,共6页Inland Earthquake
基 金:地震星火计划项目(XH14057)
摘 要:北京南口跨断层流动水准监测场地布设于南口—山前断裂与南口—孙河断裂交汇处。运用前人地质构造研究成果、监测资料和野外地质考察资料等,研究了南口跨断层流动水准场地监测和布设状况、结果表明:(1)监测场地存在未跨断裂测线;(2)4号测点不为基岩点且可能在断裂带内;(3)测线巨大突变异常是大量降雨所致,不为前兆异常或断裂活动。Cross-fault flow level site of Beijing Nankou laid the interchange of Nankou mountain fault and Nankou Sunhe fault. In this paper,the monitoring and layout of cross-fault flow level site in Beijing Nankou was studied,using the geological structure of previous research,monitoring data and field geological survey data,etc.. Result showed that:( 1) No cross-breaking survey line existed in cross-fault flow level site in Beijing Nankou.( 2) No. 4 measuring point was not bedrock point and within the fault zone.( 3) Measuring line large anomaly was caused by huge rainfall,not precursory anomaly or fault activity.
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