宁夏海原台甘盐池井水位震例分析  

Analysis of Water Level of Ganyanchi Well in Haiyuan Ningxia Hui Autonomous Region

作　　者：王晨曦 程鹏图[1] 司学芸[1] WANG Chen-xi;CHENG Peng-tu;SI Xue-yun(Earthquake Administration of Ningxia Hui Autonomous Region,Ningxia Yinchuan 750001,China)

机构地区：[1]宁夏回族自治区地震局,宁夏银川750001

出　　处：《防灾减灾学报》2018年第3期78-82,共5页Journal of Disaster Prevention And Reduction

摘　　要：海原甘盐池井位于海原断裂带内部的拉分盆地中,地处1920年海原大地震的极震区,该井自1984年观测以来,积累了30多年的数据,经过对资料的梳理,发现该井水位变化和周边是6级以上地震有较好的对应关系。Haiyuan Ganyanchi well is located in the pull apart basin inside the Haiyuan Fault zone, which is located in the epicentre area of the Haiyuan earthquake in 1920. Since 1984, this well has accumulated over 30 years of data. After combing the data, it is found that the water level changes in this well have a good correspondence with the earthquakes of over 6 earthquakes in the surrounding area.

关 键 词：海原断裂带 甘盐池井水位 6级以上地震 

分 类 号：P315.72[天文地球—地震学]