西影深井水位变化与临潼—长安断裂活动  

WATER LEVEL CHANGE AT THE XIYING DEEP WELL REFLECTS THE FAULTING ACTIVITY ONLINTONG -CHANG' AN FAULT

作　　者：景北科[1] 

机构地区：[1]陕西省地震局

出　　处：《内陆地震》1993年第1期74-80,共7页Inland Earthquake

摘　　要：把消除掉气压、固体潮效应后的西影井水位值与临潼——长安断裂带上的垂直形变值进行相关分析,发现二者有一定的相关性。可以看出,西影深井水位变化在某种程度上反映着井位附近的断层活动。最后作者对其形成原因进行了粗浅的分析。Through the correlation analysis between the water level at Xiying deep well after removing the effects of pressure and solid tide and the vertical deformation in Lintong-Chang'an fault,it is found that there is some correlation between them. We may get a conclusion that the water level change reflects the faulting activity around the well to a certain extent. Finally,the author made a roughly analysis on its cause.

关 键 词：水位 临潼─长安 断裂 相关性 地震 

分 类 号：P315.7[天文地球—地震学]