对较强地震造成喀什台H磁变仪磁系翻转的处理方法及有关问题的讨论  

METHOD TO HANDLE THE OVERTURN OF THE MAGNETIC SYSTEM OF H MAGNETIC VARI OMETER CAUSED BY STRONG EARTHQU AKES AND RELATED DISCUSSION

作　　者：郑黎明[1] 王居云[2] 高祥真[2] 范素琴 

机构地区：[1]新疆维吾尔自治区地震局喀什地震基准台,喀什844000 [2]新疆维吾尔自治区地震局乌鲁木齐地震基准台,乌鲁木齐830000

出　　处：《内陆地震》1998年第1期63-67,共5页Inland Earthquake

摘　　要：多年来，Ｈ 磁变仪磁系被地震震翻事件在多震区的地磁台常有发生。这不同程度地影响着磁变仪的正常工作及记录资料的连续性。如何解决这一矛盾，一直是地磁工作者关注的问题。文中主要总结并介绍了喀什台在这方面积累的经验。At geomegnetic stations in seismically active regions, the magnetic system of H magnetic variometers are frequently shocked over by earthquakes. This affects the normal work of the magnetic variometers and the succession of records. How to solve the problem has been concerned by geomagnetism workers. The Kashi station accumulates and sums up the experience in this aspect, and introduces the taken measures and received effects in this paper.

关 键 词：地磁仪 地磁水平分量 地磁观测 地震 磁系翻转 

分 类 号：P318.6[天文地球—固体地球物理学]