孕震过程中深部流体对浅层流体影响的研究进展概述  

Summarization of advance in study of influence of deep fluid on shallow fluid in the seismogenic process

作　　者：高安泰[1] 杨多兴[1] 刘耀炜[1] 

机构地区：[1]中国地震局兰州地震研究所,甘肃兰州730000

出　　处：《地震》2002年第4期24-29,共6页Earthquake

基　　金：十五"国家科技攻关项目(2001BA601B0203)

摘　　要：深部流体,尤其是深部热流体已成为目前研究地震孕育及前兆成因的重要内容,特别是由于深部流体活动引起浅层流体的变化,是探索地震预报方法的重要途径。由于人们在现有的能力范围内只能通过观察研究浅层流体来了解深部流体的变化,所以通过研究深部流体与浅层流体的相互关系,进而了解深部流体的变化,对于研究孕震过程、前兆成因机理以及地震预报的理论和方法,都具有十分重要的意义。Study of deep fluid, especially study of deep heat fluid has become important content for studying the seismogenic process and precursory formation. In particular, change of shallow fluid, which results from activity of deep fluid, is important way to explore the method of earthquake prediction. Because the scientists understand the change of deep fluid only by studying shallow fluid in the range of current ability, studying correlation between deep fluid and shallow fluid, finding change of deep fluid by correlation is of important significance in studying the seismogenic process and the precursory mechanism as well as the theory and method of earthquake prediction.

关 键 词：孕震过程 地下流体 深部流体 浅层流体 地震预报 

分 类 号：P315.723[天文地球—地震学]