导水裂隙带高度探测新方法综述  

ANALYSIS OF NEW METHOD OF DETECTION OF THE HEIGHT OF TRANSMISSIVE FRACTURING BELT

作　　者：熊晓英[1] 

机构地区：[1]淮南职业技术学院,安徽淮南232001

出　　处：《安徽地质》2004年第2期95-98,共4页Geology of Anhui

摘　　要：确定导水裂隙带高度的方法主要有两类:一类是实际探测法;另一类是理论计算和经验公式计算法。随着科技技术的发展,近年来又产生和发展了许多新的探测技术和方法。本文主要介绍了几种探测新方法的工作原理和方法,并对其进行了分析比较。为准确地探测导水裂隙带高度,实际应用中应根据实际情况具体分析,合理地选择探测方法和手段。There are two kinds of methods on determination of the height of transmissive fracturing belt at present.One is the practical detection.The other is by means of theoretical calculation and experiential formula.Many new methods and techniques of such kinds have been developed in recent years.The paper mainly analyzes some new methods of exploration.To accurately detect the height of a transmissive fracturing belt,a method should be reasonably chosen according to actual conditions.

关 键 词：导水裂隙带 探测 方法 

分 类 号：P641.135[天文地球—地质矿产勘探]