反射系数K法在岩溶探测中的应用  

THE APPLICATION OF REFLECTION COEFFICIENT K METHOD TO THE KARST DETECTION

作　　者：陈绍求[1] 肖志强 

机构地区：[1]中南工业大学地质系,湖南长沙410083

出　　处：《物探与化探》2000年第3期225-229,共5页Geophysical and Geochemical Exploration

摘　　要：岩溶是导致地层塌陷的主要原因。利用反射系数K法解释电测深 ρs 曲线 ,能突出溶洞引起的异常 。Karst is the main factor responsible for the collapse of strata.The application of reflection coefficient K method to the interpretation of electric sounding ρ s curve can make prominent anomalies caused by karst and obviously reflect the existence of underground karst.

关 键 词：电阻率测深 反射系数K法 岩溶 探测 

分 类 号：P642.25[天文地球—工程地质学] P631.322[天文地球—地质矿产勘探]