“离子晕法”及其方法学意义  

IONOMETRIC HALOES" METHOD AND ITS METHODOLOGICAL SIGNIFICANCE

作　　者：吴传璧[1] 

机构地区：[1]中国地质矿产信息研究院,北京市100037

出　　处：《地质与勘探》1997年第5期35-40,共6页Geology and Exploration

摘　　要：介绍了“离子晕法”的方法学背景和测量方法,对与被测物质赋存形式有关的问题进行了讨论。与地气法对比,推测离子晕法和地气法所测的物质可能是一类物质——赋存于气体中的固相微粒。这种认识可作为研制和改进一系列隐伏矿化探方法的基础。The methodological background and measurement method of 'ionometric haloes 'method are described.The problems concern-ing the occurrence form of the analyzed matter are discussed. Through comparison with the 'geogas', it is suggested that the matters measured by the 'geogas'and 'ionometric haloes'methods might be classified as a same type, i. e. the very fine solid particulates oc-curred in gases. This concept can be considered as the basement of developing and improving a series of geochemical exploration methods for concealed mineral deposits.

关 键 词：离子晕法 地球化学勘探 隐优矿床 

分 类 号：P632[天文地球—地质矿产勘探] P611.1[天文地球—地质学]