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在区域地质调查中围岩蚀变的研究方法
引用本文:刘大瞻, 张廉清. 1988. 在区域地质调查中围岩蚀变的研究方法. 地质通报, (2): 71-75.
作者姓名:刘大瞻  张廉清
作者单位:吉林省地矿局区域地质矿产调查所
摘    要:本文以实例介绍了,在区域地质调查工作中,运用数理统计方法,对围岩蚀变种类、强弱程度、矿物共生组合特点,以及它与已知矿产的成因联系等进行分析研究,并配合重砂和物化探资料的对比,在普查找矿工作方面,取得初步效果。


A METHOD FOR THE STUDY OF WALL-ROCK ALTERATIONS IN THE REGIONAL GEOLOGICAL SURVEY
LIU Da-zhan, ZHANG Lian-qing. 1988. A METHOD FOR THE STUDY OF WALL-ROCK ALTERATIONS IN THE REGIONAL GEOLOGICAL SURVEY. Geological Bulletin of China, (2): 71-75.
Authors:LIU Da-zhan  ZHANG Lian-qing
Abstract:In the past the emphasis of the study of wall-rock alterations is mostly on the field of gitology. People only made an isolated study on a certain deposit, and few regional-scale systematical studies were made. The study method proposed in this paper is as follows: wall-rock alterations are regarded as information for mineral prospecting and mathematic statistics is conducted according to the amount of occurrences of the alterations, their intensity and the features of the altered mineral association; then one delineates districts of wall-rock alteration intensity, finds the probability of occurrence of each alteration in the survey area and prospect, ascertains the altered mineral association genetically related to main useful minerals in the survey area, and changes the previous qualitative study into the quantitative one. The wall-rock alteration intensity districts delineated through preparation of the isopleth map of wall-rock alterations often yield almost the same prospecting results as the physical and chemical anomalies and heavy placer mineral anomalies. Thi work needs less costs because the primary information it requires can be collected by the way in the traverse survey. Its economic and social effectness are outstanding.
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