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吉林省放牛沟多金属矿床两种类型地球化学异常的成因研究与判别
GEONETIC STUDY AND OISCRIMINATION BETWEEN TWO KINDS OF GEOcHEMICAL ANOMALIES IN THE FANGNIUGOU POL YMETALLIC DEPOSIT,JILIN PROVINCE
【摘要】 本文通过对黄铁矿的地球化学成因研究,查明吉林省放牛沟多金属矿床的围岩中存在同生沉积成因(无找矿意义)与后生热液矿化成因(具有找矿意义)地球化学异常,两者有明显区别。根据异常的元素相关性、指示元素组合、异常强度和判别分析等特征,建立了判别两种不同成因异常的标志,并利用这些标志评价了未知异常的含矿潜力。
【Abstract】 Through the studies of geochemical genesis of pyrite ,we found out that there are syn-genetic sedimentation (having no exploratory significance)and epigenetic hydrothermal miner-alized anomaly(having exploratory significance)in the country roeks of the Fangniugou poly-metallic deposit, Jilin province,and there are obvious differences between two kinds of geo-chemicalies.The indicators discriminating two kinds of geochemical anomalies were set up ac-cording to correlation of anomaly elements,the association of anomaly element, the intensityof anomaly and the discrimination analysis etc..Meanwhile,the ore bearing of the unknownanomalies are evaluated by using the indicators.
- 【文献出处】 吉林地质 ,JILIN GEOLGY , 编辑部邮箱 ,1994年04期
- 【分类号】P618.201
- 【下载频次】101