吉林白山金矿床稳定同位素地球化学特征  

Stable isotopes geochemical characteristics of gold deposit in Baishan(Hunjiang), Jilin Province

作　　者：邵兴坤[1] 李清泉[2] 闫岩[1] 陈宇[1] 宋林旭[1] 毛永新[1] 

机构地区：[1]中国人民武装警察部队黄金第一支队,黑龙江牡丹江157000 [2]吉林大学地球探测科学与技术学院,吉林长春130026

出　　处：《吉林地质》2015年第4期31-35,共5页Jilin Geology

摘　　要：白山金矿是20世纪末21世纪初在吉林南部地区发现的一种重要类型——微细浸染型金矿床。矿床赋存在活泼性较高的元古宙老岭群珍珠门组大理岩中[1]。成矿物质具有多元性,硫、金主要来源于深部岩浆,部分来源于古老壳源——早元古代老岭群碳酸盐岩;铅主要来源于早元古代老岭群碳酸盐岩,部分来源于深部岩浆;碳、氢、氧主要来源于地下水,部分来源于岩浆水和大气水。The Baishan（Hunjiang） gold deposit is an important type-the micro-disseminated one which was discovered in recent years in the south Jilin Province. The deposit is formed in more active marble of Zhenzhumen Fro. in Proterozoic Laoling Group. Mineralization material has multiple properties. The substances of sulfur and gold mostly rooted in deep magma, partly rooted in age-old the earth＇s crust-early Proterozoic Era Laoling Group carbonated rock. The substance of lead mostly rooted in early Proterozoic era Laoling Group carbonated rock, partly rooted in deep magma. The substances of carbon, hydrogen and oxygen mostly rooted in ground water, partly rooted in magma water and atmosphere water.

关 键 词：微细浸染型金矿床 稳定同位素 成矿物质及来源 吉林南部地区 

分 类 号：P618.51[天文地球—矿床学]