黑龙江争光金矿地质地球化学研究  

GEOLOGY AND GEOCHEMISTRY OF ZHENGGUANG GOLD DEPOSIT,HEILONGJIANG PROVINCE

作　　者：武子玉[1] 孙有才 王保全 

机构地区：[1]吉林大学地球信息探测仪器教育部重点实验室,长春130026 [2]黑龙江齐齐哈尔矿产勘查开发总院,齐齐哈尔110032

出　　处：《地质与勘探》2006年第1期38-42,共5页Geology and Exploration

基　　金：中国地质调查项目(编号:199920190116);吉林大学创新基金项目(编号:403010123091)资助

摘　　要：通过氢、氧、铅同位素和流体包裹体测试,结合争光金矿床的地质、微量元素、稀土元素地球化学特征研究,表明争光金矿为岩浆低温热液矿床。成矿物质主要来源于地层,矿化类型为蚀变岩型和石英脉型。成矿流体为岩浆水、变质水和大气降水的混合液。δD值为-63‰^-85‰,1δ8O水值为-0.2‰^-7.0‰,主成矿阶段温度为133~276℃。The Zhengguang gold deposit, occurring in Yanshanian intrusive and Carboniferous ore -bearing formations, is a low temperature hydrothermal deposit. There are altered - rock type and quartz type orebodies. Geochemical investigation reveals that the ore - forming fluids originated from the mixing of magmatie, formation and meteoritic water. The measured temperature data of fluid inclusions show that gold deposit is featured with low tempera- ture （ 133℃ - 276℃ ）, δ^18 OH2O values of quartz from - 0.2‰ to - 7.0‰, δD V-SMOW values of quartz from - 63‰ to - 85 ‰,

关 键 词：地球化学 金矿床 成因 

分 类 号：P618.51[天文地球—矿床学] P632[天文地球—地质学]