黑龙江省逊克县高松山金矿床地质特征及成因分析  

GEOLOGY AND GENESIS OF THE GAOSONGSHAN GOLD DEPOSIT IN XUNKE COUNTY, HEILONGJIANG PROVINCE

作　　者：边红业 陈满[1] 刘洪利[1] 赵春荣[1] 

机构地区：[1]武警黄金第一总队,黑龙江哈尔滨150086

出　　处：《地质与资源》2009年第2期91-95,共5页Geology and Resources

摘　　要：高松山金矿床是与火山作用关系密切的低温热液型金矿床.矿石类型主要为含金石英脉、构造角砾岩蚀变岩型.矿石硫同位素组成具有深源硫特点.流体包裹体中H、O同位素反映在成矿的过程中有大气降水加入.矿床产于中生代上白垩统火山岩中,与英安岩、安山岩、安山玢岩、流纹岩关系密切.岩石化学分析反映了活动大陆边缘环境.The Gaosongshan gold deposit of epithermal type is closely associated with volcanism. The ore is mainly goldbearing quartz vein and tectonic breccia-altered rock types, with sulfur compositions of deep source. The H-O isotopic compositions of fluid inclusion represent the mixture of atmospheric precipitation. The deposit is hosted in the Mesozoic Upper Cretaceous volcanic rocks, associated with dacite, andesite, andesitic porphyrite and rhyolite. The geochemical characteristics show a background of active continental margin.

关 键 词：黑龙江高松山 金矿 低温热液型 成因 

分 类 号：P618.51[天文地球—矿床学]