鄂南地区蛇屋山与富水卡林型金矿床的矿床地质特征对比及找矿标志研究  

Study on prospecting criteria and deposit geology comparison between Shewushan and Fushui Carlin type gold deposit,southern Hubei

作　　者：刘蕴光 王敏芳[2,3] 肖凡[2] 

机构地区：[1]山东省第八地质矿产勘察院,276826 [2]中国地质大学(武汉)资源学院 [3]中国地质大学(武汉)地质过程与矿产资源国家重点实验室

出　　处：《黄金》2012年第3期17-23,共7页Gold

基　　金：国家自然科学基金青年科学基金项目(40902026);地质过程与矿产资源国家重点实验室开放课题项目(GPMR201006);中央高校基本科研业务费专项资金项目(CUG090102)

摘　　要：蛇屋山金矿床是20世纪90年代初在鄂南地区发现的最大规模的卡林型金矿床,与其相邻的富水卡林型金矿床也属同种类型。在总结前人有关研究成果的基础上,综合分析蛇屋山与富水卡林型金矿床的成矿地质条件,认为二者具有相同的成矿地质背景和矿床地质特征,并且形成于同一时期。因此,认为鄂南地区具有较好的卡林型金矿床找矿远景,并以此为基础初步对鄂南地区卡林型金矿床的找矿标志进行了总结。Shewushan gold deposit was found in early 1990s as one of the largest carlin-type deposits in south Hubei China,and the adjacent gold deposit Fushui also belongs to the Carlin type.Based on the former researchers＇achievements,we compared the geological factors of metallogenesis between Shewushan and Fushui gold deposits,which have the similar geological background of metallogenesis and geologic features of the deposits and came into form during the same metallogenetic age.Therefore,we draw a conclusion that south of Hubei has fairly good potentials for Carlin-type gold deposit prospecting.At last,several prospecting criteria in this area were summarized.

关 键 词：矿床地质特征 找矿标志 卡林型金矿床 蛇屋山金矿床 富水金矿床 鄂南地区 

分 类 号：P618.51[天文地球—矿床学]