吉林省舒兰市长安堡大型铜钼矿床地质特征及物、化探异常查证效果  

Geological features and geophysical and geochemical anomalies verification results of Chang'anpu large copper molybdenum deposit,Shulan City of Jilin Province

作　　者：王立群[1] 李明涛[1] 张旭[1] 张永力[1] 赵威[1] 蒋秀成 

机构地区：[1]吉林省有色金属地质勘查局六〇七队,吉林吉林市132001

出　　处：《吉林地质》2013年第2期40-45,共6页Jilin Geology

摘　　要：本文介绍了吉林省舒兰市长安堡大型斑岩铜钼矿床的区域地质背景,矿区地层、岩浆、构造、围岩蚀变。分别阐述了铜矿体和钼矿体特征,以及矿区物化探特征。通过与邻区同类型矿床物化探异常模式对比,推测本区物、化探异常深部存在隐伏矿体,直接采用钻探手段进行验证异常,找矿效果非常理想。最后指明了找矿方向。The paper introduces regional geological setting,strata of mining area,magma,and structure,wall-rock alteration of Chang＇anpu large copper molybdenum deposit,Shulan City of Jilin Province.Copper and molybdenum ore body features are expounded respectively,and geophysical-geochemical characteristics of the mining area.Through the same type deposits to adjacent areas geophysical-geochemical anomaly pattern contrast,speculated that there exist deep concealed ore body by geochemical anomalies in this area,validated by drilling exploration means abnormal directly,prospecting effect is very ideal.Finally pointed out the prospecting direction.

关 键 词：舒兰长安堡 大型斑岩铜钼矿床 隐伏矿体 地质特征 物化探综合异常 找矿方向 

分 类 号：P631[天文地球—地质矿产勘探] P632[天文地球—地质学]