摘要
富文金矿位于华南褶皱系五指山褶皱带北东段偏中部、昌江-琼海深大断裂南侧,产于燕山晚期花岗闪长岩体附近的鹿母湾地层的北西西向和东西向断裂带内。通过研究该矿区成矿背景、矿体地质特征、矿石特征,分析了控矿因素,结合土壤测量的化探异常特征,认为矿区成矿条件优越,深部找矿潜力较大,为该地区的矿产勘查指明了方向。
Fuwen gold deposit is in the South China fold system Wuzhishan Fold Belt in Central North East side,south of Changjiang-Qionghai deep fault zones,produced in the late Yanshan granodiorites Lumu-bay stratum neare NWW and east-west fault zones。By studying the metallogenic background,ore geological Characteristics,ore character,Analysis of orecontrolling factors and combined with geochemical soil survey anomalies,we can obtain conclusion that conditions of the metallogenic is Favorable and prospecting potential is big at deep in the area.This work will help guide the mineral survey of this area in the future.
作者
张家友
任国栋
洪彪
陈太豪
符气鑫
ZHANG Jia-you;REN Guo-dong;HONG Biao;CHEN Tai-hao;FU Qi-xin(Hainan Key Laboratory of Marine Geological Resources and Environment,Haikou 570206,China;Hainan Institute of Geological Survey,Haikou 570206,China)
出处
《世界有色金属》
2022年第22期61-64,共4页
World Nonferrous Metals
基金
中国地质调查局海南岛生态地球化学调查(200414200010)资助。
关键词
富文金矿
地质特征
化探异常
找矿前景
Fuwen gold deposit
Geological Characteristics
Geochemical anomaly
prospecting potential
