铜钼矿床的成因类型及其地质特征研究  

Study on the genetic types and geological characteristics of copper and molybdenum deposits

作　　者：朱强 ZHU Qiang(Energy geology Brigade of Jiangxi Geological Bureau,Nanchang,Jiangxi 330000)

机构地区：[1]江西省地质局能源地质大队,江西南昌330000

出　　处：《世界有色金属》2023年第18期67-69,共3页World Nonferrous Metals

摘　　要：本文以江西某铜钼矿床为例,基于江西成矿地质背景对铜钼矿床的成因类型进行研究,包括铜钼矿床形成受地层、蚀变、岩浆岩以及构造的影响以及成矿的物理化学条件。同时分析了铜钼矿床的地质特征,包括矿石结构、矿石构造、矿石类型以及成矿阶段划分。Taking a copper-molybdenum deposit in Jiangxi province as an example,the genetic types of coppermolybdenum deposit are studied based on the metallogenic geological background of Jiangxi province,including the formation of copper-molybdenum deposit under the influence of strata,alteration,magmatic rock and structure,as well as the physical and chemical conditions of metallogenic deposits.The geological characteristics of copper-molybdenum deposits include the ore structure,ore structure,ore type and metallogenic stage division.

关 键 词：铜钼矿床 成因类型 地质特征 

分 类 号：TD862[矿业工程—金属矿开采]