江西城门山铜钼矿床特征与成因研究  

Research on Characteristics and Genesis of Chengmenshan Copper-molybdenum Deposit in Jiangxi

作　　者：谭辉跃 息朝庄[2] 

机构地区：[1]湖南省有色地质勘查局一总队 [2]中南大学地学与环境工程学院

出　　处：《矿业快报》2008年第9期46-50,共5页Express Information of Mining Industry

摘　　要：从江西城门山铜钼矿床区域地质特征、矿床特征分析角度,研究矿床成因,结果表明,花岗闪长斑岩与该矿床有关,对成矿也最有利。"四带一面"控制矿体赋存部位。成矿阶段的蚀变主要是硅化,其与金属硫化物矿化的时空关系最为密切,共同组成了成矿作用中最为重要的石英硫化物阶段。Genesis of Chengmenshan copper-molybdenum deposit in Jiangxi was studied from the angle of geologic and deposit characteristics in this district. The results showed that granodiorite porphyry was related to this deposit and was favorable for mineralization. ＂Four-belt and one-face＂ controlled occurrence part of the deposit. Alteration in mineralization stage was mainly silicification, and it was in close relationship with space time in mineralization with metallic sulphide, cooperatively forming an important stage of quartz sulphide in mineralization.

关 键 词：铜钼矿床 城门山 成矿 

分 类 号：P618.65[天文地球—矿床学]