浅议矿床地球化学在斑岩铜矿研究中的应用  

A Brief Analysis of Ore Deposit Geochemistry Application in Porphyry Copper Deposit

作　　者：曹征 潘佩芬[1] 丛宝华[1] 

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《内蒙古石油化工》2010年第6期87-90,共4页Inner Mongolia Petrochemical Industry

摘　　要：矿床地球化学是矿床学与地球化学相结合的一门交叉学科,成矿物质来源、成矿流体来源和成矿年龄测定是矿床地球化学研究的三大核心科学问题,本文运用矿床地球化学研究方法探讨了我国部分斑岩铜矿床的成矿物质来源、成矿流体类型及来源和矿床形成年代,结合对斑岩铜矿的地球化学异常的概略分析,初步分析了矿床地球化学在斑岩铜矿床研究中的应用。Ore deposit geochemistry is an intersectional subject, which integrates mineral deposit geology and geochemistry, Origin of mineralization material, origin of mineralization fluid and determination of mineralization age are the key scientific topics in ore deposit geochemistry study. This paper prosecute some studies on origin of mineralization material, origin of mineralization fluid, mineralization age of porphyry copper and a brief introduction of porphyry copper geochemistry anomaly, all of those illustrate the importance of ore deposit geochemistry in researching ore deposit.

关 键 词：矿床地球化学 斑岩铜矿 成矿物质 成矿流体 成矿年代 

分 类 号：P59[天文地球—地球化学] P578.25[天文地球—地质学]