大陆碰撞成矿理论的创建及应用  

The development of continental collision metallogeny and its application

作　　者：陈衍景[1,2] 

机构地区：[1]北京大学造山带与地壳演化重点实验室,北京100871 [2]国科学院矿物学与成矿学重点实验室,广州510640

出　　处：《岩石学报》2013年第1期1-17,共17页Acta Petrologica Sinica

基　　金：国家973计划项目(2006CB403500);国家攀登预研39号项目02课题;国家科技攻关计划96-915-03-05专题;国家自然科学基金项目(40730421、40425006、U1139301);国家危机矿山项目(20089934)联合资助

摘　　要：本文阐明了大陆碰撞成矿理论的重要性,将大陆碰撞成矿理论的发展史划分为1970年以前的预备期,1971～1990年的孕育期,1991～2000年的诞生期,2001～2010年的成长期和2011年以后的成熟期;指出大陆碰撞成矿理论的核心内容是4个不同尺度(全球构造、造山带、地体、矿床)的碰撞造山流体成矿模式(CMF模式)和4种类型成矿系统的特征及其与其它环境同类成矿系统的对比;介绍了运用大陆碰撞成矿理论指导找矿预测的成功范例。事实证明,中国学者发挥中国碰撞造山带丰富的自然优势,为发展大陆碰撞成矿理论做出了重大贡献。The importance of the continental collision metallogeny is addressed in this paper. The development history of the continental collision metallogeny is divided into five periods, namely, preparation （before 1970）, incubation （1971 - 1990）, birth （1991 - 2000）, growth （2001 - 2010） and maturation （2011 and thereafter）. The hardcore of the continental collision metallogeny is considered to include four tectonic models for Collisional orogeny, Metallogeny and Fluid flow （abbreviated to CMF） at differing scales （global tectonics, orogen, terrane and deposit）. It also contains the characterizations of four classes of hydrothermal mineral systems formed in continental collision regime as well as their comparative illustrations with the mineral systems formed in other tectonic se-tings. The paper also introduces several successful ore-exploration examples guided by the continental collision metallogeny. The facts presented in the paper show that Chinese geologists have contributed much to the development of the continental collision metallogenv, by utilizing the unique conditions of abundant continental collision orogens in China.

关 键 词：大陆碰撞成矿理论 碰撞造山流体成矿模式 热液矿床 浅成作用 找矿勘查 

分 类 号：P611[天文地球—矿床学]