中国中生代矿床成矿系列类型及其演化  

Metallogenic Series Types of Mesozoic Mineral Deposits in China and Their Evolution

作　　者：梅燕雄[1] 裴荣富[1] 李进文[1] 傅旭杰[1] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037

出　　处：《矿床地质》2004年第2期190-197,共8页Mineral Deposits

基　　金：中国地质调查局地质调查项目"中国成矿体系与区域成矿评价"(编号 :K1.4)的资助

摘　　要：中国及邻区中生代地质构造的演化主要表现为欧亚大陆东部增生和中国大陆陆缘及陆内变形作用 ,受特提斯_古太平洋及太平洋_印度洋两大动力学体系的控制 ,形成滨太平洋、特提斯和中亚 3大构造域。作者在对82 9个典型矿床及大量测试数据进行综合分析的基础上 ,结合中生代成矿环境和成矿特征 ,将中国中生代矿床划分为 3个矿床成矿系列组合和 1 1个矿床成矿系列类型。着重论述了中国中生代矿床成矿系列类型的基本特征 。The Mesozoic geological-tectonic evolution of China and adjacent areas mainly finds expression in accretion of East Eurasian continent and epicontinental-intracontinental deformaion of China. Controlled by the Tethyan-Ancient Pacific and Pacific-Indian geodynamic systems, three domains, i.e., the Marginal Pacific tectonic domain, the Tethyan tectonic domain and the Middle Asia tectonic domain, were formed in Mesozoic. Based on a comprehensive analysis of 829 typical mineral deposits and lots of laboratory data, in combination with Mesozoic metallogenic environment and characteristics, the authors have classified the Mesozoic mineral deposits of China into 3 metallogenic series associations, 11 metallogenic series types and 121 metallogenic series. This paper mainly discusses the essential characteristics and evolutionary regularity of Mesozoic metallogenic series types.

关 键 词：地质学 成矿系列 成矿演化 中生代 中国 

分 类 号：P617[天文地球—矿床学]