中文摘要: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829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11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， 并简要概括了它们的时空演化规律。
Abstract:The Mesozoic geological_tectonic evolution of China and adjacent areas mainly fi nds expression in accretion of East Eurasian continent and epicontinental_intrac ontinental deformaion of China. Controlled by the Tethyan_Ancient Pacific and Pa cific_Indian geodynamic systems, three domains, i.e., the Marginal Pacific tecto nic domain, the Tethyan tectonic domain and the Middle Asia tectonic domain, wer e formed in Mesozoic. Based on a comprehensive analysis of 829 typical mineral d eposits and lots of laboratory data, in combination with Mesozoic metallogenic e nvironment and characteristics, the authors have classified the Mesozoic mineral deposits of China into 3 metallogenic series associations, 11 metallogenic seri es types and 121 metallogenic series. This paper mainly discusses the essential characteristics and evolutionary regularity of Mesozoic metallogenic series types.
keywords:geology, metallogenic series, regional metallogeny, metallogenic evolution, Mesozoic, China
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基金项目: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)
引用文本：
梅燕雄，裴荣富，李进文，傅旭杰.2004.中国中生代矿床成矿系列类型及其演化[J].矿床地质,23(2):190~197.2004.Metallogenic Series Types of Mesozoic Mineral Deposits in China and Their Evolution[J].Mineral Deposits23(2):190~197
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