中文摘要:文章通过对中国成矿体系的含义、特点、表达方式及演化过程的分析 、界定，提出中国成矿体系是指中国境内各个地质历史时期所形成的矿床及其与成矿作用 密 切相关的地质要素所共同构成的整体。这一成矿体系是中国疆域在其漫长的演化过程中逐步 形成的最终结果，具有明显的阶段性、多期叠加和成矿演化特征。应用矿床的成矿系列概念 和方法初步构筑起中国成矿体系这一复杂体系的框架，有助于今后系统地研究其形成机制， 并为成矿预测提供理论依据。这一体系大致可进一步分为太古宙的陆核成矿体系、元古宙的 陆块边缘裂谷_裂陷槽为主的成矿体系、古生代的板块成矿体系及中_新生代的大陆成矿体系 。
Abstract:China has rich mineral resources. This paper deals with the systematical summari zation of the metallogenic regularity with the purpose of serving the ore_prospe cting work better. The Chinese Continental Mineralization System (CCMS) can be r eferred to as the whole group of mineral deposits located in the present contine nt of China and their genetically related geological factors. The Chinese Contin ental Mineralization System is the final result of mineralization through the wh ole evolutionary history of Chinese continental crust, obviously characterize d b y multiple stages of ore_forming evolution and overprinted by late stages of min eralization. Although the Chinese mineralization system is very complex, its fra mework can be outlined by the concept and methodology of the minerogenic series. The Chinese mineralization system can be divided into four sub_systems of miner alization, i.e., the Archean nucleus mineralization system, the Proterozoic land marginal rifting mineralization system, the Paleozoic plate tectonic mineraliza tion system and the Mesozoic_Cenozoic continental mineralization system. The co nstruction of the framework of the Chinese mineralization system contributes gre atly to the further study of its formation mechanism and the ore prognostic work .
keywords:geology, Chinese mineralization system, minerogenic series, e volution regularity, ore prognosis
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基金项目:地质大调查项目（中国成矿体系与区域成矿评价、中国成矿体系综合研究、我国西部重要成矿区带矿产资源潜力评估）和国家科技攻关计划课题(中国西部优势矿产资源潜力评价技术及示范研究)
引用文本：
陈毓川，王登红，徐志刚，朱明玉.2006.对中国成矿体系的初步探讨[J].矿床地质,25(2):155~163陈毓川，王登红，徐志刚，朱明玉.2006.Preliminary study of Chinese mineralization system[J].Mineral Deposits25(2):155~163
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