矿床学研究的历史观  

A Historical View of Mineral Deposit Research

作　　者：翟裕生[1,2] 王建平[1,2] 

机构地区：[1]中国地质大学地质过程与矿产资源国家重点实验室,北京100083 [2]中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室,北京100083

出　　处：《地质学报》2011年第5期603-611,共9页Acta Geologica Sinica

基　　金：中国地质调查局地质矿产调查评价专项“覆盖区矿产综合预测”;内蒙古自治区科技找矿项目“内蒙古自治区大矿、富矿成矿系统及找矿预测研究”资助的成果

摘　　要：矿床是地球历史演化的产物,每一个矿床都有其特殊的形成史和变化保存史。矿床学的基本内容应是矿床成因和矿床变化保存两个方面。以历史演化的观点查明矿床形成-变化-保存全过程,有利于矿床学理论水平的提高,也是矿产勘查工作的需要。提出历史观开展矿床学研究的三个层次:①单个矿床形成变化与保存;②区域成矿演化;③全球成矿演化。单个矿床研究与区域成矿演化并重,恢复成矿作用历史,查明成矿时空分布规律以指导找矿勘查工作是矿床学研究永恒的主题;而矿床的变化和保存研究是矿床学科的一个重要方向,应引起足够的重视并加强研究。Mineral deposit is the product of the geologic evolution of Earth＇s history.Each ore deposit underwent its own formation process and post-ore change and preservation history.Thus genesis and post-ore change-preservation are two primary aspects of mineral deposit research.Employing the view of the historical evolution to ascertain the whole process of formation-change-preservation of ore deposit is not only conducive to enhancing the level of mineral deposit theory,but also to the demands for mineral exploration.The authors proposed three levels in mineral deposit research： ① single ore deposit formation-change-preservation,② regional metallogenic evolution,and ③ global metallogenic evolution.Single ore deposit research and regional metallogenic evolution should receive equal attention.Restoring metallogenic history and investigating temporal-spatial metallogenic regularities of mineral deposits to give the guide to deposit exploration has been the main theme for mineral research;while the post-ore change and preservation,as another important aspect of the mineral deposit geology,should arise enough attention and strengthen the research on it.

关 键 词：矿床学 历史观 成矿系统 叠加成矿 变化与保存 

分 类 号：P61[天文地球—矿床学]