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关于构造—流体—成矿作用研究的几个问题
引用本文:翟裕生.关于构造—流体—成矿作用研究的几个问题[J].地学前缘,1996(4).
作者姓名:翟裕生
作者单位:中国地质大学
摘    要:在成矿过程中,构造和流体是重要的控矿因素。构造、流体和矿石堆积可以作为一个系统加以研究。按成矿作用的规模,构造—流体—成矿系统有不同的尺度:①全球的;②区域的;③矿田(床)的;④微观的。文章分别阐述了矿床的和区域的构造—流体—成矿系统,结合矿床和区域实例讨论了它们的研究目的、内容和方法。具体总结了古老区域流体系统的示踪标志。论文最后讨论了关于古老成矿流体和现代成矿流体、深部成矿流体与浅部成矿流体等的研究任务。

关 键 词:构造  流体  成矿系统  区域热水系统  古流体  示踪标志

PROBLEMS IN THE STUDY OF STRUCTURE FLUID ORE FORMING PROCESSES
Zhai Yusheng.PROBLEMS IN THE STUDY OF STRUCTURE FLUID ORE FORMING PROCESSES[J].Earth Science Frontiers,1996(4).
Authors:Zhai Yusheng
Abstract:Structure and ore fluid are two main controlling factors of ore forming processes. They may be studied from the view point of “structure fluid ore forming system” so as to combine the key factors as a system for profound understanding the metallogenesis. Based on the different spatial scales of the structure fluid ore forming processes, they may be divided into four levels, namely: ① of global scale; ② of regional (metallogenic belt) scale; ③ of orefield scale and ④ of microscopic scale. This paper discusses predominantly the aim, content and approaches of the study on regional and orefield scales of structure fluid ore forming processes respectively. The main trace markers of the paleo fluid systems movement have been recognized also. Finally, the author presents main topics for the study of ore fluid systems at present and in the near future.
Keywords:structure  fluid  ore forming system  regional hydrothermal system  paleo fluids  trace marker
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