徐光平,翟建平,胡凯.成矿过程中流体的作用及其主要研究方法[J].地质找矿论丛,1999,(4):1-7,75
成矿过程中流体的作用及其主要研究方法
THE ROLES OF FLUID IN THE FORMATION OF ORE DEPOSITS AND THE MAIN STUDY METHODS
投稿时间:1999-04-26  修订日期:1999-09-15
DOI:10.6053/j.issn.1001-1412.1999.4. 001
中文关键词:  成矿流体  活化  不混溶  水-岩反应  研究方法
英文关键词:ore-forming fluids  mobilization  immiscibility  water-rock interaction  study methods
基金项目:
作者单位
徐光平 南京大学地球科学系, 南京大学成矿机制研究国家重点实验室, 江苏南京210093 
翟建平 南京大学地球科学系, 南京大学成矿机制研究国家重点实验室, 江苏南京210093 
胡凯 南京大学地球科学系, 南京大学成矿机制研究国家重点实验室, 江苏南京210093 
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中文摘要:
      流体在成矿过程中扮演着十分重要的角色,它是成矿物质得以活化、迁移、富集的主要介质,同时流体的运移还能扩展有利的成矿空间。同位素地球化学方法仍然是成矿流体研究的主要手段,实验地球化学、元素地球化学以及现代岩石学和矿物学研究方法在探讨流体的起源、演化等方面已发挥越来越重要的作用。每种方法均有其局限性,在实际工作中强调多种研究方法的结合十分必要。
英文摘要:
      Fluid plays an important role in the forming process of ore deposits, and it is also a fundamental medium for the mobilization, transportation and enrichment of ore-forming elements, which are very critical for the formation of ore deposits. Furthermore, many beneficial ore-forming spaces are produced during the transportation of fluid. Taking ore-forming fluid as the main thread, this paper introduces the latest development of the studies on the roles of the ore-forming fluid in the forming process of ore deposits and reviews the main study methods. The isotopic geochemistry method is still a very useful one in the study of the ore-forming fluid, and the methods of experimental geochemistry, elemental geochemistry and petrology & mineralogy are also becoming more and more important. However, each method has its own deficiency, and it is necessary to combine these methods together in the practical research.
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