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矿床学是研究矿床成因和矿床分布规律的地质学科,它是在找矿、勘探、采矿和选冶等生产需要的推动下,在地质学各分支的基础上逐步发展起来的.七十年代以来,矿产资源的大量开发,现代科学技术的引进、以及矿床学研究方法的改进,推动着矿产勘查工作的深入和矿床学研究水平的提高,一百多年来逐步建立并发展起来的成矿理论,正在经受着生产实践和科学实验的全面检验,需要加以补充,修改和提高.近年来新提出的一些观点和假说,特别是成矿物质多源性和矿床形成过程的复杂性,以及矿床形成与地质构造环境的紧密联系,使矿床学研究必须在对矿床本身资料深入分析的基础上,结合地质构造及其演化发展历史进行综合的研究.矿床学作为一门直接指导矿产资源的寻找和利用的地质科学,正进入一个新的发展时期.
Mineralogy is a geological discipline that studies the genesis and distribution of deposits and is developed gradually on the basis of various branches of geology, driven by the production needs of prospecting, exploration, mining and dressing and smelting etc. Since the 1970s The extensive exploitation of mineral resources, the introduction of modern science and technology, and the improvement of research methods in mineral deposits have promoted the exploration of mineral resources and the enhancement of ore deposit studies. The metallogenic theory gradually established and developed over the past 100 years , Is undergoing comprehensive tests of production practices and scientific experiments and needs to be supplemented, revised and improved. Some new ideas and hypotheses newly proposed in recent years, in particular, are the multi-source of mineralization materials and the complexity of deposit formation and the formation of deposits With the close relationship with the geological tectonic environment, the mineral deposit study must be based on the in-depth analysis of the deposit itself, combined with the geological structure and evolution history of the comprehensive study of mineral deposits as a direct guide mineral resources to find and use Of geological science, is entering a new period of development.