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金堆城斑岩型钼矿床是我国西北地区五十年代末期勘探的特大型钼矿床,驰名中外,地质学者对本矿床各方面研究的论述文章颇多。然而,专门讨论其流体包裹体特征的文章迄今尚未见到。在前人工作与积累的大量资料的基础上,1981—1984年我队铜矿专题研究小组又进一步作了调查,采取了大量样品,对矿床流体包裹体进行了初步研究,取得了一定的认识,笔者将其整理成文,以期今后对本矿床的深入研究有所裨益。
The Jinduicheng porphyry-type molybdenum deposit is a large-scale molybdenum deposit explored in the late 1950’s in the northwest of China. There are a lot of articles on the research of this deposit by geologists both at home and abroad. However, articles that discuss the characteristics of fluid inclusions have not hitherto been seen. Based on the large amount of data collected and worked by our predecessors, the copper mine research team of our team further investigated from 1981 to 1984 and took a large number of samples to conduct a preliminary study on the fluid inclusions in the ore deposit and obtained some recognition , I will organize it into writing, with a view to the future in-depth study of the deposit will be helpful.