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一、引言黄龙铺多金属钼矿田西距金堆城钼矿床7公里,北西距某铀铌铅矿田6.5公里,三者构成了小秦岭地区重要的矿产基地。自1955年以来,经过多种地质工作,现在其核心部位,已探明了数处不同规模的钼铼等矿床,证明该矿田蕴藏着钼、铼、铀、铅、铜、银、金等多种矿产资源。这里地质构造极其复杂,虽然进行过1:20万、1:5万区调,1:1万和1:2千地质填图以及大量的槽、坑、钻探工作,但对它的构造轮廓仍似是而非,很多地质现象无法解释。因此,对构造的研究不仅有其深刻的理论意义,而且成为当务之急。笔者希望通过本文的探讨,能起到抛砖引玉的作用,并有助于促进这一问题的解决。
I. INTRODUCTION Huanglongpu polymetallic molybdenum orefield is 7 kilometers west of Jinduicheng molybdenum deposit and 6.5 kilometers away from a certain uranium niobium lead orefield in the northwest. These three forms an important mineral base in the area of small Qinling Mountains. Since 1955, through various geologic work, several deposits of molybdenum and rhenium of different sizes have now been proved in the core parts of the mine, proving that the ore contains molybdenum, rhenium, uranium, lead, copper, silver and gold etc. A variety of mineral resources. Geological formations here are extremely complex. Although 1: 200,000, 1: 50,000 regions, 1: 10,000 and 1: 2,000 geological mapping, and a large number of trenches, pits and drilling work have been carried out, Paradoxical, many geological phenomena can not be explained. Therefore, the study of structure not only has its profound theoretical significance, but also becomes a top priority. The author hopes that through the discussion of this article, it can play a valuable role and help to solve this problem.