论文部分内容阅读
笔者曾对某地区的铀矿床及矿点进行过较系统地研究,化费大约四年多时间;而后,我们又较系统地研究了大约200多块岩矿薄片。在此基础上,本文拟通过该区铀矿的空间分布、成矿富集特征以及古应力差,着重阐述构造因素在铀矿成矿过程中的控制作用。一、成矿地质背景本区铀矿主要包括510、512、511、104诸矿区,它们均处于某山字型构造西翼反射弧
The author has conducted systematic research on uranium deposits and ore deposits in a certain area for about four years and then we systematically studied about 200 pieces of rock ore sheets. On this basis, this paper intends to explain the controlling role of structural factors in the process of uranium mineralization through the spatial distribution of uranium deposits, the characteristics of metallogenetic enrichment and the paleotestral stress differences in this area. First, the metallogenic geological background Uranium in this area mainly includes 510,512,511,104 various mining areas, they are in a mountain font structure of the West Wing Reflective Arc