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陕西某地的金红石矿床,首先由陕西省地质局区域地质调查队发现,后经我队进行详查工作,初步已肯定为一大型矿床,但对成矿的控制因素,众说纷云,认识不一。笔者1977年,借带学生实习之便,进行了实地观察,收集了有关这方面的一些资料,进行了分析研究,现对该矿的成矿因素和矿区是否存在旋扭构造的问题,本着“双百”方针的精神,提出肤浅的看法,和同志们商讨,但因水平的所限,认识不一定正确,仅作为引玉之砖,错误之处,望批评指正。一、矿区主要地质特征
The rutile deposit in a certain place in Shaanxi Province was first discovered by the regional geological survey team of Shaanxi Provincial Bureau of Geology. After a detailed investigation by our team, initially it has been confirmed as a large-scale deposit. However, the control factors of mineralization are numerous, one. In 1977, I borrowed the internship of students to carry out field observation, collected some information on this area, carried out analysis and research, and now on the mine’s ore-forming factors and the existence of the problem of spin-twist structure, in line with However, due to the limitation of the level, understanding is not necessarily correct, and only serves as a guide to the jade, a mistake and hope to be criticized and corrected. First, the main geological characteristics of the mining area