摘要
哈萨克斯坦板块准噶尔微板块和唐巴勒―克拉麦里古生代复合沟弧带,是该矿的分布所在,研究区由达尔步特大断裂穿过,区内发育非常频繁的岩浆活动,同时具有非常突出的断裂构造,存在明显的岩石变形特征以及热接触交代变质作用,因此区内地质特征非常复杂。
The distribution of the deposit lies in the Junggar micro-plate of the Kazakhstan plate and the Paleozoic composite trench-arc belt of Tangbale-Kramery. The study area is crossed by the Dalbur super-large fault. Magmatic activities are very frequent in the area. At the same time, it has a very prominent fracture structure, obvious rock deformation characteristics and thermal contact metamorphism. Therefore, the geological characteristics of the area are obvious. It's very complicated.
引文
[1]汪疆,张云孝.新疆托里县包古图矿区托尔特铜金矿地质特征初探[J].新疆有色金属.2010(03).
[2]谢俊,伏东红.金矿地质特征及找矿方向研究[J].世界有色金属.2017(19).