摘要
腮忽洞矿区位于乌拉特后旗-化德-赤峰Ⅰ级构造单元分界深大断裂带的南侧,华北陆块北缘中段。矿区内主要含2个综合异常,揭露矿化蚀变带1个,主要矿(化)体4个。区内铜、铁矿化体主要赋存在变质石英闪长岩中。矿化蚀变为黄铁矿化、褐铁矿化、硅化、绿帘石化、碳酸盐化、孔雀石化等。
The Yahudong mining area is located in the south side of the deep and large fault zone demarcated by the firstorder tectonic unit of Urat Houqi-Huade-Chifeng, and in the middle part of the northern margin of the North China Block.There are mainly two comprehensive anomalies in the mining area, one mineralized alteration zone and four main mineralized bodies. Copper and iron minerals mainly occur in metamorphic quartz diorite. Mineralization and alteration into pyritization,limonite, silicification, epidote, carbonation, malachite, etc.
引文