白银河砂金矿床位于内蒙地轴中段南缘,卓资盆地的北东边缘带。矿区四周群山环抱,海拔标高1300—2100米,相对比高100—300米,为浅度切割中山地形,植被和第四系覆盖甚微,冲沟发育。新构造运动造成以南北向为主的构造沟谷与近东西向基底构造踪迹,构成全区方格状水系,同时为砂金矿提供了良好的生成环境。 The Baihehe gold deposit is located in the northeastern margin of the central axis of the Inner Mongolia region and the northeastern margin of the Zhuozi Basin. Surrounded by mountains around the mining area, elevation elevation 1300-2100 meters, relatively high 100-300 meters, shallow cutting Zhongshan terrain, vegetation and Quaternary coverage of very little gully development. Neotectonic movement caused by the north-south orientation of tectonic valley and near east-west basement structure traces, forming a grid-like water system in the region, while providing a good placer gold-forming environment.