戈罗布拉戈达特铁矿床位于斯维尔德洛夫斯克州库什瓦市东北郊乌拉尔山脉的东麓,赋存于图累河的两条小支流——库什瓦河和波洛文卡河之间,这两条小河流分别汇入库什文和上图林斯克水库,并在矿床东部冲刷成波洛文金和萨尔金软泥沉积带。戈罗布拉戈达特矿床赋存于其中的乌拉尔褶皱构造,经历了漫长的地质发展历史。经古生代的剧烈火山活动和构造运动形成喷出贯入岩,使其构造极其复杂,同时沉积岩 The Gorobla Godat iron deposit is located in the eastern foot of the Ural Mountains in the northeastern outskirts of Kushwa City, Sverdlovsk region, and two small tributaries present in the Turera - Kushwa and Polovka Between the rivers, the two streams respectively flow into the Kushwen and Upper Tulinsk reservoirs, and are washed into the sediments of the Poroshenko and Salkin slimes in the eastern part of the deposit. The Ural fold structure in which the Goloburdat deposit is hosted has undergone a long history of geological development. The Paleozoic fierce volcanic activity and tectonic movement formed by spurting into the rock, making its structure is extremely complex, while sedimentary rocks