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概述白云鄂博矿属于沉积变质—岩浆期后高温热液交代多金属共生的大型矿床。矿化主要发育在白云岩及白云岩与板岩之间。矿区的各矿体均露于地表,由于长期的氧化作用,使矿石发生了不同程度的物理化学变化,所以各矿体又分为氧化带和原生带。矿床由于矿化和钠氟的交带作用受原岩岩性的控制,矿物在矿床中的各矿地段形成了有规律
Overview Baiyunebo belongs to sedimentary metamorphism - after the magmatic stage of high temperature hydrothermal metasomatic metallogenesis of large deposit. Mineralization is mainly developed between dolomite and dolomite and slate. All ore bodies in the mining area are exposed to the surface. Because of long-term oxidation, the ore undergoes different degrees of physical and chemical changes, so the ore bodies are divided into the oxidation zone and the primary zone. Because of the mineralization and the interaction of sodium and fluorine deposits under the control of the original rock lithology, mineral deposits in various mineral deposits in the formation of a regular