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苏联哈萨克斯坦矿床赋存一种铜—锌黄铁矿矿石,其特点是含有大量的二硫化铁(黄铁矿、白铁矿),矿石中矿物共生致密(在闪锌矿中胶状黄铜矿占30％或更多),含有大量的硫酸铜和硫酸锌以及次生铜的化合物和氧化铜的化合物。根据矿物的结构—构造特征、物质组成以及矿物的嵌布特征,该矿床的矿石可划分为3种基本工艺类型:胶状黄铁矿、结晶型黄铁矿和过渡型黄铁矿。
A copper-zinc pyrite deposit hosted in the Soviet Union’s Kazakhstan deposit is characterized by a large amount of iron disulfide (pyrite, marcasite) that has a symbiotic mineral density (colloidal brass in the sphalerite Ore 30% or more), compounds containing a large amount of copper sulfate and zinc sulfate and secondary copper, and copper oxide. According to the structure-structure features, the composition of the minerals and the embedded features of the minerals, the ore of the deposit can be divided into three basic types of processes: colloidal pyrite, crystalline pyrite and transitional pyrite.