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碳酸盐岩层中沉积矿床碳酸盐岩层含铝土矿建造的岩溶层状类型沉积铝土矿床形成于地槽环境,其分布规律和形成条件有很多共同点。同时,个别矿床或矿区的地质-工业类型也有特殊性。 H.A.科尔热文和H.B.费道罗夫、包里苏娜和O.A.特卡钦科(1970)以及E.C.古特金(1976)等人的著作阐明了乌拉尔铝土矿区铝土矿床的分布规律。在评价由于断裂构造破坏而复杂化的具有岩溶-层状矿床的错动铝土矿区(北乌拉尔、伊夫捷里及其它区)区域
Sedimentary Deposits in Carbonate Formation Carbonatite Bauxite-bearing karst layer-type sedimentary bauxite deposits formed in the geosyncline environment with many similarities in distribution and formation conditions. At the same time, the geology-industry type of individual deposits or mines is also special. The work by HA Colevin and HB Feldorov, Balesirina and OA Tekazinko (1970) and EC Gutrink (1976) illustrates the distribution of bauxite in the Ural bauxite area law. In assessing the area of dislocated bauxite with karst-bedded deposits (Northern Urals, Ypres and others) that have been complicated by the failure of the fault structure