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黔中麦西铝土矿地质特征及矿床成因

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麦西铝土矿位于黔中扬子地块内部的修文-清镇矿集区,矿区内褶皱和断裂构造发育,铝土矿产于下石炭统九架炉组含铝岩系中,资源储量丰富.本文以岩石学、矿物学和地球化学等方法对矿区的成矿物质来源、矿床地质特征及成因开展了系统研究.结果表明:矿区成矿物质可能来源于下伏寒武系娄山关组碳酸盐岩,并且经历了"风化初始富集-胶体聚合-脱硅富集-风化淋滤改造成矿"等多阶段复杂的成矿过程.本次研究基于"矿层露头-含矿地层-构造"的多元找矿标志,推测矿区东部及北部外围为下一步的找矿远景区.
Geological characteristics and genesis of the Maixi bauxite deposit in Central Guizhou Province
Maixi Bauxite Mine is located in the Xiuwen-Qingzhen mining area within the Yangtze block in central Guizhou.The folds and fault structures are developed in the mining area,and the bauxite deposits occur in the aluminum-bearing rock series of the Jiujialu formation in the Lower Carboniferous,rich in resources and reserves in the mining areas.This article systematically studies the sources of ore-forming compentents,geological characteristics,and genesis of ore deposits in the mining areas by the methods such as petrology,mineralogy,and geochemistry.The results indicate that the ore-forming compentents in the mining areas may come from the underlying carbonate rocks of the Loushanguan formation of the Cambrian,and have undergone a multi-stage and complex mineralization process:"Weathering leads to initial enrichment--Colloidal action leads to the polymerization---Desilication leads to enrichment--The transformation effect of weathering and leaching leads to mineralization".This study is based on the diversified exploration indicators of"ore outcrop--ore bearing strata--structure",and it is speculated that the eastern and northern periphery of the mining area can be the next exploration prospect.

Qianzhong Maixi regionBauxiteGeological characteristicsGenesis of mineral deposits

余敏华

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中化地质矿山总局贵州地质勘查院,贵州 贵阳 550002

黔中麦西地区 铝土矿 地质特征 矿床成因

2024

化工矿产地质
中化地质矿山总局地质研究院

化工矿产地质

影响因子:0.28
ISSN:1006-5296
年,卷(期):2024.46(2)