The Research of the Mineralogical and Element Geochemical Characteristics of Bauxite in Yunfeng, Qingzhen, in Central Guizhou Province, China

Yang Wu, Dai Tagen, Long Yongzhen
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Abstract

The mineralogical and geochemical characteristics of the Yunfeng bauxite in Qingzhen were investigated through the handle specimen observation, thin section analysis, XRD、SEM and Element geochemistry. The mineral analyses reveal that diaspore, kaolinite and chlorite are the major minerals in the bauxite with small amounts of boehmite and pyrite. Geochemical investigations reveal that the main components in the bauxite are Al2O3, SiO2 and TFe2O3, the minorcomponents are TiO2, MgO and P2O5. In the process of weathering, some trace elements, such as Zr, Cr, Nb and Hf, are enriched. Zr vs Hf and Nb vs Ta display higher positive correlation. Trace elements show that Loushanguan For- mation is the main source of material for the bauxite formation and there may be exist other precursor rock provide few material for the bauxite formation. Ore deposit formed in a O-poor,reducing Marine sedimentary environment.
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贵州中部清镇云峰铝土矿矿物学及元素地球化学特征研究
通过试样观察、薄片分析、x射线衍射(XRD)、扫描电镜(SEM)和元素地球化学等手段研究了清镇云峰铝土矿的矿物学和地球化学特征。矿物分析表明,铝土矿中主要矿物为一水硬铝石、高岭石和绿泥石,薄铝石和黄铁矿含量较少。地球化学研究表明,该铝土矿主要成分为Al2O3、SiO2和TFe2O3,次要成分为TiO2、MgO和P2O5。在风化过程中,部分微量元素如Zr、Cr、Nb、Hf富集。Zr与Hf、Nb与Ta表现出较高的正相关性。微量元素分析表明,娄山关组是铝土矿形成的主要物质来源,可能存在其他前体岩,为铝土矿形成提供少量物质。矿床形成于贫氧、还原海相沉积环境。
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