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中文摘要: 通过对黑土田铝土矿矿床地质特征,矿物组分、生成时间先后和成因等因素的分析,把所有矿物分为碎屑、原生、后生和表生矿物。根据成矿古地理和物质来源及矿物的形成途径分析,认为该矿床的成因类型为:钙红土—沉积—改造型。
Abstract:Through the analysis of Heitutian bauxite, including geological characteristics, mineral composition, genesis and formation of time sequence etc., all minerals are divided into several kinds, such as detritus mineral, primary mineral, epigenetic mineral and hypergenic mineral. According to the analysis of the metallogenic paleogeography, source materials and the mineral forming ways, it is considered that the genetic type is terra fusca-sedimentary-reformed type.
keywords: Bauxite geological characteristics genesis Heitutian
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杨晓飞,罗应坤.贵州省清镇市黑土田铝土矿成因浅析[J].有色金属(矿山部分),2011,63(1):18-22.
YANG Xiaofei,LUO Yingkun.The Genesis Analysis of Heitutian Bauxite Deposit in Qingzhen, Guizhou Province[J].NONFERROUS METALS(Mining Section),2011,63(1):18-22.
杨晓飞,罗应坤.贵州省清镇市黑土田铝土矿成因浅析[J].有色金属(矿山部分),2011,63(1):18-22.
YANG Xiaofei,LUO Yingkun.The Genesis Analysis of Heitutian Bauxite Deposit in Qingzhen, Guizhou Province[J].NONFERROUS METALS(Mining Section),2011,63(1):18-22.