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盱眙高家洼—梁家洼凹凸棒石粘土矿床成矿特征及成因研究

Mineralizing characters and genesis study of attapulgite clay deposit in Gaojiawa and Liangjiawa of Xuyi County,Jiangsu

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【作者】 肖书明吴仕良

【Author】 XIAO Shu-ming,WU Shi-liang(Geological Survey of Jiangsu Province,Nanjing 210018,China)

【机构】 江苏省地质调查研究院江苏省地质调查研究院 江苏南京210018江苏南京210018

【摘要】 盱眙高家洼—梁家洼凹凸棒石粘土矿床是苏皖新生代凹凸棒石粘土成矿带的典型矿床之一。分析研究了Ⅴ号粘土矿层分布特征、矿石的矿物成分、化学成分、物化性能与工艺性能,与成矿带内龙王山等矿床同层位矿石及顶底板玄武岩作了化学成分比较。分析了凹凸棒石粘土矿的成矿环境与物理化学条件,指出了矿床成因。

【Abstract】 As a typical deposit of Cenozoic attapulgite clay mineralized belt in Jiangsu and Anhui Provinces,attapulgite clay deposit in Gaojiawa and Liangjiawa of Xuyi County have excellent physical and chemical properties and abundant reserves.Compared with chemical composition of same layer ores and top and floor basalt of Lonwangshan deposit in same mineralized belt,the distribution characters,mineral and chemical compositions,physical and chemical properties of ores have been realized through investigation and analyses of No.V orebed in Gaojiawa and Liangjiawa deposits.The genesis of the deposit belongs to a inland basaltic volcano-sedimentary deposit according to the background and physical and chemical conditions of mineralization course of attapulgite ore deposit.

【关键词】 凹凸棒石粘土矿矿床成因江苏盱眙
【Key words】 Attapulgite clayOre depositGenesisXuyi,Jiangsu
【基金】 江苏省国土资源厅2001年度地质勘查补助项目(苏国土资发[2001]18号)
  • 【分类号】P619.231
  • 【被引频次】5
  • 【下载频次】211
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