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豫西南、苏北地区片岩—石英岩型蓝晶石矿床成矿作用的研究
引用本文:王克勤,李明凯.豫西南、苏北地区片岩—石英岩型蓝晶石矿床成矿作用的研究[J].中国非金属矿工业导刊,1992(4).
作者姓名:王克勤  李明凯
作者单位:国家建筑材料工业局地质研究所,国家建筑材料工业局地质研究所 北京,100010,北京,100010
摘    要:片岩—石英岩型蓝晶石矿床的成矿原岩是富铝粘土质砂岩。矿床的形成经历了三个主要的成矿阶段,即高绿片岩相区域变质成矿作用、动力变质成矿作用及气成热液成矿作用。它们在矿物组合、岩石常量化学成分、岩石微量及稀土元素地球化学、成矿的温压条件及矿物学特征等方面存在一定的差异。

关 键 词:蓝晶石  片岩—石英岩型  成矿阶段

Study on Mineralization of the Schist-Quartzite Type Kyanite Deposits in Southwest Henan and North Jiangsu
Wang Keqin.Study on Mineralization of the Schist-Quartzite Type Kyanite Deposits in Southwest Henan and North Jiangsu[J].China Non-Metallic Mining Industry Herald,1992(4).
Authors:Wang Keqin
Abstract:Ore-forming protolith of schist-quartzite type kyanite deposits is Al-rich clayey sandstone.The formation of the deposits underwent three ore-forming stages,i.e. high-grade greenschist facies regional metamorphic mineralization,dynamic metamorphic mineralization and pneumatolyto-hydrothermal mineralization,which show certain differences in mineral association,chemical compositioh of bulk elements,geochemistry of microelements and REE,temperature and pressure conditions of mineralization and mineralogical character istics and so on.
Keywords:kyanite  schist-quartzite  ore-forming stage  
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