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大河边—新晃超大型重晶石矿床地球化学特征及形成的地质背景

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方维萱 胡瑞忠 等. 大河边—新晃超大型重晶石矿床地球化学特征及形成的地质背景[J]. 岩石学报, 2002, 18(2): 247-256.
引用本文: 方维萱 胡瑞忠 等. 大河边—新晃超大型重晶石矿床地球化学特征及形成的地质背景[J]. 岩石学报, 2002, 18(2): 247-256.
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FANG WeiXuan,HU RuiZhong,SU WenChao,QI Liang,XIAO JiaFei and JIANG GuoHao1 1. Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China2. The Mineral and Geological Expiorqtion Center of Nonferrous Metals,Beijmg 100814. Geochemical characteristics of Dahebian-Gongxi superlarge barite deposits and analysis on its background of tectonic geology, China[J]. Acta Petrologica Sinica, 2002, 18(2): 247-256.
Citation: FANG WeiXuan,HU RuiZhong,SU WenChao,QI Liang,XIAO JiaFei and JIANG GuoHao1 1. Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China2. The Mineral and Geological Expiorqtion Center of Nonferrous Metals,Beijmg 100814. Geochemical characteristics of Dahebian-Gongxi superlarge barite deposits and analysis on its background of tectonic geology, China[J]. Acta Petrologica Sinica, 2002, 18(2): 247-256.
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大河边—新晃超大型重晶石矿床地球化学特征及形成的地质背景

    • [1]有色金属矿物地质调查中心，北京100814 [2]中国科学院地球化学研究所矿床地球化学开放研究实验室，贵阳550002

  • 基金项目:

    本文研究由国家重大基础研究规划项目(1999043200)，国家杰出青年科学基金(49925309)中国科学院重大项目(KZ-951-B1-411)及95-预-25联合资助

Geochemical characteristics of Dahebian-Gongxi superlarge barite deposits and analysis on its background of tectonic geology, China

    摘要
  • 本文从矿物岩石学、地球化学和沉积盆地分析角度，研究贵州天柱大河边－湖南贡溪两个超大型重晶石矿床中重晶石（矿）岩及其共生岩石的地球化学特征及构造地质背景。天柱－新晃－玉屏寒武纪热水沉积成矿盆地是发育在大陆斜坡上的断陷型热水沉积成矿盆地，由于同生断层作用将盆地切割成一系列次级盆地，大河边－碧林及龙背－铜盆盖三级热水沉积成矿盆地是大型重晶石矿床的构造定位空间。重晶石矿层主要赋存于下寒武统牛蹄塘组第一岩性段的黑色岩系中。 重晶石矿层是由海底低温热水同生沉积作用形成（105－192℃），古热水场的地球化学类型为硫酸盐型热水。硫酸盐型热水发生大规模同生沉积成岩成矿作用形成超大型重晶石矿床，重晶石矿层之上的黑色碳质粘土岩可能形成于封闭、还原、滞流的深水沉积环境，黑色碳质粘土岩构成矿层的封闭保存条件。
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修回日期:  2001-07-02
刊出日期:  2002-05-31

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