太行山北段多金属矿床地球化学特征

    GEOCHEMICAL FEATURES OF POLYMETALLIC DEPOSITS IN THE NORTHERN SECTION OF TAIHANG MOUNTAINS

    • 摘要: 太行山北段多金属矿床有3个金属元素富集带:1.中心(铜)钼矿带,形成斑岩型矿床;2.过渡带铁-铜、银-铜、铁和锌成矿带,形成矽卡岩型矿床;3.外带铅-锌-银带,形成脉状矿床.这种分带出现于多个矿区,但不同矿区显示出独特变化.一般以其中一个矿带最发育,其它两矿带次之,但有时也有两矿带相对发育.围绕花岗岩的金属元素区域分布,流体包裹体温度测定及H、O和S同位素分析结果,表明岩浆热液与冷的大气降水(含少量源于围岩的CO2和H2S)之间的混合作用可以解释金属元素沉淀及时空分带的形成.

       

      Abstract: The northern section of Taihang Mountains is a concentrated area of polymetallic deposits,with abundance of metals and mineralized types.Based on the mineralized types and spatial distribution,3 metallic concentrated systems are recognized:1)central Cu-Mo zone;2)transitional F-Cu,Ag-Cu,Fe,or Zn zone;3)outer Pb-Zn-Ag zone.The zones present in different mineralized districts,in which the characteristics are specific.Generally,only one zone is well-developed,others are secondary.But sometimes 2 zones are relatively developed.On the bases of metallic zonation around Mesozoic granites,the temperature of fluid inclusion,the isotopic analysis of H,O and S,and the mixture between magmatic hydrothermal solution and meteoritic solution can explain the precipitation and spatial distribution of metal elements in the area.

       

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