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斑铜矿

bān tóng kuàng
  • bornite;erubescite;poikilite;phillipsite
斑铜矿斑铜矿
斑铜矿[bān tóng kuàng]
  1. 辉铜矿、黄铜矿和斑铜矿的溶解动力学:Ⅰ.温度、pH和NaCl浓度的影响

    Kinetics of dissolution of chalcocite , chalcopyrite and bornite : ⅰ . the effects of temperature , pH and NaCl concentration

  2. 封面故事:硅灰石矿石中的稠密浸染状斑铜矿。

    Cover Story : Dense disseminated bornite in wollastonite skarn ore.

  3. 中期成矿矿石矿物主要是斑铜矿。

    The late ores are mainly in massive big veins .

  4. 层状主矿体中金主要以细小的自然金形式包裹于斑铜矿和黝铜矿中。

    Gold in stratiform major orebody is mainly included in bornite and tetrahedrite as fine grain of native gold .

  5. 凹地苴铜矿矿物在剖面上具从辉铜矿-斑铜矿-黄铜矿-黄铁矿分带现象。

    Metal minerals in Wadizhou copper deposit appear to be zoning of chalcosine bornite chalcopyrite pyrite on the vertical direction .

  6. 氧化铜矿物主要为孔雀石,其次是硅孔雀石,少量蓝铜矿;硫化铜矿物主要是斑铜矿,其次是辉铜矿和铜蓝,少量黄铜矿。

    Oxide copper minerals are mainly malachite , the second is chrysocolla , followed by a small amount of azurite ; and sulfide copper minerals are mainly bornite , followed by chalcocite and covellite , and a small amount of chalcopyrite .

  7. 主矿层中的矿化沿岩层厚度具有明显的垂直分带性,从底部到顶板为:辉铜矿→斑铜矿→黄铜矿→黄铁矿,为典型的化学沉积成因铜的硫化物排列组合特征。

    Along thickness of strata , mineralization of master ore bed has obviously vertical zonality in the upward order of chalcocite → bornite → chalcopyrite → pyrite , It is indicated that typical arrangement assemblage feature of sulphide of sediment orogenic copper ore.

  8. 矿石主要原生金属矿物为辉铜矿和斑铜矿,次生金属矿物主要为孔雀石等。矿石结构构造比较简单,主要为结晶粒状及溶蚀结构和侵染状胶结构造。

    The major primary metal minerals of ore are chalcocite and bornite , and the secondary metal minerals are malachite and azurite , etc. Ore texture and structure are simply , the ores are mainly in granular crystalline and dissolution textures and infection cementation structures .

  9. 研究认为,本区玄武岩具大陆拉斑玄武岩特征,铜矿属火山同生热液成矿叠加埋藏变质作用改造形成的玄武岩铜矿。

    It is believed that the basalt in the area is characterized by continental tholeiite and the copper deposit belongs to a basalt type copper deposit formed by syn-volcanic hydrothermal mineralization superimposed by buried metamorphic transformation .