亲硫元素

  • 网络sulphophile element
亲硫元素亲硫元素
  1. 找矿地球化学研究表明,矿床的成晕元素只有Pb、Zn、Ag、As、Hg等亲硫元素,原生晕极不发育,不具有组份分带以及浓度分带不明显的特点;

    The research on exploring geochemistry indicates that halo-forming elements from the deposit only include Sulphophile elements , such as Pb , Zn , Ag , As and Hg . Primary halo is poorly developed with no obvious Zoning characters of component and concentration .

  2. 沙尘气溶胶相对地壳和黄土的富集因子,以亲硫元素和亲沉积层元素为最高。

    The branch contained higher Ca and the bark had more K. The enrichment factor of sand aerosol which relate to crust and loess is the highest for absorbent sulphate and sedimental elements .

  3. 随着地壳引张作用加剧,从封闭环境转为开放系统,亲硫成矿元素衰退,大量亲氧元素沉淀(Ti、Fe、V、P)。

    With the tensional process in the crust being more and more accumulated , the closed system turns to be an open one and sulphophile ore-forming elements decreased while lithophile ore-forming elements ( Ti , Fe , V and P ) deposited in large quantity .

  4. Ⅳ、边缘坳陷构造活化带&亲硫成矿元素组合构造地球化学类型。

    Tectonic activation zone of marginal depression tectono-geochemical type of the association of chalcophile ore-forming elements .

  5. 有意义的是,铀含量高的样品,其LREE/HREE比值高,铀含量与亲硫的微量元素Pb、Zn和Mo具有相关关系,这些特征可作为铀矿化的重要标志。

    Interestingly , the uranium contents of the sandstones were positively correlated to LREE / HREE ratios and contents of sulphophile element , such as Pb , Zn and Mo. These characteristics were important marks of uranium mineralization .

  6. 结果表明,界线粘土层的铱、锇、铂、金和铼,以及一些亲铁和亲硫元素都有程度不同的富集。

    The results show that Ir , Os , Pt , Au , Re and other siderophile and chalcophile elements are more or less enriched at the boundary .