金属成矿元素

金属成矿元素金属成矿元素
  1. 局部破碎变质带内花岗岩类中Cu、Pb、Zn成矿元素含量的相关性说明多金属成矿元素来自同一围岩,总体显示成矿不但严格受构造控制,而且成矿后期改造对它的叠加作用也十分显著。

    The relevance among Cu , Pb and Zn in the granites in local fractured metamorphic belts shows that polymetallic ore-forming elements come from the same wall rock . Mineralization is not only severely controlled by structures but also obviously affected by later superimposition and reformation .

  2. 超临界地质流体以其独特的性质对金属成矿元素具有超强的萃取、层析和搬运能力,在热液矿床成矿机制研究中对揭示成矿物质的源、流和汇起着特殊和重要作用。

    Supercritical geofluids have strong capabilities of extracting , separating and transporting on metallic ore-forming elements , and play important roles on the study of the ore-forming mechanism of hydrothermal deposit to indicate the source , path and sink of ore materials .

  3. 对于大多数金属成矿元素,地壳特别是上地壳是大多数矿石和矿胎的储库,地壳丰度是元素富集成矿的物质基础。

    For most ore metals , the continental crust , especially , the upper continental crust , is the repository of all ores and protores . Therefore , the average crust abundance of metals is the material base for the enrichment of ore metals .

  4. 太平洋CC区多金属结核成矿元素迁移规律的界面地球化学研究

    Study on the Geochemical Migration Laws of Metallogenic Elements at Water sediment Interfaces During the Metallogenic Process of Polymetallic Nodules , in the CC Area , Pacific Ocean