青海省金属矿产成矿规律与控矿因素分析

    The metallgenic regularity and ore-controlling factors in Qinghai province

    • 摘要: 青海省金属矿产地质找矿工作薄弱,成矿规律和控矿因素分析急需加强。青海省金属矿产的形成,经历了前寒武期、加里东期、华力西期、印支期和燕山-喜山期,其中加里东期、印支期为主成矿期。成矿构造地质环境可以是古结晶基底、古造山带,也可以是洋壳沉积带、大陆裂谷带、洋壳俯冲带(海沟),岛弧隆起带、弧后盆地和陆缘活动带也是成矿的重要构造地质环境。因此,主要控矿因素有岩石圈构造、构造沉积环境、层位、岩性、岩相和各种转换带。

       

      Abstract: The geological prospecting work is weak in Qinghai province, so it is necessary to strengthen the study of metallogenic regularity and ore-controlling Factors. The metallogenic epoch is Precambrian, Caledonian, Hercynian, Indosinian,Yanshanian and Himalayan period, and the Caledonian and Indosinian period is main mineralization period. The tectonic environments of mineralization include Paleocrystalized basement, orogenic belt, oceanic crust sedimentary belt, continental rift system, oceanic crust subduction (trench), island arc, back-arc basin and continental margin active belt. Therefore, the main Ore-controlling Factors are lithosphere structure, tectonic-sedimentary environment, strata, lithology, lithofacies and transfer zone.

       

    /

    返回文章
    返回