非洲大陆岩石圈演化与成矿关系

    Relationship between lithospheric evolution and mineralization in Africa Continent

    • 摘要: 岩石圈深部过程与成矿关系研究是当今地球科学的前沿,对于深化成矿地质背景了解、总结成矿规律、有效开展资源潜力评价、提高矿产勘查效果等具有重要意义。以岩石圈角度划分的非洲大陆新大地构造单元为基础,分析了矿产资源的时空分布特征,讨论了克拉通型、造山带型、裂谷型等不同类型岩石圈的成矿特色。根据非洲大陆形成和岩石圈演化,区分非洲大陆不同类型岩石圈的壳-幔状态,即物质形成时代、结构形成时代,结合主要矿产空间分布、矿床类型及矿产组合,划分出现今非洲大陆27个成矿区带。从地质过程的“动态”视角审视和划分非洲大陆成矿区带,是以深部过程与成矿为主线的有益探索和尝试,为在非洲地区开展资源评价与选区提供了新的思路和参考。

       

      Abstract: The research on the relationship between deep lithospheric process and mineralization is the forefront of Geoscience. It is of great significance to deepen understanding of metallogenic geological setting, summarize metallogenic regurality, effectively assess resource potential and improve the effect of mineral exploration.Based on the new tectonic units of the African Continent divided by lithosphere, the temporal-spatial distribution of mineral resources was analyzed, and the metallogenic characteristics in different types of lithosphere such as craton, orogeny and rift were analyzed.According to the formation and lithospheric evolution of the African Continent, the crust-mantle status of different types of lithosphere in the African Continent was distinguished, that is, the age of material formation and the age of structure formation.Combined with the spatial distribution of main mineral resources, genetic types of ore deposits and assemblage of mineral resources, 27 metallogenic belts in the present African Continent were divided.It is a useful exploration and attempt to examine and divide the metallogenic belt of the African Continent from the "dynamic" view of geological process, which is based on the relationship between deep geological process and mineralization.It would provide a new idea and reference for mineral resource evaluation and prospects generation in Africa.

       

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