ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    刘伟栋,王硕,魏翔,等. 小岩体叠加成矿作用在新一轮找矿突破战略行动中的应用—以勉略宁矿集区为例[J]. 西北地质,xxxx,x(x): x−xx. doi: 10.12401/j.nwg.2024016
    引用本文: 刘伟栋,王硕,魏翔,等. 小岩体叠加成矿作用在新一轮找矿突破战略行动中的应用—以勉略宁矿集区为例[J]. 西北地质,xxxx,x(x): x−xx. doi: 10.12401/j.nwg.2024016
    LIU Weidong,WANG Shuo,WEI Xiang,et al. Application of Superimposed Mineralization of Small Intrusions in the New Round of Prospecting Breakthrough Action: A Case Study of Mian-Lue-Ning Ore Concentration Area[J]. Northwestern Geology,xxxx,x(x): x−xx. doi: 10.12401/j.nwg.2024016
    Citation: LIU Weidong,WANG Shuo,WEI Xiang,et al. Application of Superimposed Mineralization of Small Intrusions in the New Round of Prospecting Breakthrough Action: A Case Study of Mian-Lue-Ning Ore Concentration Area[J]. Northwestern Geology,xxxx,x(x): x−xx. doi: 10.12401/j.nwg.2024016

    小岩体叠加成矿作用在新一轮找矿突破战略行动中的应用—以勉略宁矿集区为例

    Application of Superimposed Mineralization of Small Intrusions in the New Round of Prospecting Breakthrough Action: A Case Study of Mian-Lue-Ning Ore Concentration Area

    • 摘要: 小岩体成(大)矿理论是汤中立院士在多年找矿实践工作过程中总结出来的重要成果。该理论以岩浆铜镍硫化物矿床为研究起点,逐渐延伸至与中酸性岩浆活动有关的热液型矿床,发展成为基性-超基性与中酸性两类岩浆并行的完整成矿理论体系。研究发现,以勉-略-宁矿集区为代表的成矿区带分布有众多两类岩浆活动的叠加区,并且两类岩浆活动导致的叠加成矿作用在该区显著。其中,煎茶岭镍钴金多金属矿床形成过程经历了早期初步的超镁铁质岩浆熔离作用使成矿元素预富集,后期花岗斑岩岩浆流体成矿作用叠加之上,最终使钴镍矿和金矿均达到了大型规模。此外,该区近年发现白雀寺基性杂岩体中的何家垭镍钴矿同样具有两类岩浆叠加成矿的特征,这为小岩体成(大)矿理论提供了新的研究方向。目前,中国新一轮找矿突破战略行动已全面开启,以Ni、Co为代表的战略性关键金属矿产仍是本轮找矿工作的重中之重,两类岩浆的小岩体叠加成(大)矿作用是Ni、Co矿形成的重要地质过程。本文通过介绍小岩体成(大)矿理论的发展过程,并以勉-略-宁矿集区为代表,提出了两类岩浆叠加成(大)矿作用的基本内涵。在此基础上,对其找矿应用和理论研究两方面做了展望,以期助力中国新一轮找矿突破战略行动。

       

      Abstract: The theory of (large) ore deposit forming in the small intrusion is an important result of decades of prospecting practice by academician Tang Zhongli. The theory started from magmatic copper-nickel sulfide deposits, gradually extended to hydrothermal deposits associated with intermediate-acid magmatism, and developed into a complete metallogenic theoretical system of basic-ultra-basic and intermediate-acid magmatism in parallel. In recent years, it has been found that the metallogenic belt represented by the Mian-Luo-Ning ore concentration area is distributed in many superimposed areas of basic-ultra-basic and intermediate-acid magmatic activities, among which the formation process of the Jianchaling cobalt-nickel-gold polymetallic deposit experienced the preliminary ultramafic magmatic liquation in the earlier stage to achieve the pre-enrichment of ore-forming elements, and the later superimposed acid magmatic fluid on eventually led to both cobalt-nickel and gold mines reaching large scale. In recent years, the Hejiaya cobalt-nickel deposit was found in the Baiqisi basic complex also has the characteristics of superimposed mineralization of two kinds of magmatism, which provides a new research direction for the theory of (large) ore deposit forming in the small intrusion. At present, the new round of prospecting breakthrough action has been fully launched. The strategic key metal minerals represented by Co and Ni are still the top priority of the prospecting work. The superposition of small rock bodies is an important geological process in the formation of Co and Ni ores. In this paper, the development process of the theory of (large) ore deposit forming in the small intrusion is introduced, and the basic connotation of the superimposition of two kinds of magmas into (large) ore is put forward by taking the Mian-Lue-Ning ore concentration area as the representative. On this basis, the prospect of prospecting application and theoretical research is made, which is expected to support the new round of prospecting breakthrough action.

       

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