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    白云岩矿的特征、成因类型、分布及开发利用价值

    Characteristics, types, distributions and utilization value of dolomite deposit

    • 摘要:
      研究目的 白云岩不仅可以作为良好的油气储层,同时也是一种非常重要的非金属矿产。白云岩矿是冶炼金属镁的重要原材料。中国是全球最大的镁资源储量国,也是全球第一的镁产量国,因此,镁资源也是重要的关键矿产资源。研究白云岩矿的特征、成因、分布及开发利用价值,有利于保障国家关键矿产安全。
      研究方法 通过搜集国内外相关文献,系统总结了白云岩矿的特征、成因、分布以及开发利用价值。
      研究结果 白云岩主要由白云石组成,三方晶系,常呈菱面体晶形。按照其成因类型,白云岩可分为原生白云岩、成岩白云岩和后生白云岩。一般认为,白云岩主要为交代成因,并对原始灰岩结构有不同程度的保留,并在不同期次的白云石化进程或胶结过程中遭到破坏。
      结论 我国白云岩几乎在各个地质时代都有分布,但绝大多数位于地下深处,仅有部分出露地表,满足矿山开采需求。白云岩在元古界和古生界分布最为广泛,中生界和新生界仅在局部地区发育。白云岩可用作冶金溶剂(MgO≥15%)及耐火材料(MgO≥18%)、提炼金属镁(MgO≥19%)、制造水泥(MgO>18%)和建筑材料、医药生产泻利盐、农用化肥(MgO>20%)和饲料等,是一种用途非常广泛的非金属矿产。中国白云岩矿资源丰富,冶金用白云岩矿产资源储量为18.75亿t,而白云岩矿也是冶炼金属镁的重要原材料。中国是全球最大的镁资源储量国,占全球总储量的20%以上,也是全球第一的镁产量国,2022年全国原镁产量为89.36万t,出口量突破50万t,因此,镁资源也是重要的关键矿产资源。镁产业的快速发展也会增大对白云岩矿产资源的需求。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objective Dolomite not only serves as an excellent oil and gas reservoir but also represents a critical non−metallic mineral resource. Dolomite ore is a vital raw material for producing metallic magnesium. China is the world's largest holder of magnesium resource reserves and the top producer of magnesium globally. Consequently, magnesium resources are considered a key strategic mineral. Investigating the characteristics, genesis, distribution, and development value of dolomite deposits is essential for safeguarding national mineral resource security.
      Methods By compiling relevant domestic and international literature, this study systematically summarizes the characteristics, genetic mechanisms, distribution patterns, and utilization value of dolomite deposits.
      Results Dolomite is primarily composed of the mineral dolomite, which crystallizes in the trigonal system and often exhibits rhombohedral crystal forms. Based on genetic classification, dolomite can be categorized into primary dolomite, diagenetic dolomite, and epigenetic dolomite. It is widely accepted that dolomite forms predominantly through metasomatic processes, retaining varying degrees of the original limestone structure, which may be disrupted during multiple phases of dolomitization or cementation.
      Conclusions In China, dolomite deposits are distributed across nearly all geological eras, though the majority are located at significant depths, with only a fraction exposed at the surface, meeting mining requirements. Dolomite is most extensively developed in the Proterozoic and Paleozoic strata, while occurrences in the Mesozoic and Cenozoic are restricted to localized regions. Dolomite has diverse industrial applications, including use as a metallurgical flux (MgO≥15%), refractory material (MgO≥18%), raw material for magnesium extraction (MgO≥19%), cement production (MgO>18%), construction materials, pharmaceutical production of Epsom salts, agricultural fertilizers (MgO>20%), and animal feed additives. As a multifunctional non−metallic resource, China boasts abundant dolomite reserves, with metallurgical−grade dolomite resources totaling 1.875 billion tons. As the world's largest magnesium reserve holder (accounting for over 20% of global reserves) and top producer, China produced 893600 tons of primary raw magnesium in 2022, with exports exceeding 500000 tons. Magnesium resources thus hold strategic importance, and the rapid growth of the magnesium industry is expected to drive increased demand for dolomite mineral resources.

       

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