中国重晶石矿床分布特征、成因类型、资源应用现状及其展望
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P619.251

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中央级公益性科研院所基本科研业务费专项(KK2005)和中国地质调查局项目(DD20230056、DD20190606、DD20221684、DD20230291)联合资助。


Distribution characteristics, genesis types, current status of resource application of barite deposits in China and its prospects
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    摘要:

    研究目的 重晶石作为中国优势矿种,存在开发利用率低等问题。为保障中国重晶石资源安全, 寻找更多的重晶石资源,本文对支撑石油勘探工业发展和拓宽应用领域具有重要意义。研究方法 本文总结了重晶石的成矿时代、成矿特征、矿床成因类型和成矿物质来源,系统梳理了中国重晶石的分布情况、资源现状以及应用情况,为我国今后对重晶石的开采和应用方面提供了参考。研究结果 中国重晶石矿床的成因类型可分为沉积型、火山沉积型、热液型、层控热液型、风化残坡积型。根据成矿流体来源重晶石可分为海底热液重晶石和生物重晶石这两个端元。全球重晶石已探明储量大约7.4亿t,中国有贵州、广西、湖南和福建等26个省份产出重晶石,作为我国关键矿产之一,是全世界第二大生产国,品位高且出口量大,被广泛应用于油气工业、高新材料、医疗、军事和环保等领域。结论 中国重晶石矿床主要形成于古生代和中生代的江南地区、秦岭地区和黔—桂地区,且以沉积型矿床为主。重晶石成矿流体来源类型繁多,通过地球化学标志可判断出成矿物质来源于海底热液,而通过生物标志性化合物和偏重的硫同位素可得出生物成因结论。重晶石作为重要的高新材料之一,在未来集约化、高效和绿色的产业发展机制中,需注重提高重晶石的精深加工水平、发展战略性新兴产业和拓宽重晶石的应用领域。中国重晶石矿找矿远景应着重加强寻找扬子地台南缘的超大型和大型重晶石矿点,对类似于甘青宁重晶石成矿区等低品位重晶石矿和伴生重晶石矿床的寻找也不容忽视,以及不断探索开发华北和新疆等地区,去寻找更丰富的重晶石资源。

    Abstract:

    This paper is the result of mineral exploration engineering. Objective Barite, as a dominant mineral resource in China, faces challenges such as low utilization efficiency. To ensure the security of China's barite resources, it is essential to further explore and develop barite reserves. This effort is of significant importance for supporting the development of the petroleum exploration industry and broadening its application fields. Methods This paper summarizes the metallogenic epochs, characteristics, genetic types, and material sources of barite deposits. Meanwhile, it systematically reviews the distribution, resource status, and applications of barite in China. This work provides a reference for future mining and application of barium sulfate in China. Results The genetic types of barite deposits in China can be classified into sedimentary, volcanic-sedimentary, hydrothermal, stratified hydrothermal, and weathering residual-slope accumulation types. Based on the sources of metallogenic fluids, barite can be divided into two end–members: submarine hydrothermal barite and biogenic barite. Globally, the proven reserves of barite are approximately 740 million tons. In China, barite is produced in 26 provinces, including Guizhou, Guangxi, Hunan, and Fujian. As one of China's critical minerals, it ranks as the world's second–largest producer, characterized by high–grade deposits and significant export volumes. Barite is widely used in various fields such as the oil and gas industry, advanced materials, medical treatment, military, and environmental protection sectors. Conclusions Barite deposits in China primarily formed during the Paleozoic and Mesozoic eras,with key regions including the Jiangnan, Qinling, and Guizhou–Guangxi areas, dominated by sedimentary–type deposits. The sources of barite metallogenic fluids for barite are diverse. Geochemical signatures indicate that the metallogenic materials originate from submarine hydrothermal fluids, while biomarker compounds and heavier sulfur isotopes indicate a biogenic origin. As one of the crucial advanced materials, barite requires a focus on enhancing its deep processing capabilities, developing its strategic emerging industries, and expanding its application fields within the framework of future intensive, efficient, and green industrial development mechanisms. The future prospecting potential for barite in China should focus on the following aspects to discover more abundant barite resources: Firstly, emphasis should be placed on exploring super–large and large barite deposits in the southern margin of the Yangtze Platform. Secondly, the exploration of low–grade barite deposits and associated barite deposits, similar to those in the Gansu–Qinghai–Ningxia barite metallogenic region, should not be overlooked. Finally, continuous exploration and development in regions such as North China and Xinjiang.

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张怡婷,钟怡江,王春连,李梦凡,张述鹏. 中国重晶石矿床分布特征、成因类型、资源应用现状及其展望[J]. 中国地质, 2025, 52(2): 495-512.
ZHANG Yiting, ZHONG Yijiang, WANG Chunlian, LI Mengfan, ZHANG Shupeng. Distribution characteristics, genesis types, current status of resource application of barite deposits in China and its prospects[J]. Geology in China, 2025, 52(2): 495-512(in Chinese with English abstract).

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  • 收稿日期:2023-10-12
  • 最后修改日期:2024-02-19
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  • 在线发布日期: 2025-05-12
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