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    中国磷矿成因类型、成矿规律及重点找矿方向

    Origin types, metallogenic regularity and prospecting direction of phosphate deposits in China

    • 摘要:
      研究目的 中国是世界磷矿资源大国,也是需求大国,2016年磷矿被纳入中国关键性矿产目录。随着对磷肥的需求日益增加、越来越多矿山的资源日趋枯竭,急需加大磷矿资源的地质找矿和勘查开发,而成矿规律研究是资源勘查开发的重要基础。
      研究方法 本文在前人工作基础上,进一步对中国磷矿资源开发利用现状、矿床类型、时空分布规律及找矿方向等进行分析与归纳,初步总结中国磷矿成矿规律及重点找矿方向。
      研究结果 中国磷矿资源丰富,但资源分布极不均匀,主要集中在云南、贵州、四川和湖北4省。依据成矿作用类型将中国磷矿划分为岩浆岩型、变质型、沉积型、次生型和鸟粪型磷矿床五大类;中国磷矿成矿时代广泛,但主要产磷时期为寒武世梅树村期、晚震旦世陡山沱期、古元古代锦屏期。按照《中国成矿区带划分方案》,可将中国磷矿划分为27个Ⅲ级成矿区带,4个成矿亚带,其中滇东-川西南成矿带、大巴山-鄂西成矿带、湘黔成矿带为中国主要磷矿成矿带。重要找矿地区为云、贵、川、湘、鄂西以及北方部分地区,南方磷矿资源以沉积型磷矿床为主;北方磷矿以岩浆岩型为主,主要分布在河北和新疆等省份。
      结论 磷关乎农业粮食安全、新能源及医疗等重要产业供应链安全稳定,作为人口大国的中国,对于磷化学品的需求量较大,面对中国磷矿分布不均匀及磷矿开采过度等问题,应加强对磷矿资源的调查研究及资源的高效综合利用研究,保障国内磷化产品供给及环境安全,推进资源的可持续发展。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objective China is a major country in terms of phosphate resources and major consumer. In 2016, phosphorus ore was included in the Catalogue of Key Mineral Resources in China. With the increasing demand for phosphorus fertilizer and the depletion of resources in more and more mines, it is urgently necessary to enhance geological prospecting and exploration development of phosphate resources. The study of mineralization regularities serves as an important foundation for resource exploration and development.
      Methods Building upon previous research, this article further analyzes and summarizes the current status of phosphate development and utilization, types of deposits, spatiotemporal distribution patterns, and prospecting directions in China. It provides a preliminary summary of the mineralization regularities and key prospecting directions for phosphorus ore in China.
      Results China possesses abundant phosphate resources, but their distribution is highly uneven, primarily concentrated in four provinces: Yunnan, Guizhou, Sichuan, and Hubei. Based on the types of mineralization processes, Chinese phosphate can be classified into five categories: magmatic rock−type, metamorphic−type, sedimentary−type, secondary−type, and guano−type deposits. The mineralization epochs of phosphate in China are extensive, with the major phosphate−bearing periods being the Meishucun period of the Cambrian, the Duoshantuo period of the Late Ediacaran, and the Jinping period of the Paleoproterozoic. According to the "Division Scheme of Metallogenic Belts in China," Chinese phosphate can be divided into 27 third−level metallogenic belts and four metallogenic sub−belts. Among them, the Dianzhong−Southwestern Sichuan Metallogenic Belt, the Daba Mountains−Western Hubei Metallogenic Belt, and the Xiang−Qian Metallogenic Belt are the main phosphate metallogenic belts in China. Important prospecting areas include Yunnan, Guizhou, Sichuan, Hunan, Western Hubei, and some regions in northern China. Southern phosphate resources are mainly sedimentary−type deposits, while northern phosphate resources are predominantly magmatic rock−type deposits, primarily distributed in Hebei and Xinjiang provinces.
      Conclusions Phosphorus is crucial for agricultural food security, as well as for important industries such as new energy and healthcare. As a populous nation, China has a significant demand for phosphorus chemicals. In the face of uneven distribution of phosphate and issues related to excessive mining, it is necessary to strengthen the investigation and research on phosphate resources, as well as study the efficient comprehensive utilization of these resources. This will ensure the stable supply of domestic phosphorus products and environmental safety, while promoting the sustainable development of resources.

       

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