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中国石膏分布、类型、产业应用现状及找矿前景分析

Distribution, origin, industrial application status and prospecting prospect of gypsum in China

  • 摘要:
    研究目的 石膏是中国储量大且分布广的优势非金属矿产之一,其应用十分广泛。总结分析中国石膏的分布、成因、应用以及找矿前景对于石膏的可持续利用具有重要意义。
    研究方法 本文从石膏矿床类型、时空分布、应用等方面入手,总结前人的研究成果以及收集相关资料,系统梳理了中国石膏的资源储量和矿山产量,提供了寻找新的石膏矿床的背景知识。
    研究结果 2022年中国石膏资源保有储量为17.58亿t,安徽省保有储量最多,矿床类型为沉积型、后生型和热液型石膏、硬石膏矿床,其中以沉积型矿床为主。中国石膏资源主要用于建材、工业、农业以及医学等行业。对石膏的再生利用,有利于缓解中国石膏资源紧张的局面。但是在利用工业副产石膏时产生的问题也不容忽视,所以也要注重天然石膏的开发、利用与保护。
    结论 石膏矿床形成主要受到气候、物源和构造的控制,封闭、半封闭的盆地,干旱、半干旱的气候条件以及充足的物质促进了石膏矿床的形成。祁连成矿带、天山—北山成矿带、西昆仑—阿尔金成矿带和长江中下游成矿带是中国石膏重要的成矿远景区。

     

    Abstract:
    This paper is the result of mineral exploration engineering.
    Objective Gypsum is one of the dominant nonmetallic minerals with large reserves and wide distribution in China, and its application is very wide. It is significant to summarize and analyse the distribution, source, application and prospect of Chinese gypsum for sustainable use.
    Methods Starting from the types, temporal and spatial distribution and application of gypsum deposits, this paper summarizes the previous research results and collects relevant data, systematically combs the resource reserves and mine output of gypsum in China, and provides the background knowledge for searching for new gypsum deposits.
    Results In 2022, the retained reserves of gypsum resources in China will be 1.758 billion tons, with the largest reserves in Anhui Province. The deposit types are sedimentary, epigenetic and hydrothermal gypsum and anhydrite deposits, among which sedimentary deposits are the main ones. China's gypsum resources are mainly used in building materials, industry, agriculture and medical industries. The regeneration and utilization of gypsum can help alleviate the tense situation of gypsum resources in our country. However, the problems caused by the use of industrial by−product gypsum can not be ignored, so we should also pay attention to the development, utilization and protection of natural gypsum.
    Conclusions The formation of gypsum deposits is mainly controlled by climate, provenance and structure. Closed and semi-closed basins, arid and semi-arid climatic conditions and sufficient materials promote the formation of gypsum deposits. Qilian metallogenic belt, Tianshan−Beishan metallogenic belt, West Kunlun Altun metallogenic belt and middle and lower Yangtze metallogenic belt are important metallogenic prospect areas of gypsum in China.

     

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