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煤系共伴生矿产地质成因与成矿过程

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目前,关于煤系共伴生矿产地质成因与成矿过程的研究多分散针对单一矿产,系统化研究仍较为缺乏.文章系统性地总结论述煤系共伴生矿产的成矿有利条件、地质成因及成矿过程等.按照主控成矿作用,煤系共伴生矿产地质成因可以分为变质作用成矿、沉积作用成矿和后生作用成矿三大类.以聚煤盆地形成演化为主线,煤系形成前期,铝、铁率先在盆地基底沉积成矿.随后煤系油页岩、高岭土等沉积型矿床多因成煤环境改变而与煤层交替沉积成矿,镓、锗等金属元素多由含矿流体携带富集于成煤沼泽之内,煤成气、富油煤及煤系石墨则是煤系有机质在各种条件下的变质分化产物.在煤系演化后期,砂岩型铀矿和各种稀有金属元素则会后生成矿于煤系内.煤系共伴生矿产成矿的主控因素主要包括适当的地质构造活动、充足的物质来源、湿热的古地理气候以及煤系内丰富的有机质等,受这些因素影响,各大聚煤期内煤系矿产资源的成矿特征存在明显差异.
Geological genesis and mineralizing process of co-existed and associated minerals in coal series
At present,research on the geological genesis and mineralizing process of co-existed and as-sociated minerals in coal series is mostly scattered,targeting a single mineral,and systematic research is still lacking.This article systematically summarizes and discusses the favorable conditions,geological genesis,and mineralizing processes of co-existed and associated minerals in coal series.According to the main mineralizing process,the geological genesis of co-existed and associated minerals in coal series can be divided into three categories:metamorphic mineralization,sedimentary mineralization,and epigenetic mineralization.Taking the formation and evolution of coal accumulation basins as the main line,alumi-num and iron were the first to deposit and mineralize in the basement of the basin in the early stage of coal series formation.Subsequently,sedimentary deposits such as coal series oil shale and kaolin were mostly deposited and mineralized alternately with coal seams due to changes in coal-forming environment.Metal elements such as gallium and germanium were mostly carried and enriched in coal-forming swamps by ore-bearing fluids.Coal-formed gas,tar-rich coal,and coal-based graphite were metamorphic and differentiated products of coal-bearing organic matter under various conditions.In the later stage of coal series evolution,sandstone type uranium deposits and various rare metal elements were formed in the coal series.The main controlling factors for the mineralization of co-existed and associated minerals in coal series mainly include appropriate geological tectonic activities,sufficient material sources,humid and warm paleogeographic climate,and abundant organic matter within the coal series.Influenced by these factors,there are significant differences in the mineralization characteristics of coal series mineral resources in different coal accumulation periods.

coal seriesco-existed and associated mineralsgeological genesismineralizationmine-ralizing process

韩晓克、黄炳香、王长申、赵兴龙、吴占伟、陈大勇

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中国矿业大学煤炭精细勘探与智能开发全国重点实验室,江苏 徐州 221116

中国矿业大学资源与地球科学学院,江苏 徐州 221116

煤系 共伴生矿产 地质成因 成矿作用 成矿过程

国家重点研发计划

2021YFC2902105

2024

采矿与安全工程学报
中国矿业大学 中国煤炭工业劳动保护科学技术学会

采矿与安全工程学报

CSTPCD北大核心
影响因子:2.054
ISSN:1673-3363
年,卷(期):2024.41(1)
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