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金属矿山 ›› 2025, Vol. 54 ›› Issue (12): 245-258.

• 地质与测量 • 上一篇    下一篇

几内亚铝土矿矿床特征、成矿规律及找矿方向

袁杨森 王滑冰 张 俊 张泽夏 郭景会 闫广厚 郭玉溪   

  1. 河南省第二地质矿产调查院有限公司,河南 郑州 450001
  • 出版日期:2025-12-15 发布日期:2025-12-31
  • 通讯作者: 王滑冰(1987—),男,高级工程师,硕士。
  • 作者简介:袁杨森(1982—),男,正高级工程师,硕士。
  • 基金资助:
    河南省豫地科技集团有限公司科技项目(编号:豫地集团[2023]60号)。

Deposit Characteristics,Metallogenic Regularity and Prospecting Direction of Bauxite in Guinea

YUAN Yangsen WANG Huabing ZHANG Jun ZHANG Zexia GUO Jinghui YAN Guanghou GUO Yuxi   

  1. Henan No.2 Institute of Geological and Mineral Resources Survey Co.,Ltd.,Zhengzhou 450001,China
  • Online:2025-12-15 Published:2025-12-31

摘要: 几内亚拥有全球最为丰富、优质的铝土矿资源,目前是中国铝土矿资源的最主要供应国。研究几内亚 铝土矿矿床特征、成矿规律及找矿方向,对于促进我国企业参与几内亚铝土矿资源勘查开发、保障我国铝土矿持续供 应具有重要意义。在系统总结几内亚铝土矿资源禀赋和典型矿床特征的基础上,探讨了铝土矿的矿床类型和时空分 布规律,划分了成矿区带。研究表明:① 几内亚已查明铝土矿资源储量巨大,居世界首位,探明资源储量主要集中分 布在西部博凯地区、科贡河—托米尼河和法塔拉—弗里亚成矿区,资源品质较好;② 将铝土矿矿床类型划分为红土 型、沉积—红土型和堆积型3类,以红土型为主;③ 铝土矿均赋存于红土风化壳中,高原台地和准平原弓(弧)形地貌 是其产出的最佳地段;④ 成矿母岩主要为中生代玄武岩、辉长(绿)岩,其次为新元古代—古生代富铝泥质岩、粉砂质 泥岩等;⑤ 成矿作用始于晚白垩世、最晚持续到早更新世,中—晚中新世是主成矿期。根据成矿条件、成矿规律和外 部开发环境,将该成矿单元进一步划分为西部博韦盆地、中部福塔—贾隆高原和东部丁吉拉伊3个二级成矿带以及 12个成矿区(远景区)。

关键词: 铝土矿 矿床特征 成矿规律 找矿方向 几内亚

Abstract: Guinea is endowed with the world's richest and highest-quality bauxite resources and is currently the main supplier of bauxite to China. Studying the characteristics,mineralization regularity,and prospecting directions of bauxite in Guinea is of great significance for promoting the participation of Chinese enterprises in the exploration and development of bauxite resources in Guinea and ensuring the continuous supply of bauxite for China.Based on the summary of bauxite resource endowment and typical deposit characteristics in Guinea,this paper discusses the deposit types,spatial and temporal distribu tion of bauxite in Guinea,and divides the mineralization zones in detail.The results show that:① Guinea has the largest proven bauxite reserves in the world,mainly concentrated in the Boke region in the west,the Kogon-Tomini River and Fatala-Fria min eralization area,with good resource quality.② The deposits are classified into three types:lateritic,sedimentary-lateritic and accumulation types,with lateritic type being the dominant one.③ All bauxite occurs in laterite weathering crust,and the distri bution and deposit characteristics of bauxite are closely related to the topography and underlying ore-forming parent rocks.④ The main ore-forming parent rocks are Mesozoic basalt and gabbro,followed by Neoproterozoic and Paleozoic aluminium-rich argillite and silty mudstone etc.⑤ Mineralization began in the Late Cretaceous and continued to the Early Pleistocene at the latest,and the Middle to Late Miocene is the main metallogenic period.According to ore-forming conditions,metallogenic regu larity and development environment,the bauxite ore-forming unit in Guinea is further divided into three secondary mineraliza tion belts:the western Bové Basin,the central Fouta-Djallon Plateau,and the eastern Dinguiraye,as well as 12 mineralization areas (prospective potential areas).

Key words: bauxite,deposit characteristics,metallogenic regularity,prospecting direction,Guinea

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