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现代矿业 ›› 2022, Vol. 38 ›› Issue (08): 65-.

• 地质·测量 • 上一篇    下一篇

广西平广林场那厘矿区熔剂用石灰岩矿矿床地质特征及成因探讨

陆世才1,2 农良春1 叶胜1 江沙1 龙鹏1 聂继绩3 陈俊宏4   

  1. 1. 中国冶金地质总局广西地质勘查院;2. 中国冶金地质总局矿产资源研究院; 3. 上思县自然资源局;4. 广西水利电力职业技术学院
  • 出版日期:2022-08-25 发布日期:2023-06-02

Geological Characteristics and Genesis of the Limestone Deposits Used for Flux in the Nali Mining Area of Pingguang Forest Farm,Guangxi

LU Shicai1,2 NONG Liangchun1 YE Sheng1 JIANG Sha1 LONG Peng1 NIE Jiji3 CHEN Junhong4   

  1. 1. Geological Prospecting Institute of Guangxi of China Metallurgical Geology Bureau; 2. Institute of Min⁃ eral Resources Research,China Metallurgical Geology Bureau; 3. Department of Natural Resources of Shangsi; 4. Guangxi Vocational College of Water Resources and Electric Power
  • Online:2022-08-25 Published:2023-06-02

摘要: 上思县平广林场那厘矿区熔剂用石灰岩矿位于十万大山复式向斜西部,上思盆地以 北。通过分析矿区地质、矿体地质、控矿因素等,总结矿床地质特征及矿床成因。矿区圈出3 个石 灰岩矿体,矿体规模大,厚度稳定,有益组分CaO 品位在54.21%~55.45%,品位较高且稳定,有害组 分含量低。矿床主要形成于早中二叠世裂谷盆地内的孤立台地,该时期沉积的茅口组地层为石灰 岩矿赋存层位,矿体展布主要受地层控制,次级褶皱及断裂造成地层的重复、缺失。

关键词: 石灰岩矿, 矿床地质, 矿床成因

Abstract: The limestone mine for flux in the Nali mining area of Pingguang Forest Farm in Shangsi County is located in the west of the Shiwanda Mountain compound syncline and in the north of the Shangsi Basin. By analyzing the mining area geology,ore body geology,ore controlling factors,etc.,the geological characteristics of the ore deposit and the genesis of the ore deposit are summarized. Three limestone ore bodies are delineated in the mining area,the ore bodies are large in scale and stable in thickness. The de⁃ posit is mainly formed in the isolated platform in the Early-middle Permian rift basin. The strata of Maokou Formation deposited during this period are limestone deposits. The distribution of ore bodies is mainly con⁃ trolled by strata,and secondary folds and faults cause stratigraphic duplication and deletion.

Key words: limestone mine, deposit geology, ore genesis