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黄陵断穹核部鳞片石墨矿床石墨矿物学研究

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文章导航 > 西北地质 > 2020 > 53(3): 76-85

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边敏, 陈松林, 刘林, 程林, 刘海, 范玖琳, 李小伟, 陈晨, 兰绿灯, 姚敬劬. 2020. 黄陵断穹核部鳞片石墨矿床石墨矿物学研究. 西北地质, 53(3): 76-85. doi: 10.19751/j.cnki.61-1149/p.2020.03.006
引用本文: 边敏, 陈松林, 刘林, 程林, 刘海, 范玖琳, 李小伟, 陈晨, 兰绿灯, 姚敬劬. 2020. 黄陵断穹核部鳞片石墨矿床石墨矿物学研究. 西北地质, 53(3): 76-85. doi: 10.19751/j.cnki.61-1149/p.2020.03.006
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BIAN Min, CHEN Songlin, LIU Lin, CHENG Lin, LIU Hai, FAN Jiulin, LI Xiaowei, CHEN Chen, LAN Lüdeng, YAO Jingqu. 2020. Mineralogical Study of Crystalline Flake Graphite Ore of Huangling Faulted Dome-shaped Core. Northwestern Geology, 53(3): 76-85. doi: 10.19751/j.cnki.61-1149/p.2020.03.006
Citation: BIAN Min, CHEN Songlin, LIU Lin, CHENG Lin, LIU Hai, FAN Jiulin, LI Xiaowei, CHEN Chen, LAN Lüdeng, YAO Jingqu. 2020. Mineralogical Study of Crystalline Flake Graphite Ore of Huangling Faulted Dome-shaped Core. Northwestern Geology, 53(3): 76-85. doi: 10.19751/j.cnki.61-1149/p.2020.03.006
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黄陵断穹核部鳞片石墨矿床石墨矿物学研究

  • 1. 湖北冶金地质研究所(中南冶金地质研究所), 湖北 宜昌 443003;

  • 2. 湖北省地勘基金管理中心, 湖北 武汉 430071

  • 基金项目:

    湖北省国土资源厅科技计划项目“黄陵背斜核部晶质石墨矿矿物岩石地球化学及成矿作用的研究”项目（ETZ2017A07）资助；湖北省自然科学基金重点项目〔2015（FA143）〕

详细信息
    作者简介: 边敏(1967-),女,高级工程师,从事矿物岩石地球化学研究。E-mail:1193417311@qq.com
    通讯作者: 程林(1985-),男,助理研究员,注册测绘师,从事地质研究。E-mail:407970142@qq.com

  • 中图分类号: P619.252

Mineralogical Study of Crystalline Flake Graphite Ore of Huangling Faulted Dome-shaped Core

  • 1. Hubei Institute of Metallurgical Geology(Central South Institute of Metallurgical Geology), Yichang 443003, Hubei, China;

  • 2. Hubei Geological Exploration Fund Management Center, Wuhan 430071, Hubei, China

More Information

    摘要
  • 笔者研究黄陵断穹核部鳞片石墨矿床中石墨的矿物学特征，分析石墨生成的世代与石墨片径的关系，指出寻找大鳞片石墨矿的方向。本区石墨有序化程度高、结晶完好，具有高中级区域变质的成因特点；石墨有3个矿物世代，分别形成于绿片岩相、角闪岩相及麻粒岩相；石墨片径随变质程度提高而增大。碳质沉积岩原岩的角闪岩相及麻粒岩相分布区是寻找大鳞片石墨的目标区。
    The authors studied the Mineralogical characteristics of crystalline flack graphites in Huangling faulted dome-shaped core and analyzed the relationship between graphites generations and diameters of graphites, indicating the target areas for prospecting larger crystalline flake graphite deposits. The graphites in this area have perfect ordering and crystallization, and generated in middle and high ranking metamorphism. The graphites have three mineral generations of greenschist, amphibolite and granulite facics. The diameters increase along with metamorphic grades.The target areas for prospecting large crystalline flake graphite deposits are where amphibolite and granulite facies of the carbonaceous original rocks exist.
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收稿日期:  2019-11-03
修回日期:  2020-03-31

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