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陕西府谷高岭土矿沉积环境与成矿关系研究

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张炳社, 徐永, 王军, 张志海, 高春华. 陕西府谷高岭土矿沉积环境与成矿关系研究[J]. 西北地质, 2013, 46(2): 174-180.
引用本文: 张炳社, 徐永, 王军, 张志海, 高春华. 陕西府谷高岭土矿沉积环境与成矿关系研究[J]. 西北地质, 2013, 46(2): 174-180.
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ZHANG Bing-she, XU Yong, WANG Jun, ZHANG Zhi-hai, GAO Chun-hua. Study on the Relationship between the Depositional Environment and Minerallization of Fugu Kaolinite Deposit in Shanxi Province[J]. Northwestern Geology, 2013, 46(2): 174-180.
Citation: ZHANG Bing-she, XU Yong, WANG Jun, ZHANG Zhi-hai, GAO Chun-hua. Study on the Relationship between the Depositional Environment and Minerallization of Fugu Kaolinite Deposit in Shanxi Province[J]. Northwestern Geology, 2013, 46(2): 174-180.
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陕西府谷高岭土矿沉积环境与成矿关系研究

  • 1.

    西安地质矿产勘查开发院, 陕西 西安 710100

  • 2.

    内蒙古国土资源勘查开发院, 内蒙古 呼和浩特 010020

  • 基金项目: 七·五国家重点项目"陕西省府谷地区高岭土矿详细普查"[陕地发(86)21号]

Study on the Relationship between the Depositional Environment and Minerallization of Fugu Kaolinite Deposit in Shanxi Province

  • 1.

    Xi'an Geolgy and Mineral Exploration and Development lnstitute, Xi'an 710100, China

  • 2.

    Lnner Mongolia Land and Resources Exploration and Development Lnsitute, Huhehaote 010020, China

    摘要
  • 通过对高岭土矿及含矿沉积环境分析,认为府谷地区沉积型硬质高岭土矿分别形成于海岸后受淡水控制的湖泊、三角洲分流间湖泊、三角洲平原湖泊和曲流河岸后湖泊等。不同沉积环境其矿体特征、矿石类型及工业用途不同。海岸后受淡水控制的湖泊、三角洲分流间湖泊型沉积高岭土矿规模巨大,分布范围广,但高岭石含量低,杂质含量高,质量较差,工业用途受限用于制瓷业。而三角洲平原湖泊和曲流河岸后湖泊型矿床规模较前者小些,但高岭石含量高,杂质含量低,质量好,用于造纸、涂布原料及分子筛等。该项研究成果对高岭土矿勘查及其工业利用有所帮助。
    Analysis of the kaolinite deposit and its ore-deposition environment shows that the areas of Fugu hard sedimentary kaolinite deposits were formed respectively in the lake controlled by freshwater behind the coast, the lake between distributary channels, delta plain lakes and medering riparian lakes. Deposits formed in different sedimentary environments varies in orebody characteristics, ore types and industrial uses. The Deposits formed in the lake controlled by freshwater behind the coast and lake between distributary channels have a large scale and a wide distribution, however, because of the low kaolinite content, high impurity content, and poor quality of the kaolinite, their industrial uses were limited in Porcelain Manufacture. In contrast, the deposits formed in delta plain lakes and meandering riparian lakes are relatively smaller, whereas due to high kaolinite content, low impurity content, and good quality, this kind of kaolinite has many advanced industrial applications, such as paper coating and molecular sieve. The research is helpful to the exploration and industrial utilization of kaolinite deposit.
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  • 陕西省地质矿产局.陕西省区域地质志[M].北京:地质出版社,1989.

    Shaanxi Bureau of Geology and Mineral Resources.Regional Geology of Shaanxi Province[M].Geological Publishing House,Beijing,1989.

    陈景山,陈昌明,译.三角洲沉积与油气勘探[M].北京:石油工业出版社,1984.

    Chen Jingshan,Chen Changming Translate. Delta deposit and petroleum exploration[M]. Petroleum Industry Press,Beijing,1984.

    孙永传,李蕙生.碎屑岩沉积相和沉积环境[M].北京:地质出版社,1986.

    Sun Yongchuan,Li Huisheng.Sedimentary facies and depositional environment of clasolite[M]. Geological Publishing House,Beijing,1986.

    陈昌明,李继亮,译.陆源碎屑沉积环境[M].北京:石油工业出版社,1984.

    Chen Changming,Li Jiliang translate. The depositional environment of terrigenous clastic rock[M]. Petroleum Industry Press,Beijing,1984.

    李思田,解习农,王华,等.沉积盆地分析基础与应用[M].北京:高等教育出版社,2004.

    Li Sitian,Jie Xinong,Wang Hua,et al. Sedimentary Basin Analysis:Principle and Application[M]. Higher Education Press,Beijing,2004.

    陕西地质矿产局第八地质队.海则庙—段寨小区高岭土矿普查报告[R].1993.

    The Eighth Geological Team,Shaanxi Bureau of Geology and Mineral Resources. General investigation report of Haizemiao-Duanzhaixiaoqu kaolinite deposit[R].1993.

    陕西地质矿产局第八地质队.陕西省陕北石炭二叠纪煤田府谷矿区沙川沟井田勘探报告[R].1989.

    The Eighth Geological Team,Shaanxi Bureau of Geology and Mineral Resources. Exploration report of Carboniferous and Permian coal mining area of Fugu Shachuangou in the north of Shaanxi province[R].1989.

    陕西省地矿局西安地质矿产勘查开发院.陕西省陕北石炭二叠纪煤田府谷矿区段寨井田勘探报告[R].2009.

    Xi'an Geology and Mineral Exploration and Development Institute, Shaanxi Bureau of Geology and Mineral Resources. Exploration report of Carboniferous and Permian coal mining area of Fugu Duanzhai in the north of Shaanxi province[R].2009.

    陕西省地矿局西安地质矿产勘查开发院.陕西省陕北石炭二叠纪煤田府谷矿区尧峁井田详查报告[R].2011.

    Xi'an Geology and Mineral Exploration and Development Institute, Shaanxi Bureau of Geology and Mineral Resources. Exploration report of Carboniferous and Permian coal mining area of Fugu Yaomao in the north of Shaanxi province[R].2011.

    陕西省地矿局西安地质矿产勘查开发院.陕西省陕北石炭二叠纪煤田府谷矿区西王寨井田勘探报告[R].2009.

    Xi'an Geology and Mineral Exploration and Development Institute, Shaanxi Bureau of Geology and Mineral Resources. Exploration report of Carboniferous and Permian coal mining area of Fugu Wangzhai in the north of Shaanxi province[R].2009.

    陕西省地矿局西安地质矿产勘查开发院.陕西省陕北石炭二叠纪煤田府谷矿区冯家塔井田勘探报告[R].2004. Xi'an Geology and Mineral Exploration and Development Institute, Shaanxi Bureau of Geology and Mineral Resources. Exploration report of Carboniferous and Permian coal mining area of Fugu Fengjiata in the north of Shaanxi province[R].2004.

    曾允孚,夏文杰.沉积岩石学[M].北京:地质出版社,1986.

    Zeng Yunfu,Xia Wenjie. Sedimentary Petrology[M]. Geological Publishing House,Beijing,1986.

    郑葆英,刘仿韩,叶俭,等.鄂尔多斯石炭二叠系泥质岩沉积相分析[J].西北地质,1999,22(1):1-4.

    Zheng Baoying,Liu Fanghan,Ye Jian,et al. Sedimentary facies analysis of Carboniferous-Permian argillaceous rock in Erdos[J].Northwest Geology,1999,22(1):1-4.

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出版历程
收稿日期:  2013-03-22
修回日期:  2013-04-18
刊出日期:  2013-06-15

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