古地理学报 ›› 2014, Vol. 16 ›› Issue (1): 9-18. doi: 10.7605/gdlxb.2014.01.009

• “黔北务正道地区铝土矿”专题 • 上一篇    下一篇

黔北务正道地区早二叠世铝土矿沉积古地理及其控矿意义*

崔滔1,2, 焦养泉2, 杜远生3, 汪小妹2, 雷志远4, 翁申富4, 金中国5   

  1. 1 贵州理工学院资源与环境工程学院,贵州贵阳 550003
    2 中国地质大学(武汉)资源学院,湖北武汉 430074
    3 中国地质大学(武汉)生物地质与环境地质国家重点实验室,湖北武汉 430074
    4 贵州省地质矿产勘查开发局,贵州贵阳 550004
    5 贵州省有色金属和核工业地质勘查局,贵州贵阳 550005
  • 收稿日期:2013-04-01 修回日期:2013-07-30 出版日期:2014-02-01 发布日期:2014-02-01
  • 作者简介:崔滔,男,1983年生,2013年毕业于中国地质大学(武汉),获博士学位,现为贵州理工学院副教授,主要从事铝土矿成矿规律的研究。E-mail: cuitao1203@163.com。
  • 基金资助:
    贵州省地勘基金“贵州务正道铝土矿基础地质与成矿规律研究”项目资助

Sedimentary palaeogeography and its mineralization significance of the Early Permian bauxite in Wuchuan-Zheng′an-Daozhen area,northern Guizhou Province

Cui Tao1,2, Jiao Yangquan2, Du Yuansheng3, Wang Xiaomei2, Lei Zhiyuan4, Weng Shenfu4, Jin Zhongguo5   

  1. 1 College of Resource and Environmental Engineering, Guizhou Institute of Technology, Guiyang 550003, Guizhou
    2 Faculty of Earth Resource,China University of Geosciences(Wuhan),Wuhan 430074,Hubei
    3 State Key Laboratory of Biogeology and Environment Geology,China University of Geosciences(Wuhan),Wuhan 430074,Hubei
    4 Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang 550004,Guizhou
    5 Non-ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou Province,Guiyang 550005,Guizhou
  • Received:2013-04-01 Revised:2013-07-30 Online:2014-02-01 Published:2014-02-01
  • About author:Cui Tao,born in 1983,obtained his Ph.D. degree from China University of Geosciences (Wuhan) in 2013. Now he is an associate professor of Guizhou Institute of Technology, and is mainly engaged in bauxite.E-mail: cuitao1203@163.com.

摘要: 通过野外地质调查、手标本观察、底板地层分布和矿体—含矿层厚度分析,对黔北务正道(务川—正安—道真)地区铝土矿沉积古地理及其与铝土矿成矿之间的关系进行了研究。结果表明:(1)铝土矿沉积盆地北以武隆为界,西北至南川,东至沿河,南至绥阳—凤冈一线;(2)研究区古地貌具南高北低的特点,沉积相带可分为海湾中心和滨岸湿地两部分,优质的铝土矿区均位于滨岸湿地;(3)沉积古地理决定了含矿层的厚度,但并不直接控制高品位铝土矿的形成,只有在其余成矿条件都适合的情况下,古地理通过控制铝土矿的沉积环境间接控制高品位铝土矿的形成。

关键词: 早二叠世, 铝土矿, 古地理, 控矿意义, 务正道地区, 贵州省

Abstract: Based on field geology,hand specimens,distribution characteristics of underlying strata,and thickness of orebody and ore beds,we conducted a comprehensive analysis on the palaeogeography and its relationship with the mineralization process of bauxite in Wuchuan-Zheng′an-Daozhen area, northern Guizhou Province. The results showed that:(1)The sedimentary basin of bauxite is bounded by Wulong area on the north, by Nanchuan area on the northwest, by Yanhe area on the east,and by Suiyang-Fenggang area on the south; (2)The south part of the basin had a higher ancient landform than the north,and the sedimentary environment of bauxite was composed by partly closed bay and shoreland glade,and the good-quality bauxite was almost in the shoreland glade;(3)Sedimentary palaeogeography controlled the thickness of ore beds but not directly controlled the forming of high-grade bauxite.Sedimentary palaeogeography indirectly controlled the forming of high-grade bauxite by controlling sedimentary environment of bauxite when other factors were beneficial.

Key words: Early Permian, bauxite, palaeogeography, mineralization significance, Wuchuan-Zheng′an-Daozhen area, Guizhou Province

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