开鲁盆地砂岩型铀矿中黄铁矿与铀矿化成因关系探讨

陈梦雅, 聂逢君, MostafaFAYEK. 2021. 开鲁盆地砂岩型铀矿中黄铁矿与铀矿化成因关系探讨[J]. 地球学报, (6): 868-880. doi: 10.3975/cagsb.2021.091702
引用本文: 陈梦雅, 聂逢君, MostafaFAYEK. 2021. 开鲁盆地砂岩型铀矿中黄铁矿与铀矿化成因关系探讨[J]. 地球学报, (6): 868-880. doi: 10.3975/cagsb.2021.091702
CHEN Meng-ya, NIE Feng-jun, Mostafa FAYEK. 2021. Discussion of the Genetic Relationship between Pyrite and Uranium Mineralization in Sandstone-type Uranium Deposits in Kailu Basin. Acta Geoscientica Sinica, (6): 868-880. doi: 10.3975/cagsb.2021.091702
Citation: CHEN Meng-ya, NIE Feng-jun, Mostafa FAYEK. 2021. Discussion of the Genetic Relationship between Pyrite and Uranium Mineralization in Sandstone-type Uranium Deposits in Kailu Basin. Acta Geoscientica Sinica, (6): 868-880. doi: 10.3975/cagsb.2021.091702

开鲁盆地砂岩型铀矿中黄铁矿与铀矿化成因关系探讨

  • 基金项目:

    本文由国家自然科学基金项目(编号: U2067202

    41772068

    41562006)和国家重点基础研究发展规划973计划“中国北方砂岩型铀矿流体成矿过程研究”(编号: 2015CB453002)联合资助

详细信息
    作者简介: 陈梦雅, 女, 1995年生。博士研究生。主要从事砂岩型铀矿研究。通讯地址: 330013, 江西省南昌市青山湖区广兰大道418号东华理工大学。E-mail: 269797285@qq.com
    通讯作者: 聂逢君, 男, 1962年生。博士, 教授。主要从事沉积学、砂岩型铀矿研究。通讯地址: 330013, 江西省南昌市青山湖区广兰大道418号东华理工大学。E-mail: niefj@263.net
  • 中图分类号: P619.14

Discussion of the Genetic Relationship between Pyrite and Uranium Mineralization in Sandstone-type Uranium Deposits in Kailu Basin

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    Corresponding author: NIE Feng-jun
  • 开鲁盆地位于松辽盆地西南部, 是中国北方砂岩型铀矿勘查的重点地区, 自钱家店铀矿床发现以来, 盆地内上白垩统姚家组目的层中相继发现了一些具有工业价值的铀矿床。为查明该层位中黄铁矿成因及其形成机制, 探讨其与铀矿化之间的关系, 本研究对含矿层砂岩中黄铁矿与铀矿物矿物学特征、黄铁矿S同位素开展细致研究。研究表明: (1)开鲁盆地姚家组砂岩中铀主要以独立铀矿物及吸附铀形式存在, 独立铀矿物以沥青铀矿为主, 含少量的钛铀矿及部分铀石, 多数沿黄铁矿周边生长。吸附态的铀与黏土矿物密切相关。(2)姚家组砂岩中黄铁矿主要以草莓状、胶状及粒状产出, 多与沥青铀矿共生, 其中黄铁矿 S同位素(d34S = –55.6‰~23.2‰), 平均值–20.87‰, 变化范围很大, 说明硫的分馏程度较高, 硫的来源范围较广。(3)分析表明黄铁矿具有细菌硫酸盐还原作用及热化学硫酸盐还原作用两种成因, 并探讨了这2种成因黄铁矿的形成机制。综合前人研究, 结合研究区成矿地质背景, 认为黄铁矿为铀成矿作用提供了发生还原反应所需要的还原剂, 且黄铁矿及铀矿物的形成与区内热流体存在紧密联系。
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收稿日期:  2021-07-23
修回日期:  2021-08-29

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