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柴西北缘花土沟地区新近系狮子沟组沉积特征与砂岩型铀矿关系分析

张超, 司庆红, 俞礽安, 王善博, 程银行, 于航, 冯平, 石广顺, 奥琮, 李志丹, 高雪峰. 2023. 柴西北缘花土沟地区新近系狮子沟组沉积特征与砂岩型铀矿关系分析[J]. 中国地质, 50(5): 1327-1342. doi: 10.12029/gc20200720004
引用本文: 张超, 司庆红, 俞礽安, 王善博, 程银行, 于航, 冯平, 石广顺, 奥琮, 李志丹, 高雪峰. 2023. 柴西北缘花土沟地区新近系狮子沟组沉积特征与砂岩型铀矿关系分析[J]. 中国地质, 50(5): 1327-1342. doi: 10.12029/gc20200720004
ZHANG Chao, SI Qinghong, YU Reng'an, WANG Shanbo, CHENG Yinhang, YU Hang, FENG Ping, SHI Guangshun, AO Cong, LI Zhidan, GAO Xuefeng. 2023. Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin[J]. Geology in China, 50(5): 1327-1342. doi: 10.12029/gc20200720004
Citation: ZHANG Chao, SI Qinghong, YU Reng'an, WANG Shanbo, CHENG Yinhang, YU Hang, FENG Ping, SHI Guangshun, AO Cong, LI Zhidan, GAO Xuefeng. 2023. Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin[J]. Geology in China, 50(5): 1327-1342. doi: 10.12029/gc20200720004

柴西北缘花土沟地区新近系狮子沟组沉积特征与砂岩型铀矿关系分析

  • 基金项目:
    中国地质调查局项目(DD20190119)和国家重点研发计划项目(2018YFC0604200)联合资助
详细信息
    作者简介: 张超, 男, 1987年生, 硕士, 高级工程师, 从事沉积地球化学、矿床学研究及矿产地质调查工作; E-mail: 402709002@qq.com
  • 中图分类号: P534

Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin

  • Fund Project: Supported by the projects of China Geological Survey (No.DD20190119) and National Key R&D Program of China (No.2018YFC0604200)
More Information
    Author Bio: ZHANG Chao, male, born in 1987, master, senior engineer, engaged in the study of sedimentary geochemistry, mineralogy and the geological survey of mineral resources; E-mail: 402709002@qq.com .
  • 研究目的

    柴西北缘花土沟地区发育典型砂岩型铀矿床,铀储层为七个泉组、狮子沟组及油砂山组,狮子沟组介于七个泉组与油砂山组之间,正确认识狮子沟组沉积特征与砂岩型铀矿关系成为亟待解决的地质问题。

    研究方法

    本文基于柴达木盆地砂岩型铀矿找矿工作,研究了狮子沟组沉积特征,分析了狮子沟组地层层序格架、成因机制、物源特征与铀矿关系。

    研究结果

    跃进2号地区ZK10杂砂岩颜色为棕红色,主体上为钙质泥砂岩,属碳酸盐陆源碎屑杂砂岩,CIA=37.79~69.14,ICV=0.84~2.13,Σ=1.39~2.14,K2O/Na2O=0.90~1.18(平均为1.06),说明杂砂岩中钾长石或钾矿物较多。224~240 m处测得的GR为0~30 API,RT为-5~45 Ω·m,测井相为箱型,曲线的幅度较大。K2O/Al2O3=0.22~0.27,Ni/Co=0.34~0.53。

    结论

    狮子沟组在该地区为河流相沉积环境,其上段源岩物质为干燥寒冷的古气候环境下的首次沉积,含有黏土物质较少。杂砂岩原岩形成于大陆岛弧环境,其源岩为浅源的碱性长石数量较少的长英质岩石,该组沉积环境非常有利于铀矿形成。

  • 加载中
  • 图 1  青藏高原及邻区大地构造简图(a,据王亮等,2010修改),柴达木盆地简要DEM图(b,据张超等,2020修改)及柴达木盆地狮子沟地区构造位置图(c,据路琳琳等,2008修改)

    Figure 1. 

    图 2  柴西北地区地层综合柱状图

    Figure 2. 

    图 3  花土沟狮子沟地区狮子沟组实测剖面图

    Figure 3. 

    图 4  花土沟狮子沟地区狮子沟组(N2s)岩性柱状图

    Figure 4. 

    图 5  狮子沟组沉积岩特征

    Figure 5. 

    图 6  跃进2号地区狮子沟组ZK10 223~241 m综合柱状图

    Figure 6. 

    图 7  狮子沟组杂砂岩样品中TiO2、Th与Al2O3相关性图解

    Figure 7. 

    图 8  柴达木盆地狮子沟组杂砂岩Fe2O3-Al2O3/SiO2构造环境判别图解(a)及F1'-F2'判别函数图(b)(底图据Bhatia, 1983

    Figure 8. 

    图 9  狮子沟组杂砂岩Ni-TiO2判别图(底图据Floyd et al., 1989

    Figure 9. 

    表 1  狮子沟组杂砂岩样品主量元素和部分微量元素测试分析结果

    Table 1.  Results of major and trace element analyses of mixed rocks of the Shizigou Formation

    下载: 导出CSV

    表 2  狮子沟组杂砂岩及各种构造环境中砂岩主要常量元素含量参考值

    Table 2.  Reference value of major element content in greywacke of Shizigou Formation and sandstone of various tectonic environments

    下载: 导出CSV
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出版历程
收稿日期:  2020-07-20
修回日期:  2020-10-01
刊出日期:  2023-10-25

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