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阿尔泰造山带喀纳斯群变质碎屑岩地球化学特征及年代学研究

李晓光, 弓小平, 裴国栋, 韩琼, 赵同阳, 郑加行. 2018. 阿尔泰造山带喀纳斯群变质碎屑岩地球化学特征及年代学研究[J]. 中国地质, 45(2): 319-333. doi: 10.12029/gc20180208
引用本文: 李晓光, 弓小平, 裴国栋, 韩琼, 赵同阳, 郑加行. 2018. 阿尔泰造山带喀纳斯群变质碎屑岩地球化学特征及年代学研究[J]. 中国地质, 45(2): 319-333. doi: 10.12029/gc20180208
LI Xiaoguang, GONG Xiaoping, PEI Guodong, HAN Qiong, ZHAO Tongyang, ZHENG Jiaxing. 2018. Geochemistry and geochronology of metamorphic rocks in Kanas Group, Altay orogenic belt[J]. Geology in China, 45(2): 319-333. doi: 10.12029/gc20180208
Citation: LI Xiaoguang, GONG Xiaoping, PEI Guodong, HAN Qiong, ZHAO Tongyang, ZHENG Jiaxing. 2018. Geochemistry and geochronology of metamorphic rocks in Kanas Group, Altay orogenic belt[J]. Geology in China, 45(2): 319-333. doi: 10.12029/gc20180208

阿尔泰造山带喀纳斯群变质碎屑岩地球化学特征及年代学研究

  • 基金项目:
    国家自然科学基金项目“新疆东准噶尔卡拉麦里金矿带成矿流体特征及其与侵入体的关系研究”(41462004)和中国地质调查局项目“阿尔泰-准噶尔北缘成矿带矿产资源调查成果集成专题”(12120113041900)联合资助
详细信息
    作者简介: 李晓光, 男, 1991年生, 硕士生, 主要从事成矿规律研究; E-mail:842627738@qq.com
    通讯作者: 弓小平, 男, 1963年生, 博士, 教授级高级工程师, 主要从事综合信息成矿预测; E-mail:gxiaoping01@163.com
  • 中图分类号: P541

Geochemistry and geochronology of metamorphic rocks in Kanas Group, Altay orogenic belt

  • Fund Project: Supported by National Natural Science Foundation of Project " Study on the characteristics of ore-forming fluids and its relationship with intrusions in the Kalamaili gold belt, Eastern Junggar, Xinjiang " (No. 41462004); China Geological Survey Project"The integration project of the mineral resources survey results of the northern margin of Altay−Junggar metallogenic belt." (No. 12120113041900)
More Information
    Author Bio: LI Xiaoguang, male, born in 1991, master candidate, majors in the regularity of ore formation; E−mail: 842627738@qq.com .
    Corresponding author: GONG Xiaoping, male, born in 1963, doctor, professor, engages in metallogenic prediction based on comprehensive information; E−mail: gxiaoping01@163.com
  • 喀纳斯群为一套巨厚的中低压型浅变质碎屑岩系,主要由片岩、片麻岩、变质砂岩等组成,其形成时代未有统一的认识,致使阿尔泰构造带的构造演化过程争议较大。对喀纳斯群变质岩进行原岩恢复,认为该套变质岩为副变质岩,考虑到变质碎屑岩的成岩物质继承母岩特征和变质程度的影响,利用碎屑岩研究方法对元素地球化学特征进行探讨,显示出喀纳斯群变质碎屑岩原岩形成环境以大陆岛弧为主,兼有活动大陆边缘的特征,CIA、ICV指数反应出原岩经历了相对温暖、湿润的风化作用,成熟度较低。锆石U-Pb定年结果表明,最年轻的锆石年龄集中在(500±3.0)Ma,代表喀纳斯群的上限年龄,认为该套地层形成于晚寒武世晚期之前,为一套形成于大陆岛弧或活动大陆边缘的复理石建造。新元古代青白口纪初期基底裂解事件,暗示着阿尔泰构造带存在前寒武纪大陆地壳基底。

  • 加载中
  • 图 1  新疆阿尔泰造山带邻区板块构造单元划分及研究区地质概况a—阿尔泰造山带构造单元划分图;b—阿尔泰造山带区域地质图;c—研究区地质概况(图a据李俊建等, 2015;图b据李天德等, 2001; 图c据1:25万冲乎尔幅建造构造图修改)

    Figure 1. 

    图 2  依列克塔斯岩组和贝留特组变质岩显微照片

    Figure 2. 

    图 3  喀纳斯群变质碎屑岩主量元素构造环境判别

    Figure 3. 

    图 4  喀纳斯群变质碎屑岩稀土元素球粒陨石标准化图(球粒陨石数据引自McLennan, 1993

    Figure 4. 

    图 5  喀纳斯群变质碎屑岩微量元素蛛网图(原始地幔标准化数据引自Thompson, 1982

    Figure 5. 

    图 6  黑云母红柱石石英片岩(QY-2-16)测年锆石CL图像

    Figure 6. 

    图 7  黑云母红柱石石英片岩(QY-2-16)锆石U-Pb谐和图

    Figure 7. 

    图 8  喀纳斯群变质碎屑岩岩K-A相关图解及西蒙南图解(据王仁民等, 1987)

    Figure 8. 

    图 9  喀纳斯群变质碎屑岩Th-Hf-Co图解及La-Th-Sc图解(据Roser et al., 1986)

    Figure 9. 

    表 1  喀纳斯群变质岩特征

    Table 1.  Characteristic table of metamorphic rocks in Kanas Group

    下载: 导出CSV

    表 2  喀纳斯群变质碎屑岩主量元素(%)、稀土元素(10-6)、微量元素(10-6)分析数据

    Table 2.  Major elements (%), rare earth elements (10-6) and trace elements (10-6) compositions of metasedimentary rocks in Kanas Group

    下载: 导出CSV

    表 3  喀纳斯群变质碎屑岩与不同构造环境杂砂岩稀土元素特征对比

    Table 3.  Comparison of REE characteristic parameters of metasedimentary rocks in Kanas Group with various tectonic settings

    下载: 导出CSV

    表 4  喀纳斯群变质碎屑岩与不同构造环境杂砂岩微量元素特征对比

    Table 4.  Comparison of trace elements characteristic parameters of metasedimentary rocks in Kanas Group with various tectonic settings

    下载: 导出CSV

    表 5  黑云母红柱石石英片岩(QY-2-16)锆石的LA-ICP-MS定年分析结果

    Table 5.  LA-ICP-MS U-Pb zircon analyses of the Bi-And-Q schist (QY-2-16) in Kanas Group

    下载: 导出CSV

    表 6  喀纳斯群变质碎屑岩原岩恢复相关系数计算结果

    Table 6.  The indexes for recovering protoliths of metasedimentary rocks in Kanas Group

    下载: 导出CSV
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出版历程
收稿日期:  2016-08-30
修回日期:  2018-03-11
刊出日期:  2018-04-25

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