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黄河源地区晚更新世湖泛事件及其意义

韩建恩 罗鹏 余佳 邵兆刚 孟庆伟 王津 朱大岗

韩建恩, 罗鹏, 余佳, 等, 2020. 黄河源地区晚更新世湖泛事件及其意义. 地质力学学报, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022
引用本文: 韩建恩, 罗鹏, 余佳, 等, 2020. 黄河源地区晚更新世湖泛事件及其意义. 地质力学学报, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022
HAN Jian'en, LUO Peng, YU Jia, et al., 2020. Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance. Journal of Geomechanics, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022
Citation: HAN Jian'en, LUO Peng, YU Jia, et al., 2020. Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance. Journal of Geomechanics, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022

黄河源地区晚更新世湖泛事件及其意义

doi: 10.12090/j.issn.1006-6616.2020.26.02.022
基金项目: 

国家自然科学基金 41772381

中国地质科学院地质力学研究所基本科研业务费 DZLXJK201710

中国地质科学院地质力学研究所基本科研业务费 DZLXJK200902

中国地质调查局项目 12120113006100

中国地质调查局项目 1212011087114

详细信息
    作者简介:

    韩建恩(1980-), 男, 博士, 高级工程师, 主要从事青藏高原晚新生代沉积相与古环境研究。E-mail:hanjianen@163.com

  • 中图分类号: P534.63

Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance

  • 摘要: 通过青海玛多湖相地层剖面沉积特征,结合ESR样品年代测试结果,分析认为黄河源地区在13万年左右的晚更新世时期发生过湖泛事件。湖泛时期,玛多"四姐妹湖"相互连通,形成一个面积巨大的湖泊,约是现今"四姐妹湖"总面积的4.1倍。玛多地区此次湖泛事件与深海氧同位素MIS 6(Marine isotope stages 6)向MIS 5(Marine isotope stages 5)转变时期相对应,显示出青藏高原气候变化与全球气候变化密切相关,然而黄河源地区湖相地层对全球气候变化反应更敏感,记录的气候转换时间早于其他地区。玛多剖面湖相地层剖面沉积物的粒度、碳酸盐、磁化率分析表明,在132±10~128±12 ka年间,黄河源地区湖相沉积可分为9个阶段,表明青藏高原在MIS 6向MIS 5转变时期的气候变化是一个波动上升过程。13万年左右,黄河源地区大面积的湖相地层结束沉积,认为由于青藏高原共和运动,下游的多石峡被切开,湖水突然外泄所形成。

     

  • 图  1  黄河源地区构造地貌特征及玛多实测剖面位置图

    Figure  1.  Structural and geomorphological characteristics of the source area of the Yellow River and the measured profile location of Maduo County, Qinghai Province

    图  2  黄河源玛多湖相地层剖面特征

    a—玛多剖面地层划分、采样位置;b—剖面野外照片

    Figure  2.  Characteristics of the measured lacustrine strata profile in Maduo County

    图  3  玛多剖面沉积物粒度、碳酸盐和磁化率分析结果

    Figure  3.  Particle size, carbonate, susceptibility results of the Maduo profile

    图  4  玛多“四姐妹湖”及湖泛期时古湖泊范围对比

    a—玛多“四姐妹湖”现今遥感影像;b—玛多“四姐妹湖”湖泛期古湖泊范围

    Figure  4.  Comparison of the coverage of four lakes with that of the paleo-lake during the pan-lake period in Maduo County, Qinghai Province

    图  5  玛多剖面环境代用指标曲线与深海氧同位素曲线比较

    Figure  5.  Comparison of the environmental proxy curves of the Maduo profile with the deep-sea oxygen isotope curve

    上覆:表土层 0.30~0.40 m
    ①褐红色细砂层 30 cm
    ②褐红色中砂层,中夹小砾石 5 cm
    ③褐红色细砂层 50 cm
    ④褐黄色含砾中粗砂层,砾石呈薄片状 5 cm
    ⑤褐黄色含砾细砂层,夹铁锈色条带,见水平层理、斜层理,产状250°∠30° 70 cm
    ⑥褐红色含砾粗砂层,砾石棱角状、次棱角状,大小在0.5~1 cm 30 cm
    ⑦褐红色含细砾细砂层,砾石砾径约2 mm左右 30 cm
    ⑧灰白色含砾中砂层,中含粗砂层透镜体,砾石薄片状,见交错层理 15 cm
    ⑨褐红色细砂层,夹青灰色条带,局部见砂包泥现象,含螺化石 85 cm
    ———未见底———
    下载: 导出CSV

    表  1  黄河源地区玛多剖面湖相沉积物ESR测年结果

    Table  1.   ESR dating of lacustrine sediments of the Maduo profile, the source area of the Yellow River

    样品编号 深度/cm 古剂量/Gy 年剂量/mGy 年龄/kaB.P.
    2010P1-3ESR/B18 60 295.4 2.301 128±12
    2010P1-2ESR/B17 130 367.7 2.813 131±12
    2010P1-1ESR/B16 320 750.4 5.671 132±10
    注:由成都理工大学ESR实验室梁兴中教授测定
    下载: 导出CSV

    表  2  黄河源地区玛多剖面岩性与中值粒径、磁化率、碳酸盐含量变化

    Table  2.   Variations of median particle diameter, susceptibility and carbonate content with lithology in lacustrine strata of Maduo county, the source area of the Yellow River

    分段 深度/cm 岩性 中值粒径/μm 磁化率/×10-6 SI 碳酸盐含量/%
    I 0~30 褐红色细砂层 49.44~95.10 23.68~38.42 3.21~7.18
    H 30~35 褐红色中砂层 94.49~94.49 11.03~11.03 3.51~3.51
    G 35~85 褐红色细砂层 68.93~85.81 24.72~34.60 5.08~6.33
    F 85~90 褐黄色含砾中粗砂层 65.73~65.73 6.77~6.77 3.76~3.76
    E 90~160 褐黄色含砾细砂层 77.48~127.66 20.37~26.71 3.27~6.38
    D 160~190 褐红色含砾粗砂层 57.20~57.20 5.33~5.33 3.52~3.52
    C 190~220 褐红色含细砾细砂层 74.00~102.73 14.17~28.59 4.20~7.20
    B 220~235 灰白色含砾中砂层 10.31~10.31 9.57~9.57 2.59~2.59
    A 235~320 褐红色细纱层 46.89~75.60 21.58~30.56 4.14~5.69
    下载: 导出CSV
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  • 收稿日期:  2020-01-21
  • 修回日期:  2020-03-10
  • 刊出日期:  2020-04-28

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