可可西里西段羊湖盆地沉积、构造特征及其动力学意义

李亚林, 朱利东, 戴紧根, 王立成, 杨文光, 魏玉帅. 2013. 可可西里西段羊湖盆地沉积、构造特征及其动力学意义. 岩石学报, 29(3): 1017-1026.
引用本文: 李亚林, 朱利东, 戴紧根, 王立成, 杨文光, 魏玉帅. 2013. 可可西里西段羊湖盆地沉积、构造特征及其动力学意义. 岩石学报, 29(3): 1017-1026.
LI YaLin, ZHU LiDong, DAI JinGen, WANG LiCheng, YANG WenGuang, WEI YuShuai. 2013. Sedimentation and deformation of the Yanghu basin and its tectonic implications in the western Hoh Xil, Central Tibet. Acta Petrologica Sinica, 29(3): 1017-1026.
Citation: LI YaLin, ZHU LiDong, DAI JinGen, WANG LiCheng, YANG WenGuang, WEI YuShuai. 2013. Sedimentation and deformation of the Yanghu basin and its tectonic implications in the western Hoh Xil, Central Tibet. Acta Petrologica Sinica, 29(3): 1017-1026.

可可西里西段羊湖盆地沉积、构造特征及其动力学意义

  • 基金项目:

    本文受国家自然科学基金项目(41172129)、国家重点基础研究发展规划项目(2011CB822001)和中国地质调查局项目(1212011221103)联合资助.

详细信息
    作者简介:

    李亚林,男,1968年生,教授,构造地质学专业,E-mail: liyalin@cugb.edu.cn

  • 中图分类号: P542

Sedimentation and deformation of the Yanghu basin and its tectonic implications in the western Hoh Xil, Central Tibet

  • 对可可西里西段新生代盆地缺乏了解是导致该区新生代地质演化存在争议的重要原因。本文以沉积学和构造变形分析为主要手段,对可可西里西段羊湖盆地时代、充填序列、物源区和变形特征进行了分析,结果表明,羊湖盆地新生界沉积厚度大于1302m,主要由下部雅西错组冲积扇相碎屑岩和上部五道梁群湖泊相碳酸盐岩组成,其岩石组合和充填序列与可可西里东段具有一致性,同时古流向和碎屑锆石U-Pb年代学分析显示盆地物源来南部的羌塘地块,盆地形成演化受南部褶皱冲断带制约,盆地构造变形强烈,沿褶皱冲断带和羊湖盆地地壳分别发生51%和41%的缩短。沉积充填结构和变形特征表明,羊湖盆地与东段可可西里盆地具有相同的演化历史和性质,预示青藏高原中部在渐新世-中新世在存在一个大的、统一的可可西里盆地。

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  • 图 1 

    青藏高原中部新生代沉积盆地分布与构造格局

    Figure 1. 

    Tectonic map of the central Tibetan Plateau showing major tectonic units and distribution of the Cenozoic basins

    图 2 

    雪环湖-若拉错地区地质图

    Figure 2. 

    Geological map of the Xuehuanhu-Ruolacuo area

    图 3 

    羊湖盆地与可可西里盆地东段地层对比图(据Wang et al., 2008修改)

    Figure 3. 

    Comparisons of lithologic sections between the Yanghu basin, western Hoh Xil and the Fenghuoshan-Tongtianhe area, eastern Hoh Xil basin (revised after Wang et al., 2008)

    图 4 

    羊湖盆地沉积与构造变形特征

    Figure 4. 

    Outcrop photos showing the depositions and deformation of the Yanghu basin

    图 5 

    可可西里盆地东西部与拉萨-羌塘地体碎屑锆石U-Pb年龄对比图

    Figure 5. 

    U-Pb age probability plots for the Cenozoic sediments from the Hoh Xil Basin and the pre-Cenozoic sediments from the Qiangtang and Lhasa block

    图 6 

    雪环湖-若拉错地区构造剖面图

    Figure 6. 

    Xuehuanhu-Ruolacuo balanced cross-section and its evolution, showing the deformation of the Yanghu basin and southern fold-thrust belt

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出版历程
收稿日期:  2012-09-29
修回日期:  2013-01-09
刊出日期:  2013-03-01

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