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藏南及邻区典型晚新生代盆地磁性地层研究现状与时代对比分析

何林 吴中海 哈广浩 张海军

何林, 吴中海, 哈广浩, 等, 2016. 藏南及邻区典型晚新生代盆地磁性地层研究现状与时代对比分析. 地质力学学报, 22 (1): 135-151.
引用本文: 何林, 吴中海, 哈广浩, 等, 2016. 藏南及邻区典型晚新生代盆地磁性地层研究现状与时代对比分析. 地质力学学报, 22 (1): 135-151.
HE Lin, WU Zhong-hai, HA Guang-hao, et al., 2016. COMPARATIVE ANALYSIS ON THE MAGNETIC STRATA DEVELOPED IN THE LATE CENOZOIC BASINS IN THE SOUTHERN TIBET PLATEAU AND ITS ADJACENT AREAS. Journal of Geomechanics, 22 (1): 135-151.
Citation: HE Lin, WU Zhong-hai, HA Guang-hao, et al., 2016. COMPARATIVE ANALYSIS ON THE MAGNETIC STRATA DEVELOPED IN THE LATE CENOZOIC BASINS IN THE SOUTHERN TIBET PLATEAU AND ITS ADJACENT AREAS. Journal of Geomechanics, 22 (1): 135-151.

藏南及邻区典型晚新生代盆地磁性地层研究现状与时代对比分析

基金项目: 

国家自然科学基金项目 41171009

中国地质调查局项目"青藏高原东南缘重要活动断裂厘定与活动构造体系综合研究" 1212011120163

中国地质科学院地质力学研究所基本科研业务费项目 DZLXJK201202

详细信息
    作者简介:

    何林(1992-), 男, 硕士研究生, 研究方向为构造盆地与磁性地层学。E-mail:1009322912@qq.com

    通讯作者:

    吴中海(1974-), 男, 研究员, 从事第四纪地质和活动构造研究。E-mail:wzhh4488@sina.com

  • 中图分类号: P542

COMPARATIVE ANALYSIS ON THE MAGNETIC STRATA DEVELOPED IN THE LATE CENOZOIC BASINS IN THE SOUTHERN TIBET PLATEAU AND ITS ADJACENT AREAS

  • 摘要: 在系统梳理扎达盆地、尼泊尔Thakkhola半地堑盆地、吉隆—沃马盆地、乌郁盆地磁性地层研究成果的基础上, 对古地磁年代所代表的地质事件进行了对比和分析, 认为藏南及邻区各近南北向裂谷盆地自形成以来均发育2次明显的沉积变动事件, 第一次为距今10.6~8.1 Ma期间各盆地分别开始接受沉积, 第二次为距今3.5~2.0 Ma各湖盆的连续消亡; 总结高原的气候变化可以发现, 高原在距今约8 Ma及3 Ma左右也有明显的2次气候变化, 即沉积事件与气候变化事件在时间上具有近同时性。扎达盆地、吉隆—沃马盆地、达涕盆地三趾马化石的时代都处于距今7.0~6.5 Ma之间, 也具有近同时性。结合高原的整体演化, 认为其可能在距今10.6~8.1 Ma、3.5~2.0 Ma发生了2期比较强烈的隆升运动。同时, 分析指出了青藏高原南部及邻区晚新生代盆地磁性地层研究过程中存在的问题及解决方法, 并对今后青藏高原南部及邻区地区晚新生代磁性地层研究提出了建议。

     

  • 图  1  青藏高原南部及邻区进行过磁性地层研究的晚新生代主要盆地大地构造简图(据文献[10]修改)

    1—扎达盆地;2—Thakkhola盆地;3—吉隆—沃马盆地;4—达涕盆地;5—帕里盆地;6—乌郁盆地

    Figure  1.  The tectonic diagram of late Cenozoic basins magnetostratigraphic study in the Southern Tibetan plateau and its adjacent area

    图  2  扎达盆地磁性地层多解性对比[13](a为原文,b为重新解释)

    Figure  2.  Magnetic stratigraphy multiple solutions contrast figure of the Zhada basin

    图  3  吉隆—沃马盆地磁性地层多解性对比图[15](a为原文结果,b为重新解释后结果)

    Figure  3.  Magnetic stratigraphy multiple solutions contrast figure of the Gyirong-Oma basin

    图  4  青藏高原南部及邻区晚新生代盆地磁性地层对比图

    1—泥岩;2—砂岩;3—砾岩;4—含砾灰岩;5—泥灰岩;6—化石层;7—褐煤;8—砂岩-黏土互层;9—正极性带;10—负极性带;11—硅化木;12—脊椎动物化石;13—螺;14—轮藻;15—植物叶化石;Ⅰ—扎达盆地扎达-波林剖面(王世峰等,2008);Ⅱ—Thakkhola半地堑盆地Tetan村剖面(carmalaN.Garzione等,2000);Ⅲ—吉隆-沃马盆地龙骨沟剖面(岳乐平等,2004);Ⅳ—吉隆-沃马盆地塔千沟剖面(王富葆等,1996);Ⅴ—吉隆-沃马盆地加莫沟剖面(王富葆等,1996);Ⅵ—吉隆-沃马盆地龙骨沟剖面(王富葆等,1996);Ⅶ—乌郁盆地乌郁玛曲剖面(陈贺海等,2007)

    Figure  4.  magnetic stratigraphy contrast figure of mainly late Cenozoic basins in the southern Tibetan plateau and its adjacent area

    表  1  青藏高原南部及邻区晚新生代主要盆地地层对比

    Table  1.   Stratigraphic correlation of mainly late Cenozoic basins in the Southern Tibetan plateau and its adjacent area

    表  2  青藏高原南部及邻区晚新生代主要盆地磁性地层研究结果整理与重新分析

    Table  2.   Magnetic stratigraphy results of mainly late Cenozoic basins in the Southern Tibetan plateau and its adjacent area

    盆地采样剖面
    地层名称
    地层厚度/
    m
    采样间距/
    m
    采样数量/
    原来确定的
    地层时代/Ma
    重新解释
    结果/Ma
    资料来源
    扎达香孜组,札达组未知未知样点81个,每
    个样点2~4块
    6.15~1.25钱方等, 1999
    扎达组,托林组7502~32689.5~2.69.1~3.5王世峰等,2008
    ThakkholaTetang组230未知5510.6~9.610.6~9.6CarMa la N.
    Garzione等,2000
    吉隆—沃马贡巴南木林组,卧马组,仲喀组320~440未知1897.0~1.79.0~2.2王富葆等,1996
    沃马组1600.53487.2~3.27.2~3.2岳乐平等,2004
    达涕达涕组未知未知49高斯正向期
    (2.4~3.4)
    朱志文等,1980
    帕里帕里湖相层32.5144高斯正向期
    (2.4~3.4)
    朱志文等,1980
    乌郁乌郁湖相层(朱迎堂等[34]称为乌郁群,包括下伏乌郁组与上覆达孜组)1450.52708.1~2.58.1~2.5陈贺海等,2007
    下载: 导出CSV
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  • 收稿日期:  2015-10-22
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