塔里木盆地中部满深1断裂带的多期断裂活动

黄少英, 张玮, 罗彩明, 李曰俊, 李洪辉, 周慧, 李程, 吴根耀, 黄智斌, 刘亚雷, 文磊. 2021. 塔里木盆地中部满深1断裂带的多期断裂活动. 地质科学, 56(4): 1015-1033. doi: 10.12017/dzkx.2021.053
引用本文: 黄少英, 张玮, 罗彩明, 李曰俊, 李洪辉, 周慧, 李程, 吴根耀, 黄智斌, 刘亚雷, 文磊. 2021. 塔里木盆地中部满深1断裂带的多期断裂活动. 地质科学, 56(4): 1015-1033. doi: 10.12017/dzkx.2021.053
Huang Shaoying, Zhang Wei, Luo Caiming, Li Yuejun, Li Honghui, Zhou Hui, Li Cheng, Wu Genyao, Huang Zhibin, Liu Yalei, Wen Lei. 2021. The faults and faulting phases of the Manshen-1 fault belt, central Tarim Basin. Chinese Journal of Geology, 56(4): 1015-1033. doi: 10.12017/dzkx.2021.053
Citation: Huang Shaoying, Zhang Wei, Luo Caiming, Li Yuejun, Li Honghui, Zhou Hui, Li Cheng, Wu Genyao, Huang Zhibin, Liu Yalei, Wen Lei. 2021. The faults and faulting phases of the Manshen-1 fault belt, central Tarim Basin. Chinese Journal of Geology, 56(4): 1015-1033. doi: 10.12017/dzkx.2021.053

塔里木盆地中部满深1断裂带的多期断裂活动

  • 基金项目:

    国家科技重大专项(编号:2017ZX05008-004,2016ZX05004-004)、中国石油股份科技项目(编号:kt2018-02-01)和中石油塔里木油田科技项目(编号:041019120072)资助。

详细信息
    作者简介:

    黄少英,男,1977年生,博士,高级工程师,构造地质学专业。E-mail:104281545@qq.com

  • 中图分类号: P542

The faults and faulting phases of the Manshen-1 fault belt, central Tarim Basin

  • 满深1断裂带位于塔里木盆地中部的阿满过渡带,走向NNE-SSW,是三维地震解释发现的一条断裂带。精细的三维地震解释识别出6期断裂,从老到新包括:南华—震旦纪正断层、晚奥陶世—早志留世逆冲断层、中志留世—石炭纪正断层、二叠纪正断层、三叠纪逆冲断层和侏罗纪正断层。中志留世—石炭纪的正断层可以进一步划分为中志留世—中泥盆世正断层和晚泥盆世—石炭纪正断层两期。前者为主,是昆仑—阿尔金早古生代碰撞造山带的造山后构造;后者是前者的复活。中志留世—石炭纪正断层作用形成一系列近南北走向的正断层,组合成一条NNE-SSW走向的右列左旋张扭性断层带,形成满深1断裂带。二叠纪裂谷作用成因的正断层和岩浆活动显著改造断裂带,使之基本定型。三叠纪的冲断构造叠加于依合2构造之上。侏罗纪伸展作用对构造带有一定的调整影响。南华—震旦纪正断层和晚奥陶世—早志留世的冲断构造与满深1断裂带相交,对构造带的形成影响不大。侏罗纪正断层的发现,是塔里木盆地当时处于区域性伸展构造背景的重要证据。
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收稿日期:  2020-11-10
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