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    郯庐断裂带辽东湾段新生代右旋走滑时限的探讨

    李伟 李嘉 吴宛秋 张同杰 陈兴鹏 蒙美芳 曹明月 张巧

    李伟, 李嘉, 吴宛秋, 张同杰, 陈兴鹏, 蒙美芳, 曹明月, 张巧, 2024. 郯庐断裂带辽东湾段新生代右旋走滑时限的探讨. 地球科学, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480
    引用本文: 李伟, 李嘉, 吴宛秋, 张同杰, 陈兴鹏, 蒙美芳, 曹明月, 张巧, 2024. 郯庐断裂带辽东湾段新生代右旋走滑时限的探讨. 地球科学, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480
    Li Wei, Li Jia, Wu Wanqiu, Zhang Tongjie, Chen Xingpeng, Meng Meifang, Cao Mingyue, Zhang Qiao, 2024. Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone. Earth Science, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480
    Citation: Li Wei, Li Jia, Wu Wanqiu, Zhang Tongjie, Chen Xingpeng, Meng Meifang, Cao Mingyue, Zhang Qiao, 2024. Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone. Earth Science, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480

    郯庐断裂带辽东湾段新生代右旋走滑时限的探讨

    doi: 10.3799/dqkx.2022.480
    基金项目: 

    中海油课题资助 CCL2013TJXSBS1881-03

    详细信息
      作者简介:

      李伟(1978-),男,副教授,主要从事构造地质学方面的研究.ORCID:0000-0003-3567-7911. E-mail:20070017@upc.edu.cn

    • 中图分类号: P618

    Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone

    • 摘要: 新生代郯庐断裂带经历了复杂的演化过程,争议主要集中在右旋走滑开始的时期.以渤海海域郯庐断裂带辽东湾段为例,基于各种地质、地球物理资料及前人研究成果,从构造学和沉积学两个方面基于多种证据系统探讨了郯庐断裂带的右旋走滑活动时限.结果表明:郯庐断裂带辽东湾段走滑活动切割改造了早期(孔店组-沙三段沉积期)伸展断裂系统,R剪切断裂形成于渐新世晚期东营组沉积期,走滑派生构造主要发育在东营组沉积期至今;郯庐断裂带辽东湾段的右旋走滑活动错开了先期(孔店组-沙河街组沉积期)形成的沉积体,同沉积期走滑活动导致了鱼跃式砂体、轴向或斜向砂体的发育展布,弯曲走滑断裂的释压作用控制了的局部洼陷的形成.郯庐断裂带辽东湾段新生代右旋走滑主要在古近纪渐新世晚期东营组沉积期,此后逐渐减弱、持续至今.

       

    • 图  1  辽东湾坳陷主要断裂展布及构造单元区划图

      F1.辽东1号断层;F2.辽中1号断层;F3.辽中2号断层;F4.辽西1号断层;F5.辽西2号断层;F6.辽西3号断层;F7.辽西南1号断层;F8.辽西走滑断裂;据李伟等(2019b)修改

      Fig.  1.  Map showing the distribution of the main faults and structural units in Liaodong Bay depression

      图  2  辽东湾坳陷地层垂向发育特征(据李伟等,2019b修改)

      Fig.  2.  Vertical development of strata in Liaodong Bay depression(modified from Li et al., 2019b)

      图  3  辽东湾坳陷走滑断裂切割早期伸展断裂剖面特征及模式

      a~c.辽中1号、辽东1号断裂切割辽中2号断裂;d~f.辽西走滑断裂切割辽西南1号断裂

      Fig.  3.  Characteristics and patterns of early extensional faults cut by strike-slip faults in the Liaodong Bay depression

      图  4  辽东湾坳陷辽中南洼走滑断裂平面及剖面特征

      a.1 000 ms水平相干切片;b.过雁列式R剪切断裂带NE向剖面

      Fig.  4.  Plane and section characteristics of strike-slip fault in southern Liaozhong sag, Liaodong Bay depression

      图  5  辽中1号断裂尾端发育的走滑派生次级断裂平面及剖面特征

      a.平面特征(1 200 ms等时相干切片);b, c.垂直于走滑派生断裂的的NE向剖面

      Fig.  5.  Plane and section characteristics of strike-slip derived secondary faults developed at the tail end of Liaozhong.1 fault

      图  6  辽东湾坳陷辽东带沙二-沙一段沉积相图(据徐长贵,2006; 加东辉等,2007)

      Fig.  6.  Sedimentary facies of the second and first members of Shahejie Formation in Liaodong Bay depression (modified from Xu, 2006; Jia et al., 2007)

      图  7  金县1-1地区走滑断裂水平位移与辫状河三角洲“鱼跃式”迁移

      a.东营组辫状河三角洲砂体的鱼跃时迁移特征(剖面位置见图b);b.东营组沉积相图; 据徐长贵等(2017)

      Fig.  7.  Horizontal displacement of strike-slip faults and "diving" migration of braided river deltas in Jinxian 1-1 area

      图  8  辽东湾坳陷南部古近纪构造-沉积充填模式

      a.沙三段沉积期;b.东营组沉积期;据Li et al. (2021)修改

      Fig.  8.  Paleogene tectonic-sedimentary filling model in southern Liaodong Bay depression

      图  9  辽东湾坳陷辽东1号断裂南段弯曲走滑释压段构造特征

      a.辽中2号断裂南端馆陶组底界面拉平后东营组底界面立体显示;b.原始地震剖面c.地震剖面特征(测线位置见图 1a-a’)

      Fig.  9.  Structural characteristics of the south section of Liaodong.1 fault in Liaodong Bay depression

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    出版历程
    • 收稿日期:  2022-09-18
    • 网络出版日期:  2024-07-11
    • 刊出日期:  2024-06-25

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