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    郯庐断裂带渤南段构造特征及其控盆作用

    张婧 李伟 吴智平 李春锐 杨波 张晓庆

    张婧, 李伟, 吴智平, 李春锐, 杨波, 张晓庆, 2017. 郯庐断裂带渤南段构造特征及其控盆作用. 地球科学, 42(9): 1549-1564. doi: 10.3799/dqkx.2017.110
    引用本文: 张婧, 李伟, 吴智平, 李春锐, 杨波, 张晓庆, 2017. 郯庐断裂带渤南段构造特征及其控盆作用. 地球科学, 42(9): 1549-1564. doi: 10.3799/dqkx.2017.110
    Zhang Jing, Li Wei, Wu Zhiping, Li Chunrui, Yang Bo, Zhang Xiaoqing, 2017. Structural Characteristics of Tan-Lu Fault Zone in South Area of Bohai Sea and Its Control on Basin Structure. Earth Science, 42(9): 1549-1564. doi: 10.3799/dqkx.2017.110
    Citation: Zhang Jing, Li Wei, Wu Zhiping, Li Chunrui, Yang Bo, Zhang Xiaoqing, 2017. Structural Characteristics of Tan-Lu Fault Zone in South Area of Bohai Sea and Its Control on Basin Structure. Earth Science, 42(9): 1549-1564. doi: 10.3799/dqkx.2017.110

    郯庐断裂带渤南段构造特征及其控盆作用

    doi: 10.3799/dqkx.2017.110
    基金项目: 

    国家油气重大专项课题 No.2011ZX05023-006-05

    详细信息
      作者简介:

      张婧(1988-), 女, 博士, 主要从事油区构造解析及含油气盆地分析方面的研究

      通讯作者:

      李伟

    • 中图分类号: P542

    Structural Characteristics of Tan-Lu Fault Zone in South Area of Bohai Sea and Its Control on Basin Structure

    • 摘要: 渤南地区郯庐断裂带具有很好的油气勘探前景,但由于其构造特征复杂,目前对渤南地区油气成藏条件、主控因素及富集规律的认识尚不明晰.通过对三维地震和地质资料的分析解释,结合前人研究成果,探讨了渤南地区郯庐断裂带构造特征的时空差异及其对盆地结构的控制作用.研究表明,渤南地区郯庐断裂带具有3组分支断裂,每组分支断裂由2~4条断裂构成,均表现出了明显的走滑特征,整体由东向西、由深至浅走滑程度逐渐减弱.新生代古新世-早始新世郯庐断裂带渤南段左旋走滑,东部分带活动明显、强度大,中带和西带不活动或活动较弱,渤南地区中生代发育的NWW向伸展断裂系统复活,形成北断南超的复式半地堑或南北双断式结构;中始新世以来,渤南地区郯庐断裂带转为右旋走滑,3组分支断裂均开始活动,表现为强烈的走滑兼伸展运动,强度由东向西逐渐减弱,中带分支断裂形成的中央构造脊将黄河口凹陷分割成东、西两个次洼,并开始逐渐发育一系列次级断层,与主断裂构成帚状断裂组合;新近纪-第四纪郯庐断裂渤南段表现为右旋走滑兼挤压,主走滑断裂不连续,代之以大量规模较小的次级断裂系统.太平洋区板块俯冲方向、俯冲速率的变化以及深部动力背景的变迁共同造成了渤南地区郯庐断裂不同分支构造发育演化及其控盆作用的差异性,由于右旋走滑位移量小于先期的左旋走滑,现今渤南地区构造单元分布仍具左旋特征.

       

    • 图  1  渤南地区区域构造位置及主要断裂和构造单元区划

      漆家福等(2008)修改

      Fig.  1.  Regional structural location of the south area of Bohai Sea shows the mainly fault system and tectonic unit division

      图  2  郯庐断裂带渤南段大地电磁测深二维连续介质反演剖面

      宋国奇(2006)

      Fig.  2.  Magnetotelluric sections across Tan-Lu fault zone in the south area of Bohai Sea

      图  3  渤南地区不同层系底界面立体显示

      a.新生代底界面;b.沙二段底界面;c.明化镇组底界面

      Fig.  3.  Stereoscopic displays of the bottom of each layer in the south area of Bohai Sea

      图  4  渤南地区郯庐断裂东带平面及剖面特征

      a.500 ms水平相干切片;b.EW向剖面Ⅰ;c.SN向剖面Ⅱ

      Fig.  4.  Structural patterns of the east branch of Tan-Lu fault zone in the south area of Bohai Sea in plane and section

      图  5  渤南地区郯庐断裂带中带平面及剖面特征

      a.1 000 ms水平相干切片;b.EW向剖面Ⅲ;c.EW向剖面Ⅳ;d.SN向剖面Ⅴ

      Fig.  5.  Structural patterns of the middle branch of Tan-Lu fault zone in the south area of Bohai Sea in plane and section

      图  6  渤南地区郯庐断裂带西支1号、2号断裂平面及剖面特征

      a.1 200 ms水平相干切片;b.2 500 ms水平相干切片;c.EW向剖面Ⅵ

      Fig.  6.  Structural patterns of fault 1 and fault 2 of the west branch of Tan-Lu fault zone in the south area of Bohai Sea in plane and section

      图  7  渤南地区郯庐断裂带西支3号、4号断裂平面及剖面特征

      a.1 000 ms水平相干切片;b.2 800 ms水平相干切片;c.EW向剖面Ⅶ

      Fig.  7.  Structural patterns of fault 3 and fault 4 the west branch of Tan-Lu fault zone in the south area of Bohai Sea in plane and section

      图  8  渤南地区过黄河口和莱州湾凹陷典型地震剖面反映角度不整合的发育

      a.过莱州湾凹陷SE向剖面;b.过黄河口凹陷SE向剖面.剖面位置见图 1

      Fig.  8.  The seismic sections show angular unconformity developed in Huanghekou sag and Laizhouwan sag in the south area of Bohai Sea

      图  9  渤南地区新生代各层系残留地层展布等值线

      a.孔店组~沙四段;b.沙三段;c.沙二段~沙一段;d.东营组

      Fig.  9.  Remnant formation distributive sketch of each layer in Cenozoic in the south area of Bohai Sea

      图  10  渤南地区过黄河口东洼-莱北低凸起-莱州湾凹陷及过黄河口西洼地震剖面

      a.过黄河口东洼-莱北低凸起-莱州湾凹陷NE向地震剖面;b.过黄河口西洼NE向地震剖面.剖面位置见图 1

      Fig.  10.  The seismic sections through Huanghekou western sag-Laibei low uplift-Laizhouwan sag and Huanghekou eastern sag

      图  11  渤南地区不同方向断裂断层活动速率

      a.NNE向郯庐断裂带分支断裂各时期平均断层活动速率;b.近EW向、NWW向断裂各时期平均断层活动速率

      Fig.  11.  Average fault activity rate in each period of different trending faults in the south area of Bohai Sea

      图  12  渤南地区构造演化模式

      Fig.  12.  Tectonic evolution pattern in the south area of Bohai Sea

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