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陈江欣, 侯方辉, 李日辉, 温珍河. 渤海海域中西部新构造运动特征[J]. 海洋地质与第四纪地质, 2018, 38(4): 83-91. doi: 10.16562/j.cnki.0256-1492.2018.04.007
引用本文: 陈江欣, 侯方辉, 李日辉, 温珍河. 渤海海域中西部新构造运动特征[J]. 海洋地质与第四纪地质, 2018, 38(4): 83-91. doi: 10.16562/j.cnki.0256-1492.2018.04.007
shu
CHEN Jiangxin, HOU Fanghui, LI Rihui, WEN Zhenhe. Neotectonics in the western and central Bohai Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(4): 83-91. doi: 10.16562/j.cnki.0256-1492.2018.04.007
Citation: CHEN Jiangxin, HOU Fanghui, LI Rihui, WEN Zhenhe. Neotectonics in the western and central Bohai Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(4): 83-91. doi: 10.16562/j.cnki.0256-1492.2018.04.007
shu

渤海海域中西部新构造运动特征

  • 1.

    自然资源部天然气水合物重点实验室青岛海洋地质研究所，青岛 266071

  • 2.

    青岛海洋科学与技术国家实验室海洋矿产资源评价与探测技术功能实验室，青岛 266071

  • 基金项目:
    中国地质调查“1:100万天津幅海洋区域地质调查项目” (1212011220113);国家自然科学基金“冷泉流体活动地貌产生机制及其活动性——以中建南盆地为例” (41606077)
详细信息
    作者简介: 陈江欣(1987—), 男, 博士, 助理研究员, 主要从事海洋地质与地球物理研究, E-mail:jiangxin_chen@sina.com

  • 中图分类号: P736.1

Neotectonics in the western and central Bohai Sea

  • 1.

    The Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China

  • 2.

    Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and TechnologyQingdao 266071, China

    摘要

  • 依据最新的高分辨率单道地震测网, 结合前人研究成果, 编制了渤海中西部海域中更新统、上更新统、全新统和中更新统以来的地层厚度图, 揭示受到喜马拉雅造山运动的影响, 区域应力场从岩石圈热沉降中的裂后弱伸展环境转变为北东东—东西向水平挤压应力场, 第四纪以前以渤中凹陷和歧口凹陷中北部为沉降中心差异沉积, 早更新世和中更新世, 张家口-蓬莱断裂带与秦皇岛-旅顺断裂带沿NW向左旋走滑, 发生显著差异沉降, 沉降中心北移, 并被秦皇岛-旅顺断裂所控制, 等厚度线整体呈NW向。共轭NE向新生庙西北-黄河口断裂带发育活动并发生右旋剪切平移, 郯庐断裂南段由于其北北东走向受到区域应力场的抑制至少在中更新世以前便失去整体活动性。晚更新世和全新世, 区域受喜马拉雅造山运动影响显著减弱, 以区域整体沉降和均衡沉降为主, 断裂活动减弱, 数量也大大减少。

    From the high resolution single-channel seismic reflection data recently acquired, the sediment thickness of the middle Pleistocene, upper Pleistocene, Holocene and the sediment thickness since middle Pleistocene to Holocene are produced.Results reveal that affected by the Himalayan orogeny, the stress field of the region has changed from a weak stretching environment of post-rift thermal subsidence to a NEE-WE horizontal compressive stress field.Sedimentation was then differentiated in two subsiding centers of the Bozhong depression and north-central Qikou depression before Quaternary.During the early and middle Pleistocene Epoch, the Zhangjiakou-Penglai fault zone and the Qinhuangdao-Lvshun fault zone were leftlateral strike-slip fault zones along the NW direction.Under the control of the Qinhuangdao-Lvshun fault, significant differentiation of subsidence occurred and the subsidence center moved to the north.Isopach map displays a preferential NW orientation.Conjugated and newly generated NE Yellow River estuary-northwest Miao fault zone was activated as a dextral strike-slip shear zone.The southern part of the Tanlu fault zone was inactive at least before middle Pleistocene, due to its NNE trending prohibited by a regional stress field.This region suffered regional isostatic subsidence during the period from late Pleistocene to Holocene, while the activity of the fault zone became weak, and the number of faults decreased significantly.

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  • 图 1  研究区位置(a)、构造概况[11] (b)及单道地震测网(c)

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  渤海中西部海域中更新统(Q2)厚度图(主要凸起和凹陷名称见图 1)

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  渤海中西部海域中更新统至全新统(Q2、Q3、Q4)厚度图(主要凸起和凹陷名称见图 1)

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  渤海中西部海域上更新统(Q3)厚度图(主要凸起和凹陷名称见图 1)

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  渤海中西部海域全新统(Q4)厚度图

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  多道地震剖面C1 (a), 其黄色虚框的放大图(b)和图b中黄色虚框多道地震剖面对应的单道地震剖面A11 (c)

    Figure 6. 

    下载: 全尺寸图片 幻灯片

    表 1  渤海中西部海域新生代地层序列与构造演化简表[6, 16, 17]

    Table 1.  Simplified stratigraphic sequence and structural evolution stages of the western and central Bohai Sea[6, 16, 17]

    下载: 导出CSV
    • 参考文献(21)
  • [1]

    龚再升, 王国纯.渤海新构造运动控制晚期油气成藏[J].石油学报, 2001, 22 (2) :1-7. http://d.old.wanfangdata.com.cn/Periodical/syxb200102001

    GONG Zaisheng, WANG Guochun.Neotectonism and late hydrocarbon accumulation in Bohai Sea[J].Acta Petrolei Sinica, 2001, 22 (2) :1-7. http://d.old.wanfangdata.com.cn/Periodical/syxb200102001

    [2]

    龚再升, 中国近海含油气盆地新构造运动与油气成藏[J].地球科学—中国地质大学学报, 2004, 29(5):513-517. http://d.old.wanfangdata.com.cn/Periodical/dqkx200405002

    GONG Zaisheng.Neotectonics and petroleum accumulation in offshore chinese basins[J].Earth Science- Journal of China University of Geosciences, 2004, 29(5):513-517. http://d.old.wanfangdata.com.cn/Periodical/dqkx200405002

    [3]

    Gong Z S, Zhang G C, Cai D S, et al.Late-stage hydrocarbon accumulation in the Bozhong depression of the Bohai Bay Basin as controlled by neotectonism[J].Acta Geologica Sinica, 2004, 78 (3) :632-639.

    [4]

    周斌, 邓志辉, 徐杰, 等.渤海新构造运动及其对晚期油气成藏的影响[J].地球物理学进展, 2009, 24 (6) :2135-2144. doi: 10.3969/j.issn.1004-2903.2009.06.028

    ZHOU Bin, DENG Zhihui, XU Jie, et al.Characteristics of neotectonism and their relationship with late hydrocarbon accumulation in the Bohai Sea[J].Progress in Geophysics, 2009, 24 (6) :2135-2144. doi: 10.3969/j.issn.1004-2903.2009.06.028

    [5]

    Gong Z S, Huang L F, Chen P H, et al.Neotectonic controls on petroleum accumulations, offshore China[J].Journal of Petroleum Geology, 2011, 34 (1) :5-27. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=1e9fcfd0a4b97feca60cde156dc5d47c

    [6]

    米立军.新构造运动与渤海海域上第三系大型油气田[J].中国海上油气:地质, 2001, 15 (1) :21-28. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200101005

    MI Lijun.The neotectonism and major neogene oil and gas fields in Bohai Sea[J].China Offshore Oil and Gas (Geology), 2001, 15 (1) :21-28. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200101005

    [7]

    徐杰, 冉勇康, 单新建, 等.渤海海域第四系发育概况[J].地震地质, 2004, 26 (1) :24-32. doi: 10.3969/j.issn.0253-4967.2004.01.003

    XU Jie, RAN Yongkang, SHAN Xinjian, et al.Development of the Quaternary system in the Bohai Sea area, China[J].Seismology and Geology, 2004, 26 (1) :24-32. doi: 10.3969/j.issn.0253-4967.2004.01.003

    [8]

    李西双, 刘保华, 赵月霞, 等.渤海海域晚更新世—全新世的活动构造[J].海洋学报, 2010, 32 (5) :52-59. http://d.old.wanfangdata.com.cn/Periodical/hyxb201005007

    LI Xishuang, LIU Baohua, ZHAO Yuexia, et al.Late Pleistocene—Holocene submarine active structures in the Bohai Sea[J].Acta Oceanologica Sinica, 2010, 32 (5) :52-59. http://d.old.wanfangdata.com.cn/Periodical/hyxb201005007

    [9]

    龚再升.中国近海新生代盆地至今仍然是油气成藏的活跃期[J].石油学报, 2005, 26 (6) :1-6. http://d.old.wanfangdata.com.cn/Periodical/syxb200506001

    GONG Zaisheng.Cenozoic China offshore basins keeping active hydrocarbon accumulation to present[J].Acta Petrolei Sinica, 2005, 26 (6) :1-6. http://d.old.wanfangdata.com.cn/Periodical/syxb200506001

    [10]

    徐杰, 周本刚, 计凤桔, 等.渤海地区新构造格局[J].石油学报, 2011, 32 (3) :442-449. http://d.old.wanfangdata.com.cn/Periodical/syxb201103010

    XU Jie, ZHOU Bengang, JI Fengju, et al.A primary study on the neotectonic pattern of the Bohai area in China[J].Acta Petrolei Sinica, 2011, 32 (3) :442-449. http://d.old.wanfangdata.com.cn/Periodical/syxb201103010

    [11]

    侯贵廷.渤海湾盆地形成机制研究[J].北京大学学报:自然科学版, 1998, 34 (4) :503-509. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800188296

    HOU Guiting.The Origin of the Bohai Bay Basin[J].Universitatis Pekinensis (Acta Scientiarum Naturalium), 1998, 34 (4) :503-509. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800188296

    [12]

    詹润, 朱光, 杨贵丽, 等.渤海海域新近纪断层成因与动力学状态[J].地学前缘, 2013, 20 (4) :151-165. http://d.old.wanfangdata.com.cn/Periodical/dxqy201304012

    ZHAN Run, ZHU Guang, Yang Guili, et al.The genesis of the faults and the geodynamic environment during Neogene for offshore of the Bohai sea[J].Earth Science Frontiers, 2013, 20 (4) :151-165. http://d.old.wanfangdata.com.cn/Periodical/dxqy201304012

    [13]

    汤良杰, 万桂梅, 周心怀, 等.渤海盆地新生代构造演化特征[J].高校地质学报, 2008, 14 (2) :191-198. doi: 10.3969/j.issn.1006-7493.2008.02.008

    TANG Liangjie, WAN Huimei, ZHOU Xinhuai, et al.Cenozoic geotectonic evolution of the Bohai Basin[J].Geological Journal of China Universities, 2008, 14 (2) :191-198. doi: 10.3969/j.issn.1006-7493.2008.02.008

    [14]

    周心怀, 余一欣, 汤良杰, 等.渤海海域新生代盆地结构与构造单元划分[J].中国海上油气, 2010, 22 (5) :285-289. doi: 10.3969/j.issn.1673-1506.2010.05.001

    ZHOU Xinhuai, YU Yixin, TANG Liangjie, et al.Cenozoic offshore basin architecture and division of structural elements in Bohai sea[J].China Offshore Oil and Gas, 2010, 22 (5) :285-289. doi: 10.3969/j.issn.1673-1506.2010.05.001

    [15]

    余一欣, 周心怀, 徐长贵, 等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质, 2011, 32 (2) :273-279. http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201102016

    YU Yixin, ZHOU Xinhuai, XU Changgui, et al.Characteristics and formation mechanisms of the Cenozoic faults in the Bohai Sea waters[J].Oil & Gas Geology, 2011, 32 (2) :273-279. http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201102016

    [16]

    朱伟林.渤海海域油气成藏与勘探[M].北京:科学出版社, 2009.

    ZHU Weilin.Hydrocarbon accumulation and exploration in Bohai Sea[M].Beijing:Science Press, 2009.

    [17]

    Yao Z, Shi X, Liu Q, et al.Paleomagnetic and astronomical dating of sediment core BH08from the Bohai Sea, China:Implications for glacial-interglacial sedimentation[J].Palaeogeography Palaeoclimatology Palaeoecology, 2014, 393 (393) :90-101.

    [18]

    中国科学院海洋研究所海洋地质研究室.渤海地质[M].北京:科学出版社, 1985.

    Department of Marine Geology, Institute of Oceanology, CAS.Geology of the Bohai Sea[M].Beijing:Science Press, 1985.

    [19]

    蔡东升, 罗毓晖, 武文来, 等.渤海浅层构造变形特征, 成因机理与渤中坳陷及其周围油气富集的关系[J].中国海上油气(地质), 2001, 15 (1) :35-43. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200101007

    CAI Dongsheng, LUO Yuhui, WU Wenlai, et al.Shallow tectonic deformation and its relationship to hydrocarbon enrichment in Bozhong Depression and adjacent areas, Bohai Bay Basin[J].China Offshore Oil and Gas (Geology), 2001, 15 (1) :35-43. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200101007

    [20]

    贾承造, 何登发, 石昕, 等.中国油气晚期成藏特征[J].中国科学:D辑, 2006, 36 (5) :412-420. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200605002

    JIA Chengzao, HE Dengfa, SHI Xin, et al.Characteristics of late hydrocarbon accumulation in China[J].Science China (series D), 2006, 36 (5) :412-420. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200605002

    [21]

    徐杰, 张进, 周本刚, 等.渤海东南部NE向黄河口—庙西北新生断裂带的存在[J].地震地质, 2007, 29 (4) :845-854. doi: 10.3969/j.issn.0253-4967.2007.04.015

    XU Jie, ZHANG Jin, ZHOU Bengang, et al.The newlygenerated NE-trending yellow river estuary-northwest miao fault zone in southeastern Bohai Basin[J].Seismology and Geology, 2007, 29 (4) :845-854. doi: 10.3969/j.issn.0253-4967.2007.04.015

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收稿日期:  2017-01-27
修回日期:  2017-07-27
刊出日期:  2018-08-28

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