辽东湾坳陷新生代构造变形特征及营潍断裂带的表现

doi:10.7623/syxb2019S2007

石油学报 ›› 2019, Vol. 40 ›› Issue (S2): 79-90.DOI: 10.7623/syxb2019S2007

辽东湾坳陷新生代构造变形特征及营潍断裂带的表现

康琳¹, 吕丁友¹, 尚锁贵², 高京华¹, 张江涛¹

1. 中海石油(中国)有限公司天津分公司渤海石油研究院天津 300459;
2. 中海石油(天津)有限公司天津分公司勘探部天津 300459

收稿日期:2019-10-12 修回日期:2019-12-16 出版日期:2019-12-25 发布日期:2020-04-24
通讯作者: 康琳,男,1988年1月生,2010年获东北石油大学学士学位,2013年获东北石油大学硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院工程师,主要从事地球物理勘探及构造解析研究工作。Email:kanglin2@cnooc.com.cn
作者简介:康琳,男,1988年1月生,2010年获东北石油大学学士学位,2013年获东北石油大学硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院工程师,主要从事地球物理勘探及构造解析研究工作。Email:kanglin2@cnooc.com.cn
基金资助:
国家科技重大专项课题"近海大中型油气田形成条件与分布"（2011ZX05023-006）资助。

Characteristics of Cenozoic tectonic deformation and performance of Yingwei fault zone in Liaodongwan depression

Kang Lin¹, Lü Dingyou¹, Shang Suogui², Gao Jinghua¹, Zhang Jiangtao¹

1. Bohai Oilfield Research Institute, Tianjin Branch, CNOOC China Limited, Tianjin 300459, China;
2. Exploration department, Tianjin Branch, CNOOC China Limited, Tianjin 300459, China

Received:2019-10-12 Revised:2019-12-16 Online:2019-12-25 Published:2020-04-24

摘要/Abstract

摘要：

基于最新的连片三维地震资料和构造制图对辽东湾坳陷断裂系统的构造几何学和运动学特征展开了分析，论证了营潍断裂带在辽东湾坳陷的表现形式。研究表明：1辽东湾坳陷的断裂体系可划分为伸展断裂系统和走滑断裂系统，其中，伸展断裂系统包括NE向、NNE向主干断层及SEE向基底断裂，主要控制了古近系的构造演化及沉积充填，形成辽东湾坳陷"三凹夹两凸"的构造特征，走滑断裂系统主要包括3条NE向切割基底的走滑断层、主干伸展断层之上发育的伸展-走滑型断层以及走滑作用伴生的相关构造，断层在全区分布广泛并向下切割至新近系，使得现今辽东湾坳陷的构造格局更加复杂化；2营潍断裂带在辽东湾坳陷可分为东支断裂带和西支断裂带，共同构成了5个大尺度（凹陷级别）以及多个小尺度（主断裂级别）的走滑双重构造带，成为新生代营潍断裂带的重要构造表现形式；3营潍断裂带的活动可分为始新世的强伸展弱走滑、渐新世的弱伸展强走滑和中新世至今的弱伸展弱走滑3个演化阶段，其中，东支主断裂的伸展位移量和走滑位移量都要明显强于西支主断裂，且活动时间更早，这与辽东湾地区地壳东薄西厚的深部背景有关。

关键词: 断裂系统, 构造变形, 新生代, 营潍断裂带, 辽东湾坳陷

Abstract:

Based on the latest merging 3D seismic data and structural mapping, this paper analyzes the structural geometry and kinematics characteristics of fault system in Liaodongwan depression, and demonstrates the developing pattern of Yingwei fault zone in Liaodongwan depression. The study shows as follows. (1) The fault system of Liaodongwan depression can be divided into extensional fault system and strike-slip fault system. Among them, the extensional fault system includes NE-trending, NNE-trending main faults and SEE-trending basement faults, which mainly control the structural evolution and sedimentary filling in Paleogene, forming the tectonic characteristics of "three depressions sandwiched by two uplifts" in Liaodongwan depression. The strike-slip fault system mainly includes three NE-trending strike-slip faults cutting the basement, and the extensional strike-slip faults developed above the main extensional fault and related structures associated with strike-slip. The faults are widely distributed throughout the whole region and cut down to the Neogene, resulting in a more complicated tectonic framework in Liaodongwan depression. (2) The Yingwei fault zone in the Liaodongwan depression can be divided into the east and west branch fault zones constituting five large-scale (sag levels) and multiple small-scale (main fault levels) strike-slip duplex structural belts, which have become the important tectonic patterns in the Cenozoic Yingwei fault zone. (3) The activities of the Yingwei fault zone can be divided into three evolutionary stages: strong extension and weak strike-slip in Eocene, weak extension and strong strike-slip in Oligocene, as well as weak extension and weak strike-slip since Miocene. The extension and strike-slip displacements of the east branch of the main fault are significantly stronger than those of the western branch of the main fault, and the active time of the former is also earlier, which is related to the deep background of thin crust in the east and thick crust in the west of Liaodongwan area.

Key words: fault system, tectonic deformation, Cenozoic, Yingwei fault zone, Liaodongwan depression

中图分类号:

TE121.2

康琳, 吕丁友, 尚锁贵, 高京华, 张江涛. 辽东湾坳陷新生代构造变形特征及营潍断裂带的表现[J]. 石油学报, 2019, 40(S2): 79-90.

Kang Lin, Lü Dingyou, Shang Suogui, Gao Jinghua, Zhang Jiangtao. Characteristics of Cenozoic tectonic deformation and performance of Yingwei fault zone in Liaodongwan depression[J]. Acta Petrolei Sinica, 2019, 40(S2): 79-90.

参考文献

[1] 王应斌,黄雷.渤海海域营潍断裂带展布特征及新生代控盆模式[J].地质学报,2013,87(12):1811-1818.
WANG Yingbin,HUANG Lei.Distribution characteristic of the Ying-Wei fault zone offshore the Bohai Sea and Cenozoic basin-controlling model[J].Acta Geologica Sinica,2013,87(12):1811-1818.
[2] 漆家福,邓荣敬,周心怀,等.渤海海域新生代盆地中的郯庐断裂带构造[J].中国科学 D辑:地球科学,2008,38(S1):19-29.
QI Jiafu,DENG Rongjing,ZHOU Xinhuai,et al.Structural characteristics of the Tan-Lu fault zone in Cenozoic basins offshore the Bohai Sea[J].Science in China Series D:Earth Sciences,2008,51(2):20-31.
[3] 姜建平.营口-潍坊断裂带新生代运动学特征[J].海洋地质与第四纪地质,2008,28(4):57-64.
JIANG Jianping.Cenozoic kinematics of the Yingkou-Weifang fault zone in Eastern China[J].Marine Geology & Quaternary Geology,2008,28(4):57-64.
[4] 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.
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.
[5] 蔡少武,周东红,王德英,等.渤海湾盆地秦南凹陷构造发育特征与有利勘探方向[J].石油学报,2019,40(5):532-541.
CAI Shaowu,ZHOU Donghong,WANG Deying,et al.Tectonic development characteristics and favorable exploration direction of Qinnan sag in Bohai Bay Basin[J].Acta Petrolei Sinica,2019,40(5):532-541.
[6] 张江涛,吴奎,王冰洁,等.渤海海域辽西凸起北段新生代构造演化的磷灰石裂变径迹证据[J].石油学报,2018,39(11):1262-1271.
ZHANG Jiangtao,WU Kui,WANG Bingjie,et al.Apatite fission track evidence of Cenozoic tectonic evolution in the northern section of Liaoxi uplift,Bohai Sea[J].Acta Petrolei Sinica,2018,39(11):1262-1271.
[7] 薛永安.渤海海域油气运移"汇聚脊"模式及其对新近系油气成藏的控制[J].石油学报,2018,39(9):963-970.
XUE Yong'an.The "catchment ridge" model of hydrocarbon migration in Bohai Sea and its control on Neogene hydrocarbon accumulation[J].Acta Petrolei Sinica,2018,39(9):963-970.
[8] 金强,侯庆杰,程付启,等.成熟探区有效烃源岩的评价方法——以辽东湾地区为例[J].石油学报,2019,40(3):257-267.
JIN Qiang,HOU Qingjie,CHENG Fuqi,et al.Evaluation method of effective source rock in mature exploration area:a case study of Liaodong Bay[J].Acta Petrolei Sinica,2019,40(3):257-267.
[9] 施炜,张岳桥,董树文.郯庐断裂带中段第四纪活动及其分段特征[J].地球学报,2003,24(1):11-18.
SHI Wei,ZHANG Yueqiao,DONG Shuwen.Quaternary activity and segmentation behavior of the middle portion of the Tan-Lu fault zone[J].Acta Geoscientia Sinica,2003,24(1):11-18.
[10] 单家增,张占文,孙红军,等.营口-佟二堡断裂带成因机制的构造物理模拟实验研究[J].石油勘探与开发,2004,31(1):15-17.
SHAN Jiazeng,ZHANG Zhanwen,SUN Hongjun,et al.Modeling experiments of generation mechanism of Yingkou-Tongerbu fracture zone in the Liaohe depression[J].Petroleum Exploration and Development,2004,31(1):15-17.
[11] 徐长贵.渤海走滑转换带及其对大中型油气田形成的控制作用[J].地球科学,2016,41(9):1548-1560.
XU Changgui.Strike-slip transfer zone and its control on formation of medium and large-sized oilfields in Bohai Sea area[J].Earth Science,2016,41(9):1548-1560.
[12] 漆家福,周心怀,王谦身.渤海海域中郯庐深断裂带的结构模型及新生代运动学[J].中国地质,2010,37(5):1231-1242.
QI Jiafu,ZHOU Xinhuai,WANG Qianshen.Structural model and Cenozoic kinematics of Tan-Lu deep fracture zone in Bohai Sea area[J].Geology in China,2010,37(5):1231-1242.
[13] 曹忠祥,任凤楼,宋国奇,等.营口-潍坊断裂带对辽东湾坳陷东部凸起的形成及构造分段的控制作用——来自物理模拟实验和断层几何学特征的证据[J].地质科学,2008,43(2):238-250.
CAO Zhongxiang,REN Fenglou,SONG Guoqi,et al.Formation and segmentation of the East Rise,Liaodong Bay depression controlled by the Yingkou-Weifang fault zone:evidence from physical modeling and structural geometry[J].Chinese Journal of Geology,2008,43(2):238-250.
[14] 王应斌,黄雷,刘廷海.渤海新构造运动主要特征与构造型式[J].中国海上油气,2012,24(增刊1):6-10.
WANG Yingbin,HUANG Lei,LIU Tinghai.The main characteristics and structural styles of Bohai newtectonism[J].China Offshore Oil and Gas,2012,24(S1):6-10.
[15] 徐长贵,任健,吴智平,等.辽东湾坳陷东部地区新生代断裂体系与构造演化[J].高校地质学报,2015,21(2):215-222.
XU Changgui,REN Jian,WU Zhiping,et al.Cenozoic fault system and tectonic evolution of the eastern Liaodong Bay depression[J].Geological Journal of China Universities,2015,21(2):215-222.
[16] 漆家福,李晓光,于福生,等.辽河西部凹陷新生代构造变形及"郯庐断裂带"的表现[J].中国科学:地球科学,2013,43(8):1324-1337.
QI Jiafu,LI Xiaoguang,YU Fusheng,et al.Cenozoic structural deformation and expression of the "Tan-Lu Fault Zone" in the west sag of Liaohe depression,Bohaiwan Basin province,China[J].Science China Earth Sciences,2013,56(10):1707-1721.
[17] 孙磉礅.营潍断裂带结构特征及其与相邻盆地的关系[J].大地构造与成矿学,2008,32(4):418-426.
SUN Sangdun.The structural characteristics of the Yingwei fault zone and its relationship with the adjacent basins[J].Geotectonica et Metallogenia,2008,32(4):418-426.
[18] 高战武,徐杰,赵铁虎,等.营口-潍坊断裂带新构造和新构造活动的再认识[J].地震地质,2017,39(1):43-53.
GAO Zhanwu,XU Jie,ZHAO Tiehu,et al.Re-cognition of the neotectonics and activities of the Yingkou-Weifang fault zone[J].Seismology and Geology,2017,39(1):43-53.
[19] 周斌,邓志辉,晁洪太,等.营潍断裂带走滑构造特征、演化及动力学机制[J].西北地震学报,2008,30(2):117-123.
ZHOU Bin,DENG Zhihui,CHAO Hongtai,et al.Strike-slip tectonic characteristics,evolution and dynamic Mechanism of Yingwei fault zone[J].Northwestern Seismological Journal,2008,30(2):117-123.
[20] WOODCOCK N H,FISCHER M.Strike-slip duplexes[J].Journal of structural Geology,1986,8(7):725-735.
[21] CEMBRANO J,GONZÁLEZ G,ARANCIBIA G,et al.Fault zone development and strain partitioning in an extensional strike-slip duplex:a case study from the Mesozoic Atacama fault system,Northern Chile[J].Tectonophysics,2005,400(1/4):105-125.
[22] 万桂梅,汤良杰,金文正.辽东湾JZ27-33区块伸展型右行走滑双重构造系统[J].中国地质,2010,37(6):1584-1591.
WAN Guimei,TANG Liangjie,JIN Wenzheng.The extensional dextral strike-slip duplex of JZ27-33 Block in Liaodong Bay[J].Geology in China,2010,37(6):1584-1591.
[23] MITRA S,PAUL D.Structural geometry and evolution of releasing and restraining bends:insights from laser-scanned experimental models[J].AAPG Bulletin,2011,95(7):1147-1180.
[24] MCCLAY K,BONORA M.Analog models of restraining stepovers in strike-slip fault systems[J].AAPG Bulletin,2001,85(2):233-260.
[25] DOOLEY T P,MONASTERO F,HALL B,et al.Scaled sandbox modeling of transtensional pull-apart basins-applications to the Coso geothermal system[J].Geothermal Resources Council Transactions,2004,28:637-641.
[26] DOOLEY T P,SCHREURS G.Analogue modelling of intraplate strike-slip tectonics:a review and new experimental results[J].Tectonophysics,2012,574-575:1-71.
[27] 童亨茂,宓荣三,于天才,等.渤海湾盆地辽河西部凹陷的走滑构造作用[J].地质学报,2008,82(8):1017-1026.
TONG Hengmao,MI Rongsan,YU Tiancai,et al.The strike-slip tectonics in the western Liaohe depression,Bohai Bay Basin[J].Acta Geologica Sinica,2008,82(8):1017-1026.
[28] 侯贵廷,钱祥麟,蔡东升.渤海湾盆地中、新生代构造演化研究[J].北京大学学报:自然科学版,2001,37(6):845-851.
HOU Guiting,QIAN Xianglin,CAI Dongsheng.The tectonic evolution of Bohai Basin in Mesozoic and Cenozoic time[J].Acta Scientiarum Naturalium:Universitatis Pekinensis,2001,37(6):845-851.
[29] ALLEN M B,MACDONALD D I M,XUN Zhao,et al.Early Cenozoic two-phase extension and Late Cenozoic thermal subsidence and inversion of the Bohai Basin,Northern China[J].Marine and Petroleum Geology,1997,14(7/8):951-972.
[30] HSIAO L Y,GRAHAM S A,TILANDER N.Seismic reflection imaging of a major strike-slip fault zone in a rift system:paleogene structure and evolution of the Tan-Lu fault system,Liaodong Bay,Bohai,offshore China[J].AAPG Bulletin,2004,88(1):71-97.
[31] 邱楠生,左银辉,常健,等.中国东西部典型盆地中-新生代热体制对比[J].地学前缘,2015,22(1):157-168.
QIU Nansheng,ZUO Yinhui,CHANG Jian,et al.Characteristics of Meso-Cenozoic thermal regimes in typical eastern and western sedimentary basins of China[J].Earth Science Frontiers,2015,22(1):157-168.
[32] ISOZAKI Y,AOKI K,NAKAMA T,et al.New insight into a subduction-related orogen:a reappraisal of the geotectonic framework and evolution of the Japanese islands[J].Gondwana Research,2010,18(1):82-105.
[33] 万桂梅,汤良杰,周心怀,等.渤海海域新近纪-第四纪断裂特征及形成机制[J].石油学报,2010,31(4):591-595.
WAN Guimei,TANG Liangjie,ZHOU Xinhuai,et al.Neogene-Quaternary fault characteristics and its formation mechanism in Bohai Sea[J].Acta Petrolei Sinica,2010,31(4):591-595.
[34] 漆家福.渤海湾新生代盆地的两种构造系统及其成因解释[J].中国地质,2004,31(1):15-22.
QI Jiafu.Two tectonic systems in the Cenozoic Bohai Bay Basin and their genetic interpretation[J].Geology in China, 2004,31(1):15-22.
[35] 肖庆辉,刘勇,冯艳芳,等.中国东部中生代岩石圈演化与太平洋板块俯冲消减关系的讨论[J].中国地质,2010,37(4):1092-1101.
XIAO Qinghui,LIU Yong,FENG Yanfang,et al.A preliminary study of the relationship between Mesozoic lithosphere evolution in eastern China and the subduction of the Pacific plate[J].Geology in China,2010,37(4):1092-1101.
[36] 赵利,李理.渤海湾盆地晚中生代以来伸展模式及动力学机制[J].中国地质,2016,43(2):470-485.
ZHAO Li,LI Li.The extensional pattern and dynamics of Bohai Bay Basin in Late Mesozoic-Cenozoic[J].Geology in China,2016,43(2):470-485.
[37] MARUYAMA S,ISOZAKI Y,KIMURA G,et al.Paleogeographic maps of the Japanese islands:plate tectonic synthesis from 750 Ma to the present[J].Island Arc,1997,6(1):121-142.
[38] SETON M,MVLLER R D.Reconstructing the junction between Panthalassa and Tethys since the Early Cretaceous[C]//PESA Eastern Australasian Basins Symposium III.Sydney:PESA,2008:263-266.
[39] THORKELSON D J.Subduction of diverging plates and the principles of slab window formation[J].Tectonophysics,1996,255(1/2):47-63.

辽东湾坳陷新生代构造变形特征及营潍断裂带的表现

Characteristics of Cenozoic tectonic deformation and performance of Yingwei fault zone in Liaodongwan depression

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	韩剑发, 苏洲, 刘永福, 张超, 陈军, 张慧芳, 吉云刚, 黄腊梅. 塔里木盆地牙哈断块潜山带控储控藏机理与油气勘探潜力[J]. 石油学报, 2018, 39(10): 1081-1091.
[2]	陈红汉, 米立军, 刘妍鷨, 韩晋阳, 孔令涛. 珠江口盆地深水区CO₂成因、分布规律与风险带预测[J]. 石油学报, 2017, 38(2): 119-134.
[3]	陈东旭, 章凤奇, 陈汉林, 杨树锋, 曹婷, 蒙启安. 新生代辉绿岩岩体识别及油气地质意义——以中国东北地区方正断陷为例[J]. 石油学报, 2016, 37(6): 757-767.
[4]	徐长贵, 王冰洁, 王飞龙, 宛良伟, 张如才. 辽东湾坳陷新近系特稠油成藏模式与成藏过程——以旅大5-2北油田为例[J]. 石油学报, 2016, 37(5): 599-609.
[5]	王一博, 张功成, 赵志刚, 谢晓军, 刘世翔, 管红, 董伟, 宋双. 南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例[J]. 石油学报, 2016, 37(4): 474-482.
[6]	白冰, 王清斌, 赵国祥, 刘晓健. 蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据[J]. 石油学报, 2015, 36(9): 1098-1107.
[7]	岳军培, 张艳, 沈怀磊, 尤龙, 鲁宝亮, 王璞珺. 华南陆缘地质特征对南海北部盆地基底的约束[J]. 石油学报, 2013, 34(增刊二): 120-128.
[8]	唐　永　梅廉夫　肖安成　陈友智　罗开平 . 川东北宣汉-达县地区晚中生代-新生代构造应力场转化及其油气意义[J]. 石油学报, 2013, 34(1): 59-70.
[9]	程晓敢雷刚林陈汉林杜治利廖林罗俊成师骏. 西昆仑山前甫沙—克里阳地区新生代变形特征及油气控制作用[J]. 石油学报, 2011, 32(1): 83-89.
[10]	祁鹏任建业史双双卢刚臣. 歧口凹陷沿岸带新生代构造特征及其形成机制[J]. 石油学报, 2010, 31(6): 900-905.
[11]	崔敏汤良杰. 黔南碳酸盐岩地区断层周缘构造变形及封闭性[J]. 石油学报, 2010, 31(5): 781-786.
[12]	朱伟林. 南海北部深水区油气地质特征[J]. 石油学报, 2010, 31(4): 521-527.
[13]	张功成. 南海北部陆坡深水区构造演化及其特征[J]. 石油学报, 2010, 31(4): 528-533.
[14]	苏劲张水昌杨海军朱光有陈建平张斌. 断裂系统对碳酸盐岩有效储层的控制及其成藏规律[J]. 石油学报, 2010, 31(2): 196-203.
[15]	能源, 漆家福, 张春峰, 杨立干, 张克鑫. 金湖凹陷石港断层构造演化及油气聚集特征[J]. 石油学报, 2009, 30(5): 667-671,677.