渤海西部沙垒田凸起区走滑断层演化及其对油气的控制作用

doi:10.7623/syxb201202004

石油学报 ›› 2012, Vol. 33 ›› Issue (2): 204-212.DOI: 10.7623/syxb201202004

渤海西部沙垒田凸起区走滑断层演化及其对油气的控制作用

彭文绪 1,2　张志强 2　姜利群 2　石文龙 2　陈国童 2

1同济大学海洋与地球科学学院　上海　200092；2中海油渤海油田勘探开发研究院　天津　300452

收稿日期:2011-09-11 修回日期:2012-01-09 出版日期:2012-03-25 发布日期:2012-05-17
通讯作者: 彭文绪
作者简介:彭文绪，男，1972年9月生，1998年毕业于中国石油大学（北京），现为同济大学海洋与地球科学学院在读博士研究生、中海油渤海油田勘探开发研究院高级工程师，主要从事油气勘探研究。
基金资助:
国家重大科技专项“近海大中型油气田形成条件及勘探技术”（2008ZX05023）资助。

Evolution of strike-slip faults in the Shaleitian bulge of the western Bohai offshore and their control on hydrocarbons

PENG Wenxu 1,2　ZHANG Zhiqiang 2　JIANG Liqun 2　SHI Wenlong 2　CHEN Guotong 2

Received:2011-09-11 Revised:2012-01-09 Online:2012-03-25 Published:2012-05-17

摘要/Abstract

摘要：

渤海海域西部沙垒田凸起区潜山为太古界花岗岩，新近系河流相碎屑岩直接覆盖在基底潜山之上。该区发育长约20 km的NE向右旋走滑断层，斜切整个凸起。潜山内发育的NE和NW向两组走滑断层走向夹角约100°，NE向主走滑断层持续活动至今；NW向断层延续较短，局部表现为沟道，新近纪停止活动。该区走滑断层整体表现为负花状构造。新近纪构造运动在主走滑断层附近诱发大量近EW向左旋张扭性小断层并对主走滑断层形成切割。高分辨率三维地震资料精细解释表明，该区断层演化经历了三个阶段，即新近纪前基底断裂走滑阶段、新近纪早期盖层张性断裂弱雁列化阶段、新近纪晚期盖层张扭性断裂强雁列化阶段。凸起区走滑断层的多期活动不仅形成了断背斜圈闭，而且控制了走滑断层两盘古近系的沉积，对油气聚集和重新分配产生影响。

关键词: 走滑断层, 花状构造, 沙垒田凸起, 渤海湾盆地

Abstract:

Buried hills in the Shaleitian bulge of the western Bohai offshore are composed of Archaeozoic granite, which is immediately covered by Neogene fluvial clasolites. In this area there is a well-developed NE dextral strike-slip fault that stretches for about 20km and slantingly cuts through the whole Shaleitian bulge. The angle between the NE and NW strike-slip faults within the buried hills is about 100°. The major NE strike-slip fault keeps unceasingly active, while NW faults being no longer active in Neogene extend discontinuously with partial segments displayed as channels. Strike-slip faults in this area commonly show a minus flower structure and the Neogene tectonic movement induced numerous approximately-EW dextral extensional minor faults near the major strike-slip fault, which cut the major strike-slip fault occasionally. Based on detailed interpretations of high-resolution seismic data, we divided the evolution of faults in this area into three stages: the formation of base strike-slip faults in pre-Neogene, the formation of feebly-en-echelon faults in cover strata in early Neogene and the formation of tenso-shear and strongly-en-echelon faults in cover strata in late Neogene. Multiperiodic activities of strike-slip faults in the uplifted area not only formed faulted-anticline traps but also controlled Paleogene deposits on both sides of the faults, exerting an influence on the accumulation and redistribution of hydrocarbons.

Key words: strike-slip fault, flower structure, Shaleitian Bulge, Bohai Bay Basin

彭文绪　张志强　姜利群　石文龙　陈国童. 渤海西部沙垒田凸起区走滑断层演化及其对油气的控制作用[J]. 石油学报, 2012, 33(2): 204-212.

PENG Wenxu　ZHANG Zhiqiang　JIANG Liqun　SHI Wenlong　CHEN Guotong. Evolution of strike-slip faults in the Shaleitian bulge of the western Bohai offshore and their control on hydrocarbons[J]. Editorial office of ACTA PETROLEI SINICA, 2012, 33(2): 204-212.

参考文献

[1]彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30(5):654-660.

Peng Wenxu,Xin Renchen,Sun Hefeng,et al.Formation and evolution of Laizhou Bay Sag in Bohai Bay[J].Acta Petrolei Sinica, 2009,30(5):654-660.

[2]徐杰,牛嘉玉,吕悦军,等.营口—潍坊断裂带的新构造和新构造活动[J].石油学报,2009,30(4):498-505.

Xu Jie,Niu Jiayu,Lü Yuejun,et al.Neotectonics and neotectonic activities of Yingkou-Weifang fault zone[J].Acta Petrolei Sinica, 2009,30(4):498-505.

[3]万桂梅,汤良杰,周心怀,等.郯庐断裂带在渤海海域渤东地区的构造特征[J].石油学报,2009,30(3):342-346.

Wan Guimei,Tang Liangjie,Zhou Xinhuai,et al.Tectonic characteristics of the Tanlu fault zone in Bodong area of Bohai Sea[J].Acta Petrolei Sinica,2009,30(3):342-346.

[4]龚再升,蔡东升,张功成.郯庐断裂对渤海海域东部油气成藏的控制作用[J].石油学报,2007,28(4):1-10.

Gong Zaisheng,Cai Dongsheng,Zhang Gongcheng.Dominating action of Tanlu Fault on hydrocarbon accumulation in eastern Bohai Sea area[J].Acta Petrolei Sinica,2007,28(4):1-10.

[5]杨明慧.渤海湾盆地变换构造特征及其成藏意义[J].石油学报,2009,30(6):816-823.

Yang Minghui.Transfer structure and its relation to hydrocarbon exploration in Bohai Bay Basin[J].Acta Petrolei Sinica,2009,30(6): 816-823.

[6]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.

[7]陈书平,吕丁友,王应斌,等.渤海盆地新近纪—第四纪走滑作用及油气勘探意义[J].石油学报,2010,31(6):894-899.

Chen Shuping,Lü Dingyou,Wang Yingbin,et al.Neogene Quaternary strike-slip movement in Bohai Basin and its significance in petroleum exploration[J].Acta Petrolei Sinica,2010,31(6):894-899.

[8]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.

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.

[9]朱伟林,王国纯,周毅.渤海油气资源浅析[J].石油学报,2000,21(3):1-7.

Zhu Weilin,Wang Guochun,Zhou Yi.Potential of petroleum resources in the offshore of Bohai Bay Basin[J].Acta Petrolei Sinica, 2000,21(3):1-7.

[10]董月霞，汪泽成，郑红菊，等.走滑断层作用对南堡凹陷油气成藏的控制[J].石油勘探与开发,2008,35(4)：424-430.

Dong Yuexia,Wang Zecheng,Zheng Hongju,et al.Control of strike-slip faulting on reservoir formation of oil and gas in Nanpu sag[J].Petroleum Exploration and Development,2008,35(4):424-430.

[11]Sylvester A G.Strike-slip faults[J].Geological Society of America Bulletin,1988,100(11):1666-1703.

[12]Swanson M T.Late Paleozoic strike-slip faults and related vein arrays of Cape Elizabeth,Maine[J].Journal of Structural Geology,2006,28:456-473.

[13]Ghosh N,Chattopadhyay A.The initiation and linkage of surface fractures above a buried strike-slip fault:an experimental approach[J].Journal of Earth Systern.Science,2008,117(1):23-32.

[14]王义强，孙丰月，吕古贤.韧性剪切带向剪破裂的转化与成岩成矿作用[J].地质力学学报,1997,3(1):38-44.

Wang Yiqiang,Sun Fengyue,Lü Guxian.Transformation from ductile shear zones to shear fracture and related litho-metallogenesis[J].Journal of Geomechanics,1997,3(1):38-44.

[15]Naylor M A,Mandl G,Sijpesteijn C H K.Fault geometries in basement-induced wrench faulting under different initial stress states[J].Journal of Structural Geology,1986,8:737-752.

[16]Cembrano J,Gonzalez 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,2005,400:105-125.

[17]Davis G H.“Riedel relays” in deformation band shear zones,Colorado Plateau,Utah[J].Geological Society of America Abstracts with Programs,1996,28:A-188.

[18]Pachell M A ,Evans J P.Growth,linkage and termination processes of a 10-km-long strike-slip fault in jointed granite:the Gemini Fault zone Sierra Nevada,California[J].Journal of Structural Geology,2002,24:1903-1924.

[19]Flodin E A,Aydin A.Evolution of a strike-slip fault network,Valley of Fire State Park,southern Nevada[J].Geological Society of America Bulletin,2004,116:42-59.

[20]Willemse E J M,Peacock D C P,Aydin A.Nucleation and growth of strike-slip faults in limestones from Somerset,UK[J].Journal of Structural Geology,1997,19:1461-1477.

[21]Kelly P J,Sanderson D J,Peacock D C P.Linkage and evolution of conjugate strike-slip fault zones in limestones of Somerset and Northumbria[J].Journal of Structural Geology,1998,20:1477-1493.

[22]Cox S J D,Scholz C H.On the formation and growth of faults:an experimental study[J].Journal of Structural Geology,1988,10:413-430.

[23]Faulkner D R,Jacskon C L,Lunn,et al.A review of recent developments concerning the structure,mechanics and fluid flow properties of fault zones[J].Journal of Structural Geology,2010,32(11):1557-1575.

[24]Moody J D,Hill M J.Wrench-fault tectonics[J].Geological Society of America Bulletin,1956,67:1207-1246.

[25]单家增,张占文,肖乾华.辽河坳陷古近纪两期构造演化的构造物理模拟实验[J].石油勘探与开发,2004,31(3):14-17.

Shan Jiazeng,Zhang Zhanwen,Xiao Qianhua.Modeling experiments of two-phase structural evolution in the Liaohe Depression, Paleogene[J].Petroleum Exploration and Development,2004,31(3):14-17.

[26]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.

Dong 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.

[27]曹忠祥.营口—潍坊断裂带新生代走滑拉分—裂陷盆地伸展量、沉降量估算[J].地质科学,2008,43(1):65-81.

Cao Zhongxiang.Calculation of extension and subsidence of the Cenozoic pull-apart and rift basins along the Yingkou-Weifang fault zone[J].Chinese Journal of Geology,2008,43(1):65-81.

[28]Morlay C K.How successful are analogue models in addressing the influence of pre-existing fabrics on rift structure[J].Journal of Structural Geology,1999,21:1267-1274.

[29]Morley C K.Variations in late Cenozoic-recent strike-slip and oblique-extensional geometries within Indochina:the influence of pre-existing fabrics[J].Journal of Structural Geology,2004,26:1803-1829.

[30]Morlay C K,Seutthiya G K.Fault superimposition and linkage resulting from stress changes during rifting:examples from 3D seismic data,Phitsanulok basin,Tailand[J].Journal of Structural Geology,2007,29:646-663.

[31]Atmaoui N,Kukowski N,Stockhert B,et al.Initiation and development of pull-apart basins with Riedel shear mechanism:insight from scaled clay experiments[J].International Journal of Earth Sciences,2006,95(2):225-238.

[32]彭文绪,史浩,孙和风,等.郯庐走滑断层右旋走滑的地震切片证据[J].石油地球物理勘探,2009,44(6):755-759.

Peng Wenxu,Shi Hao,Sun Hefeng,et al.Dextral strike-slip evidence on seismic slice for Tanlu strike-slip fault[J].Oil Geophysical Prospecting,2009,44(6):755-759.

[33]朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003,22(3):200-207.

Zhu Guang,Liu Guosheng,Niu Manlan,et al.Transcurrent movement and genesis of the Tan-Lu fault zone[J].Geological Bulletin of China,2003,22(3):200-207.

[34]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.

[35]万天丰,朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996,2(1):14-27.

Wan Tianfeng,Zhu Hong.The maximum sinistral strike-slip and its forming age of Tancheng-Lujiang fault zone[J].Geological Journal of Universities,1996,2(1):14-27.

[36]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-324.

Xu Jiawei,Ma Guofeng.Review of ten years (1981-1991)of research on the Tancheng-Lujiang fault zone[J].Geological Review, 1992,38(4):316-324.

渤海西部沙垒田凸起区走滑断层演化及其对油气的控制作用

Evolution of strike-slip faults in the Shaleitian bulge of the western Bohai offshore and their control on hydrocarbons

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