[1]陈兴鹏,李 伟,吴智平.2019.“伸展-走滑”复合作用下构造变形的物理模拟.大地构造与成矿学,43(6):1106-1116.doi:10.16539/j.ddgzyckx.2019.06.003
 CHEN Xingpeng,LI Wei,WU Zhiping.2019.Structural Characteristics of Combined Extension and Strike-slip: Insights from Analogue Modeling.Geotectonica et Metallogenia,43(6):1106-1116.doi:10.16539/j.ddgzyckx.2019.06.003
点击复制

“伸展-走滑”复合作用下构造变形的物理模拟
分享到:

《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2019年43卷06期
页码:
1106-1116
栏目:
构造地质学
出版日期:
2019-12-15

文章信息/Info

Title:
Structural Characteristics of Combined Extension and Strike-slip: Insights from Analogue Modeling
文章编号:
1001-1552(2019)06-1106-011
作者:
陈兴鹏12 李 伟12 吴智平12* 徐长贵3 任 健3
1.中国石油大学(华东) 地球科学与技术学院, 山东 青岛 266580; 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, 山东 青岛 266071; 3.中海石油(中国)有限公司 天津分公司, 天津 300452
Author(s):
CHEN Xingpeng12 LI Wei12 WU Zhiping12* XU Changgui3 and REN Jian3
1. School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China; 2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, Shandong, China; 3. Tianjin Technical Department, CNOOC, Tianjin 300452, China
关键词:
构造变形 伸展-走滑复合作用 构造物理模拟 渤海湾盆地
Keywords:
structural deformation extension and strike-slip combined action analogue modeling Bohai Bay Basin
分类号:
P67
DOI:
10.16539/j.ddgzyckx.2019.06.003
文献标志码:
A
摘要:
新生代渤海湾盆地为典型的“伸展-走滑”复合盆地, NNW-SSE向伸展作用和NE-SW向走滑作用的复合效应导致盆地内部构造样式的复杂性和多样性。本文针对走滑作用方向与伸展作用方向垂直的情况, 就不同“伸展-走滑”复合条件下的断裂发育特征与演化过程开展了3类13组构造物理模拟实验, 结果表明: ①在先伸展后走滑的条件下, 早期发育的伸展断层被晚期走滑断层强烈切割、改造, 平面上表现为雁列式组合或主走滑断层, 剖面上发育花状构造; ②先走滑后伸展的条件下, 平面上表现为早期雁列式的R剪切复活, 作为晚期伸展正断层的转换断层, 剖面上表现为似花状构造; ③伸展和走滑同时作用的情况下, 伸展与走滑作用的强弱配比关系影响断裂的发育特征, 可建立“走滑强于伸展”、“走滑伸展强度相近”和“伸展强于走滑”三类模式。实验结果在辽东湾坳陷得到了印证, 可为渤海湾盆地及类似伸展-走滑复合盆地的构造解析及动力成因机制分析提供指导和借鉴。
Abstract:
The Bohai Bay Basin is a typical Cenozoic basin characterized by combined extension and strike-slip. The combined effect of the NNW-SSE extension and NE-SW strike-slip leads to the complexity and diversity of structural styles in the basin. We proposed three geology models and carried out analogue experiments on combined extension and strike-slip to delineate the characteristics and processes of fault development. The strike-slip direction is vertical to that of extension in the modeling. The results show that: (1) extension after strike-slip, the extensional faults developed in the early stage were strongly cut and transformed by late strike-slip faults, which were manifested as echelon combination or main strike-slip faults on the plane, and flower structures were developed on the section; (2) strike-slip after extension, the plane showed an early stage echelon R shear reactivation, which was the conversion fault of the late extensional normal fault, and the section showed flower-like structure; (3) for synchronous extension and strike-slip, the structural deformation can be classified into 3 types based on the proportion of extension and strike-slip. (a) “Strike-slip surpass extension” pattern is characterized by the mutual cut between “R faults”, “P shear faults” and extensional faults and main strike-slip faults developed in the plane, and negative flower structure in vertical; (b) “Extension and strike-slip equal” pattern is the fault combinations where en-echelon faults was cut by extensional faults in the plane, which couldn’t form main extensional-faults. Vertically, it was composed of a series of normal faults with flower liking structure; (c) “Extension surpass strike-slip” pattern is brush or comb structures in the plane and horsetail or multiple Y shape fault complex. The experimental results are consistent with the structures observed in the Liaodong Bay Depression, which can provide guidance and reference for the structural and genetic mechanism analysis of the Bohai Bay Basin and other basins characterized by combined extension and strike-slip.

参考文献/References:

邓宾, 杨刚, 赖冬, 何宇, 周政, 罗强, 王兴建, 刘树根. 2018. 弧形走滑砂箱构造物理模型及其大地构造意义. 成都理工大学学报(自然科学版), 45(1): 99-108.
侯贵廷, 钱祥麟, 蔡东升. 2001. 渤海湾盆地中、新生代构造演化研究. 北京大学学报(自然科学版), 37(6): 845- 851.
侯贵廷, 钱祥麟, 宋新民. 1998. 渤海湾盆地形成机制研究. 北京大学学报(自然科学版), 34(4): 503-509.
李理, 赵利, 刘海剑, 房贤云. 2015. 渤海湾盆地晚中生代-新生代伸展和走滑构造及深部背景. 地质科学, 50(2): 446-472.
李三忠, 索艳慧, 戴黎明, 刘丽萍, 金宠, 刘鑫, 郝天珧, 周立宏, 刘保华, 周均太, 焦倩. 2010. 渤海湾盆地形成与华北克拉通破坏. 地学前缘, 17(4): 64-89.
李伟, 陈兴鹏, 吴智平, 张婧, 任健, 刘超, 李春锐. 2016. 渤海海域辽中南洼压扭构造带成因演化及其控藏作用. 高校地质学报, 22(3): 502-511.
李伟, 平明明, 周东红, 吴奎, 张婧, 房璐, 陈兴鹏. 2018. 辽东湾坳陷新生代主干断裂走滑量的估算及其地质意义. 大地构造与成矿学, 42(3): 445-454.
吕丁友, 李伟, 郭睿朋, 吴奎, 张江涛. 2018. 辽东湾坳陷辽中南洼构造发育演化特征与成因机制. 海洋地质前沿, 34(4): 25-32.
漆家福, 邓荣敬, 周心怀, 张克鑫. 2008. 海海域新生代盆地中的郯庐断裂带构造. 中国科学: 地球科学, 38(S1): 19-29.
漆家福, 李晓光, 于福生, 于天才. 2013. 辽河西部凹陷新生代构造变形及“郯庐断裂带”的表现. 中国科学: 地球科学, 43(8): 1324-1337.
任健, 官大勇, 陈兴鹏, 刘朋波. 2017. 走滑断裂叠置拉张区构造变形的物理模拟及启示. 大地构造与成矿学, 41(3): 455-465.
单家增, 张占文, 肖乾华. 2004. 辽河坳陷古近纪两期构造演化的构造物理模拟实验. 石油勘探与开发, 31(3): 14-17.
于福生, 董月霞, 童亨茂, 熊连桥, 龙娴. 2015. 渤海湾盆地辽河西部凹陷古近纪变形特征及成因. 石油与天然气地质, 36(1): 51-60.
于俊峰, 夏斌, 许静. 2006. 对渤海湾盆地张扭、压扭性构造的一点认识. 天然气地球科学, 17(4): 473-476.
张晓庆, 吴智平, 周心怀, 牛成民, 李伟, 任健, 张婧. 2017. 渤海南部新生代构造发育与演化特征. 大地构造与成矿学, 41(1): 50-60.
Allen M B, Macdonald D I M and Xun Z, Vincent S J and Brouet-Menzies C. 1998. Transtensional deformation in the evolution of the Bohai Basin, northern China. Geological Society, London, Special Publications, 135(1): 215-229.
Basile C and Brun J P. 1999. Transtensional faulting patterns ranging from pull-apart basins to transform continental margins: An experimental investigation. Journal of Structural Geology, 21(1): 23-37.
Cerca M, Ferrari L, Corti G, Bonini M and Manetti P. 2010. Analogue model of inversion tectonics explaining the structural diversity of Late Cretaceous shortening in southwestern Mexico. Lithosphere, 2(3): 172-187.
Dooley T. 1994. Geometries and kinematics of strike-slip fault systems: Insights from physical modeling and ?eld studies. Royal Holloway: University of London Doctoral Dissertation.
Dooley T P and Schreurs G. 2012. Analogue modelling of intraplate strike-slip tectonics: A review and new experimental results. Tectonophysics, 574-575(11): 1-71.
Eisenstadt G and Sims D. 2005. Evaluating sand and clay models: Do rheological differences matter? Journal of Structural Geology, 27(8): 1399-1412.
Fossen H, Tikoff B and Teyssier C. 1994. Strain modeling of transpressional and transtensional deformation. Norsk Geologisk Tidsskrift, 74(3): 134-145.
Higgs W G and McClay K R. 1993. Analogue sandbox modelling of Miocene extensional faulting in the outer moray firth. Geological Society of London Special Publications, 71(1): 141-162.
Jagger L J and McClay K R. 2018. Analogue modelling of inverted domino-style basement fault systems. Basin Research, 30(suppl.1): 363-381.
Mansfield C and Cartwright J. 2001. Fault growth by linkage: Observations and implications from analogue models. Journal of Structural Geology, 23(5): 745-763.
Marques F O and Nogueira C R. 2008. Normal fault inversion by orthogonal compression: Sandbox experiments with weak faults. Journal of Structural Geology, 30(6): 761-766.
McClay K R. 1990. Extensional fault systems in sedimentary basins: A review of analogue model studies. Marine and Petroleum Geology, 7(3): 206-233.
McClay K and Dooley T. 1995. Analogue models of pull-apart basins. Geology, 23(8): 711-714.
McClay K, Dooley T, Whitehouse P, Whitehouse P and Anadon-Ruiz S. 2005. 4D analogue models of extensional fault systems in asymmetric rifts: 3D visualisations and comparisons with natural examples // Petroleum Geology Conference, Geological Society of London: 1543-1556.
Pinto L, Mu?oz C, Nalpas T and Charrier R. 2010. Role of Sedimentation during basin inversion in analogue modelling. Journal of Structural Geology, 32(4): 554- 565.
Richard P and Krantz R W. 1991. Experiments on fault reactivation in strike-slip mode. Tectonophysics, 188(1-2): 117-131.
Richard P D, Naylor M A and Koopman A. 1995. Experimental models of strike-slip tectonics. Petroleum Geoscience, 1(1): 71-80.
Sims D, Ferrill D A and Stamatakos J A. 1999. Role of a ductile décollement in the development of pull-apart basins: Experimental results and natural examples. Journal of Structural Geology, 21: 533-554.
Tentler T and Temperley S. 2003. Segment linkage during evolution of intracontinental rift systems: Insights from analogue modelling. Geological Society, London, Special Publications, 212(1): 181-196.
Ventisette C D, Montanari D, Bonini M and Sani F. 2005. Positive fault inversion triggering ‘Intrusive Diapirism’: An analogue modelling perspective. Terra Nova, 17(5): 478-485.
Viola G, Odonne F and Mancktelow N S. 2004. Analogue modelling of reverse fault reactivation in strike-slip and transpressive regimes: Application to the Giudicarie fault system, Italian Eastern Alps. Journal of Structural Geology, 26(3): 401-418.
Wu J E, McClay K, Whitehouse P, and Dooley T. 2009. 4D analogue modelling of transtensional pull-apart basins. Marine and Petroleum Geology, 26(8): 1608-1623.
Yamada Y and McClay K. 2003. Application of geometric models to inverted listric fault systems in sandbox experiments. Paper 2: Insights for possible along strike migration of material during 3d hanging wall deformation. Journal of Structural Geology, 25(8): 1331-1336.

相似文献/References:

[1]鲁如魁,钟华明,童劲松.西藏洛扎地区拆离断层构造变形特征.大地构造与成矿学,2005.29(2):189.
 LU Rukui,ZHONG Huaming,TONG Jingsong.TECTONIC DEFORMATION FEATURES OF THE DETACHMENT FAULT IN LUOZHA AREA, TIBET.Geotectonica et Metallogenia,2005.43(6):189.
[2]张拴宏,周显强.青海省哇洪山断裂带中段构造变形特征及X光岩组分析.大地构造与成矿学,2003.27(1):029.
 ZHANG Shuan hong and ZHOU Xian qiang.CHARACTERISTICS OF DEFORMATION AND X-RAY PETROFABRIC IN MIDDLE WAHONGSHAN FAULT ZONE, QINGHAI PROVINCE.Geotectonica et Metallogenia,2003.43(6):029.
[3]宋春彦,王剑,付修根.羌塘盆地波尔藏陇巴背斜构造特征及其油气地质意义.大地构造与成矿学,2012.36(1):008.
 SONG Chunyan,WANG Jian,FU Xiugen.Structural Characteristics and its Petroleum Geological Significance of the Boerzanglongba Anticline in the Qiangtang Basin, Northern Tibetan Plateau, China.Geotectonica et Metallogenia,2012.43(6):008.
[4]姚运生,罗登贵,刘锁旺.江汉洞庭盆地及邻区晚中生—新生代以来的构造变形.大地构造与成矿学,2000.24(2):140.
 Yao Yun-sheng,Luo Deng-gui,Liu Suo-wang.TECTONIC DEFORMATION OF THE JIANGHAN-DONGTINGBASIN AND ITS SURROUNDING AREAS FROMLATE MESOZOIC TO CENOZOIC.Geotectonica et Metallogenia,2000.43(6):140.
[5]杨明慧,刘池阳,杨斌谊.冀中坳陷中生代构造变形的转换及油气.大地构造与成矿学,2001.25(2):113.
 YANG Minghui,LIU Chiyang,YANG Binyi.TECTONIC TRANSFORM OF THE MESOZOIC AND THEIR RELATIONS TO HYDROCARBON TRAPS IN THE JIZHONG(CENTRAL HEBEI PROVINCE) BASIN,CHINA.Geotectonica et Metallogenia,2001.43(6):113.
[6]赵志忠.阿尔泰山南缘东部岩石构造变形与金的构造成矿机理.大地构造与成矿学,2001.25(3):302.
 ZHAO Zhizhong.TECTONIC DEFORMATION AND THE TECTONIC- METALLOGENIC MECHANISM OF GOLD DEPOSITES IN THE EAST OF SOUTHERN MARGIN OF ALTAI MOUNTAIN.Geotectonica et Metallogenia,2001.43(6):302.
[7]王令占,田洋,涂兵.鄂西利川齐岳山高陡背斜带的古应力分析.大地构造与成矿学,2012.36(4):490.
 WANG Lingzhan,TIAN Yang,TU Bing.Paleostress Analysis of the Qiyue Shan Highangle Anticline in the Lichuan Area, Western Hubei Province, China.Geotectonica et Metallogenia,2012.43(6):490.
[8]冯娟萍,欧阳征健.平衡地质剖面技术在鄂尔多斯盆地西缘中南段中的应用.大地构造与成矿学,2013.37(3):393.
 FENG Juanping,OUYANG Zhengjian,and HUANG Zhengliang.The Application of Balance Geological Section Technology in the Mid-South Section of the Western Margin of the Ordors Basin.Geotectonica et Metallogenia,2013.43(6):393.
[9]胡国成,吴传军,许德如.海南抱伦矿区构造变形、成矿时代与金矿化关系研究.大地构造与成矿学,2016.4(2):367.doi:10.16539/j.ddgzyckx.2016.02.014
 HU Guocheng,WU Chuanjun,XU Deru.Structural Deformation, Age of Ore-formation and Origin of Baolun Gold Deposit in Hainan Island, South China.Geotectonica et Metallogenia,2016.43(6):367.doi:10.16539/j.ddgzyckx.2016.02.014
[10]刘 峰,周 峰,刘 强.藏南仲巴地体中段构造变形特征及构造演化分析.大地构造与成矿学,2018.优先出版:001.doi:10.16539/j.ddgzyckx.2019.03.015
 LIU Feng,ZHOU Feng,LIU Qiang and XIANG Shuyuan.Structural Characteristics in the Middle of the Zhongba Terrane, Southern Tibet and its Tectonic Evolution.Geotectonica et Metallogenia,2018.43(6):001.doi:10.16539/j.ddgzyckx.2019.03.015

备注/Memo

备注/Memo:
收稿日期: 2018-03-21; 改回日期: 2019-03-28 项目资助: 国家油气重大专项课题(2016ZX05006-007)资助。 第一作者简介: 陈兴鹏(1990–), 男, 博士研究生, 构造地质学专业。Email: cxp_upc2010@163.com 通信作者: 吴智平(1967–), 男, 教授, 博士生导师, 从事含油气盆地构造解析。Email: wuzp@upc.edu.cn
更新日期/Last Update: 2019-12-15