高邮凹陷南断阶调节带断层构造特征分析与数值模拟

姜芹芹, 谢成龙, 朱光. 高邮凹陷南断阶调节带断层构造特征分析与数值模拟[J]. 地质科学, 2013, 48(3): 647-664. doi: 10.3969/j.issn.0563-5020.2013.03.006
引用本文: 姜芹芹, 谢成龙, 朱光. 高邮凹陷南断阶调节带断层构造特征分析与数值模拟[J]. 地质科学, 2013, 48(3): 647-664. doi: 10.3969/j.issn.0563-5020.2013.03.006
Jiang Qinqin, Xie Chenglong, Zhu Guang. Fault characteristic analysis and numerical modeling for accommodation zones in the southern fault step zone of the Gaoyou Sag[J]. Chinese Journal of Geology, 2013, 48(3): 647-664. doi: 10.3969/j.issn.0563-5020.2013.03.006
Citation: Jiang Qinqin, Xie Chenglong, Zhu Guang. Fault characteristic analysis and numerical modeling for accommodation zones in the southern fault step zone of the Gaoyou Sag[J]. Chinese Journal of Geology, 2013, 48(3): 647-664. doi: 10.3969/j.issn.0563-5020.2013.03.006

高邮凹陷南断阶调节带断层构造特征分析与数值模拟

详细信息
    作者简介:

    姜芹芹, 女, 1986年8月生, 硕士研究生, 构造地质学专业。E-mail: jiangqq122 @126.com

  • 中图分类号: P542

Fault characteristic analysis and numerical modeling for accommodation zones in the southern fault step zone of the Gaoyou Sag

  • 在高邮凹陷南断阶北界上,始新世出现的总体北北东走向、左阶雁列状真②断层带内发育了许庄与方巷调节带。各反射层构造图显示,这两个调节带内部发育了连接与非连接两大类断层。其中连接断层可分为垂向连接、斜向连接与弧形连接3类,而非连接断层可分为同向平行断层、区域斜向正断层、斜向与横向断坡拉张断层、斜向与垂向连接—扩展断层、派生斜列断层、网状断层8类。本文通过有限差分法与有限单元法数值模拟,再现了调节带内各类断层的发育过程。结果表明,调节带内的断层一方面是区域应力直接作用的产物,另一方面是边界断层斜向拉张与扩展、断坡弯曲等影响的结果。故而,调节带内断层的发育受多种因素影响,常形成复杂的断层组合。
  • 加载中
  • [1]

    陈发景.2003.调节带(或传递带)的基本概念和分类.现代地质, 17 (2): 186.

    [2]

    Chen Fajing.2003.Basic concept and classification of accommodation zone(or transfer zone).Geoscience, 17 (2): 186.

    [3]

    陈发景,汪新文,陈昭年.2011.伸展断陷中的变换构造分析.现代地质, 25 (4): 617—625.

    [4]

    Chen Fajing,Wang Xinwen and Chen Zhaonian.2011.Analysis of transform structures in extensional fault depression.Geoscience, 25 (4): 617—625.

    [5]

    戴俊生,王霞田,季宗镇等.2011.高邮凹陷南断阶东部阜宁期构造应力场及其对断层的控制作用.中国石油大学学报(自然科学版), 35 (2): 1—5.

    [6]

    Dai Junsheng,Wang Xiatian,Ji Zongzhen et al.2011.Structural stress field of Funing sedimentary period and its control on faults in the east of south fault terrace in Gaoyou Sag.Journal of China University of Petroleum(Edition of Natural Sciences), 35 (2): 1—5.

    [7]

    邓丽娟,夏连军,张列平等.2009.苏北盆地隐蔽油气藏勘探方法探讨——以高邮凹陷为例.复杂油气藏, 2 (1): 14—19.

    [8]

    Deng Lijuan,Xia Lianjun,Zhang Lieping et al.2009.The exploration methods research of subtle reservoir in north Jiangsu Basin——Taking Gaoyou depression for example.Complex Hydrocarbon Reservoirs, 2 (1): 14—19.

    [9]

    邓宗策,崔军文,冯晓枫等.1990.青藏高原构造动力及变形机制的弹性有限元分析.中国地质科学院院报, 21: 65—76.

    [10]

    Deng Zongce,Cui Junwen,Feng Xiaofeng et al.1990.The analysis of tectonic dynamics and deformation mechanics of the Qinghai-Tibet Plateau by elastic finite element method.Bulletin of the Chinese Academy of Geological Sciences, 21: 65—76.

    [11]

    丁文龙,樊太亮,黄晓波等.2011.塔里木盆地塔中地区上奥陶统古构造应力场模拟与裂缝分布预测.地质通报, 30 (4): 588—594.

    [12]

    Ding Wenlong,Fan Tailiang,Huang Xiaobo et al. 2011.Upper Ordovician paleo tectonic stress field simulating and fracture distribution forecasting in Tazhong area of Tarim Basin,Xinjiang,China.Geological Bulletin of China, 30 (4): 588—594.

    [13]

    刚文哲,王 勇,高 岗等.2011.高邮凹陷真武油田成藏期与动态成藏过程分析.沉积学报, 29 (3): 580—586.

    [14]

    Gang Wenzhe,Wang Yong,Gao Gang et al.2011.Accumulation period and dynamic accumulation process analysis of Zhenwu oil field in Gaoyou Sag.Acta Sedimentologica Sinica, 29 (3): 580—586.

    [15]

    韩 露,丁 毅,张贵宾.2003.中国岩石圈三维结构数值模拟数据库.地球物理学进展, 18 (2): 312—316.

    [16]

    Han Lu,Ding Yi and Zhang Guibin.2003.Numerical simulation database of China 3-D lithosphere structure.Progress in Geophysics, 18 (2): 312—316.

    [17]

    黄立功,钟建华,王海侨等.2004.柴西地区的构造应力场演化模拟.石油勘探与开发, 31 (6): 75—77.

    [18]

    Huang Ligong,Zhong Jianhua,Wang Haiqiao et al.2004.Evolution simulation of stress field in west Qaidam Basin,NW China.Petroleum Exploration and Development, 31 (6): 75—77.

    [19]

    蒋有录,张 乐,鲁雪松等.2005.基于ANSYS的应力场模拟在库车坳陷克拉苏地区的初步应用.天然气工业, 25 (4): 42—44.

    [20]

    Jiang Youlu,Zhang Le,Lu Xuesong et al.2005.Application of the tectonic stress simulation based on ANSYS in Kelasu region of Kuche depression.Natural Gas Industry, 25 (4): 42—44.

    [21]

    柯光明,郑荣才,石 和.2006.苏北盆地古近纪构造—层序岩相古地理特征与演化.中国地质, 33 (6): 1305—1311.

    [22]

    Ke Guangming,Zheng Rongcai and Shi He.2006.Lithofacies and paleogeography of Paleogene tectonic sequences in the Subei Basin and their evolution.Geology in China, 33 (6): 1305—1311.

    [23]

    劳海港,吴孔友,陈清华.2010.冀中坳陷调节带构造特征及演化.地质力学学报, 16 (3): 294—309.

    [24]

    Lao Haigang,Wu Kongyou and Chen Qinghua.2010.Geologic character and evolution of the accommodation zone in the Jizhong depression,Journal of Geomechanics, 16 (3): 294—309.

    [25]

    刘剑平,汪新文,周章保等.2000.伸展地区变换构造研究进展.地质科技情报, 19 (3): 27—32.

    [26]

    Liu Jianping,Wang Xinwen,Zhou Zhangbao et al.2000.Research advance in transition structure in extended region.Geological Science and Technology Information, 19 (3): 27—32.

    [27]

    李淑恩,张绍辉,岳 奎等.2001.构造应力场数值模拟分析技术及其应用.工油气地质与采收率, 8 (6): 38—42.

    [28]

    Li Shuen,Zhang Shaohui,Yue Kui et al.2001.Numerical simulation analysis technique of structural stress field and its application.Petroleum Geology and Recovery Efficiency, 8 (6): 38—42.

    [29]

    刘玉瑞,刘启东,杨小兰.2004.苏北盆地走滑断层特征与油气聚集关系.石油与天然气地质, 25 (3): 279—293.

    [30]

    Liu Yurui,Liu Qidong and Yang Xiaolan.2004.Relation between features of strike-slip faults and hydrocarbon accumulation in Subei Basin.Oil & Gas Geology, 25 (3): 279—293.

    [31]

    罗焕炎,徐煜坚,宋惠珍等.1982.青藏高原近代隆起原因及其与地震关系的有限单元分析.地震地质, 4 (1): 31—37.

    [32]

    Luo Huanyan,Xu Yujian,Song Huizhen et al.1982.Finite element analysis for recent Qinghai-Xizang Plateau uplift and its relation to seismicity.Seismology and Geology, 4 (1): 31—37.

    [33]

    马晓鸣,戴俊生.2007.高邮凹陷南部断阶带构造演化特征.新疆石油地质, 28 (4): 476—479.

    [34]

    Ma Xiaoming and Dai Junsheng.2007.Structural evolution of south terrace in Gaoyou Sag.Xinjiang Petroleum Geology, 28 (4): 476—479.

    [35]

    漆家福.2007.裂陷盆地中的构造变换带及其石油地质意义.海相油气地质, 12 (4): 43—51.

    [36]

    Qi Jiafu.2007.Structural transfer zones and significance for hydrocarbon accumulation in rifting basins.Marine Origin Petroleum Geology, 12 (4): 43—51.

    [37]

    邱旭明.2005.苏北盆地真武—吴堡断裂带的构造样式及圈闭类型.石油天然气学报(江汉石油学院学报), 27 (3): 278—280.

    [38]

    Qiu Xunming.2005.Structural style and trap type of Zhenwu-Wubao fault zone in Subei Basin.Journal of Oil and Gas Technology, 27 (3): 278—280.

    [39]

    任文忠.1990.伸展地区重要的调整构造—传递断层.煤田地质与勘探,(2): 20—26.

    [40]

    Ren Wenzhong.1990.An important adjustment structure-transform fault in extending region.Coal Geology & Exploration,(2): 20—26.

    [41]

    舒良树,王 博,王良书等.2005.苏北盆地晚白垩世—新近纪原型盆地分析.高校地质学报, 11 (4): 534—543.

    [42]

    Shu Liangshu,Wang Bo,Wang Liangshu et al.2005.Analysis of north Jiangsu prototype basin from Late Cretaceous to Neogene.Geological Journal of China Universities, 11 (4): 534—543.

    [43]

    王勖成,邵 敏.1997.有限单元法基本原理和数值方法.北京:清华大学出版社.1—568.

    [44]

    Wang Maocheng and Shao Ming.1997.Basic Principle and Numerical Method of the Finite Element Method.Beijing:Tsinghua University Press.1—568.

    [45]

    王秀娟,李元昊,侯加根.2004.对伸展域变换构造研究的两点思考.中国煤田地质, 16 (2): 4—6.

    [46]

    Wang Xujuan,Li Yuanhao and Hou Jiagen.2004.Two considerations in research of transition structures in extended region.Coal Geology of China, 16 (2): 4—6.

    [47]

    张 彤,李忠权,蒙启安等.2010.构造变换带的识别及其在乌尔逊凹陷的应用.岩性油气藏, 22 (4): 52—56.

    [48]

    Zhang Tong,Li Zhongquan,Meng Qi'an et al.2010.Identification of structural transfer zone and its applications in depression.Lithologic Reservoirs, 22 (4): 52—56.

    [49]

    张涵信,沈孟育.2003.计算流体力学:差分方法的原理和应用.北京市:国防工业出版社.1—488.

    [50]

    Zhang Hanxin and Shen Mengyu.2003.Computational Fluid Dynamics:Principle and Application of the Finite Difference Method.Beijing:National Defence Industry Press.1—488.

    [51]

    周建生,杨池银,陈发景等.1997.黄骅坳陷横向变换带的构造特征及成因.现代地质, 11 (4): 425—433.

    [52]

    Zhou Jiansheng,Yang Chiyin,Chen Fajing et al. 1997.Structural characteristics and origin of transverse transfer zone in Huanghua subbasin.Geoscience, 11 (4): 425—433.

    [53]

    周建勋,周建生.2006.渤海湾盆地新生代构造变形机制:物理模拟和讨论.中国科学(D辑), 36 (6): 507—519.

    [54]

    Zhou Jianxun and Zhou Jiansheng.2006.Mechanisms of Cenozoic deformation in the Bohai Basin,northeast China:Physical modelling and discussions.Science in China(Series D), 49 (3): 258—271.

    [55]

    朱 光,朴学峰,张 力等.2011.合肥盆地伸展方向的演变及其动力学机制.地质论评, 57 (2): 153—166.

    [56]

    Zhu Guang,Piao Xuefeng,Zhang Li et al.2011.Evolution of extensional direction in the Hefei Basin and its dynamic mechanism.Geological Review, 57 (2): 153—166.

    [57]

    朱 光,姜芹芹,朴学峰等.2013.基底断层在断陷盆地断层系统发育中的作用——以苏北盆地南部高邮凹陷为例.地质学报, 87 (4): 441—452.

    [58]

    Zhu Guang,Jiang Qinqin,Piao Xuefeng et al.2012.Role of basement faults in faulting system development in a rift basin:An example from the Gaoyou Sag in southern Subei Basin.Acta Geologica Sinica, 87 (4): 441—452.

    [59]

    Benes V and Davy P.1996.Modes of continental lithospheric extension:Experimental verification of strain localization processes. Tectonophysics, 254 (1—2): 69—87.

    [60]

    Bina C R.1997.Patterns of deep seismicity reflect buoyancy stresses due to phase transitions.Geophysical Research Letters, 24 (24): 3301—3304.

    [61]

    Bott M H P.1996.Flexure associated with planar faulting.Geophysical Journal International, 126: 21—26.

    [62]

    Faulds J E and Varga R J.1998.The role of accommondation zone and transfer zone in the regional segmentation of extended terranes.In:Faulds J E,Stewart J H(Eds.).Accommondation Zones and Tansfer Zones:The Regional Segmentation of the Basin and Range Provinces.Geology Society of America Special Paper, 323.1—45.

    [63]

    Fossen H.1997.Geometric analysis and scaling relations of deformation bands in porous sandstone.Journal of Structural Geology, 19 (12): 1479—14931.

    [64]

    Gibbs A D.1984.Structural evolution of extensional basin margins.Journal of the Geological Society, 141: 609—620.

    [65]

    Gibbs A D.1989.Structural styles in basin formation.AAPG Memoir, 46: 81—93.

    [66]

    Harry D L and Sawyer D S.1992.A dynamic model of extension in the Baltimore Canton Trough region.Tectonics, 11 (2): 420—436.

    [67]

    Morley C K,Nelson R A,Patton T L et al.1990.East African rift system and their relevance to hydrocarbon exploration in rifts.AAPG Bulletin, 74 (8): 1234—1253.

    [68]

    Rosendahl B R.1987.Architecture of continental rifts with special reference to east Africa.Annual Review of Earth and Planetary Sciences, 15: 3143.

    [69]

    Scholz C H and Gupta A.2000.Fault interactions and seismic hazard.Journal of Geodynamics, 29 (3—5): 459—467.

    [70]

    Young M J,Gawthorpe R L and Hardy S.2001.Growth and linkage of a segmented normal fault zone; the Late Jurassic Murchinson Statfjord North Fault,northern North Sea.Journal of Structural Geology, 23 (12): 933—1952.

    [71]

    Zhu G,Jiang D Z,Zhang B L et al.2012.Destruction of the eastern North China Craton in a backarc setting:Evidence from crustal deformation kinematics.Gondwana Research, 22 (1): 86—103.

  • 加载中
计量
  • 文章访问数:  3665
  • PDF下载数:  676
  • 施引文献:  0
出版历程
收稿日期:  2012-10-16
修回日期:  2013-04-10
刊出日期:  2013-07-25

目录