南阳凹陷边界断层三维几何学及运动学特征

doi:10.11885/j.issn.1674-5086.2019.07.18.01

西南石油大学学报(自然科学版) ›› 2020, Vol. 42 ›› Issue (5): 48-62.DOI: 10.11885/j.issn.1674-5086.2019.07.18.01

南阳凹陷边界断层三维几何学及运动学特征

李智^1,2, 张志业^1,2, 何登发¹, 罗曦², 熊健²

1. 中国地质大学(北京)能源学院, 北京海淀 100083;
2. 中国石化河南油田分公司, 河南南阳 473400

收稿日期:2019-07-18 出版日期:2020-10-10 发布日期:2020-10-10
通讯作者: 何登发,E-mail:hedengfa282@163.net
作者简介:李智,1989年生,男,汉族,河南镇平人,工程师,硕士,主要从事盆地构造解析和石油地质综合研究工作。E-mail:lizhicug@163.com;张志业,1991年生,女,汉族,河南禹州人,工程师,硕士,主要从事地震资料解释和构造地质研究工作。E-mail:zhangzhy169@163.com;何登发,1967年生,男,汉族,四川阆中人,教授,博士,主要从事构造地质学、石油地质学研究工作。E-mail:hedengfa282@163.net;罗曦,1984年生,女,汉族,四川射洪人,高级工程师,硕士,主要从事油气勘探研究工作。E-mail:360355631@qq.com;熊健,1986年生,男,汉族,湖北十堰人,助理研究员,主要从事石油物探地震地质综合解释工作。E-mail:panda_866@163.com
基金资助:
国家科技重大专项（2017ZX05001-001）；国家重点研发计划项目（2017YFC0601405-03）

3D Geometrical and Kinematic Characteristics of the Boundary Fault in Nanyang Depression

LI Zhi^1,2, ZHANG Zhiye^1,2, HE Dengfa¹, LUO Xi², XIONG Jian²

1. School of Energy Resources, China University of Geosciences(Beijing), Haidian, Beijing 100083, China;
2. Henan Oilfield Company, SINOPEC, Nanyang, Henan 473400, China

Received:2019-07-18 Online:2020-10-10 Published:2020-10-10

摘要/Abstract

摘要： 新野断层位于南襄盆地南阳凹陷南部的控凹边界断裂，研究其三维几何学和运动学特征对分析南阳凹陷的形成演化至关重要。以2/3D地震、钻井及测井资料为基础，以正断层相关褶皱理论和构造复原理论为指导，深入剖析新野断层的三维几何学和运动学特征及其对凹陷形成的控制作用。根据断层平面走向，结合倾角和断距变化，将新野断层分为西、中、东3段；空间上认为，新野断层是由多个等倾角面构成的复杂曲面，通过两个垂向轴面和4个横向轴面，将新野断层断面分为11个等倾角区。根据平衡地质剖面复原结果对比，认为新野断层西段、东段形成于晚白垩世，中段形成于始新世大仓房期并逐渐与西段、东段硬连接形成一条断层；断层及其上盘地层旋转程度自西向东逐渐增强；断层反转强度自西向东亦逐渐变大。新野断层西段为"座椅式"正断层，中段由"转折式"正断层转"犁式"正断层，东段为"犁式"正断层。沿断层走向的差异沉降和断面形态差异是南阳凹陷构造特征及形成演化的重要控制因素。

关键词: 南阳凹陷, 新野断层, 几何学特征, 运动学特征, 正断层相关褶皱理论, 构造复原

Abstract: Xinye Fault is a boundary fault in the south of Nanyang Depression, Nanxiang Basin. It is very important to study its 3D geometrical and kinematic characteristics in analyzing the formation and evolution of Nanyang Depression. Based on 2/3D seismic, drilling and logging data, guided by normal fault related fold theory and structural restoration theory, the 3D geometrical and kinematic characteristics of Xinye Fault are analyzed in this paper. According to plane strike, combined with dip angle and fault distance changes, Xinye Fault is divided into three segments, i.e. west, central and east. The fault plane, which could be subdivided into 11 subzones by 2 vertical axial planes and 4 transversal axial planes, is a curved surface consisting of several dip domains. Based on the balanced geologic cross-sections, we established that the west and east segments of this fault developed in the late Cretaceous; the central segment formed in the sedimentary period of Dacangfang Formation in the Eocene, then the three segments linked into one fault. The rotation degree of the fault weakens from east to west. The largest reverse degree appears on the east segment, followed by the central segment and the west segment. The seat-type normal fault form developed in the west segment; the central segment is a turning normal fault instead of listric form and listric in the east segment. The differential subsidence along fault strike and the difference of section shape are important controlling factors for the formation and evolution of Nanyang Depression.

Key words: Nanyang Depression, Xinye Fault, geometrical characteristic, kinematic characteristic, normal fault related fold theory, structural restoration

中图分类号:

TE122

李智, 张志业, 何登发, 罗曦, 熊健. 南阳凹陷边界断层三维几何学及运动学特征[J]. 西南石油大学学报(自然科学版), 2020, 42(5): 48-62.

LI Zhi, ZHANG Zhiye, HE Dengfa, LUO Xi, XIONG Jian. 3D Geometrical and Kinematic Characteristics of the Boundary Fault in Nanyang Depression[J]. 西南石油大学学报(自然科学版), 2020, 42(5): 48-62.

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参考文献

[1] SUPPE J. Principles of structural geology[M]. Englewood Cliffs, N J:Prentice-Hall, Inc., 1985:341-367.
[2] SHAW J H, HOOK S C, SUPPE J. Structural trend analysis by axial surface mapping[J]. AAPG Bulletin, 1994, 78(5):700-721. doi:10.1306/a25fe38d-171b-11d7-8645000102c1865d
[3] SHAW J H, HOOK S C, SUPPE J. Structural trend analysis by axial surface mapping:Reply[J]. AAPG Bulletin, 1996, 80(5):780-787.
[4] 漆家福,杨桥,童亨茂,等. 构造因素对半地堑盆地的层序充填的影响[J]. 地球科学——中国地质大学学报, 1997, 22(6):603-608. QI Jiafu, YANG Qiao, TONG Hengmao, et al. Sequence construction response to tectonic process in extensional half-garben basin[J]. Earth Science-Journal of China University of Geosciences, 1997, 22(6):603-608.
[5] 张岳桥,赵越,董树文,等. 中国东部及邻区早白垩世裂陷盆地构造演化阶段[J]. 地学前缘, 2004, 11(3):123-133. doi:10.3321/j.issn:1005-2321.2004.03.014 ZHANG Yueqiao, ZHAO Yue, DONG Shuwen, et al. Tectonic evolution stages of the early Cretaceous rift basins in eastern china and adjacent areas and their geodynamic background[J]. Earth Science Frontiers, 2004, 11(3):123-133. doi:10.3321/j.issn:1005-2321.2004.03.014
[6] 何登发, SUPPE J,贾承造. 断层相关褶皱理论与应用研究新进展[J]. 地学前缘, 2005, 12(4):353-364. doi:10.3321/j.issn:1005-2321.2005.04.004 HE Dengfa, SUPPE J, JIA Chengzao. New advances in theory and application of fault-related folding[J]. Earth Science Frontiers, 2005, 12(4):353-364. doi:10.3321/j.issn:1005-2321.2005.04.004
[7] 郭卫星,漆家福. 同沉积褶皱生长地层中沉积与构造关系[J]. 现代地质,2008,22(4):520-524. doi:10.3969/j.issn.1000-8527.2008.04.005 GUO Weixing, QI Jiafu. Relationship of sedimentation and tectonism in growth strata developed by growth folding[J]. Geoscience, 2008, 22(4):520-524. doi:10.3969/j.issn.1000-8527.2008.04.005
[8] 陈玮常,闫晶晶,孙冠宇,等. 南堡凹陷老爷庙地区断裂构造与油气成藏[J]. 西南石油大学学报(自然科学版), 2018, 40(2):46-56. doi:10.11885/j.issn.1674-5086.2016.11.04.02 CHEN Weichang, YAN Jingjing, SUN Guanyu, et al. Fault tectonics and petroleum entrapment in the Laoyemiao Region of the Nanpu Depression[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2018, 40(2):46-56. doi:10.11885/j.issn.1674-5086.2016.11.04.02
[9] RICH J L. Mechanics of low-angle overthrust faulting as illustrated by Cumberland Thrust Block, Virginia, Kentucky and Tennessee[J]. AAPG Bulletin, 1934, 18(12):1584-1596.
[10] SUPPE J. Geometry and kinematics of fault-bend folding[J]. American Journal of Science, 1983, 283:684-721. doi:10.1016/0013-7952(89)90033-1
[11] IMBER J, TUCKWELL G W, CHILDS C, et al. Three-dimensional distinct element modelling of relay growth and breaching along normal faults[J]. Journal of Structural Geology, 2004, 26(10):1897-1911. doi:10.1016/j.jsg.2004.02.010
[12] SOLIVA R, BENEDICTO A. A linkage criterion for segmented normal faults[J]. Journal of Structural Geology, 2004, 26, 2251-2267. doi:10.1016/j.jsg.2004.06.008
[13] DULA W F. Geometric models of listric normal faults and rollover folds[J]. AAPG Bulletin, 1991, 75(10):1609-1625. doi:10.1016/0148-9062(92)93666-8
[14] XIAO Hongbing, SUPPE J. Origin of rollover[J]. AAPG Bulletin, 1992, 76:509-529.
[15] RENATO M, DARROS de M. Geometry of the hanging wall above a system of listric normal faults:A numerical solution[J]. AAPG Bulletin, 1993, 77(11):1839-1859.
[16] WITHJACK M O, ISLAM Q T, POINTE P R L. Normal faults and their hanging-wall deformation:An experimental study[J]. AAPG Bulletin, 1995, 79(1):1-18. doi:10.1306/8d2b1494-171e-11d7-8645000102c1865d
[17] WITHJACK M O, CALLAWAY S. Active normal faulting beneath a salt layer:An experimental study of deformation patterns in the cover sequence[J]. AAPG Bulletin, 2000, 84(5):627-651. doi:10.1306/C9EBCE73-1735-11D7-8645000102C1865D
[18] SCHLISCHE R W, WITHJACK M O, EISENSTADT G. An experimental study of the secondary deformation produced by oblique-slip normal faulting[J]. AAPG Bulletin, 2002, 86(5):885-906. doi:10.1306/61eedbca-173e-11d7-8645000102c1865d
[19] POBLET J, BULNES M. Predicting strain using forward modelling of restored cross-sections:Application to rollover anticlines over listric normal faults[J]. Journal of Structural Geology, 2007, 29, 1960-1970. doi:10.1016/j.jsg.2007.08.003
[20] LONG J J, IMBER J. Geometrically coherent continuous deformation in the volume surrounding a seismically imaged normal fault-array[J]. Journal of Structural Geology, 2010, 32(2):222-234. doi:10.1016/j.jsg.2009.11.009
[21] 蔡佳,姜华,甘华军,等. 南阳凹陷南部边界大断裂活动性及其对沉积的控制[J]. 西安石油大学学报(自然科学版), 2009, 24(4):9-12. doi:10.3969/j.issn.1673-064X.2009.04.002 CAI Jia, JIANG Hua, GAN Huajun, et al. Activities of the boundary major fault in the south of Nanyang Sag and their control effect on deposition[J]. Journal of Xi'an Shiyou University (Natural Science), 2009, 24(4):9-12. doi:10.3969/j.issn.1673-064X.2009.04.002
[22] 夏东领,杨道庆,林社卿,等. 南襄盆地中、新生代构造演化与油气成藏[J]. 油气地质与采收率, 2007, 14(6):32-34. doi:10.3969/j.issn.1009-9603.2007.06.010 XIA Dongling, YANG Daoqing, LIN Sheqing, et al. Tectonic evolution and hydrocarbon accumulation in Mesozoic-Cenozoic Era, Nanxiang Basin[J]. Petroleum Geology and Recovery Efficiency, 2007, 14(6):32-34. doi:10.3969/j.issn.1009-9603.2007.06.010
[23] 蔡佳,王华,罗家群. 基于层序地层格架的南阳凹陷油气成藏模式[J]. 西南石油大学学报(自然科学版), 2011, 33(3):67-73. doi:10.3863/j.issn.1674-5086.2011.03.010 CAI Jia, WANG Hua, LUO Jiaqun. Hydrocarbon ceneration models based on the sequence stratigraphic framework in Nanyang Sag[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2011, 33(3):67-73. doi:10.3863/j.issn.1674-5086.2011.03.010
[24] LI Shuguang, XIAO Yilin, LIOU Deliang, et al. Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites:Timing and processes[J]. Chemical Geology, 1993, 109(1-4):89-111. doi:10.1016/0009-2541(93)90063-o
[25] LI Shuguang, JAGOUTZ E, CHEN Yizhi, et al. SmNd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains, Central China[J]. Geochimica et Cosmochimica Acta, 2000, 64(6):1077-1093. doi:10.1016/S0016-7037(99)00319-1
[26] 解东宁,何明喜,周立发,等. 东秦岭大别造山带北缘逆冲推覆构造特征及油气前景[J]. 石油与天然气地质,2006,27(1):48-55. doi:10.3321/j.issn:0253-9985.2006.01.009 XIE Dongning, HE Mingxi, ZHOU Lifa, et al. Characteristics of overthrust structures on northern edge of east Qinling-Dabie orogenic belt and hydrocarbon potentials[J]. Oil & Gas Geology, 2006, 27(1):48-55. doi:10.3321/j.issn:0253-9985.2006.01.009
[27] 程学峰,于群达,吴跃通,等. 层序地层学研究及隐蔽油气藏预测以南阳凹陷古近系为例[J]. 新疆地质, 2003, 21(2):206-209. doi:10.3969/j.issn.1000-8845.2003.02.013 CHENG Xuefeng, YU Qunda, WU Yuetong, et al. Sequence stratigraphic research and prediction about subtle pools[J]. Xinjiang Geology, 2003, 21(2):206-209. doi:10.3969/j.issn.1000-8845.2003.02.013
[28] 田纳新,吴官生,李锋,等. 南襄盆地南阳凹陷构造特征与油气分布[J]. 石油天然气学报, 2008, 30(6):51-55. doi:10.3969/j.issn.1000-9752.2008.06.009 TIAN Naxin, WU Guansheng, LI Feng, et al. The structural characteristics and petroleum distribution of Nanyang Sag in Nanxiang Basin[J]. Journal of Oil and Gas Technology, 2008, 30(6):51-55. doi:10.3969/j.issn.1000-9752.2008.06.009
[29] 桂宝玲,何登发,闫福旺,等. 大兴断层的三维几何学与运动学及其对廊固凹陷成因机制的约束[J]. 地学前缘, 2012, 19(5):86-99. GUI Baoling, HE Dengfa, YAN Fuwang, et al. 3D geometry and kinematics of Daxing Fault:Its constraints on the origin of Langgu Depression, Bohaiwan Gulf Basin, China[J]. Earth Science Frontiers, 2012, 19(5):86-99.
[30] 高丽明,何登发,桂宝玲,等. 东营凹陷民丰洼陷边界断层三维几何学及运动学特征[J]. 石油勘探与开发, 2014, 41(5):546-553. doi:10.11698/PED.2014.05.05 GAO Liming, HE Dengfa, GUI Baoling, et al. 3D geometrical and kinematic characteristics of boundary faults in Minfeng Subsag, Donying Sag, Bohai Bay Basin[J]. Petroleum Exploration and Development, 2014, 41(5):546-553. doi:10.11698/PED.2014.05.05
[31] 张志业,何登发,李智,等. 珠江口盆地开平凹陷边界断层三维几何学与运动学[J]. 地球物理学报, 2018, 61(10):4296-4307. doi:10.6038/cjg2018L0560 ZHANG Zhiye, HE Dengfa, LI Zhi, et al. 3D geometry and kinematics of the boundary fault in the Kaiping Depression, Pearl River Mouth Basin[J]. Chinese Journal of Geophysics, 2018, 61(10):4296-4307. doi:10.6038/cjg2018L0560
[32] 王忠楠,柳广弟,陈婉,等. 利用声波速度计算南阳凹陷古近纪末地层抬升量[J]. 岩性油气藏, 2014, 26(6):69-74. doi:10.3969/j.issn.1673-8926.2014.06.012 WANG Zhongnan, LIU Guangdi, CHEN Wan, et al. Quantification of Late Paleogene Uplift in Nanyang Sag using acoustic velocity[J]. Lithologic Reservoirs, 2014, 26(6):69-74. doi:10.3969/j.issn.1673-8926.2014.06.012

南阳凹陷边界断层三维几何学及运动学特征

3D Geometrical and Kinematic Characteristics of the Boundary Fault in Nanyang Depression

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