Post-Rift Faulting Migration, Transition and Dynamics in Zhu Ⅰ Depression, Pearl River Mouth Basin
-
摘要: 珠江口盆地裂后期断裂作用对新近系油气成藏具有重要影响，但人们对其发育特征及动力学演化规律的认识一直不够.利用钻井约束的高精度三维及二维地震资料对珠一坳陷裂后期断裂的几何学与运动学特征进行了分析，结果表明珠一坳陷裂后期存在南海期和东沙期两期断裂作用，从南海期断裂作用到东沙期断裂作用，断裂的几何学、运动学特征以及动力学机制均发生了转换.南海期断裂作用具有从南向北迁移的特征；而东沙期断裂具有由东向西迁移的特征.两期断裂都以伸展为主，其中东沙期断裂具有微弱扭性特征.南海期断裂区域伸展方向为NNE10°～15°，东沙期为NNE20°～25°，区域伸展方向发生了5°～10°的顺时针偏转.南海期断裂作用发生于南海同扩张期，可能与南海扩张期间北部陆缘残留的伸展作用有关.东沙期断裂作用形成于南海后扩张期的东沙运动，该时期区域主应力轴σ2方向与吕宋岛弧和欧亚大陆的挤压碰撞方向一致.东沙期断裂特征进一步证实了东沙运动是中中新世以来吕宋岛弧与欧亚大陆碰撞的结果.研究结果对整个南海地区裂后期南海运动与东沙运动的进一步认识具有重要意义.Abstract: Post-rift fault plays an important role in hydrocarbon accumulation of the Neogene in Pearl River Mouth basin, but understanding of the features and dynamics evolution is to be enhanced in this paper, post-rift fault system in Zhu Ⅰ depression is studied by geometric and kinematic analysis methods using high quality 3D seismic reflection data. The analysis reveals two episodes of faulting in the post-rift stage, namely, Nanhai-phase faulting and Dongsha-phase faulting. Transition of fault geometry and kinematics from Nanhai-phase to Dongsha-phase indicates a change of dynamics. Both Nanhai-phase faulting and Dongsha-phase faulting have migration. The former migrates from south to north, and the latter migrates from east to west. The two periods of faulting are both extensional faults, with a slight component of shear in Dongsha-phase. Regional extensional direction transforms from NNE10°-15° in Nanhai-phase faulting to NNE20°-25° in Dongsha-phase faulting, with 5°-10° clockwise rotation. The Nanhai-phase faulting is related to the remaining extension in the northern margin of SCS. The Dongsha-phase faults formed after the cease of the sea-floor spreading of SCS. Coincidently, direction of the regional intermediate principal strain (σ2) during the Dongsha-phase faulting is consistent with the collision direction between the Luzon arc and the Eurasian plate. This feature of the Dongsha-phase faulting in Zhu Ⅰ depression confirms the conclusion that Dongsha movement is the result of the collision between the Luzon arc and the Eurasian plate since Middle Miocene. This study is significant for better understanding of Nanhai movement and Dongsha movement.
-
Key words:
- Zhu Ⅰ depression /
- post-rift /
- fault /
- migration /
- transition /
- tectonics.
-
图 2 珠一坳陷地层与构造演化综合柱状图
Fig. 2. Seismic stratigraphy and geological evolution of Zhu Ⅰ depression
图 3 珠一坳陷裂后期断裂平均活动速率
Fig. 3. Average active rate of post-rift faults in Zhu Ⅰ depression
图 5 珠一坳陷南海期断裂发育分布
a.断裂走向玫瑰花图；b.断裂倾角玫瑰花图；①～⑦见图 9
Fig. 5. The distribution of Nanhai stage faults in Zhu Ⅰ depression
图 6 珠一坳陷东沙期断裂发育分布
a.断裂走向玫瑰花图；b.断裂倾角玫瑰花图
Fig. 6. The distribution of Dongsha stage faults in Zhu Ⅰ depression
图 8 珠一坳陷南海期与东沙期断裂长度统计
Fig. 8. Length statistics of Nanhai and Dongsha stage faults in Zhu Ⅰ depression
图 9 珠一坳陷裂后期断裂作用迁移特征
Fig. 9. The migration pattern of post-rift faulting in Zhu Ⅰ depression
图 10 南海期新生断裂与东沙期新生断裂特征对比
Fig. 10. Different features of Nanhai and Dongsha stage faults
图 11 珠一坳陷裂后期应力场转换
Fig. 11. The transition of post-rift stress field in Zhu Ⅰ depression
表 1 珠一坳陷裂后期不同类型断裂发育统计
Table 1. The statistics of different types of post-rift faults in Zhu Ⅰ depression
断裂期次 类型 恩平凹陷 西江凹陷 惠州凹陷 珠一坳陷 数量(条) 总长度(km) 数量(条) 总长度(km) 数量(条) 总长度(km) 数量(条) 走向平均值(°) 总长度(km) 东沙期 Ⅱa 42 147 30 124 105 304 177 112 575 Ⅱb 80 285 21 58 47 193 148 108 536 Ⅱc 73 621 17 106 28 141 118 104 868 Ⅱd 28 228 21 152 96 907 145 103 1287 总数 223 1 281 89 440 276 1 545 588 - 3266 南海期 Ⅰa 151 372 30 78 70 147 251 104 597 Ⅰb 129 835 18 40 71 277 218 103 1152 Ⅰc 50 232 37 259 169 1 192 256 101 1683 总数 330 1 439 85 377 310 1 616 725 - 3432 注：断裂统计包含研究区中3个凹陷南部隆起区域内的断裂. 
下载: 导出CSV
-
Bertotti,G.,Gouiza,M.,2012.Post-Rift Vertical Movements and Horizontal Deformations in the Eastern Margin of the Central Atlantic:Middle Jurassic to Early Cretaceous Evolution of Morocco.International Journal of Earth Sciences,101(8):2151-2165.doi: 10.1007/s00531-012-0773-4 Briais,A.,Patriat,P.,Tapponnier,P.,1993.Updated Interpretation of Magnetic Anomalies and Seafloor Spreading Stages in the South China Sea:Implications for the Tertiary Tectonics of Southeast Asia.Journal of Geophysical Research:Solid Earth,98(B4):6299-6328.doi: 10.1029/92JB02280 Cai,Z.R.,Liu,W.L.,Wan,Z.F.,et al.,2010.Determination of Cenozoic Tectonic Movement in the Northern South China Sea and the Relationship between Oil-Gas Reservoir and Tectonic Movement.Marine Science Bulletin,29(2):161-165 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=e7474cca7cbafa17d5efafd8c2e0ddf5&encoded=0&v=paper_preview&mkt=zh-cn Chen,H.Z.,Wu,X.J.,Zhou,D.,et al.,2005.Meso-Cenozoic Faults in Zhujiang River Mouth Basin and Their Geodynamic Background.Journal of Tropical Oceanography,24(2):52-61 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=7439d4574411344345f1192add64e0e8&encoded=0&v=paper_preview&mkt=zh-cn Cheng,S.X.,Li,S.Z.,Suo,Y.H.,et al.,2012.Cenozoic Tectonics and Dynamics of Basin Groups of the Northern South China Sea.Marine Geology & Quaternary Geology,32(6):79-93 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=c37ffb43771a0d53d10cce2369f8ab9e&encoded=0&v=paper_preview&mkt=zh-cn Cloetingh,S.,Beekman,F.,Ziegler,P.A.,et al.,2008.Post-Rift Compressional Reactivation Potential of Passive Margins and Extensional Basins.Geological Society,London,Special Publications,306(1):27-70.doi: 10.1144/SP306.2 Cogné,N.,Gallagher,K.,Cobbold,P.R.,2011.Post-Rift Reactivation of the Onshore Margin of Southeast Brazil:Evidence from Apatite (U-Th)/He and Fission-Track Data.Earth and Planetary Science Letters,309(1):118-130.doi: 10.1016/j.epsl.2011.06.025 Cohen,H.A.,McClay,K.,1996.Sedimentation and Shale Tectonics of the Northwestern Niger Delta Front.Marine and Petroleum Geology,13(3):313-328.doi: 10.1016/0264-8172(95)00067-4 Corti,G.,Philippon,M.,Sani,F.,et al.,2013.Re-Orientation of the Extension Direction and Pure Extensional Faulting at Oblique Rift Margins:Comparison between the Main Ethiopian Rift and Laboratory Experiments.Terra Nova,25(5):396-404.doi: 10.1111/ter.12049 Dooley,T.P.,Jackson,M.P.A.,Hudec,M.R.,2013.Coeval Extension and Shortening above and below Salt Canopies on an Uplifted,Continental Margin:Application to the Northern Gulf of Mexico.AAPG Bulletin,97(10):1737-1764.doi: 10.1306/03271312072 Gabrielsen,R.H.,Kyrkjebo,R.,Faleide,J.I.,et al.,2001.The Cretaceous Post-Rift Basin Configuration of the Northern North Sea.Petroleum Geoscience,7(2):137-154.doi: 10.1144/petgeo.7.2.137 Holford,S.P.,Tuitt,A.K.,Hillis,R.R.,et al.,2014.Cenozoic Deformation in the Otway Basin,Southern Australian Margin:Implications for the Origin and Nature of Post-Breakup Compression at Rifted Margins.Basin Research,26(1):10-37.doi: 10.1111/bre.12035 Huang,C.Y.,Xia,K.,Yuan,P.B.,et al.,2001.Structural Evolution from Paleogene Extension to Latest Miocene-Recent Arc-Continent Collision Offshore Taiwan:Comparison with on Land Geology.Journal of Asian Earth Sciences,19(5):619-639.doi: 10.1016/S1367-9120(00)00065-1 Huang,C.Y.,Yuan,P.B.,Tsao,S.J.,2006.Temporal and Spatial Records of Active Arc-Continent Collision in Taiwan:A Synthesis.Geological Society of America Bulletin,118(3-4):274-288.doi: 10.1130/B25527.1 Kao,H.,Huang,G.C.,Liu,C.S.,2000.Transition from Oblique Subduction to Collision in the Northern Luzon Arc-Taiwan Region:Constraints from Bathymetry and Seismic Observations.Journal of Geophysical Research:Solid Earth,105(B2):3059-3079.doi: 10.1029/1999JB900357 Li,P.L.,1993.Cenozoic Tectonic Movement in the Pearl River Mouth Basin.China Offshore Oil and Gas (Geology),7(6):11-17 (in Chinese with English abstract). Li,P.L.,1994.Structural Features and Oil-Gas Accumulation in Pearl River Mouth Basin.Guangdong Geology,9(4):21-28 (in Chinese with English abstract). Li,S.Z.,Suo,Y.H.,Liu,X.,et al.,2012.Basin Dynamics and Basin Groups of the South China Sea.Marine Geology & Quaternary Geology,32(6):55-78 (in Chinese with English abstract). Lin,C.S.,Gao,J.Y.,Yu,X.J.,et al.,2006.Characteristics of Tectonic Movement in the Northern Part of South China Sea during the Cenozoic.Acta Oceanologica Sinica,28(4):81-86 (in Chinese with English abstract). Liu,M.H.,Mei,L.F.,Yang,Y.J.,et al.,2015.Temporal-Spatial Differences of Subsidence between Syn- and Post-Rift Stages in Northern Huizhou Sag of Pearl River Mouth Basin and Their Main Control Factors.Journal of Earth Sciences and Environment,37(2):31-43 (in Chinese with English abstract). Lüdmann,T.,Wong,H.K.,1999.Neotectonic Regime on the Passive Continental Margin of the Northern South China Sea.Tectonophysics,311(1):113-138.doi: 10.1016/S0040-1951(99)00155-9 Mao,K.N.,Xie,X.N.,Xie,Y.H.,et al.,2015.Post-Rift Tectonic Reactivation and Its Effect on Deep-Water Deposits in the Qiongdongnan Basin,Northwestern South China Sea.Marine Geophysical Research,36(2):227-242.doi: 10.1007/s11001-015-9248-x McKenzie,D.,1978.Some Remarks on the Development of Sedimentary Basins.Earth and Planetary Science Letters,40(1):25-32.doi: 10.1016/0012-821X(78)90071-7 Mogi,K.,1967.Effect of the Intermediate Principal Stress on Rock Failure.Journal of Geophysical Research Atmospheres,72(20):5117-5131.doi: 10.1029/JZ072i020p05117 Morley,C.K.,2010.Stress Re-Orientation along Zones of Weak Fabrics in Rifts:An Explanation for Pure Extension in ‘Oblique’ Rift Segments?Earth and Planetary Science Letters,297(3):667-673.doi: 10.1016/j.epsl.2010.07.022 Morley,C.K.,Haranya,C.,Phoosongsee,W.,et al.,2004.Activation of Rift Oblique and Rift Parallel Pre-Existing Fabrics during Extension and Their Effect on Deformation Style:Examples from the Rifts of Thailand.Journal of Structural Geology,26(10):1803-1829.doi: 10.1016/j.jsg.2004.02.014 Nogueira,F.C.C.,Marques,F.O.,Bezerra,F.H.R.,et al.,2015.Cretaceous Intracontinental Rifting and Post-Rift Inversion in NE Brazil:Insights from the Rio do Peixe Basin.Tectonophysics,644-645:92-107.doi: 10.1016/j.tecto.2014.12.016 Obrien,G.W.,Lisk,M.,Duddy,I.R.,et al.,1999.Plate Convergence,Foreland Development and Fault Reactivation:Primary Controls on Brine Migration,Thermal Histories and Trap Breach in the Timor Sea,Australia.Marine and Petroleum Geology,16(6):533-560.doi: 10.1016/S0264-8172(98)00070-1 Pereira,R.,Alves,T.M.,Cartwright,J.,2011.Post-Rift Compression on the SW Iberian Margin (Eastern North Atlantic):A Case for Prolonged Inversion in the Ocean-Continent Transition Zone.Journal of the Geological Society,168(6):1249-1263.doi: 10.1144/0016-76492010-151 Philippon,M.,Willingshofer,E.,Sokoutis,D.,et al.,2015.Slip Re-Orientation in Oblique Rifts.Geology,43(2):147-150.doi: 10.1130/G36208.1 Rao,C.T.,Li,P.L.,Zhong,H.P.,1993.Discussion on Fault Features and Their Sealing in Pearl River Mouth Basin.China Offshore Oil and Gas (Geology),7(4):7-15 (in Chinese with English abstract). Rowan,M.G.,Peel,F.J.,Vendeville,B.C.,2004.Gravity-Driven Fold Belts on Passive Margins.AAPG Memoir,82:157-182.doi: 10.1306/61EECE28-173E-11D7-8645000102C1865D Schlische,R.W.,Withjack,M.O.,Olsen,P.E.,2003.Relative Timing of CAMP,Rifting,Continental Breakup,and Basin Inversion:Tectonic Significance.Geophysical Monograph Series,136:33-59.doi: 10.1029/136gm03 Seno,T.,Stein,S.,Gripp,A.E.,1993.A Model for the Motion of the Philippine Sea Plate Consistent with NUVEL-1 and Geological Data.Journal of Geophysical Research,98(B10):17941-17948.doi: 10.1029/93JB00782 Sibuet,J.C.,Hsu,S.K.,Pichon,X.L.,et al.,2002.East Asia Plate Tectonics since 15 Ma:Constraints from the Taiwan Region.Tectonophysics,344(1):103-134.doi: 10.1016/S0040-1951(01)00202-5 Silva,S.R.P.,Maciel,R.R.,Severino,M.C.G.,1998.Cenozoic Tectonics of Amazon Mouth Basin.Geo-Marine Letters,18(3):256-262.doi: 10.1007/s003670050077 Song,Y.,2010.The Post-Rift Tectonic Inversion of Songliao Basin,NE China and Its Dynamical Background (Dissertation).China University of Geoscience,Wuhan,5-12 (in Chinese with English abstract). Soofi,M.A.,King,S.D.,1999.A Modified Beam Analysis Effect of Lateral Forces on Lithospheric Flexure and Its Implication for Post-Rift Evolution of the Midcontinent Rift System.Tectonophysics,306(2):149-162.doi: 10.1016/S0040-1951(99)00048-7 Soofi,M.A.,King,S.D.,2002.Post-Rift Deformation of the Midcontinent Rift under Grenville Tectonism.Tectonophysics,359(3):209-223.doi: 10.1016/S0040-1951(02)00512-7 Sun,J.L.,Xu,H.L.,Cao,J.H.,2011.Crustal Movement and Its Dynamic Mechanism of the Taiwan-Luzon Convergent Zone.Chinese Journal of Geophysics,54(12):3016-3025 (in Chinese with English abstract). Sun,X.M.,Wang,P.J.,Hao,F.J.,et al.,2006.Space-Time Distribution Features,Migration Regularities and Genetic Types of Regional Fault System of Meso-Cenozoic in the Central Section of Epicontinent of the East China.Journal of Jilin University (Earth Science Edition),35(5):554-563 (in Chinese with English abstract). Sun,Z.,Xu,Z.,Sun,L.,et al.,2014.The Mechanism of Post-Rift Fault Activities in Baiyun Sag,Pearl River Mouth Basin.Journal of Asian Earth Sciences,89:76-87.doi: 10.1016/j.jseaes.2014.02.018 Sun,Z.,Zhou,D.,Zhong,Z.H.,et al.,2006.Research on the Dynamics of the South China Sea Opening:Evidence from Analogue Modeling.Science in China (Series D),49(10):1053-1069.doi: 10.1007/s11430-006-1053-6 Suppe,J.,1984.Kinematics of Arc-Continent Collision,Flipping of Subduction,and Back-Arc Spreading near Taiwan.Memoir of the Geological Society of China,6:21-33. Tian,P.,Mei,L.F.,Yu,H.L.,et al.,2008.The Faults in Huizhou Sag and Their Controls on the Petroleum Accumulation.Xinjiang Petroleum Geology,29(5):591-594 (in Chinese with English abstract). Tian,W.,He,M.,Yang,Y.J.,et al.,2015.Complex Linkage and Transformation of Boundary Faults of Northern Huizhou Sag in Pearl River Mouth Basin.Earth Science,40(12):2037-2051 (in Chinese with English abstract). Tong,H.M.,Nie,J.Y.,Meng,L.J.,et al.,2009.The Law of Basement Pre-Existing Fabric Controlling Fault Formation and Evolution in Rift Basin.Earth Science Frontiers,16(4):97-104 (in Chinese with English abstract). Wan,T.F.,1983.Tension Joints and Its Mechanism.Earth Science,(3):58-61,148 (in Chinese with English abstract). Withjack,M.O.,Schlische,R.W.,2005.A Review of Tectonic Events on the Passive Margin of Eastern North America.25th Annual Bob F.Perkins Research Conference:Petroleum Systems of Divergent Continental Margin Basins,Houston,203-235.doi: 10.5724/gcs.05.25.0203 Withjack,M.O.,Schlische,R.W.,Olsen,P.E.,1998.Diachronous Rifting,Drifting,and Inversion on the Passive Margin of Central Eastern North America:An Analog for Other Passive Margins.AAPG Bulletin,82(5):817-835.doi: 10.1306/1d9bc60b-172d-11d7-8645000102c1865d Wu,S.G.,Liu,Z.,Wang,W.Y.,et al.,2004.Late Cenozoic Neotectonics in the Dongsha Islands Region and Its Responds to Collision between Chinese Continental Margin and Luzon.Oceanologia et Limnologia Sinica,35(6):481-490 (in Chinese with English abstract). Xia,B.,Lü,B.F.,Wu,G.G.,et al.,2007.The Cenozoic Tectonic Transport and Its Control on the Source Rock in the Northern South China Sea.Natural Gas Geoscience,18(5):629-634 (in Chinese with English abstract). Xu,X.M.,Chen,S.H.,Wang,F.G.,et al.,2014.Structural Features and Its Impacts on Hydrocarbon Accumulation of Neogene in Enping Sag,Pearl River Mouth Basin.Geoscience,28(3):543-550 (in Chinese with English abstract). Yao,B.C.,1998.The Tectonic Evolution and Sedimentary Basins of South China Sea in Cenozoic.Geological Research of South China Sea,(10):1-17 (in Chinese with English abstract). Yin,X.L.,Li,S.T.,Yang,J.H.,et al.,2002.Correlations between Overpressure Fluid Activity and Fault System in Yinggehai Basin.Acta Geoscientia Sinica,23(2):141-146 (in Chinese with English abstract). Yu,S.M.,Chen,X.F.,Mei,L.F.,et al.,2012.The Effect of Fault Zone Characteristics of Zhu Ⅰ Depression on Hydrocarbon Accumulation.Journal of Oil and Gas Technology,34(1):50-54 (in Chinese with English abstract). Zhao,S.J.,Wu,S.G.,Shi,H.S.,et al.,2012.Structures and Dynamic Mechanism Related to the Dongsha Movement at the Northern Margin of South China Sea.Progress in Geophysics,27(3):1008-1019 (in Chinese with English abstract). Zhao,Z.X.,Zhou,D.,Liao,J.,et al.,2010.Lithospheric Stretching Modeling of the Continental Shelf in the Pearl River Mouth Basin and Analysis of Post-Breakup Subsidence.Acta Geologica Sinica,84(8):1135-1145 (in Chinese with English abstract). Zhou,D.,Sun,Z.,Liao,J.,et al.,2009.Filling History and Post-Breakup Acceleration of Sedimentation in Baiyun Sag,Deepwater Northern South China Sea.Journal of Earth Science,20(1):160-171.doi: 10.1007/s12583-009-0015-2 Zhu,H.T.,Li,S.,Liu,H.R.,2016.The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin:An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression,Pearl River Mouth Basin.Earth Science,41(3):361-372 (in Chinese with English abstract). Ziegler,P.A.,Cloetingh,S.,2004.Dynamic Processes Controlling Evolution of Rifted Basins.Earth-Science Reviews,64(1):1-50.doi: 10.1016/S0012-8252(03)00041-2 蔡周荣, 刘维亮, 万志峰, 等, 2010.南海北部新生代构造运动厘定及与油气成藏关系探讨.海洋通报, 29(2): 161-165. http://www.cnki.com.cn/Article/CJFDTOTAL-HUTB201002010.htm 陈汉宗, 吴湘杰, 周蒂, 等, 2005.珠江口盆地中新生代主要断裂特征和动力背景分析.热带海洋学报, 24(2): 52-61. http://www.cnki.com.cn/Article/CJFDTOTAL-RDHY200502006.htm 程世秀, 李三忠, 索艳慧, 等, 2012.南海北部新生代盆地群构造特征及其成因.海洋地质与第四纪地质, 32(6): 79-93. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201206011.htm 李平鲁, 1993.珠江口盆地新生代构造运动.中国海上油气(地质), 7(6): 11-17. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199306003.htm 李平鲁, 1994.珠江口盆地构造特征与油气聚集.广东地质, 9(4): 21-28. 李三忠, 索艳慧, 刘鑫, 等, 2012.南海的盆地群与盆地动力学.海洋地质与第四纪地质, 32(6): 55-78. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201206010.htm 林长松, 高金耀, 虞夏军, 等, 2006.南海北部新生代的构造运动特征.海洋学报, 28(4): 81-86. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC200604009.htm 刘明辉, 梅廉夫, 杨亚娟, 等, 2015.珠江口盆地惠州凹陷北部裂陷期与拗陷期沉降作用时空差异及主控因素.地球科学与环境学报, 37(2):31-43. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201502006.htm 饶春涛, 李平鲁, 钟宏平, 1993.珠江口盆地断层特征及封闭性研究.中国海上油气(地质), 7(4): 7-15. 宋鹰, 2010.松辽盆地裂后期构造反转及其动力学背景分析(博士学位论文).武汉: 中国地质大学, 5-12. http://cdmd.cnki.com.cn/Article/CDMD-10491-2010250515.htm 孙金龙, 徐辉龙, 曹敬贺, 2011.台湾-吕宋会聚带的地壳运动特征及其动力学机制.地球物理学报, 54(12): 3016-3025. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201112006.htm 孙晓猛, 王璞珺, 郝福江, 等, 2005.中国东部陆缘中区中-新生代区域断裂系统时空分布特征, 迁移规律及成因类型.吉林大学学报(地球科学版), 35(5): 554-563. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200505001.htm 田鹏, 梅廉夫, 于慧玲, 等, 2008.惠州凹陷断裂特征及其对油气成藏的控制.新疆石油地质, 29(5): 591-594. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200805019.htm 田巍, 何敏, 杨亚娟, 等, 2015.珠江口盆地惠州凹陷北部边界断裂复合联接和转换.地球科学, 40(12): 2037-2051. http://www.earth-science.net/WebPage/Article.aspx?id=3207 童亨茂, 聂金英, 孟令箭, 等, 2009.基底先存构造对裂陷盆地断层形成和演化的控制作用规律.地学前缘, 16(4): 97-104. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200904012.htm 万天丰, 1983.张节理及其形成机制.地球科学, (3): 58-61,148. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198303005.htm 吴时国, 刘展, 王万银, 等, 2004.东沙群岛海区晚新生代构造特征及其对弧-陆碰撞的响应.海洋与湖沼, 35(6): 481-490. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ200406000.htm 夏斌, 吕宝凤, 吴国干, 等, 2007.南海北部新生代盆地构造迁移及其对烃源岩的制约作用.天然气地球科学, 18(5): 629-634. http://www.cnki.com.cn/Article/CJFDTOTAL-TDKX200705000.htm 许新明, 陈胜红, 王福国, 等, 2014.珠江口盆地恩平凹陷断层特征及其对新近系油气成藏的影响.现代地质, 28(3): 543-550. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201403011.htm 姚伯初, 1998.南海新生代的构造演化与沉积盆地.南海地质研究, (10): 1-17. http://www.cnki.com.cn/Article/CJFDTOTAL-NHDZ199800000.htm 殷秀兰, 李思田, 杨计海, 等, 2002.莺歌海盆地超压流体活动与断裂系统的相互关系.地球学报, 23(2): 141-146. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200202009.htm 于水明, 陈雪芳, 梅廉夫, 等, 2012.珠一坳陷断层特征及对油气成藏的作用.石油天然气学报, 34(1): 50-54. http://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201201011.htm 赵淑娟, 吴时国, 施和生, 等, 2012.南海北部东沙运动的构造特征及动力学机制探讨.地球物理学进展, 27(3): 1008-1019. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ201203023.htm 赵中贤, 周蒂, 廖杰, 等, 2010.珠江口盆地陆架区岩石圈伸展模拟及裂后沉降分析.地质学报, 84(8): 1135-1145. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201008007.htm 朱红涛, 李森, 刘浩冉, 等, 2016.陆相断陷湖盆迁移型层序构型及意义: 以珠Ⅰ坳陷古近系文昌组为例.地球科学, 41(3): 361-372. http://www.earth-science.net/WebPage/Article.aspx?id=3256 -
点击查看大图
图(11) / 表(1)
计量
- 文章访问数: 4858
- HTML全文浏览量: 2542
- PDF下载量: 62
- 被引次数: 0
