珠江口盆地西江主洼低角度边界正断层特征及成因演化

doi:10.11743/ogg20200316

石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (3): 606-616.doi: 10.11743/ogg20200316

珠江口盆地西江主洼低角度边界正断层特征及成因演化

邓棚^1,2,3, 梅廉夫³, 杜家元⁴, 叶青³, 许新明⁴, 吴静⁴, 董小云⁴

1. 中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126;
2. 浙江大学地球科学学院, 浙江杭州 310027;
3. 中国地质大学(武汉)构造与油气资源教育部重点实验室, 湖北武汉 430074;
4. 中海石油(中国)有限公司深圳分公司研究院, 广东深圳 518000

收稿日期:2019-03-03 修回日期:2020-02-10 发布日期:2020-06-16
通讯作者: 梅廉夫(1961-),男,教授、博士生导师,盆地构造分析。E-mail:lfmei@cug.edu.cn。 E-mail:lfmei@cug.edu.cn
作者简介:邓棚(1990-),男,博士、助理研究员,石油勘探构造分析。E-mail:dengpeng_003@163.com。
基金资助:
国家科技重大专项（2016ZX05026-003-001）。

Characteristics and genetic development of a low-angle boundary normal fault in Xijiang Main Sag,Pearl River Mouth Basin,China

Deng Peng^1,2,3, Mei Lianfu³, Du Jiayuan⁴, Ye Qing³, Xu Xinming⁴, Wu Jing⁴, Dong Xiaoyun⁴

1. Wuxi Research Institute of Petroleum Geology, Petroleum Exploration and Production Research Institute, SINOPEC, Wuxi, Jiangsu 214126, China;
2. School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China;
3. Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China;
4. Research Institute of Shenzhen Branch of CNOOC Ltd., Shenzhen, Guangdong 518000, China

Received:2019-03-03 Revised:2020-02-10 Published:2020-06-16

摘要/Abstract

摘要： 西江主洼位于珠江口盆地珠一坳陷的中西部，是珠江口盆地重要的富生烃凹陷之一。为了认识珠江口盆地西江主洼边界断层（Fxj33）属性特征，基于钻井约束的高精度三维地震资料，对Fxj33断层几何学和运动学进行了综合分析。研究揭示Fxj33边界断层为低角度生长正断层，倾角5°~36°，呈NEE走向，长度约55 km，最大水平位移达9.5 km左右。在多幕裂陷演化过程中，Fxj33断层沿走向上表现为分段差异活动特征，并与两排EW向高角度断裂共同控制着西江主洼各次级洼陷的发育演化。中生代基底中发育的叠瓦状构造、残留山和先存断面等一系列构造表明Fxj33边界断层为中生代先存逆冲构造体系在新生代反转形成，并且在断陷中晚期进一步被一系列EW向高角度断面切割改造，形成现今形态。期望研究结果对被动陆缘断陷盆地边界断层的形成和演化研究有指示意义。

关键词: 先存构造体系, 多幕裂陷作用, 低角度正断层, 西江主洼, 珠江口盆地

Abstract: The Xijiang Main Sag,located in the west-central Zhu-1 Depression,is one of the most important hydrocarbon-rich sags in the Pearl River Mouth Basin,China.To recognize the properties of the boundary fault (Fxj33) in the Xijiang Main Sag,we comprehensively analyze the geometry and kinematics of Fxj33,using high-resolution 3-D seismic data under the constraints of well data.The results show that the boundary fault Fxj33 of about 55 km long and up to 9.5 km displacement at most,is a NEE-trending low-angle normal fault with a dip of 5°-36°.During the evolution of multistage rifting,the fault Fxj33 is characterized by differential activities of different segments along the strike,and jointly controls the evolution of the sub-sags in the Xjiang Main Sag together with the two lines of EW-trending high-angle normal faults.Various structures developed in the Mesozoic basement,including imbricate structures,residual hills and pre-existing fault planes,indicate that the boundary fault Fxj33 was developed by the inversion of the pre-existing Mesozoic thrusting system in the Cenozoic,and subsequently reformed by the EW-trending high-angle fault planes cutting into it during the middle-to-late rifting stage.The research results are expected to be of referential meaning to the study of the boundary faults during rifting in passive margin faulted basins.

Key words: pre-existing structural system, multistage rifting, low-angle normal fault, Xijiang Main Sag, Pearl River Mouth Basin

中图分类号:

TE121.1

邓棚,梅廉夫,杜家元,等. 珠江口盆地西江主洼低角度边界正断层特征及成因演化[J]. 石油与天然气地质, 2020, 41(3): 606-616. doi: 10.11743/ogg20200316 Deng Peng,Mei Lianfu,Du Jiayuan,et al. Characteristics and genetic development of a low-angle boundary normal fault in Xijiang Main Sag,Pearl River Mouth Basin,China[J]. Oil & Gas Geology, 2020, 41(3): 606-616. doi: 10.11743/ogg20200316

参考文献

[1] Anderson E M.The dynamics of faulting(2nd edition)[M].Edinburgh,UK:Oliver and Boyd,1951.
[2] Jackson J A,White N J.Normal faulting in the upper continental crust:Observations from regions of active extension[J].Journal of Structural Geology,1989,11(1-2):15-36.
[3] Morley C K.Extension,detachments and sedimentation in continental rifts (with particular reference to East Africa)[J].Tectonics,1989,8(6):1175-1192.
[4] Jackson J A,White N J,Garfunkel Z,et al.Relations between normal-fault geometry,tilting and vertical motions in extensional terranes:An example from the southern Gulf of Suez[J].Journal of Structural Geology,1988,10(2):155-170.
[5] Whipp P S,Jackson C A-L,Gawthorpe R L,et al.Normal fault array evolution above a reactivated rift fabric:A subsurface example from the northern Horda Platform,Norwegian North Sea[J].Basin Research,2013,26:1-27.
[6] Axen G J.Research focus:Significance of large-displacement,low-angle normal faults[J].Geology,2007,35(3):287-288.
[7] Wernicke B.Low-angle normal faults in the basin and range province:Nappe tectonics in an extending orogen[J].Nature,1981,291:645-648.
[8] Garcés M,Gee J S.Paleomagnetic evidence of large footwall rotations associated with low-angle faults at the Mid-Atlantic Ridge[J].Geology,2007,35(3):279-282.
[9] Tucholke B E,Lin J,Kleinrock M.Megamullions and mullion structure defining oceanic metamorphic core complexes on the Mid-Atlantic Ridge[J].Journal of Geophysical Research,1998,103(B5):9857-9866.
[10] Morley C K.Geometry and evolution of low-angle normal faults (LANF) within a Cenozoic high-angle rift system,Thailand:Implications for sedimentology and the mechanisms of LANF development[J].Tectonics,2009,28:1-30.
[11] Morley C K.The widespread occurrence of low-angle normal faults in a rift setting:Review of examples from Thailand,and implications for their origin and evolution[J].Earth-Science Reviews,2014,133:18-42.
[12] Parsons T,Thompson G A.Does magmatism influence low-angle normal faulting?[J].Geology,1993,21(3):247-250.
[13] Lister G S,Davis G A.The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region,USA[J].Journal of Structural Geology,1989,11(1-2):65-94.
[14] Westaway R.The mechanical feasibility of low-angle normal faulting[J].Tectonophysics,1999,308:407-443.
[15] Collettini C,Sibson R H.Normal faults,normal friction?[J].Geology,2001,29(10):927-930.
[16] Numelin T,Marone C,Kirby E.Frictional properties of natural fault gouge from a low-angle normal fault,Panamint Valley,California[J].Tectonics,2007,26:1-14.
[17] Haines S H,van der Pluijm B A,Ikari M J,et al.Clay fabric intensity in natural and artificial fault gouges:Implications for brittle fault zone processes and sedimentary basin clay fabric evolution[J].Journal of Geophysical Research,2009,114:1-22.
[18] Haines S H,van der Pluijm B A.Patterns of mineral transformations in clay gouge,with examples from low-angle normal fault rocks in the western USA[J].Journal of Structural Geology,2012,43:2-32.
[19] Faulkner D R,Mitchell T M,Healy D,et al.Slip on ‘weak’ faults by the rotation of regional stress in the fracture damage zone[J].Nature,2006,444(7121):922-925.
[20] Healy D.Anisotropy,pore fluid pressure and low angle normal faults[J].Journal of Structural Geology,2009,31(6):561-574.
[21] Lecompte E,Le Pourhiet L,Lacombe O.Mechanical basis for slip along low-angle normal faults[J].Geophysical Research Letters,2012,39:1-6.
[22] Enfield M A,Coward M P.The structure of the west Orkney Basin,northern Scotland[J].Journal of the Geological Society,1987,144(6):871-884.
[23] Jarrige J J.Variation in extensional fault geometry related to heterogeneities within basement and sedimentary sequences[J].Tectonophysi-cs,1992,215(1-2):161-166.
[24] Withjack M O,Olsen P E,Schlische R W.Tectonic evolution of the Fundy rift basin,Canada:Evidence of extension and shortening during passive margin development[J].Tectonics,1995,14(2):390-405.
[25] Jolivet L,Lecomte E,Huet B,et al.The north cycladic detachment system[J].Earth and Planetary Science Letter,2010,289(1):87-104.
[26] Li J H,Zhang Y Q,Dong S W,et al.The Hengshan low-angle normal fault zone:Structural and geochronological constraints on the Late Mesozoic crustal extension in South China[J].Tectonophysics,2013,606:97-115.
[27] Sibson R H.A note on fault reactivation[J].Journal of Structural Geology,1985,7(6):751-754.
[28] Collettini C,De Paola N,Holdsworth R E.The development and behaviour of low-angle normal faults during Cenozoic asymmetric extension in the Northern Apennines,Italy[J].Journal of Structural Geology,2006,28(2):333-352.
[29] Clemenzi L,Storti F,Balsamo F,et al.Fluid pressure cycles,variations in permeability,and weakening mechanisms along low-angle normal faults:The Tellaro detachment,Italy[J].Geological Society of America Bulletin,2015,127(11-12):1689-1710.
[30] Collettini C,Viti C,Smith S,et al.Development of interconnected talc networks and weakening of continental low-angle normal faults[J].Geology,2009,37(6):567-570.
[31] Bolognesi F,Bistacchi A.Weakness and mechanical anisotropy of phyllosilicate-rich cataclasites developed after mylonites of a low-angle normal fault (Simplon Line,Western Alps)[J].Journal of Structural Geology,2016,83:1-12.
[32] Wang J H,Pang X,Liu B,et al.The Baiyun and Liwan Sags:Two supradetachment basins on the passive continental margin of the northern South China Sea[J].Marine and Petroleum Geology,2018,95:206-218.
[33] Zhao Y H,Ren J Y,Pang X,et al.Structural style,formation of low angle normal fault and its controls on the evolution of Baiyun Rift,northern margin of the South China Sea[J].Marine and Petroleum Geology,2018,89:687-700.
[34] Ye Q,Mei L,Shi H,et al.A low-angle normal fault and basement structures within the Enping Sag,Pearl River Mouth Basin:Insights into late Mesozoic to early Cenozoic tectonic evolution of the South China Sea area[J].Tectonophysics,2018,731-732:1-16.
[35] 何勇,梅廉夫,施和生,等.低角度断陷盆地成因模式及结构特征——以珠江口盆地恩平低角度断陷为例[J].海相油气地质,2018,23(3):73-81. He Yong,Mei Lianfu,Shi Hesheng,et al.Structural characteristics and genetic model of the low-angle fault depression:A case in Enping Depression of Pearl River Mouth Basin[J].Marine Origin Petroleum Geology,2018,23(3):73-81.
[36] Huang C J,Zhou D,Sun Z,et al.Deep crustal structure of Baiyun Sag,northern South China Sea revealed from deep seismic reflection profile[J].Chinese Science Bulletin,2005,50(11):1131-1138.
[37] Briais A,Patriat P,Tapponnier P.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:Implications for the Tertiary tectonics of Southeast Asia[J].Journal of Geophysical Research,1993,98(B4),6299-6328.
[38] Barckhausen U,Engels M,Franke D et al.Evolution of the South China Sea:Revised ages for breakup and seafloor spreading[J].Marine and Petroleum Geology,2014,58:599-611.
[39] Li C F,Xu X,Lin J,et al.Ages and magnetic structures of the South China Sea constrained by the deep tow magnetic surveys and IODP Expedition 349[J].Geochemistry,Geophysics,Geosystems,2014,15(12):4958-4983.
[40] 宫越,林畅松,何敏,等.中国南海北部珠江口盆地早渐新世末破裂不整合特征及其地质意义[J].石油与天然气地质,2019,40(4):851-863. Gong Yue,Lin Changsong,He Min,et al.Characteristics and geological significance of unconformities at the late Early Oligocene in the Pearl River Mouth Basin,northern South China Sea[J].Oil & Gas Geology,2019,40(4):851-863.
[41] 赵中贤,孙珍,谢辉,等.白云深水区新生代沉降及岩石圈伸展变形[J].地球物理学报,2011,54(12):3336-3343. Zhao Zhongxian,Sun Zhen,Xie Hui,et al.Baiyun deepwater Cenozoic subsidence and lithospheric stretching deformation[J].Chinese Journal of Geophysics,2011,54(12):3336-3343.
[42] 廖杰,周蒂,赵中贤,等.珠江口盆地白云凹陷裂后异常沉降的数值模拟[J].中国科学:地球科学,2011,41(4):504-517. Liao Jie,Zhou Di,Zhao Zhongxian,et al.Numerical modeling of the anomalous post-rift subsidence in the Baiyun Sag,Pearl River Mouth Basin[J].Scientia Sinica(Terrae),2011,41(4):504-517.
[43] Xie H,Zhou D,Li Y,et al.Cenozoic tectonic subsidence in deepwater sags in the Pearl River Mouth Basin,northern South China Sea[J].Tectonophysics,2014,615-616:182-198.
[44] 庞雄,陈长民,邵磊,等.白云运动:南海北部渐新统-中新统重大地质事件及其意义[J].地质评论,2007,53(2):145-150. Pang Xiong,Chen Changmin,Shao Lei,et al.Baiyun movement,a great tectonic event on the Oligocene-Miocene boundary in the northern South China Sea and its implications[J].Geological Review,2007,53(2):145-150.
[45] Franke D.Rifting,lithosphere breakup and volcanism:Comparison of magma-poor and volcanic rifted margins[J].Marine and Petroleum Geology,2013,43:63-87.
[46] Deng P,Mei L F,Liu J,et al.Episodic normal faulting and magmatism during the syn-spreading stage of the Baiyun sag in Pearl River Mouth Basin:Response to the multi-phase seafloor spreading of the South China Sea[J].Marine Geophysical Research,2019,40(1):33-50.
[47] 赵淑娟,吴时国,施和生,等.南海北部东沙运动的构造特征及动力学机制探讨[J].地球物理学进展,2012,27(3):1008-1019. Zhao Shujuan,Wu Shiguo,Shi Hesheng,et al.Structures and dynamic mechanism related to the Dongsha movement at the northern margin of South China Sea[J].Progress in Geophysics,2012,27(3):1008-1019.
[48] 汪旭东,张向涛,何敏,等.珠江口盆地陆丰凹陷南部文昌组储层发育特征及其控制因素[J].石油与天然气地质,2017,38(6):1147-1155. Wang Xudong,Zhang Xiangtao,He Min,et al.Characteristics and controlling factors of reservoir development in the Wenchang Formation,Southern Lufeng Sag,Pearl River Mouth Basin[J].Oil & Gas Geology,2017,38(6):1147-1155.
[49] 刘志峰,吴克强,柯岭,等.珠江口盆地珠一坳陷北部洼陷带油气成藏主控因素[J].石油与天然气地质,2017,38(3):561-569. Liu Zhifeng,Wu Keqiang,Ke Ling,et al.Main factors controlling hydrocarbon accumulation in northern subsag belt of the Zhu-1 Depression,Pearl River Mouth Basin[J].Oil & Gas Geology,2017,38(3):561-569.
[50] Cowie P A,Scholz C H.Displacement-length scaling relationship for faults:Data synthesis and discussion[J].Journal of Structural Geology,1992,14(10):1149-1156.
[51] Dawers N H,Anders M H,Scholz C H.Growth of normal faults:Displacement length scaling[J].Geology,1993,21(12):1107-1110.
[52] Kim Y S,Sanderson D J.The relationship between displacement and length of faults:A review[J].Earth-Science Reviews, 2005,68(3):317-334.
[53] Wong M S,Gans P B.Geologic,structural and thermochronologic constraints on the tectonic evolution of the Sierra Mazatan core complex,Sonora,Mexico:New insights into metamorphic core complex formation[J].Tectonics,2008,27(4):1-31.
[54] Whitney D L,Teyssier C,Rey P,et al.Continental and oceanic core complexes[J].Geological Society of America Bulletin,2013,125(3-4):273-298.
[55] Collettini C.The mechanical paradox of low-angle normal faults:Current understanding and open questions[J].Tectonophysics,2011,510(3-4):253-268.
[56] 邵磊,尤洪庆,郝沪军,等.南海东北部中生界岩石学特征及沉积环境[J].地质论评,2007,53(2):164-169. Shao Lei,You Hongqing,Hao Hujun,et al.Petrology and depositional environments of Mesozoic strata in the northeastern South China Sea[J].Geological Review,2007,53(2):164-169.
[57] 陈汉宗,吴湘杰,周蒂,等.珠江口盆地中新生代主要断裂特征和动力背景分析[J].热带海洋学报,2005,24(2):52-61. Chen Hanzong,Wu Xiangjie,Zhou Di,et al.Meso-Cenozoic faults in Zhujiang River Mouth basin and their geodynamic background[J].Journal of Tropical Oceanography,2005,24(2):52-61.
[58] 孙晓猛,张旭庆,张功成,等.南海北部新生代盆地基底结构及构造属性[J].中国科学:地球科学,2014,44(6):1312-1323. Sun X M,Zhang X Q,Zhang G C,et al.2014.Texture and tectonic attribute of Cenozoic basin basement in the northern South China Sea[J].Science China:Earth Sciences,2014,44(6):1312-1323.
[59] 周蒂,王万银,庞雄,等.地球物理资料所揭示的南海东北部中生代俯冲增生带[J].中国科学(D辑:地球科学),2006,36(3):209-218. Zhou D,Wang W Y,Pang X,et al,Subducted accretionary zone revealed by the geophysical data in the northeastern South China Sea[J].Science in China(Series D:Earth Sciences),2006:36(3):209-218.
[60] Zhou D,Yao B C.Tectonics and sedimentary basins of the South China Sea:Challenges and progresses[J].Journal Earth Science,2009,20(1):1-12.
[61] Ren J Y,Tamaki K,Li S T,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J].Tectonophysics,2002,344(3):175-205.
[62] 李武显,周新民.中国东南部晚中生代俯冲带探索[J].高校地质学报,1999,5(2):164-169. Li Wuxian,Zhou Xinmin.Late Mesozoic subduction zone of southeastern China[J].Geological Journal of China Universities,1999,5(2):164-169.
[63] 索艳慧,李三忠,戴黎明,等.东亚及其大陆边缘新生代构造迁移与盆地演化[J].岩石学报,2012,28(8):2602-2618. Suo Yanhui,Li Sanzhong,Dai Liming,et al.Cenozoic tectonic migration and basin evolution in East Asia and its continental margins[J]. Acta Petrologica Sinica,2012,28(8):2602-2618.
[64] 李三忠,余珊,赵淑娟,等.东亚大陆边缘的板块重建与构造转换[J].海洋地质与第四纪地质,2013,33(3):65-94. Li Sanzhong,Yu Shan,Zhao Shujuan,et al.Tectonic transition and plate reconstructions of the East Asian continental margin[J].Marine Geology and Quaternary Geology,2013,33(3):65-94.
[65] 王家豪,刘丽华,陈胜红,等.珠江口盆地恩平凹陷珠琼运动二幕的构造-沉积响应及区域构造意义[J].石油学报,2011,32(4):588-595. Wang Jiahao,Liu Lihua,Chen Shenghong,et al.Tectonic-sedimentary responses to the second episode of the Zhu-Qiong movement in the Enping Depression,Pearl River Mouth Basin and its regional tectonic significance[J].Acta Petrolei Sinica,2011,32(4):588-595.
[66] 漆家福,吴景富,马兵山,等.南海北部珠江口盆地中段伸展构造模型及其动力学[J].地学前缘,2019,26(2):203-221. Qi Jiafu,Wu Jingfu,Ma Bingshan,et al.The structural model and dynamics concerning middle section,Pearl River Mouth Basin in north margin of South China Sea[J].Earth Science Frontiers,2019,26(2):203-221.
[67] 任建业,庞雄,雷超,等.被动陆缘洋陆转换带和岩石圈伸展破裂过程分析及其对南海陆缘深水盆地研究的启示[J].地学前缘,2015,22(1):102-114. Ren Jianye,Pang Xiong,Lei Chao,et al.Ocean and continent transition in passive continental margins and analysis of lithospheric extension and breakup process:Implication for research of the deepwater basins in the continental margins of South China Sea[J].Earth Science Frontiers,2015,22(1):102-114.

珠江口盆地西江主洼低角度边界正断层特征及成因演化

Characteristics and genetic development of a low-angle boundary normal fault in Xijiang Main Sag,Pearl River Mouth Basin,China

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

[1]	宫越, 林畅松, 何敏, 张忠涛, 张博, 舒梁峰, 冯轩, 洪芳浩. 中国南海北部珠江口盆地早渐新世末破裂不整合特征及其地质意义[J]. 石油与天然气地质, 2019, 40(4): 851-863.
[2]	姜静, 张忠涛, 李浩, 罗祎, 田洪训, 刘汉尧. 珠江口盆地东北陆架边缘斜坡带晚中新世—第四纪层序模式与单向迁移水道[J]. 石油与天然气地质, 2019, 40(4): 864-874.
[3]	张曼莉, 林畅松, 何敏, 张忠涛, 李浩. 珠江口盆地晚渐新世陆架边缘三角洲沉积层序结构及演化[J]. 石油与天然气地质, 2019, 40(4): 875-885.
[4]	李美俊, 张忠涛, 陈聪, 杨程宇, 卢晓林, 付健, 代金慧, 唐友军. 珠江口盆地白云凹陷储层沥青成因及其对油藏调整改造的启示[J]. 石油与天然气地质, 2019, 40(1): 133-141.
[5]	杨璐, 王英民, 何敏, 陈维涛, 徐少华, 卓海腾, 王星星, 李文静. 珠江口盆地白云凹陷13.8 Ma前后深水扇差异沉积过程及主控因素[J]. 石油与天然气地质, 2018, 39(4): 791-800.
[6]	徐少华, 何敏, 庞雄, 陈维涛, 王英民, 卓海腾, 秦春雨. 被动陆缘层序地层结构的侧向变化及其启示——以珠江口盆地中中新世13.8 Ma为例[J]. 石油与天然气地质, 2018, 39(4): 811-822.
[7]	焦鹏, 郭建华, 王玺凯, 刘辰生, 郭祥伟. 珠江口盆地韩江-陆丰凹陷珠江组下段碎屑锆石来源与储层物源示踪[J]. 石油与天然气地质, 2018, 39(2): 239-253.
[8]	赵钊, 汤良杰, 赵志刚, 杨海长, 杨东升, 黄萱. 南海北部珠二坳陷超深水区断层系统分析中的高精度相干技术[J]. 石油与天然气地质, 2018, 39(1): 165-174.
[9]	汪旭东, 张向涛, 何敏, 张素芳, 余一欣, 吴陈冰洁. 珠江口盆地陆丰凹陷南部文昌组储层发育特征及其控制因素[J]. 石油与天然气地质, 2017, 38(6): 1147-1155.
[10]	万琼华, 刘伟新, 罗伟, 王秀玲, 陈晨, 衡立群, 曹珮. 珠江口盆地陆丰凹陷A油田储层质量差异及低渗储层主控因素[J]. 石油与天然气地质, 2017, 38(3): 551-560.
[11]	刘志峰, 吴克强, 柯岭, 王升兰, 于开平, 朱文奇. 珠江口盆地珠一坳陷北部洼陷带油气成藏主控因素[J]. 石油与天然气地质, 2017, 38(3): 561-569.
[12]	江宁, 何敏, 刘军, 薛怀艳, 郑金云, 张青林. 珠江口盆地靖海凹陷多边形断层系统成因及油气成藏意义[J]. 石油与天然气地质, 2017, 38(2): 363-370.
[13]	胡阳, 吴智平, 钟志洪, 张江涛, 于伟高, 王光增, 刘一鸣, 王守业. 珠江口盆地珠一坳陷始新世中-晚期构造变革特征及成因[J]. 石油与天然气地质, 2016, 37(5): 779-785.
[14]	易雪斐, 张昌民, 李少华, 杜家元, 罗明, 李向阳. 珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比[J]. 石油与天然气地质, 2014, 35(5): 670-678.
[15]	丁琳, 张昌民, 杜家元, 施和生, 罗明, 王湘蜀, 贾培蒙. 珠江口盆地惠州凹陷珠江组K系列陆架砂脊沉积演化与成因[J]. 石油与天然气地质, 2014, 35(3): 379-385.