|本期目录/Table of Contents|

[1]赵晓明 葛家旺 谭程鹏 张文彪 陆文明.深海水道储层构型及其对同沉积构造响应机理的研究现状与展望[J].中国海上油气,2019,31(05):76-87.[doi:10.11935/j.issn.1673-1506.2019.05.010 ]
 ZHAO Xiaoming,GE Jiawang,TAN Chengpeng,et al.Research status and prospect of deep sea channel reservoir architecture and its response mechanism to synsedimentary structure[J].China Offshore Oil and Gas,2019,31(05):76-87.[doi:10.11935/j.issn.1673-1506.2019.05.010 ]
点击复制

深海水道储层构型及其对同沉积构造响应机理的研究现状与展望()

《中国海上油气》[ISSN:1673-1506/CN:11-5339/TE]

卷:
第31卷
期数:
2019年05期
页码:
76-87
栏目:
深海油气田开发成果专辑(特邀主编胡光义)
出版日期:
2019-10-10

文章信息/Info

Title:
Research status and prospect of deep sea channel reservoir architecture and its response mechanism to synsedimentary structure
文章编号:
1673-1506(2019)05-0088-19
作者:
赵晓明12 葛家旺12 谭程鹏12 张文彪3 陆文明3
(1. 天然气地质四川省重点实验室 四川成都 610500; 2. 西南石油大学地球科学与技术学院 四川成都 610500; 3. 中国石化石油勘探开发研究院 北京 100083)
Author(s):
ZHAO Xiaoming1 2 GE Jiawang1 2 TAN Chengpeng1 2 ZHANG Wenbiao3 LU Wenming3
(1. Key Laboratory of Natural Gas Geology of Sichuan Province, Chengdu, Sichuan 610500, China; 2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500,China; 3. Sinopec Exploration & Production Research Institute, Beijing 100083, China)
关键词:
深海水道 储层构型 同沉积构造 流动路径 构型样式 响应机理 研究进展 研究展望
Keywords:
deep sea channel reservoir architecture synsedimentary structure flow path architecture style response mechanism research progress research prospect
分类号:
P618.13
DOI:
10.11935/j.issn.1673-1506.2019.05.010
文献标志码:
A
摘要:
近期研究表明,深海水道沉积构型对同沉积构造的响应机制研究已成为当前地质学领域关注的热点问题。同沉积断层生长/褶皱及盐岩(泥岩)塑性活动对深海水道的流动路径、侵蚀能力、几何形态及储层构型样式均具有重要的控制作用。与同沉积构造有关的水道是深海油气藏勘探的主要目标,其内部储层结构复杂多变、非均质性强,这大大增加了该类油气藏的开发难度,弄清深海水道储层构型对同沉积构造的响应机理是解决开发问题的关键理论基础,而当前相关研究十分薄弱。本文以深海水道储层构型及其对同沉积构造的响应机理为主线,结合笔者十年来从事深海油气田开发地质研究的认识,系统梳理了全球水道体系、复合水道和单一水道储层构型研究现状,重点探讨了水道流动路径、叠置样式和内部充填物对同沉积构造响应机理的研究进展,认为深海水道流动路径、构型样式和内部储集相对同沉积构造的响应机理,是今后深海水道储层构型控制机理的重点理论研究方向之一。
Abstract:
Recent studies show that the response mechanism of deep sea channel architecture to the synsedimentary structure has become a hot study topic in the field of geology. The synsedimentary fault growth/fold and salt(mudstone/magma)diapirism control the flow path, erosional capacity, geometry and reservoir architecture of deep sea channels. The channel related to the synsedimentary structure is the main target of deep sea oil and gas reservoir exploration. However, the complexity and high heterogeneity of these deep sea channel reservoirs pose a great difficulty in developing and producing such reservoirs. Therefore, a better understanding of the response mechanism of the deep sea channel reservoir architecture to the synsedimentary structure is the key theoretical basis to promote the oil and gas development. However, few literatures in this field are published. Taking the deep sea channel reservoir architecture and its response mechanism to the synsedimentary structure as the main line, this paper, based on author's understanding from ten years of experience in geology study for deep sea oil and gas field development, systematically summarizes the research status of reservoir architectures of the global channel system, channel complex and single channel, and discusses the research progress on the response mechanism of the flow path, superimposed style and internal fillings of the channel to the synsedimentary structure. It is believed that the response mechanism of the deep sea channel flow path, architecture style and internal reservoir facies to the synsedimentary structure would be one of key theoretical research areas relating to the control mechanism of deep sea channel reservoir architecture in the future.

参考文献/References:

[1] POSAMENTIER H W,KOLLA V. Seismic geomorphology and stratigraphy of depositional elements in deep-water settings[J].Journal of Sedimentary Research.2003,73(3):367-388. [2] 卢景美,张金川,严杰,等.墨西哥湾北部深水区Wilcox沉积特征及沉积模式研究[J].沉积学报,2014,32(6):1132-1139. LU Jingmei,ZHANG Jinchuan,YAN Jie,et al.Study on depositional characteristics and model of Wilcox in the deep waters of northern gulf of Mexico[J].Acta Sedimentologica Sinica,2014,32(6):1132-1139. [3] GEE M J R,GAWTHORPE R L.Submarine channels controlled by salt tectonics:Examples from 3D seismic data offshore Angola[J].Marine and Petroleum Geology,2006,23(4):443-458. [4] HEINIÖ P,DAVIES R J.Knickpoint migration in submarine channels in response to fold growth,western Niger Delta[J].Marine and Petroleum Geology,2007,24(6-9):434-449. [5] 韩文明,邓运华,于水,等.尼日尔三角洲深水勘探研究面临的挑战及其对策[J].地质学报,2012,86(4):671-678. HAN Wenming,DENG Yunhua,YU Shui,et al.Challenges faced with deep water exploration and research in Niger Delta and its strategies[J].Acta Geologica Sinica,2012,86(4):671-678. [6] 蔡露露,王雅宁,王颖,等.西非深水沉积类型特征及油气勘探意义[J].石油学报,2016,37(增刊1):131-142. CAI Lulu,WANG Yaning,WANG Ying,et al.Type feature and hydrocarbon exploration significance of deepwater sedimentary in West Africa[J].Acta Petrolei Sinica,2016,37(S1):131-142. [7] RAGAGNIN G M,MORAES M A S.Seismic geomorphology and connectivity of deep-water reservoirs[J].SPE Reservoir Evaluation & Engineering,2018,11(4):686-695. [8] 康洪全,孟金落,程涛,等.巴西坎波斯盆地深水沉积体系特征[J].石油勘探与开发,2018,45(2):93-104. KANG Hongquan,MENG Jinluo,CHENG Tao,et al.Characteristics of deep-water depositional system in Campos basin,Brazil[J].Petroleum Exploration and Development,2018,45(2):93-104. [9] DMITRIEVA E,JACKSON C A L,HUUSE M,et al.Paleocene deep-water depositional systems in the North Sea Basin:a 3D seismic and well data case study,offshore Norway[J].Petroleum Geoscience,2012,18(1):97-114. [10] SAMUEL A,KNELLER B,RASLAN S,et al.Prolific deep-marine slope channels of the Nile Delta,Egypt[J].AAPG Bulletin,2003,87(4):541-560. [11] 陈宇航,姚根顺,吕福亮,等.东非鲁伍马盆地深水区构造-沉积演化过程及油气地质特征[J].海相油气地质,2016,21(2):39-46. CHEN Yuhang,YAO Genshun,LÜ Fuliang,et al.Tectonic-sedimentary evolution and petroleum geology characteristics in deepwater area in Rovuma basin,East Africa[J].Marine Origin Petroleum Geology,2016,21(2):39-46. [12] CASTELINO J A,REICHERT C,JOKAT W.Response of Cenozoic turbidite system to tectonic activity and sea-level change off the Zambezi Delta[J].Marine Geophysical Research,2017,38(3):1-18. [13] RACEY A,RIDD M F.Chapter 1 introduction to the petroleum geology of Myanmar[J].Geological Society London Memoirs,2015,45(1):1-6. [14] 秦雁群,张光亚,计智峰,等.印度东部盆地群地质特征、油气成藏与深水区勘探潜力[J].石油勘探与开发,2017,44(5):691-703. QIN Yanqun,ZHANG Guangya,JI Zhifeng,et al.Geological features,hydrocarbon accumulation and deep water potential of East Indian basins[J].Petroleum Exploration and Development,2017,44(5):691-703. [15] 胡文瑞,鲍敬伟,胡滨.全球油气勘探进展与趋势[J].石油勘探与开发,2013,40(4):409-413. HU Wenrui,BAO Jingwei,HU Bin.Trend and progress in global oil and gas exploration[J].Petroleum Exploration and Development,2013,40(4):409-413. [16] 朱伟林.南海北部深水区油气地质特征[J].石油学报,2010,31(4):521-527. ZHU Weilin.Petroleum geology in deepwater area of northern continental margin in South China Sea[J].Acta Petrolei Sinica,2010,31(4):521-527. [17] 张迎朝,徐新德,甘军,等.琼东南盆地深水大气田地质特征、成藏模式及勘探方向研究[J].地质学报,2017,91(7):1620-1633. ZHANG Yingzhao,XU Xinde,GAN Jun,et al.Study on the geological characteristic, accumulation model and exploration direction of giant deepwater gas field in the Qiongdongnan basin[J].Acta Geologica Sinica,2017,91(7):1620-1633. [18] 张强,吕福亮,贺晓苏,等.南海近5年油气勘探进展与启示[J].中国石油勘探,2018,23(1):54-61. ZHANG Qiang,LÜ Fuliang,HE Xiaosu,et al.Progress and enlightenment of oil and gas exploration in the South China Sea in recent five years[J].China Petroleum Exploration,2018,23(1):54-61. [19] KHRIPOUNOFF A,VANGRIESHEIM A,BABONNEAU N,et al.Direct observation of intense turbidity current activity in the Zaire submarine valley at 4 000 m water depth[J].Marine Geology,2003,194(3-4):151-158. [20] 吴时国,秦蕴珊.南海北部陆坡深水沉积体系研究[J].沉积学报,2009,27(5):922-930. WU Shiguo,QIN Yunshan.The research of deepwater depositional system in the Northern South China Sea[J].Acta Sedimentologica Sinica,2009,27(5):922-930. [21] MAYALL M,JONES E,CASEY M.Turbidite channel reservoirs:Key elements in facies prediction and effective development[J].Marine and Petroleum Geology,2006,23(8):821-841. [22] WEIMER P,SLATT R M,BOUROULLEC R,et al.Introduction to the petroleum geology of deepwater setting[M].Tulsa,OK USA:AAPG/Datapages,2017. [23] 赵晓明,吴胜和,刘丽.尼日尔三角洲盆地Akpo油田新近系深水浊积水道储层构型表征[J].石油学报,2012,33(6):1049-1058. ZHAO Xiaoming,WU Shenghe,LIU Li.Characterization of reservoir architecture for Neogene deepwater turbidity channels of Akpo oilfield,Niger Delta Basin[J].Acta Petrolei Sinica,2012,33(6):1049-1058. [24] 陈亮,庞雄,刘军,等.珠江口盆地白云凹陷深水重力流优质砂岩储集层特征及识别方法[J].石油勘探与开发,2015,42(4):463-471. CHEN Liang,PANG Xiong,LIU Jun,et al.Characteristics and identification of high quality deep-water gravity flow sandstone reservoirs in Baiyun sag,Pearl River Mouth Basin,South China Sea[J].Petroleum Exploration and Development,2015,42(4):463-471. [25] ZHANG J J,WU S H,FAN T E,et al.Research on the architecture of submarine-fan lobes in the Niger Delta Basin,offshore West Africa[J].Journal of Palaeogeography,2016,5(3):185-204. [26] 张文彪,段太忠,刘志强,等.深水浊积水道沉积构型模式及沉积演化:以西非M油田为例[J].地球科学—中国地质大学学报,2017,42(2):273-285. ZHANG Wenbiao,DUAN Taizhong,LIU Zhiqiang,et al.Architecture model and sedimentary evolution of deepwater turbidity channel:A case study of M oilfield in West Africa[J].Earth Science—Jounal of China University of Geosciences,2017,42(2):273-285. [27] OLUBOYO A P,GAWTHORPE R L,BAKKE K,et al.Salt tectonic controls on deep-water turbidite depositional systems:Miocene,southwestern Lower Congo Basin,offshore Angola[J].Basin Research,2014,26(4):597-620. [28] ZUCKER E,GVIRTZMAN Z,STEINBERG J,et al.Diversion and morphology of submarine channels in response to regional slopes and localized salt tectonics,Levant Basin[J].Marine and Petroleum Geology,2017,81:98-111. [29] WOOD L J,MIZE-SPANSKY K L.Quantitative seismic geomorphology of a Quaternary leveed-channel system,offshore eastern Trinidad and Tobago,northeastern South America[J].AAPG Bulletin,2009,93(1):101-125. [30] PETTINGILL H S,WEIMER P.Worlwide deepwater exploration and production:Past,present,and future[J].Leading Edge,2012,21(4):371-376. [31] ALPAK F O,BARTON M D,NARUK S J.The impact of fine-scale turbidite channel architecture on deep-water reservoir performance[J].AAPG Bulletin,2013,97(2):251-284. [32] LIU L,ZHANG T S,ZHAO X M,et al.Sedimentary architecture models of deepwater turbidite channel systems in the Niger Delta continental slope,West Africa[J].Petroleum Science,2013,10(2):139-148. [33] LABOURDETTE R,BEZ M.Element migration in turbidite systems:Random or systematic depositional processes?[J].AAPG Bulletin,2010,94(3):345-368. [34] 赵晓明,吴胜和,刘丽.西非陆坡区深水复合水道沉积构型模式[J].中国石油大学学报(自然科学版),2012,36(6):1-5,12. ZHAO Xiaoming,WU Shenghe,LIU Li.Sedimentary architecture model of deep-water channel complexes in slope area of West Africa[J].Journal of China University of Petroleum,2012,36(6):1-5,12. [35] PEAKALL J,MCCAFFREY B,KNELLER B.A process model for the evolution,morphology,and architecture of sinuous submarine channels[J].Journal of Sedimentary Research,2000,70(3):434-448. [36] KNELLER B.The influence of flow parameters on turbidite slope channel architecture[J].Marine and Petroleum Geology,2003,20(6-8):901-910. [37] PIRMEZ C,IMRAN J.Reconstruction of turbidity currents in Amazon Channel[J].Marine and Petroleum Geology,2003,20(6-8):823-849. [38] WYNN R B,CRONIN B T,PEAKALL J.Sinuous deep-water channels:Genesis,geometry and architecture[J].Marine and Petroleum Geology,2007,24(6-9):341-387. [39] 李磊,王英民,张莲美,等.南海北部白云深水区水道与朵体沉积序列及演化[J].海洋地质与第四纪地质,2009,29(4):71-76. LI Lei,WANG Yingmin,ZHANG Lianmei,et al.Sedimentary sequence and evolution of submarine channel-lobe in Baiyun deepwater area,Northern South China Sea[J].Marine Geology & Quaternary Geology,2009,29(4):71-76. [40] 李云,郑荣才,高博禹,等.深水扇沉积研究现状和展望:以珠江口盆地白云凹陷珠江深水扇系统为例[J].地质论评,2012,56(4):549-560. LI Yun,ZHENG Rongcai,GAO Boyu,et al.Reviews and prospects on submarine fan deposition:A case study of Zhujiang submarine fan system in Baiyun Depression,Pearl River Mouth Basin[J].Geological Review,2012,56(4):549-560. [41] 解习农,陈志宏,孙志鹏,等.南海西北陆缘深水沉积体系内部构成特征[J].地球科学—中国地质大学学报,2012,37(4):627-634. XIE Xinong,CHEN Zhihong,SUN Zhipeng,et al.depositional architecture characteristics of deepwater depositional system on the continental margins of Northwestern South China Sea[J].Earth Science — Journal of China University of Geosciences,2012,37(4):627-634. [42] 李胜利,于兴河,刘玉梅,等.水道加朵体型深水扇形成机制与模式:以白云凹陷荔湾3-1地区珠江组为例[J].地学前缘,2012,19(2):32-40. LI Shengli,YU Xinghe,LIU Yumei,et al.Mechanism and model of a deepwater fan with channels and lobes:A case study of the Zhujiang Formation in Liwan 3-1 area,Baiyun Depression[J].Earth Science Frontiers,2012,19(2):32-40. [43] 陶泽,林畅松,张忠涛,等.珠江口盆地白云凹陷中新统韩江组中上部层序结构及深水重力流沉积[J].古地理学报,2017,19(4):623-634. TAO Ze,LIN Changsong,ZHANG Zhongtao,et al.Sequence architecture and deep water gravity-flow deposits of the middle and upper member of Hanjiang Formation of Miocene in Baiyun sag,Pearl River Mouth Basin[J].Journal of Palaeogeography,2017,19(4):623-634. [44] STOW D A V,HOWELL D G,NELSON C H.Sedimentary,tectonic,and sea-level controls[J].Submarine Fans and Relkated Turbidite Systems,1985:15-22. [45] DAMUTH J E,FLOOD R D,KOWSMANN R O,et al.Anatomy and growth pattern of Amazon deep-sea fan as revealed by long-range side-scan sonar(GLORIA)and high-resolution seismic studies[J].AAPG Bull etin,1988,72(8):885-911. [46] 林畅松,刘景彦,蔡世祥,等.莺-琼盆地大型下切谷和海底重力流体系的沉积构成和发育背景[J].科学通报,2001,46(1):69-72. LIN Changsong,LIU Jingyan,CAI Shixiang,et al.Sedimentary composition and development background of large incised valleys and submarine gravity flow systems in Ying-Qiong basin[J].Chinese Science Bulletin,2001,46(1):69-72. [47] 庞雄,陈长民,施和生,等.相对海平面变化与南海珠江深水扇系统的响应[J].地学前缘,2005,12(3):167-177. PANG Xiong,CHEN Changmin,SHI Hesheng,et al.The response between relative sea level change and the Pearl River deep water fan system in South China Sea[J].Earth Science Frontiers,2005,12(3):167-177. [48] MALLARINO G,BEAUBOUEF R T,DROXLER A W,et al.Sea level influence on the nature and timing of a minibasin sedimentary fill(northwestern slope of the Gulf of Mexico)[J].AAPG Bulletin,2006,90(7):1089-1119. [49] 彭大钧,庞雄,陈长民,等.南海珠江深水扇系统的形成特征与控制因素[J].沉积学报,2006,24(1):12-20. PENG Dajun,PANG Xiong,CHEN Changmin,et al.The characteristics and controlling factors for the formation of deep-water fan system in South China Sea[J].Acta Sedimentologica Sinica,2006,24(1):12-20. [50] 郑荣才,李云,戴朝成,等.白云凹陷珠江组深水扇砂质碎屑流沉积学特征[J].吉林大学学报(地球科学版),2012,42(6):1581-1589. ZHENG Rongcai,LI Yun,DAI Chaocheng,et al.Depositional features of sandy debris flow of submarine fan in Zhujiang Formation,Baiyun sag[J].Journal of Jilin University(Earth Science Edition),2012,42(6):1581-1589. [51] 李磊,王英民,徐强,等.南海北部陆坡地震地貌及深水重力流沉积过程主控因素[J].中国科学:地球科学,2012,42(10):1533-1543. LI Lei,WANG Yingmin,XU Qiang,et al.Seismic geomorphology and main controls of deep-water gravity flow sedimentary process on the slope of the northern South China Sea[J].Science China:Earth Sciences,2012,42(10):1533-1543. [52] 王振奇,李士涛,于水,等.尼日尔三角洲盆地深水沉积的二元结构特征及层序划分[J].地质学报,2013,87(8):1149-1157. WANG Zhenqi,LI Shitao,YU Shui,et al.Characters of two-component constitution of deep-water deposit and classification of sequence stratigraphy in the Niger Delta Basin[J].Acta Geologica Sinica,2013,87(8):1149-1157. [53] GAMBERI F,ROVERE M,MARANI M P,et al.Modern submarine canyon feeder-system and deep-sea fan growth in a tectonically active margin(northern Sicily)[J].Geosphere,2015,11(2):307-319. [54] JOBE Z R,SYLVESTER Z,PARKER A O,et al.Rapid adjustment of submarine channel architecture to changes in sediment supply[J].Journal of Sedimentary Research,2015,85(6):729-753. [55] 王大伟,吴时国,王英民,等.琼东南盆地深水重力流沉积旋回[J].科学通报,2015,60(10):933-943. WANG Dawei,WU Shiguo,WANG Yingmin,et al.Deep-water sediment cycles in the Qiongdongnan Basin[J].Chinese Science Bulletin,2015,60(10):933-943. [56] GONG C,STEEL R J,WANG Y,et al.Grain size and transport regime at shelf edge as fundamental controls on delivery of shelf-edge sands to deepwater[J].Earth-Science Reviews,2016(157):32-60. [57] POCHAT S,CASTELLTORT S,CHOBLET G,et al.High-resolution record of tectonic and sedimentary processes in growth strata[J].Marine and Petroleum Geology,2009,26(8):1350-1364. [58] MAYALL M,LONERGAN L,BOWMAN A,et al.The response of turbidite slope channels to growth-induced seabed topography[J].Aapg Bulletin,2010,94(7):1011-1030. [59] BAYLISS N,PICKERING K T.Transition from deep-marine lower-slope erosional channels to proximal basin-floor stacked channel-levée-overbank deposits,and syn-sedimentary growth structures,Middle Eocene Banastón System,Ainsa Basin,Spanish Pyrenees[J].Earth-Science Reviews,2015,144:23-46. [60] JOLLY B A,LONERGAN L,WHITTAKER A C.Growth history of fault-related folds and interaction with seabed channels in the toe-thrust region of the deep-water Niger delta[J].Marine and Petroleum Geology,2016,70:58-76. [61] CLARK I R,CARTWRIGHT J A.Interactions between submarine channel systems and deformation in deepwater fold belts:Examples from the Levant Basin,Eastern Mediterranean sea[J].Marine and Petroleum Geology,2009,26(8):1465-1482. [62] CLARK I R,CARTWRIGHT J A.Key controls on submarine channel development in structurally active settings[J].Marine and Petroleum Geology,2011,28(7):1333-1349. [63] KANE I A,CATTERALL V,MCCAFFREY W D,et al.Submarine channel response to intrabasinal tectonics:The influence of lateral tilt[J].AAPG Bulletin,2010,94(2):189-219. [64] MUTTI E,NORMARK W R.Chapter 1 Comparing examples of modern and ancient turbidite systems:problems and concepts[M].Springer,Dordrecht,1990:1-38. [65] LAMB M A,ANDERSON K,GRAHAM S.Stratigraphic Architecture of a Sand-Rich,Deep-Sea Depositional System[M].Pacific Section AAPG Special Publication,2003. [66] 赵晓明,吴胜和,岳大力,等.深水海底扇储层构型浅析:以西非某油田为例[C]∥王涛.第五届油气成藏机理与油气资源评价国际学术研讨会论文集.北京:石油工业出版社,2010:7. ZHAO Xiaoming,WU Shenghe,YUE Dali,et al.Shallow analysis on reservoir architecture of deep submarine fan:a case study of an oil field in West Africa[C]∥WANG Tao.Proceedings of the 5th International Symposium on Petroleum Accumulation Mechanism and Evaluation of Petroleum Resources.Beijing:Petroleum Industry Press,2010:7. [67] BOUMA A H.Introduction to submarine fans and related turbidite systems[M].New York:Springer New York,1985:3-5. [68] RICHARDS M.Turbidite systems in deep-water basin margins classified by grain size and feeder system[J].AAPG Bulletin,1994,78(5):792-822. [69] 蒋恕,王华,WEIMER P.深水沉积层序特点及构成要素[J].地球科学—中国地质大学学报,2008,33(6):825-833. JIANG Shu,WANG Hua,Weimer PAUL.Sequence stratigraphy characteristics and sedimentary elements in deepwater[J].Earth Science—Journal of China University of Geosciences,2008,33(6):825-833. [70] 王振峰.深水重要油气储层——琼东南盆地中央峡谷体系[J].沉积学报,2012,30(4):646-653. WNAG Zhenfeng.Important deepwater hydrocarbon reservoirs:The central canyon system in the Qiongdongnan Basin[J].Acta Sedimentologica Sinica,2012,30(4):646-653. [71] 苏明,张成,解习农,等.深水峡谷体系控制因素分析:以南海北部琼东南盆地中央峡谷体系为例[J].中国科学:地球科学,2014,44(8):1807-1820. SU Ming,ZHANG Cheng,XIE Xinong,et al.Controlling factors on the submarine canyon system:a case study of the Central Canyon System in the Qiongdongnau Basin,northern South China Sea[J].Science China:Earth Sciences,2014,44(8):1807-1820. [72] 王琳霖,王振奇,肖鹏.下刚果盆地A区块中新统深水沉积体系特征[J].石油与天然气地质,2015,36(6):963-974. WANG Linlin,WANG Zhenqi,XIAO Peng.Characterization of deep water sedimentary system in the Miocene of Block A in Lower Congo Basin[J].Oil & Gas Geology,2015,36(6):963-974. [73] 廖计华,徐强,陈莹,等.白云-荔湾凹陷珠江组大型深水水道体系沉积特征及成因机制[J].地球科学—中国地质大学学报,2016,41(6):1041-1054. LIAO Jihua,XU Qiang,CHEN Ying,et al.Sedimentary characteristics and genesis of the deepwater channel system in Zhujiang Formation of Baiyun-Liwan Sag[J].Earth Sciences—Journal of China University of Geosciences,2016,41(6):1041-1054. [74] 蔡露露,刘春成,吕明,等.西非下刚果盆地深水水道发育特征及沉积储层预测[J].中国海上油气,2016,28(2):60-70.DOI:10.11935/j.issn.1673-1506.2016.02.007. CAI Lulu,LIU Chuncheng,LYU Ming,et al.the development characteristic of deep water channel and sedimentary reservoir prediction in Lower Congo basin,West Africa[J].China of Offshore Oil And Gas,2016,28(2):60-70.DOI:10.11935/j.issn.1673-1506.2016.02.007. [75] 刘宝珺,余光明,徐强,等.雅鲁藏布中新生代深水沉积盆地形成和演化(Ⅰ):喜马拉雅造山带沉积特征及演化[J].沉积与特提斯地质,1993,13(1):32-49. LIU Baojun,YU Guangming,XU Qiang,et al.Formation and evolution of the Mesozoic and Cenozoic deep-water sedimentary basins along the Yalung Zangbo River(I):sedimentary characteristics and evolution of the Himaiayan orogenic zone[J].Lithofacies Paleogeography,1993,13(1):32-49. [76] NORMARK W R,PIPER D J W,HISCOTT R N.Sea level controls on the textural characteristics and depositional architecture of the Hueneme and associated submarine fan systems,Santa Monica Basin,California[J].Sedimentology,1998,45(1):53-70. [77] FUGELLI E M G,OLSEN T R.Screening for deep-marine reservoirs in frontier basins:Part 1—Examples from offshore mid-Norway[J].AAPG Bulletin,2005,89(7):853-882. [78] RUIG M J D,HUBBARD S M.Seismic facies and reservoir characteristics of a deep-marine channel belt in the Molasse foreland basin,Puchkirchen Formation,Austria[J].AAPG Bulletin,2006,90(5):735-752. [79] PICKERING K T,CORREGIDOR J,CLARK J D.Architecture and stacking patterns of lower-slope and proximal basin-floor channelised submarine fans,Middle Eocene Ainsa System,Spanish Pyrenees:An integrated outcrop-subsurface study[J].Earth-Science Reviews,2015,144:47-81. [80] PEAKALL J,KANE I A,MASSON D G,et al.Global(latitudinal)variation in submarine channel sinuosity[J].Geology,2011,40(1):11-14. [81] PICOT M,DROZ L,MARSSET T,et al.Controls on turbidite sedimentation:Insights from a quantitative approach of submarine channel and lobe architecture(Late Quaternary Congo Fan)[J].Marine and Petroleum Geology,2016,72:423-446. [82] 赵晓明,刘丽,谭程鹏,等.海底水道体系沉积构型样式及控制因素:以尼日尔三角洲盆地陆坡区为例[J].古地理学报,2018,20(5):825-840. ZHAO Xiaoming,LIU Li,TAN Chengpeng,et al.Styles of submarine-channel architecture and its controlling factors:A case study from the Niger Delta Basin slope[J].Journal of Palaeogeography(Chinese Edition),2018,20(5):825-840. [83] DEPTUCK M E,STEFFENS G S,BARTON M,et al.Architecture and evolution of upper fan channel-belts on the Niger Delta slope and in the Arabian Sea[J].Marine and Petroleum Geology,2003,20(6-8):649-676. [84] 刘新颖,于水,胡孝林,等.深水水道坡度与曲率的定量关系及控制作用:以西非Rio Muni盆地为例[J].吉林大学学报(地球科学版),2012,42(增刊1):127-134. LIU Xinying,YU Shui,HU Xiaolin,et al.Quantitative relation between the gradient and sinuosity of deepwater channel and its control:a case study in the Rio Muni Basin,West Africa[J].Journal of Jilin University(Earth Science Edition),2012,42(S1):127-134. [85] 张文彪,段太忠,张旭彪,等.安哥拉深水沉积贯入砂岩的识别特征及成因模式[J].地质科技情报,2017,36(2):97-104. ZHANG Wenbiao,DUAN Taizhou,ZHANG Xubiao,et al.Deep-water sedimentary sandstone injectite identification and its genetic model in Angola[J].Geological Science and Technology Information,2017,36(2):97-104. [86] KANE I A,MCGEE D T,JOBE Z R.Halokinetic effects on submarine channel equilibrium profiles and implications for facies architecture:conceptual model illustrated with a case study from Magnolia Field,Gulf of Mexico[J].Geological Society London,Special Publications,2012,363(1):289-302. [87] VAN der MERWE W C,HODGSON D M,BRUNT R L,et al.Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2 500 km2 area[J].Geosphere,2014,10(6):1076-1093. [88] DEPTUCK M E,SYLVESTER Z,PIRMEZ C,et al.Migration-aggradation history and 3-D seismic geomorphology of submarine channels in the Pleistocene Benin-major Canyon,western Niger Delta slope[J].Marine and Petroleum Geology,2007,24(6-9):406-433. [89] BABONNEAU N,SAVOYE B,CREMER M,et al.Sedimentary architecture in meanders of a submarine channel:detailed study of the present Congo turbidite channel(Zaiango Project)[J].Journal of Sedimentary Research,2010,80(10):852-866. [90] 袁圣强,曹锋,吴时国,等.南海北部陆坡深水曲流水道的识别及成因[J].沉积学报,2010,28(1):68-75. YUAN Shengqiang,CAO Feng,WU Shiguo,et al.Architecture and origin of deepwater sinuous channel on the slope of Northern South China Sea[J].Acta Sedimentologica Sinica,2010,28(1):68-75. [91] 李华,何幼斌,王振奇.深水高弯度水道—堤岸沉积体系形态及特征[J].古地理学报,2011,13(2):139-149. LI Hua,HE Youbin,WANG Zhenqi.Morphology and characteristics of deep water high sinuous channel-levee system[J].Journal of Palaeogeography,2011,13(2):139-149. [92] 李磊,邵子玮,都鹏燕,等.穆尼盆地第四纪深水弯曲水道:沉积构型、成因及沉积过程[J].现代地质,2012,26(2):349-354. LI Lei,SHAO Ziwei,DU Pengyan,et al.Quaternary sinuous submarine channel in Muni Basin:architecture,genesis and process[J].Geoscience,2012,26(2):349-354. [93] ZHAO X M,QI K,LIU L,et al.Quantitative characterization and controlling factor analysis of the morphology of bukuma-minor channel on southern Niger Delta slope[J].Interpretation,2018,6:57-69. [94] KOLLA V,BOURGES P,URRUTY J M,et al.Evolution of deep-water Tertiary sinuous channels offshore Angola(west Africa)and implications for reservoir architecture[J].AAPG Bulletin,2001,85(8):1373-1405. [95] LABOURDETTE R.Integrated three-dimensional modeling approach of stacked turbidite channels[J].AAPG Bulletin,2007,91(11):1603-1618. [96] FUNK J E,SLATT R M,PYLES D R.Quantification of static connectivity between deep-water channels and stratigraphically adjacent architectural elements using outcrop analogs[J].AAPG Bulletin,2012,96(2):277-300. [97] 李华,王英民,徐强,等.深水单向迁移水道-堤岸沉积体系特征及形成过程[J].现代地质,2013,27(3):653-661. LI Hua,WANG Yingmin,XU Qiang,et al.Characteristics and processes of deep water unidirectionally-migrating channel-levee system[J].Geoscience,2013,27(3):653-661. [98] GONG C,WANG Y,STEEL R J,et al.Flow processes and sedimentation in unidirectionally migrating deep-water channels:From a three-dimensional seismic perspective[J].Sedimentology,2016,63(3):645-661. [99] ADEOGBA A A,MCHARGUE T R,GRAHAM S A.Transient fan architecture and depositional controls from near-surface 3-D seismic data,Niger Delta continental slope[J].AAPG Bulletin,2005,89(5):627-643. [100] HAUGHTON P D W.Evolving turbidite systems on a deforming basin floor,Tabernas,SE Spain[J].Sedimentology,2000,47(3):497-518. [101] PRATHER B E.Controls on reservoir distribution,architecture and stratigraphic trapping in slope settings[J].Marine and Petroleum Geology,2003,20(6):529-545. [102] HODGSON D M,HAUGHTON P D W.Impact of syndepositional faulting on gravity current behaviour and deep-water stratigraphy:Tabernas-Sorbas Basin,SE Spain[J].Geological Society London Special Publications,2004,222(1):135-158. [103] 刘睿,周江羽,张莉,等.南海西北次海盆深水扇系统沉积演化特征[J].沉积学报,2013,31(4):706-717. LIU Rui,ZHOU Jiangyu,ZHANG Li,et al.Depositional architecture and evolution of deepwater fan system in the northwestern sub-basin,South China Sea[J].Acta Sedimentologica Sinica,2013,31(4):706-717. [104] ZHAO X M,QI K,LIU L,et al.Development of a partially-avulsed submarine channel on the Niger Delta continental slope:architecture and controlling factors[J].Marine & Petroleum Geology,2018,95:30-49. [105] ZHAO X M,QI K,MARCO P,et al.Submarine channel network evolution above an extensive mass-transport complex:A 3D seismic case study from the Niger delta continental slope[J].Marine and Petroleum Geology,2019,104:231-248. [106] SMITH R.Silled sub-basins to connected tortuous corridors:sediment distribution systems on topographically complex sub-aqueous slopes[J].Confined Turbidite Systems,2004,222:23-43. [107] CRONIN B T.Structurally-controlled deep sea channel courses:examples from the Miocene of southeast Spain and the Alboran Sea,southwest Mediterranean[J].Geological Society London Special Publications,1995,94(1):115-135. [108] MORGAN R.Structural controls on the positioning of submarine channels on the lower slopes of the Niger delta[J].Geological Society London Memoirs,2004,29(1):45-52. [109] CROSS N E,CUNNINGHAM A,COOK R J,et al.Three-dimensional seismic geomorphology of a deep-water slope-channel system:The Sequoia field,offshore west Nile Delta,Egypt[J].AAPG Bulletin,2009,93(8):1063-1086. [110] MAYALL M,STEWART I.The architecture of turbidite slope channels[C]∥WEIMER P,SLATT R M,COLEMAN J L,et al,Deep-water reservoirs of the world.Gulf Coast section SEPM foundation 20th annual bob F Perkins research conference.Houston,Texas:2000, [111] SOREGHAN M J,SCHOLZ C A,WELLS J T.Coarse-grained,deep-water sedimentation along a border fault margin of Lake Malawi,Africa; seismic stratigraphic analysis[J].Journal of Sedimentary Research,1999,69(4):832-846. [112] BROUCKE O,TEMPLE F,ROUBY D,et al.The role of deformation processes on the geometry of mud-dominated turbiditic systems,Oligocene and Lower-Middle Miocene of the Lower Congo basin(West African Margin)[J].Marine & Petroleum Geology,2004,21(3):327-348. [113] SHULTZ M R.Sedimentology,stratigraphic architecture,and ichnology of gravity-flow deposits partially ponded in a growth-fault-controlled slope minibasin,Tres Pasos Formation(Cretaceous),Southern Chile[J].Journal of Sedimentary Research,2005,75(3):440-453. [114] MICALLEF A,MOUNTJOY J J,BARNES P M,et al.Geomorphic response of submarine canyons to tectonic activity:Insights from the Cook Strait canyon system,New Zealand.Geosphere,2014,10(5):905-929. [115] GROSS F,KLEIN E,URLAUB M,et al.Patterns of seafloor morphology as a response to tectonic- and sedimentary processes south of the Messina Strait,Italy[C]∥EGU General Assembly,2017. [116] PRATHER B E,BOOTH J R,STEFFENS G S,et al.Classification,lithologic calibration,and stratigraphic succession of seismic facies of intraslope basins,deep-water Gulf of Mexico[J].AAPG Bulletin,1998,82(5):701-728. [117] BEAUBOUEF R,FRIEDMANN S.High resolution seismic/sequence stratigraphic framework for the evolution of Pleistocene intra slope basins,western Gulf of Mexico:depositional models and reservoir analogs[C]∥Deep-water reservoirs of the world:Gulf Coast Section SEPM 20th Annual Research Conference.SEPM,2000:40-60. [118] ANDERSON J E,CARTWRIGHT J,DRYSDALL S J,et al.Controls on turbidite sand deposition during gravity-driven extension of a passive margin:Examples from Miocene sediments in Block 4,Angola[J].Marine and Petroleum Geology,2000,17(10):1165-1203. [119] 赵晓明,吴胜和,岳大力,等.西非某油田深水海底扇岩石相类型及其识别方法研究[J].测井技术,2010,34(5):505-510. ZHAO Xiaoming,WU Shenghe,YUE Dali.Research on litho facies types and identification method of deep-water submarine fan taking one oilfield of West African as a case[J].Well Logging Technology,2010,34(5):505-510. [120] 李云,郑荣才,朱国金,等.珠江口盆地白云凹陷中新统珠江组深水灰岩沉积-成岩作用特征[J].地学前缘,2014,21(2):301-311. LI Yun,ZHENG Rongcai,ZHU Guojin,et al.Deposition and diagenesis of the Miocene deep-water limestones of Zhujiang Formation in Baiyun sag,Pearl River Mouth Basin[J].Earth Science Frontiers,2014,33(2):301-311. [121] 赵鹏飞,李丹,杨香华,等.尼日尔三角洲前缘重力流水道砂体的沉积构成特征[J].地质科技情报,2014,21(2):28-37. ZHAO Pengfei,LI Dan,YANG Xianghua,et al.sedimentary architecture characteristic of the gravity flow channel sandbodies in the Niger Delta front[J].Geological Science and Technology Information,2014,33(2):28-37. [122] ALBERTÃO G A,MULDER T,ESCHARD R.Impact of salt-related palaeo-topography on the distribution of turbidite reservoirs:Evidence from well-seismic analyses and structural restorations in the Brazilian offshore[J].Marine & Petroleum Geology,2011,28(5):1023-1046.

相似文献/References:

[1]段瑞凯 胡光义 宋来明 陈 筱 卜范青 张 旭 王宗俊 陈国宁 李晨曦.深海水道沉积体系精细刻画及表征方法[J].中国海上油气,2019,31(05):113.[doi:10.11935/j.issn.1673-1506.2019.05.012]
 DUAN Ruikai HU Guangyi SONG Laiming CHEN Xiao BU Fanqing ZHANG Xu WANG Zongjun CHEN Guoning LI Chenxi.Fine description and characterization of deep sea channel sedimentation system: Taking the A oil group of M oilfield in the Niger Delta basin of West Africa as an example[J].China Offshore Oil and Gas,2019,31(05):113.[doi:10.11935/j.issn.1673-1506.2019.05.012]

备注/Memo

备注/Memo:
*国家自然科学基金项目“海底水道储层构型对泥岩底辟区同沉积构造的响应机理(编号:41872142)”“泥岩底辟型微盆地中的深海浊积朵叶沉积系列构型模式及控制因素(编号:41602145)”、“十三五”国家科技重大专项“安哥拉深水浊积岩油藏高效开发技术(编号:2016ZX05033-003-005)”部分研究成果。 第一作者简介: 赵晓明,男,副教授,博士生导师,长期从事深水沉积学、油气田开发地质学领域的教学和科研工作。地址:四川省成都市新都大道8号(邮编:610500)。E-mail:zhxim98@163.com。
更新日期/Last Update: 1900-01-01