Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (2): 323-345.doi: 10.13278/j.cnki.jjuese.20170302

Previous Articles     Next Articles

Genesis Classification, Development Mechanism and Sedimentary Model of Deep-Lacustrine Gravity Flow in Fushan Sag of Beibuwan Basin

Li Yuan1,2, Lin Song1, Lin Zhengliang3, Ma Qinglin4   

  1. 1. Key Laboratory of Earthquake Geodesy, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China;
    2. Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China;
    3. Petroleum Geophysical Research Institute, SINOPEC, Nanjing 210014, China;
    4. Southern Petroleum Exploration and Development Co., Ltd., PetroChina, Guangzhou 510240, China
  • Received:2012-11-14 Online:2019-03-26 Published:2019-03-28
  • Supported by:
    Supported by National Natural Science Foundation of China (41472084) and Social Public Welfare Research Project of China Seismological Bureau (IS201626261)

PDF (PC)

442

Abstract: Fushan sag is a Cenozoic faulted lake basin on the slope of Hainan uplift in the southern margin of Beibuwan basin. This paper makes full use of the high-resolution three-dimensional seismic data covering the whole study area. Guided by various theories such as sequence stratigraphy and sedimentology, combined with relevant technologies such as sedimentary petrology and seismic sedimentology,a comprehensive study of the whole study area is carried out. In the period of SQEls2EST+LST of Liushagang Formation in Paleogene, four types of deep-lacustrine gravity flow sedimentary lithofacies were identified in Fushan sag. Through lithofacies assemblage and its transformation characteristics, sand dispersion system and seismic facies analysis, the distribution characteristics of sedimentary system were carefully analyzed, and then the sedimentary model of deep-lacustrine gravity flow in Fushan sag was established. The lake floor fan deposits with typical turbidite channel developed mainly in the western eastern regions. In this area, the distal solitary bodies formed by sandy clastic deposits are dominant. This study not only has direct significance for the study of sedimentary system in Fushan sag, but also provides theoretical support for many continental fault basins with the same background in Southern China.

Key words: deep-lacustrine gravity flow, sandy clastics, turbidite, sub-lacustrine fan, Fushan sag

CLC Number: 

  • P586
[1] 刘丽军,高振中.海南福山凹陷下第三系沉积体系域研究与储集体预测[J].地学前缘,2000,7(4):390. Liu Lijun,Gao Zhenzhong.Study on Lower Tertiary Sedimentary System Tract and Reservoir Prediction in Fushan Depression[J].Earth Science Frontiers,2000,7(4):390.
[2] 刘丽军,佟彦明,纪云龙,等.北部湾盆地福山凹陷流沙港组湖底扇沉积特征及发育背景[J].石油实验地质,2003,25(2):110-115. Liu Lijun,Tong Yanming,Ji Yunlong,et al.Sedimentary Characteristics and Developing Background of the Sublacustrine Fan in the Liushagang Formation of the Fushan Depression,the Beibuwan Basin[J].Experimental Petroleum Geology,2003,25(2):110-115.
[3] 何幼斌,高振中.海南岛福山凹陷古近系流沙港组沉积相[J].古地理学报,2006,8(3):365-376. He Youbin,Gao Zhenzhong.Sedimentary Facies of the Liushagang Formation of Paleogene in Fushan Sag of Hainan Island[J].Journal of Palaeogeography,2006,8(3):365-376.
[4] 鲜本忠,万锦峰,姜在兴,等.断陷湖盆洼陷带重力流沉积特征与模式:以南堡凹陷东部东营组为例[J].地学前缘,2012,19(1):121-135. Xian Benzhong,Wan Jinfeng,Jiang Zaixing,et al.Sedimentary Characteristics and Model of Gravity Flow Deposition in the Depressed Belt of Rift Lacusustrine Basin:A Case Study from Dongying Formation in Nanpu Depression[J].Earth Science Frontiers,2012,19(1):121-135.
[5] Kuenen P H,Migliorini C I.Turbidity Currents as a Cause of Graded Bedding[J].The Journal of Geology,1950,58(2):1-127.
[6] Walker R G.Deep-Water Sandstone Facies and Ancient Submarine Fans:Models for Exploration for Stratigraphic Traps[J].AAPG Bulletin-American Association of Petroleum Geologists,1978,62(8):932-966.
[7] Shanmugam G.50 Years of the Turbidite Paradigm (1950s-1990s):Deep-Water Processes and Facies Models:A Critical Perspective[J].Marine and Petroleum Geology,2000,17(5):285-342.
[8] 柳成志,霍广君,张冬玲.辽河盆地西部凹陷冷家油田沙三段扇三角洲:湖底扇沉积模式[J].大庆石油学院学报,1999,23(1):1-4. Liu Chengzhi,Huo Guangjun,Zhang Dongling.Fan Delta-Sublacustrine Fan Sedimentary Models of S3 Member in Lengjia Oilfield in Liaohe Basin[J].Journal of Daqing Petroleum Institute,1999,23(1):1-4.
[9] 蔺连第,朗艳,金蕙,等.二连盆地乌里雅斯太凹陷早白垩世湖底扇[J].石油勘探与开发,2005,32(3):23-32. Lin Liandi,Lang Yan,Jin Hui,et al.Early Cretaceous Sublacustrine Fan in Wuliyasitai Sag,Erlian Basin[J].Petroleum Exploration and Development,2005,32(3):23-32.
[10] Shanmugam G,Spalding T D,Rofheart D H.Process Sedimentology and Reservoir Quality of Deep-Marine Bottom-Current Reworked Sands (Sandy Contourites):An Example from the Gulf of Mexico[J].AAPG Bulletin-American Association of Petroleum Geologists,1993,77(1):1241-1259.
[11] Shanmugam G.High-Density Turbidity Currents:Are They Sandy Debris Flows?[J].Journal of Sedimentary Research,1996,66(12):2-10.
[12] 罗进雄,何幼斌,高振中,等.海南福山凹陷古近系流沙港组重力流沉积研究[J].海洋石油,2007,27(3):13-21. Luo Jinxiong,He Youbin,Gao Zhenzhong,et al.Gravity Flow Deposits of Paleogene Liushagang Formation in Fushan Sag,Hainan Province[J].Offshore Oil,2007,27(3):13-21.
[13] 李媛,刘菊,马庆林.福山凹陷古近系流一段重力流沉积特征[J].特种油气藏,2010,17(5):30-32. Li Yuan,Liu Ju,Ma Qinglin.Sedimentary Characteristics of Gravity Flows in Paleogene Liu1 Formation of the Fushan Sag[J].Special Oil & Gas Reservoirs,2010,17(5):30-32.
[14] 李媛,王华,刘恩涛,等,北部湾盆地福山凹陷层序地层格架下油气藏分布规律与控制因素[J].中南大学学报(自然科学版),2014,45(5):1542-1554. Li Yuan,Wang Hua,Liu Entao,et al.Distribution Regularities and Control Factors for Reservoir Formation Within Sequence Stratigraphic Framework in Fushan Sag,Beibuwan Basin[J].Journal of Central South University (Science and Technology),2014,45(5):1542-1554.
[15] Hampton M A.Role of Subaqueous Debris Flow in Generating Turbidity Currents[J].Journal of Sedimentary Petrology,1972,42(1):775-793.
[16] Postma G,Nemec W,Kleinspehn K L.Large Floating Clasts in Turbidites:A Mechanism for Their Emplacement[J].Sedimentary Geology,1988,58(13):47-61.
[17] Shanmugam G.The Bouma Sequence and the Turbidite Mind Set[J].Earth-Science Reviews,1997,42(2):201-229.
[18] Shanmugam G.Deep-Marine Tidal Bottom Currents and Their Reworked Sands in Modern and Ancient Submarine Canyons[J].Marine and Petroleum Geology,2003,20(1):471-491.
[19] Shanmugam G,Shrivastava S K,Das B.Sandy Debrites and Tidalites of Pliocene Reservoir Sands in Upper-Slope Canyon Environments,Offshore Krishna-Godavari Basin (India)[J].Journal of Sedimentary Research,2009,79(15):736-756.
[20] Shanmugam G.New Perspectives on Deep-Water Sandstones:Implications[J].Petroleum Exploration and Development,2013,40(3):316-324.
[21] Stow D A V,Johansson M.Deep-Water Massive Sands:Nature,Origin and Hydrocarbon Implications[J].Marine and Petroleum Geology,2000,17(11):145-174.
[22] Stow D A V,Mayall M.Deep-Water Sedimentary Systems:New Models for the 21st Century[J].Marine and Petroleum Geology,2000,17(5):125-135.
[23] 王德坪.湖相内成碎屑流的沉积及形成机理[J].地质学报,1991,65(4):299-317. Wang Deping.The Sedimentation and Formation Mechanism of Lacustrine Endogenic Debris Flow[J].Acta Geological Sinica,1991,65(4):299-317.
[24] 董冬,陈洁,邱明文.河流相储集层中剩余油类型和分布规律[J].地质学报,1999,6(3):39-46. Dong Dong,Chen Jie,Qiu Mingwen.Types and Distribution of Residual Oil in Fluvial Reservoirs[J].Oil and Gas Recovery Technology,1999,6(3):39-46.
[25] 鲜本忠,王永诗,周廷全,等.断陷湖盆陡坡带砂砾岩体分布规律及控制因素:以渤海湾盆地济阳坳陷车镇凹陷为例[J].石油勘探与开发,2007,34(4):429-436. Xian Benzhong,Wang Yongshi,Zhou Tingquan.et al.Distribution and Controlling Factors of Glutinite Bodies in the Actic Region of a Rift Basin:An Example from Chezhen Sag,Bohai Bay Basin[J].Petroleum Exploration and Development,2007,34(4):429-436.
[26] 邹才能,陶士振,袁选俊,等.连续型油气藏形成条件与分布特征[J].石油学报,2009,30(3):324-331. Zou Caineng,Tao Shizhen,Yuan Xuanjun,et al.The Formation Conditions and Distribution Characteristics of Continuous Petroleum Accumulations[J].Acta Petrolei Sinica,2009,30(3):324-331.
[27] 田在艺,王善书.我国海域地质构造与含油气沉积盆地特征[J].石油学报,1985,6(3):1-10. Tian Zaiyi,Wang Shanshu.Geological Structures and Oil and Gas Sedimentary Basins in the China Sea[J].Acta Petrolei Sinica,1985,6(3):1-10.
[28] 杜振川.南海北部湾盆地构造特征及对沉积的控制作用[J].河北煤炭建筑工程学院学报,1997,1(1):55-59. Du Zhenchuan.Structural Features and the Controlling Function of Sedimentary from Tertiary in Beibuwan Basin,the South China Sea[J].Journal of Hebei Mining and Civil Engineering Institute,1997,1(1):55-59.
[29] 胡望水,吴婵,梁建设,等.北部湾盆地构造迁移特征及对油气成藏的影响[J].石油与天然气地质,2011,32(54):920-927. Hu Wangshui,Wu Chan,Liang Jianshe,et al.Tectonic Transport Characteristics and Their Influences on Hydrocarbon Accumulation in Beibuwan Basin[J].Oil & Gas Geology,2011,32(54):920-927.
[30] 赵建章,石彦民,孙维昭,等.海南福山凹陷火成岩分布特征及对油气勘探的影响[J].中国石油勘探,2007,1(1):38-42,93. Zhao Jianzhang,Shi Yanmin,Sun Weizhao,et al.Distribution of Lgneous Rock and Its Effect on Petroleum Exploration in Fushan Sag[J].China Petroleum Exploration,2007,1(1):38-42,93.
[31] 刘恩涛,王华,李媛,等.北部湾盆地福山凹陷构造转换带对层序及沉积体系的控制[J].中国石油大学学报(自然科学版),2013,37(3):17-22,29. Liu Entao,Wang Hua,Li Yuan,et al.Control of Transfer Zone over Sequences and Depositional System in Fushan Sag,Beibuwan Basin[J].Journal of China University of Petroleum (Edition of Natural Science),2013,37(3):17-22,29.
[32] 赵迎冬,王华,甘华军,等.海南福山凹陷盆地形态演化分析[J].中国矿业大学学报,2014,43(6):1078-1086. Zhao Yingdong,Wang Hua,Gan Huajun,et al.Analysis of Basin Morphological Evolution in Fushan Depression,Hainan[J].Journal of China University of Mining & Technology,2014,43(6):1078-1086.
[33] 石彦民,刘菊,张梅珠,等.海南福山凹陷油气勘探实践与认识[J].华南地震,2007,27(3):57-68. Shi Yanmin,Liu Ju,Zhang Meizhu,et al.Experience and Understand in Oil and Gas Exploration in Fushan Sag,Hainan Province[J].South China Journal of Seismology,2007,27(3):57-68.
[34] 罗群,庞雄奇.海南福山凹陷顺向和反向断裂控藏机理及油气聚集模式[J].石油学报,2008,29(3):363-367. Luo Qun,Pang Xiongqi.Reservoir Controlling Mechanism and Petroleum Accumulation Model for Consequent Fault and Antithetic Fault in Fushan Depression of Hainan Area[J].Acta Petrolei Sinica,2008,29(3):363-367.
[35] 林正良,王华,李红敬,等.北部湾盆地福山凹陷古近系双层结构形成机制[J].地球科学:中国地质大学学报,2015,40(1):169-178. Lin Zhengliang,Wang Hua,Li Hongjing,et al.Genetic Mechanism of Doble-Layer Structure in Paleogene of Fushan Sag,Beibuwan Basin[J].Earth Science:Journal of China University of Geosciences,2015,40(1):169-178.
[36] 刘恩涛,王华,林正良,等.北部湾盆地福山凹陷构造转换带及其油气富集规律[J].中南大学学报(自然科学版),2012,43(10):3946-3953. Liu Entao,Wang Hua,Lin Zhengliang,et al.Characteristics and Hydrocarbon Enrichment Rules of Transfer Zone in Fushan Sag,Beibuwan Basin[J].Journal of Central South University (Science and Technology),2012,43(10):3946-3953.
[37] 马庆林,赵淑娥,廖远涛,等.北部湾盆地福山凹陷古近系流沙港组层序地层样式及其研究意义[J].地球科学:中国地质大学学报,2012,37(4):667-678. Ma Qinglin,Zhao Shue,Liao Yuantao,et al.Sequence Architectures of Paleogene Liushagang Formation and Its Significance in Fushan Sag of the Beibuwan Basin[J].Earth Science:Journal of China University of Geosciences,2012,37(4):667-678.
[38] 王观宏,黄传炎,刘恩涛,等.福山凹陷南部缓坡流沙港组坡折带特征及对沉积、油气成藏的控制[J].中南大学学报(自然科学版),2014,45(5):1531-1541. Wang Guanhong,Huang Chuanyan,Liu Entao,et al.Characteristics of Slope-Breaks and Its Control on Sedimentation and Hydrocarbon Accumulation of Liushagang Formation in Gentle Slope of South Fushan Sag[J].Journal of Central South University (Science and Technology),2014,45(5):1531-1541.
[39] 李美俊,卢鸿,王铁冠,等.北部湾盆地福山凹陷岩浆活动与CO2成藏的关系[J].天然气地球科学,2006,17(1):55-59. Li Meijun,Lu Hong,Wang Tieguan,et al.Relationship Between Magma Activity and CO2 Gas Accumulation in Fushan Depression,Beibuwan Basin[J].Natural Gas Geoscience,2006,17(1):55-59.
[40] Elverhoi A.Emerging in Sights in to the Dynamics of Submarine Debris Flows[J].Natural Hazards,Earth System Sciences,2005,5(3):633-648.
[41] Shanmugam G.Reinterpretation of Depositional Processes in a Classic Flysch Sequence (Pennsylvanian Jackford Group),Ouachita Mountains,Arkansas,Oklahoma[J].APPG,1995,79(16):672-695.
[42] 曾洪流.地震沉积学在中国:回顾和展望[J].沉积学报,2011,29(3):417-426. Zeng Hongliu.Seismic Sedimentology in China:A Review[J].Acta Sedimentologica Sinica,2011,29(3):417-426.
[43] 朱兆群,林承焰,张宪国,等.断陷湖盆早期浅水三角洲沉积:以高邮凹陷永安地区戴一段为例[J].吉林大学学报(地球科学版),2017,47(3):659-673. Zhu Zhaoqun,Lin Chengyan,Zhang Xianguo,et al.Shallow Water Delta Deposits in a Rifting Lacustrine Basin During Early Stage:A Case Study of the First Member of Dainan Formation at Yong'an Area,Gaoyou Sag[J].Journal of Jilin University (Earth Science Edition),2017,47(3):659-673.
[44] 余江浩,廖远涛,林正良,等.福山凹陷古近系沉降特征时空差异性及其形成机制[J].油气地质与采收率,2012,19(5):34-38. Yu Jianghao,Liao Yuantao,Lin Zhengliang,et al.Reasearch on Temporal Diversity of Settlement Characteristics of Paleogene,Fushan Sag[J].Petroleum Geology and Recovery Efficiency,2012,19(5):34-38.
[1] Xu Shouyu, Lu Yan, Wang Ya. Study on Flow Units of Turbidite Fan Low Permeability Reservoir Based on Support Vector Machine [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(5): 1330-1341.
[2] Zhu Chuanhua, Wang Weifeng, Wang Qingzhen, Li Yukun. Numerical Simulation of Structural Strain for Turbidite Sands Reservoirs of Low Permeability [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(5): 1580-1588.
[3] Li Baojuan, Dong Chunmei, Lin Chengyan, Cheng Junyang, Ren Lihua, Guo Wei. Seismic Sedimentology Research on Turbidite Fan Body of Different Stages:In case of the Gentle Slope Belt of Chexi Depression's Che40-44 Area of Upper Submember of Es3 [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 65-79.
[4] LIU Chang-li, ZHU Xiao-min, HU You-shan, LIAO Fei-yan, WANG Zheng-guo. Application of Seismic Sedimentology on Lacustrine Turbidite Deposition Indetification [J]. J4, 2011, 41(3): 657-664.
[5] LIU Chang-li, SHU Xiao-min, WANG Xing-minh, REN Hong-min, LI Shu-jing. Sequence Stratigraphic Framework and Sedimentary Characteristics |of Taizhou Formation in Haian Depression of Subei Basin [J]. J4, 2010, 40(3): 519-526.
[6] ZHANG Jing，WANG Wei-feng，RONG Qi-hong，SHI Wen-dong. Deep-Water Turbidite Fan Deposits and Relation to Hybrocarbon of the Upper Sha-4 of Shahejie Formation at Yong-55 Block in Dongying Sag [J]. J4, 2007, 37(3): 519-0524.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
Copyright © Journal of Jilin University(Earth Science Edition), All Rights Reserved.
Tel: +86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
Powered by Beijing Magtech Co. Ltd