天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学

• 天然气地质学 • 上一篇    下一篇

深水浊积朵叶储层构型模式研究

林煜,吴胜和，王星，赵晓明，凌云，路瑶，张佳佳   

  1. 1.中国石油大学(北京)地球科学学院，北京 102249；
    2.中国石油集团东方地球物理勘探有限责任公司，河北 涿州 072050；
    3.中海油研究总院，北京 100027；4.西南石油大学资源与环境学院，四川 成都 610500
  • 收稿日期:2013-08-07 修回日期:2014-04-11 出版日期:2014-08-10 发布日期:2014-08-10
  • 作者简介:林煜(1985-)，男，陕西延长人，博士后，主要从事精细油藏描述及开发地质学研究. E-mail：lin66yu@163.com.
  • 基金资助:
    国家科技重大专项(编号：2011ZX05030-005；2011ZX05009-003)；国家自然科学青年科学基金项目(编号：40902035)联合资助.

Research on Reservoir Architecture Models of Deep-water Turbidite Lobes

LIN Yu，WU Sheng-he，WANG Xing，ZHAO Xiao-ming,LING Yun，LU Yao，ZHANG Jia-jia   

  1. 1.College of Geosciences,China University of Petroleum,Beijing 102249,China;
    2.BGP Inc.,China National Petroleum Corporation,Zhuozhou 072750,China;
    3.Research Institute,China National Offshore Oil Corp.,Beijing 100027,China;
    4.College of Resource & Environment,Southwest Petroleum University,Chengdu 610500,China
  • Received:2013-08-07 Revised:2014-04-11 Online:2014-08-10 Published:2014-08-10

PDF (PC)

575

摘要：

深水沉积是世界油气增储上产的重要领域之一。目前，国外学者针对深水沉积的构型模式开展了大量研究，但研究对象多为浊积水道，而对于浊积朵叶的关注则甚少。为此，以西非尼日尔三角洲盆地某深水区块地下储层和中国甘南西秦岭地区某深水露头作为原型，采用地震相分析、地震沿层切片、露头观察描述等多种手段相结合的方法，分级次开展了浊积朵叶的构型模式研究。研究表明，浊积朵叶的构型单元可划分为7级，其中3～5构型单元分别为：单一朵叶、复合朵叶和朵叶体系。朵叶体系由多个复合朵叶叠置而成。复合朵叶内部发育树枝状的下切水道，底部发育块体搬运沉积，其常常对下伏地层有明显侵蚀。单一朵叶由受平行、亚平行界面约束的多期板状砂岩垂向加积而成，依据其内部沉积特征的差异，可进一步分为近朵叶端、中朵叶端和远朵叶端3部分。通过研究不仅可以深化浊积朵叶的地质理论，而且可以有效降低此类油气田的勘探开发风险，具有重要的实际意义。

关键词: 浊积朵叶, 构型模式, 原型, 发育样式, 充填样式

Abstract:

Deep-water sediments are the main field which increases oil & gas reserve and production around the world.Although extensive researches on architecture models of deep-water sediments have been carried out,most of them focus on turbidite channels rather than turbidite lobes.In this study,taking the subsurface reservoirs of deep-water area in the Niger Delta Basin and the outcrops of submarine fan in West Qingling Mountains of Gannan area as prototypes,architecture models of turbidite lobes is constructed from different hierarchies.These researches are based on outcrop observations and descriptions,seismic facies analyses,seismic horizon slices and so on.The results show that architecture units of turbidite lobes can be divided into seven hierarchies.Lobes,lobe complexes and lobe systems are architecture units from 3rd hierarchy to 5th hierarchy.Generally,a lobe system contains several overlying lobe complexes.Incised channel deposits showing treelike shape and mass transport deposits (MTDs) erode strongly underlying strata are widely developed at lobe complexes.A lobe consists of multi-period tabular sandstones confined by sub-parallel or parallel interfaces and can be divided into three parts according to internal sedimentary differences.These parts are the proximal,the middle and the distal parts.This study brings deep understandings to the geological theory of turbidite lobes and it also reduces the risk on exploration and development about this type of reservoir.Thus,it has significant theory and practice meanings.
 

Key words: Turbidite lobes, Architecture models, Prototypes, Development patterns, Filling patterns

中图分类号: 

  • TE122.2

［1］Qu Hui,Zheng Min,Li Jianzhong, et al. Advances of deep-water hydrocarbon explorations in global passive continental margin and their implication[J].Natural Gas Geoscience,2010,21(2):193-200.［瞿辉,郑民,李建忠,等.国外被动陆缘深水油气勘探进展及启示[J].天然气地球科学,2010,21(2):193-200.］
［2］Wang Zhen,Chen Chuanying,Zhao Lin.Present situation and challenge of exploration and production for deep water oil and gas in the whole world[J].Sino-global Energy,2010,15(1):46-48.［王震,陈船英,赵林.全球深水油气资源勘探开发现状及面临的挑战[J].中外能源,2010,15(1):46-48.］
［3］Maill A D.Architectural-element analysis:A new method of facies analysis applied to fluvial deposits[J].Earth Science Reviews,1985,22(2):261-308.
［4］Zhou Xinmao,Gao Xingjun,Tian Changbin, et al. Quantiative description of internal architecture in point bar of meandering river[J].Natural Gas Geoscience,2010,21(3):421-426.［周新茂,高兴军,田昌炳,等.曲流河点坝内部构型要素的定量描述及应用[J].天然气地球科学,2010,21(3):421-426.］
［5］Lin Yu,Wu Shenghe,Yue Dali, et al. Fine anatomizing reservoir architecture of fan-delta front:A case study on Dujiatai reservoir in Shu 2-6-6 block,Liaohe Oilfield[J].Natural Gas Geoscience,2013,24(2):335-344.［林煜,吴胜和,岳大力,等.扇三角洲前缘储层构型精细解剖——以辽河油田曙2-6-6区块杜家台油层为例[J].天然气地球科学,2013,24(2):335-344.］
［6］Posamentier H W,Kolla V.Seismic geomorphology and stratigraphy of depositional elements in deep-water settings[J].Journal of Sedimentary Research,2003,73:367-388.
［7］Wynn R B,Cronin B T,Peakall J.Sinuous deep-water channels:Genesis,geometry and architecture[J].Marine and Petroleum Geology,2007,24:341-387.
［8］Mutti E,Normark W R.Comparing Examples of Modern and Ancient Turbidite Systems:Problems and Concepts[M].London:Graham and Trotman,1987:1-38.
［9］Lamb M A,Anderson K S,Graham S A.Stratigraphic Architecture of a Sand-Rich,Deep-sea Depositional System:The Stevens Sandstone,San Joaquin Basin,California[M].Oklahoma:AAPG Pacific Section,2003:13.
［10］Richard L.Integrated three-dimensional modeling approach of stacked turbidite channels[J].AAPG Bulletin,2007,91(11):1603-1618.
［11］Kolla V,Bourges Ph,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.
［12］Menno J D R,Stephen M H.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.
［13］Clark J D,Pickering K T.Submarine Channels:Processes and Architecture[M].London:Vallis Press,1996:231.
［14］Peakall J,McCaffrey W D,Kneller B C.A process model for the evolution,morphology and architecture of sinuous submarine channels[J].Journal of Sedimentary Research,2000,70(3):434-448.
［15］Menard H W.Deep-sea channels topography and sedimentation[J].AAPG Bulletin,1995,39(2):236-255.
［16］Lin Yu,Wu Shenghe,Wang Xing, et al. Research on architecture model of deep-water turbidite channel system:A case study on X area of deep-water in Niger delta basin,West Africa[J].Geological Review,2013,59(3):510-520.［林煜,吴胜和,王星,等.深水浊积水道体系构型模式研究——以西非尼日尔三角洲盆地某深水研究区为例[J].地质论评,2013,59(3):510-520.］
［17］Wang Ying,Lv Ming.Reservoir characteristic sediment in Nigeria deep-water area[J].Natural Gas Geoscience,2009,20(2):228-236.［王颖,吕明.深水沉积储层特征——以尼日利亚OML130区块为例[J].天然气地球科学,2009,20(2):228-236.］
［18］Zhao Yanjun,Bao Zhidong,Wang Xing, et al. Control factors of a submarine fan in Niger Basin[J].Journal of Xi'an Shiyou University:Natural Science Edition,2012,27(2):6-12.［赵艳军,鲍志东,王星,等.尼日尔盆地某深水海底扇发育的控制因素[J].西安石油大学学报:自然科学版,2012,27(2):6-12.］
［19］Deng Rongjing,Deng Yunhua,Yu Shui, et al. Hydrocarbon geology and reservoir formation characteristics of Niger delta basin[J].Petroleum Exploration and Development,2008,35(6):755-762.［邓荣敬,邓运华,于水,等.尼日尔三角洲盆地油气地质与成藏特征[J].石油勘探与开发,2008,35(6):755-762.］
［20］Liu Jianping,Pan Xiaohua,Ma Jun, et al. Petroleum geology and resources in West Africa:An overview[J].Petroleum Exploration and Development,2008,35(3):378-384.［刘剑平,潘校华,马君,等.西部非洲地区油气地质特征及资源概述[J].石油勘探与开发,2008,35(3):378-384.］
［21］Fang Guoqing,Zhang Xiaobao,Li Yuci.Rift-faultings of hercynian-Indosinan epoch of Western Qingling orogenic belt and its relationship with Palaeotethys[J].Acta Sedimentologica Sinica,1994,13(3):76-81.［方国庆,张晓宝,李育慈.西秦岭海西—印支期裂陷活动及其与古特提斯的关系[J].沉积学报,1994,13(3):76-81.］
［22］Zhang Xiaobao,Fang Guoqing,He Haiqing.Features and model of sedimentary environments of Upper Triassic seaf loor fans in West Qingling Mts[J].Scientia Geologica Sinica,1996,31(2):154-162.［张晓宝,方国庆,何海清.西秦岭上三叠统海底扇沉积环境特征与模式[J].地质科学,1996,31(2):154-162.］
［23］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.［李磊,王英民,张莲美,等.南海北部白云深水区水道与朵叶沉积序列及演化[J].海洋地质与第四纪地质,2009,29(4):71-76.］
［24］Li Lei,Li Bin,Wang Yingmin.Sedimentary architecture of submarine lobe and its implications on petroleum prospecting[J].Journal of Shandong University of Science and Technology:Natural Science,2012,31(4):37-43.［李磊,李彬,王英民.深水朵体沉积构型及其油气勘探意义[J].山东科技大学学报:自然科学版,2012,31(4):37-43.］
［25］Ma Liwu,Yu Shui,Tao Weixiang, et al. Analysis of deepwater sedimentary characteristics,southern Africa [J].Natural Gas Geoscience,2008,19(4):499-502.［马立武,于水,陶维祥,等.非洲南部某深水区沉积特征分析[J].天然气地球科学,2008,19(4):499-502.］
［26］Curray J R,Emmel F J.The Bengal Fan:morphology,geometry,stratigraphy,history and processes[J].Marine and Petroleum Geology,2002,19(10):1191-1223.
［27］Naini B R,Kolla V.Acoustic character and thickness of sediments of the Indus Fan and the continental margin of western India[J].Marine Geology,1982,47(3/4):181-195.
［28］Damuth J E,Kumar N.Amazon Cone:morphology,sediments,age and growth pattern[J].Geological Society of America Bulletin,1975,86(6):873-878.
［29］Pirmez C,Imran J.Reconstruction of turbidite currents in Amazon Channel[J].Marine and Petroleum Geology,2003,20(6-8):823-849.
［30］Normark W R,Piper D J W,Hess G R.Distributary channels,sandy lobes,and meso-topography of Navy submarine fan,California Borderland,with applications to ancient fan sediments[J].Sedimentology,1979,26(6):749-774.
［31］Sawyer D E,Flemings P B,Shipp R C, et al. Seismic geomorphology,lithology,and evolution of the late Pleistocene Mars-Ursa turbidite region,Mississippi canyon area,northern gulf of Mexico[J].AAPG Bulletin,2007,91(2):215-234.
［32］Garziglia S.Mass-transport deposits on the Rosetta province (NW Nile deep-sea turbidite system,Egyptian margin):Characteristics,distribution and potential causal processes[J].Marine Geology,2008,250(3/4):180-198.
［33］Wang Dawei,Wu Shiguo,Dong Dongdong, et al. Seismic characteristics of Quaternary mass transport deposits in Qiongdongnan Basin[J].Marine Geology and Quaternary Geology,2009,29(3):69-74.［王大伟,吴时国,董冬冬,等.琼东南盆地第四纪块体搬运体系的地震特征[J].海洋地质与第四纪地质,2009,29(3):69-74.］
［34］Li Lei,Wang Yingmin,Zhang Lianmei, et al. Identification and evolution of mass transport complexes and its significance for oil and gas exploration[J].Acta Sedimentologica Sinica,2010,28(1):76-82.［李磊,王英民,张莲美,等.块体搬运复合体的识别、演化及其油气勘探意义[J].沉积学报,2010,28(1):76-82.］
［35］Li Lei,Li Bin,Wang Yingmin, et al. Seismic geomorphology and sedimentary architectures of mass transport deposits:Cases from Pearl River Mouth Basin and Niger delta basin[J].Journal of Central South University:Science and Technology,2013,44(6):2410-2416.［李磊,李彬,王英民,等.块体搬运沉积体系地震地貌及沉积构型:以珠江口盆地和尼日尔三角洲盆地为例[J].中南大学学报:自然科学版,2013,44(6):2410-2416.］
［36］Dam G,Sonderholm M.Low stand slope channels of the Itilli succession (Maastrichtian lower Paleocene),Nuussuaq,west Greenland[J].Sedimentary Geology,1994,94(1/2):49-71.
［37］Cronin B,Owen D,Hartley A, et al. Slumps,debris flows and sandy deep-water channel systems:Implications for the application of sequence stratigraphy to deepwater clastic sediments[J].Journal of the Geological Society,1998,155(3):429-432.
［38］Martinez J F,Cartwright J,Hall B.3D seismic interpretation of slump complexes:Examples from the continental margin of Israel[J].Basin Research,2005,17(1):83-108.
［39］Sullivan M,Jensen G,Goulding F, et al. Architectural analysis of deep-water outcrops:Implications for exploration and development of the Diana Sub-basin,western Gulf of Mexico[C]//Weimer P,Slatt R M,Coleman J L,et al(Eds.).20th annual Bob F.Perkins research conference.USA(Houston):Society for Sedimentary Geology,Gulf Coast Section,2000:1010-1031.
[1] 刘兴旺, 郑建京, 杨鑫, 刘玉虎. 三塘湖盆地及其周缘地区古生代构造演化及原型盆地研究[J]. 天然气地球科学, 2010, 21(6): 947-954.
[2] 姚亚明;周继军;何明喜;付代国;陈建军;. 对焉耆盆地油气地质条件的认识[J]. 天然气地球科学, 2006, 17(4): 463-467.
[3] 刘朝露;夏斌;. 济阳坳陷中生代原型盆地的初步恢复及其主控因素[J]. 天然气地球科学, 2006, 17(1): 60-63.
[4] 李梅;包建平;汪海;张秋茶;郑多明;卢玉红;黄龙藏;. 库车前陆盆地烃源岩和烃类成熟度及其地质意义[J]. 天然气地球科学, 2004, 15(4): 367-378.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!