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天然气地球科学

• 天然气地质学 • 上一篇    下一篇

雅布赖盆地小湖次凹细粒沉积岩岩相特征与沉积环境探

张少敏，操应长，朱如凯，王尉，涂建琪，毛治国，白斌   

  1. (1.中国石油大学(华东)地球科学与技术学院，山东 青岛 266580；2.中国石油勘探开发研究院，北京 100083)
  • 收稿日期:2015-04-20 修回日期:2015-07-13 出版日期:2016-02-10 发布日期:2016-02-10
  • 通讯作者: 操应长(1969)，男，安徽潜山人，教授，博士生导师，主要从事沉积学及油气储层地质学方面的教学与科研工作. Email:cyc8391680@163.com.
  • 作者简介:张少敏(1989)，女，山东东营人，博士研究生，主要从事沉积学和油气储层地质学研究. Email:zhangshaomin0813@126.com.
  • 基金资助:

    国家自然科学基金石油化工联合基金重点项目(编号:U1262203);国家重点基础研究发展计划(“973”)项目(编号:2014CB239002);中央高校基本科研业务费专项资金资助(编号:15CX06009A);中国石油天然气股份有限公司重大科技专项(编号:2012E3302)联合资助.

The lithofacies and depositional environment of finegrained sedimentaryrocks of Xiaohu Subsag in Yabulai Basin

Zhang Shaomin，Cao Yingchang，Zhu Rukai，Wang Wei，Tu Jianqi，Mao Zhiguo，Bai Bin   

  1. (1.School of Geosciences,China University of Petroleum(east china),Qingdao 266555,China;
    2.Research Institute of Petroleum Exploration & Development,Beijing 100083,China)
  • Received:2015-04-20 Revised:2015-07-13 Online:2016-02-10 Published:2016-02-10

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摘要：

通过岩心观察、薄片鉴定、X射线衍射、有机碳分析等技术，综合矿物成分、有机质含量、沉积构造等因素，对雅布赖盆地小湖次凹新河组下段半深湖—深湖细粒沉积岩岩相进行研究，形成了细粒沉积岩四组分三端元的岩相划分方案。结果表明:新河组下段半深湖—深湖细粒沉积岩发育9种岩相类型，其中以贫有机质块状黏土质细粒长英沉积岩、贫有机质纹层状硅质碎屑型混合细粒沉积岩、贫有机质块状长英质黏土岩、中有机质纹层状硅质碎屑型混合细粒沉积岩、中有机质纹层状长英质黏土岩、富有机质纹层状碳酸盐型混合细粒沉积岩等6种岩相为主。岩相类型与特征反映沉积环境和沉积机理的差异，在前三角洲—半深湖的环境中，波浪增强型沉积物重力流普遍发育，形成纵向上贫有机质块状黏土质细粒长英沉积岩—纹层状硅质碎屑型混合细粒沉积岩—块状长英质黏土岩的叠置，反映水动力渐弱的过程；在半深湖—深湖环境中，水体相对安静，悬浮沉积为主，陆源碎屑输入少，碳酸盐和黏土较发育，形成中—富有机质纹层状混合细粒沉积岩和黏土岩。

关键词: 细粒沉积, 岩相特征, 沉积环境, 新河组, 雅布赖盆地

Abstract:

Taking the finegrained sedimentary rocks of the lower Xinhe Formation in Yabulai Basin as a research object,the lithofacies were subdivided using “four componentsthree endmembers” classification scheme with integrated analysis of minerals,structures and organic carbon content by core observation,thin section identification,Xray diffraction and organic carbon test. The results showed that there were nine lithofacies types that could be identified in the finegrained sedimentary rocks of the lower Xinhe Formation,and six of them are mainly developed,which were organiclean massive clayrich siltstone,organiclean laminated siliceous mixed finegrained sedimentary rocks,organiclean massive felsic claystone,organiccontained laminated siliceous mixed finegrained sedimentary rocks,organiccontained laminated felsic claystone and organicrich laminated carbonate mixed finegrained sedimentary rocks. The different lithofacies types and characteristics reflected the differences of sedimentary environment and depositional mechanism. In the prodelta to semideep lacustrine,the waveenhanced sediment gravity flows are widely developed,which formed the superimposed deposition combination of organiclean massive clayrich siltstonelaminated siliceous mixed finegrained sedimentary rocksmassive felsic claystone from bottom to top. In the semideep to deep lacustrine,the water was relatively quiet with a small amount of terrigenous clast input,and the carbonate and clays were more developed,forming organiccontained to rich laminated mixed finegrained sedimentary rocks and claystones.

Key words: Finegrained sediments, Lithofacies, Depositional environment, Xinhe Formation, Yabulai Basin

中图分类号: 

  • TE121.3+1

[1]Picard M D.Classification of finegrained sedimentary rocks[J].Journal of Sedimentary Research,1971,41(1):179195.
[2]Schieber J,Zimmerle W.The history and promise of shale research[C]//Schieber J,Zimmerle W,Sethi P.Shales and mudstones:Vol.1:Basin studies,sedimentology and paleontology.Stuttgart:Schweizerbart Science Publishers,1998:110.
[3]Aplin A C,Macquaker J H S.Mudstone diversity:Origin and implications for source,seal,and reservoir properties in petroleum systems[J].AAPG Bulletin,2011,95(12):20312059.
[4]Jiang Zaixing,Liang Chao,Wu Jing,et al.Several issues in sedimentological studies on hydrocarbonbearing finegrained sedimentary rocks[J].Acta Petrolei Sinica,2013,34(6):10311039.[姜在兴,梁超,吴靖,等.含油气细粒沉积岩研究的几个问题[J].石油学报,2013,34(6):10311039.]
[5][KG*4/5]Aplin A C,Fleet A J,Macquaker J H S.Muds and Mudstones:Physical and Fluid Flow Properties[R].The Geological Society of London Special Publication,1999,158:18.
[6][KG*4/5]Yuan Xuanjun,Lin Senhu,Liu Qun,et al.Lacustrine finegrained sedimentary features and organicrich shale distribution pattern:A case study of Chang 7 member of Triassic Yanchang Formation in Ordos Basin,NW China[J].Petroleum Exploration and Development,2015,42 (1):3443.[袁选俊,林森虎,刘群,等.湖盆细粒沉积特征与富有机质页岩分布模式—以鄂尔多斯盆地延长组长7油层组为例[J].石油勘探与开发,2015,42(1):3443.]
[7]Zou Caineng,Yang Zhi,Cui Jingwei,et al.Formation mechanism,geological characteristics,and development strategy of nonmarine shale oil in China[J].Petroleum Exploration and Development,2013,40(1):1426.[邹才能,杨智,崔景伟,等.页岩油形成机制、地质特征及发展对策[ J].石油勘探与开发,2013,40(1):1426.]
[8]Zhang Shun,Chen Shiyue,Yan Jihua,et al.Characteristics of shale lithofacies and reservoir space in the 3rd and 4th members of Shahejie Formation,the west of Dongying Sag[J].Natural Gas Geoscience,2015,26(2):320332.[张顺,陈世悦,鄢继华,等.东营凹陷西部沙三下亚段沙四上亚段泥页岩岩相及储层特征[J].天然气地球科学,2015,26(2):320332.]
[9]Robert G,Stephen C R.Mississippian Barnett Shale:Lithofacies and depositional setting of a deepwater shalegas succession in the Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):579601.
[10]Liu Shugen,Ma Wenxin,LUBA Jansa,et al.Characteristics of the shale gas reservoir rocks in the Lower Sichuan Longmaxi Formation,east Sichuan Basin,China[J].Acta Petrologica Sinica,2011,27(8):22392252.[刘树根,马文辛,LUBA Jansa,等.四川盆地东部地区下志留统龙马溪组页岩储层特征[J].岩石学报,2011,27(8):22392252.]
[11]Liang Chao,Jiang Zaixing,Yang Yiting,et al.Characteristics of shale lithofacies and reservoir space of the WufengLongmaxi Formation,Sichuan Basin[J].Petroleum Exploration and Development,2012,39(6):691698.[梁超,姜在兴,杨镱婷,等.四川盆地五峰组—龙马溪组页岩岩相及储集空间特征[J].石油勘探与开发,2012,39(6):691698.]
[12]Plint A G,Macquaker J H S,Varban B L.Bedload transport of mud across a wide,storminfluenced ramp:Cenomanian Turonian Kaskapau Formation,western Canada Foreland Basin [J].Journal of Sedimentary Research,2012,82(11):801822.
[13]Bai Zhiqiang,Liu Shugen,Sun Wei,et al.Reservoir characteristics of Wufeng FormationLongmaxi Formation in southwest of Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science &Technology Edition,2013,4(5):521531.[白志强,刘树根,孙玮,等.四川盆地西南雷波地区五峰组—龙马溪组页岩储层特征[J].成都理工大学学报:自然科学版,2013,4(5):521531.]
[14]Plint A G.Mud dispersal across a Cretaceous prodelta:Stormgenerated,waveenhanced sediment gravity flows inferred from mudstone microtexture and microfacies[J].Sedimentology,2014,61(3):609647.
[15]Zhang Shun,Chen Shiyue,Cui Shiling,et al.Characteristics and types of finegrained sedimentary rocks lithofacies in semideep and deep lacustrine,Dongying Sag[J].Journal of China University of Petroleum:Edition of Natural Science,2014,38(5):919.[张顺,陈世悦,崔世凌,等.东营凹陷半深湖—深湖细粒沉积岩岩相类型及特征[J].中国石油大学学报:自然科学版,2014,38(5):919.]
[16]Macquaker J H S,Samuel J B,Kevin M B.Waveenhanced sedimentgravity flows and mud dispersal across continental shelves:Reappraising sediment transport processes operating in ancient mudstone successions[J].Geology,2010,3(10):947950.
[17]Wilson R D,Schieber J.Muddy prodeltaic hyperpycnites in the lower genesee group of central New York,USA:Implications for mud transport in epicontinental seas[J].Journal of Sedimentary Research,2014,84(10):866874.
[18]Mulder T,Sycitski J P M.Turbidity currents generated at river mouths during exceptional discharges to the world oceans[J].Journal of Geology,1995,103(3):285299.
[19]Potter P E.Mudrocks[M]//Middleton G V.Encyclopedia of Sediments and Sedimentary Rocks.Dordrecht,Kluwer:Scientific Publishers,2003:451459.
[20]Schieber J,Southard J,Thaisen K.Accretion of mudstone beds from migrating floccule ripples[J].Science,2007,318(5857):1760.
[21]Baas J H,Best J L,Peakall J.Depositional processes,bedform development and hybrid bedformation in rapidly decelerated cohesive (mudsand)sedimentflows[J].Sedimentology,2011,58(7):19531987.
[22]Wu Maobing,Liu Chunyan,Zheng Menglin,et al.Jurassic depositional tectonic evolution in the Yabulai Basin,western Inner Mongolia,China and direction of petroleum exploration[J].Geological Bulletin of China,2007,26(7):857863.[吴茂炳,刘春燕,郑孟林,等.内蒙古西部雅布赖盆地侏罗纪沉积构造演化及油气勘探方向[J].地质通报,2007,26(7):857863.][JP]
[23]Wu Xiaozhi,Wang Guijun,Zheng Min,et al.Structural evolution and hydrocarbon accumulation in Yabulai Basin[J].Chinese Journal of Geology,2015,50(1):7487.[吴晓智,王桂君,郑民,等.雅布赖盆地构造演化与油气聚集[J].地质科学,2015,50(1):7487.]
[24]Li Juyuan.Analysis on mineral components and frangibility of shales in Dongying Depression[J].Acta Sedimentologica Sinica,2013,31(4):616620.[李钜源.东营凹陷泥页岩矿物组成及脆度分析[ J].沉积学报,2013,31(4):616620.]
[25]Huang Difan.Terrestrial Organic Matter Evolution and Hydrocarbon Generation Mechanism[M].Beijing:Petroleum Industry Press,1984.[黄第藩.陆相有机质演化和成烃机理[M].北京:石油工业出版社,1984.]
[26]Jiang Zaixing.Sedimentology[M].Beijing:Petroleum Industry Press,2003.[姜在兴.沉积学[M].北京:石油工业出版社,2003.]
[27]Liu Chuanlian,Shu Xiaoxin,Liu Zhiwei.Microcharacteristics of Paleogene lacustrine petroleum source rocks in Jiyang Depression[J].Acta Sedimentologica Sinica,2001,19(2):293297.[刘传联,舒小辛,刘志伟.济阳坳陷下第三系湖相生油岩的微观特征[J].沉积学报,2001,19(2):293297.]
[28]Wang Guanmin.Laminae Combination and genetic classification of eogene shale in Jiyang Depression[J].Journal of Jilin University,2012,42(3):666673.[王冠民.济阳坳陷古近系页岩的纹层组合及成因分类[J].吉林大学学报:地球科学版,2012,42(3):666673.]
[29]Bhattacharya J P,MacEachern J A.Hyperpycnal rivers and prodeltaic shelves in the Cretaceous Seaway of North America[J].Journal of Sedimentary Research,2009,79(4):184209.
[30]Zhang Shun,Chen Shiyue,Tan Mingyou,et al.Characterization of sedimentary microfacies of shale in the lower third submember of Shahejie Formation,western Dongying Sag[J].Acta Petrolei Sinica,2014,35(4):633645.[张顺,陈世悦,谭明友,等.东营凹陷西部沙河街组三段下亚段泥页岩沉积微相[J].石油学报,2014,35(4):633645.]
[31]Talling P J,Masson D G,Sumner E J,et al.Subaqueous sediment density flows:Depositional processes and deposit types[J].Sedimentology,2012,59(7):19372003.
[32]Stow O A V.Finegrained sediments in deep water:An overview of processes and facies models[J].GeoMarine Letters,1985,5(1):1723.
[33]Liu Qun,Yuan Xuanjun,Lin Senhu,et al.The classification of lacustrine mudrock and research on its depositional environment[J].Acta Sedimentologica Sinica,2014,32(6):10161025.[刘群,袁选俊,林森虎,等.鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J].沉积学报,2014,32(6):10161025.]
[34]Yang Tian,Cao Yingchang,Wang Yanzhong,et al.Status and trends in research on deepwater gravity flow deposits[J].Acta Geological Sinica:English Edition,2015,89(2):610631.
[35]Wang Guanmin,Zhong Jianhua.A review and the prospects of the researches on sedimentary mechanism of lacustrine laminae[J].Acta Petrologica Mineralogica,2004,23(1):4348.[王冠民,钟建华.湖泊纹层的沉积机理研究评述与展望[J].岩石矿物学杂志,2004,23(1):4348.]
[36]Pan Shuxin,Chen Bintao,Liu Huaqing,et al.Deepwater bottom current rework sand(BCRS)in lacustrine basins:Sedimentary characteristics,identification criterion,formation mechanism and its significance for unconventional oil/gas exploration[J].Natural Gas Geoscience,2014,25(10):15771585.[潘树新,陈彬滔,刘华清,等.陆相湖盆深水底流改造砂:沉积特征、成因及其非常规油气勘探意义[J].天然气地球科学,2014,25(10):15771585.]
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