用户名: 密码: 验证码:
饶阳凹陷层序地层格架下烃源岩特性与油气聚集研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
本文充分运用了层序地层学理论和方法完善了饶阳凹陷体系域为单元的层序地层格架,并在层序地层格架的控制下对沉积体系的类型、平面展布和垂向叠置关系进行了研究。依据测井方法对烃源岩的纵向特征进行了精细刻画,通过TOC与HI关系,建立了湖相源岩的评价标准。与层序地层研究相结合,实现了对烃源岩空间分布特征较为准确地预测。并认为优质烃源岩的发育第一层次(三级层序)受湖泛面和高有机质生产力控制,第二层次(5级层序及以下)受沉积速率和可容纳空间控制,即体系域和沉积相带是控制烃源岩沉积特征和有机地球化学参数差异性的重要原因。同时通过油源对比及资源量计算表明了优质烃源岩在油气成藏中的关键作用。利用三维盆地模拟技术结合流体势分析,对饶阳凹陷四大领域重点区块,从油气生成、运移到聚集成藏过程进行反演模拟,实现资源-目标一体化评价,指明未来油气勘探的现实接替领域。
The theory and method of sequence stratigraphy are sufficiently used to improve sequence stratigraphy framework on the basis of system tract in Raoyang Sag. The relations of type, plane distribution and vertical superposition of sedimentary system controlled by sequence stratigraphy framework have been studied. The method to calculate total organic carbon (TOC) in source rock by logging is used to delicately portray the vertical characteristic of source rock cross section. The evaluation criterion of lacustrine source rock is based on the relationship between TOC and hydrogen index (HI). Combined with sequence stratigraphy, It's quite accuracy to predict the spatial distribution characteristic of lacustrine source rock. The study shows that the excellent source rock is firstly controlled by the change of lake level (third-order sequence), secondly affected by sediment supply rate and accommodation (fifth-order sequence or below). Therefore, system tract and sedimentary facies are the main controlled factors of the sedimentary characteristic and organic geochemistry parameter diversity of source rock. The results of oil-source correlation and the amount of resource show that excellent source rock plays important role in petroleum accumulation. 3D basin modelling technique and fluid potential inversion are used to model the process of petroleum generation, migration and accumulation, from the four exploration fields of Raoyang Sag, to realize the integrative evaluation of resource and target, to indicate the future replace exploration field.
引文
[1]贾承造,池英柳.中国岩性地层油气藏资源潜力与勘探技术[A].见:隐蔽油气藏形成机理与勘探实践[C],李坯龙主编,北京:石油工业出版社,2004.
    [2]沈守文,彭大钧,颜其彬等.层序地层学预测隐蔽油气藏的原理和方法.地球学报,2000,21(3):300-305.
    [3]Vail P.R,Mitchum R.M,Thompson S.Global cycles of relative changes of sea level.AAPG,1977(26),99-116.
    [4]Van Wagoner J C,et al. An overview of the fundamentals of sequence stratigraphy and key definitions.SEMP Special Publication,1988(42),39-45.
    [5]C.K.威尔格斯等编,徐怀大等译,层序地层学原理-海平面变化综合分析.石油工业出版社,1993.4.
    [6]吴因业.含油气盆地层序解释技术与应用.石油工业出版社,2000.
    [7]Galloway W.E.Genetic stratigraphic sequence in basin analysis1:architecture and gensis of flooding-surface bounded depositional units.AAPG Bull,1989 (73),125-142.
    [8]Cross T A.Controls on coal distribution in transgressive-ingressive cycles.Upper Cretaceous, Western Interoir,USA.In:Wilgus C K.Hastings B S,Kendall C G St C,et al.Sea level changes:an integrated approach.SEPM Special Publication,1988(42),371-380.
    [9]Cross T A.High-resolution stratigraphic correlation from the perspective of base-level cycles and sediment accommodation.North west Europe conference of sequence stratigraphy,1994.
    [10]Van Wagoner J C.An overview of the fundamentals of sequence stratigraphy and key difinations[A].Wilgus C K. Sea-level Changes:An Integrated Approach[C].Society of Economic Paleonto logiste and Mineralogists Special Publication,1988,125-154.
    [11]Ken J.Woolfe等著,胡润苗,赖海英译.低水位期河流无需下切大陆架-利用澳大利亚大堡礁的实例推断层序地层模型.国外油气勘探,1998,10(6):702-706.
    [12]G.Shanmugam等著,黄忠范译.北海的盆底扇:层序地层学模式与沉积相.国外油气勘探,1996,8(1):28-50.
    [13]R. Eschard等著,伊培荣等译.综合运用层序地层学、地质统计模拟和生产数据来模拟Chaunoy油田的冲积储集层(法国三叠系).国外油气勘探,1999,11(3):259-276.
    [14]X.Liu,W.E.Galloway著,王晓钦译.定量测定北海盆地第三系沉积物补给.国外油气勘探,1999,11(2):148-153.
    [15]张万选.陆相断陷盆地区域地震地层学研究.北京:石油大学出版社,1988.
    [16]柳永清,李寅,刘晓文.层序地层旋回地层与多重地层划分-以京西冀北下古生界为例.中国区域地质,1997,16(1):81-88.
    [17]罗群,郑德山,孙宏智.地质地震综合地层划分对比法及其应用.江汉石油学院学报,2001,23(1):26-29.
    [18]Alistair R. Brown著,严又生译.地震属性及其分类.国外油气勘探.1997,9(4):529-530.
    [19]李思田,潘元林,陆永潮等.断陷湖盆隐蔽油气藏预测及勘探的关键技术-高精度地震探测基础上的层序地层学研究.地球科学,2002,27(5):592-598.
    [20]胡受权,陈萍,闫福旺.泌阳断陷湖盆陡坡带陆相层序油气成藏类型及分布规律探讨.河南石油,2001,15(2):7-10.
    [21]尹太举,张昌民.层序地层格架内的油气勘探.天然气地球科学,2005,16(1):25-30.
    [22]解习农,程守田,陆永潮.陆相盆地幕式构造旋回与层序构成.地球科学-中国地质大学学报,1996,21(1),27.
    [23]解习农,任建业,焦养泉等.断陷盆地构造作用与层序样式.地质论评,1996,42(3),239.
    [24]李思田,程守田,杨士恭等.鄂尔多斯盆地东北部层序地层及沉积体系分析,北京:地质出版社,1992.
    [25]李思田,林畅松,解习农等.大型陆相盆地层序地层学研究.地学前缘,1995,2(4):133-136.
    [26]吴根耀.构造层序地层学.地球科学进展,1996,11(3):310-313.
    [27]池英柳,张万选,张厚福等.陆相断陷盆地层序成因初探.石油学报,1996,17(3):19-26.
    [28]许效松.层序地层学在油储勘查研究中的新思维.海相油气地质,1997,2(2):16-21.
    [29]纪友亮,张世奇,张宏等.层序地层学原理及层序成因机制模式.地质出版社,1998.2.
    [30]魏魁生,徐怀大,叶淑芬等.松辽盆地白垩系高分辨率层序地层格架.石油天然气地质,1997,18(1):7-18.
    [31]林畅松,潘元林,肖建新等.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学-中国地质大学学报,2000,25(3):260-266.
    [32]Van Wagoner.J. C.,Mitchum,R. M.,Campion,K.M.and Rahamanian,V. D. Siliciclastic sequence stratigraphy in well logs,cores and outcrops:concepts for high-resolution correlation of time and facies.AAPQMethods in Exploration Series,1990,No.7 11-55.
    [33]Mitchum R. M. and Van Wagoner J. C. High-frequency sequences and their stacking patterns:sequence stratigraphic evidence of high-frequency eustatic cycles Sediemntary Geology.1991,Vol.70:131-160.
    [34]林畅松,刘景彦,刘丽军等.高精度层序地层分析:建立沉积相和储层规模的等时地层格架.现代地质.2002.16(3):276-281.
    [35]Aitken,J. Rand Howell,J.A. High resolution sequence stratigraphy:innovations, applications and future prospects. In:Howell,J. A. and Aitken, J. F. (eds.) High Resolution Sequence Stratigraphy:Innovations and Applications. Geological Society,London,Special Publication,1996,No.104.1-9.
    [36]Howell, J. A. and Aitken, J. F.,1996 (eds.), High Resolution Sequence Stratigraphy:Innovations and Applications. Geological Society, London, Special Publication No.104.371.
    [37]Hesselbo, S. P. And Parkinson.D. N.,1996(eds),Sequence Stratigraphy in British Geology. Geological Society, London, Special Publication No.103.277.
    [38]Gardner, T. W., Williams, E. G. and Holbrook, P.W. Pedogenesis of some Pennsylvanian underclays; Ground-water, topographic, and tectonic controls Geological Society of America Special paper 1988,216, 81-101.
    [39]黄绍甫.层序地层有机地球化学研究进展及其意义.南方国土资源,2005,6:30-33.
    [40]KATZ B J,PRATT L M. Source rocks in a st ratigraphic framework.AAPG Studies in Geology,1993,37:1-247.
    [41]李思田.盆地动力学与能源资源-世纪之交的回顾与展望.地学前缘,2000,7(3):1-9.
    [42]PETERS K E,SNEDDEN J W,SULAEMAN A,et al. A new geochemical-sequence stratigraphic model for the Mahakam Delta and Makassar Slope, Kalimantan,Indonesia. AAPG Bulletin,2000,84 (1):12-44.
    [43]BOHACS K M,CAROLL A R,NEAL J E,et al. Lake-basin type,source potential, and hydrocarbon character: An integrated sequence-stratigraphic-geochemical framework [A].GIERLOWSKI E H, KORDESCH,KEL TS K R. Lake basins through space and time. AAPG Studies in Geology,2000,46:3-34.
    [44]TOBIAS H D.PAYENBERG, MI ALL A D. A new geochemical-sequence stratigraphic model for the Mahakam Deltaand Makassar slope,Kalimantan,Indonesia:Discuss.AAPG Bulletin,2001,86 (6).
    [45]JOHN W S,SARGJ F,PETERS K E. A new geochemicalsequence stratigraphic model for the Mahakam Delta andMakassar slope, Kalimantan,Indonesia:Reply. AAPG Bulletin,2001,86 (6).
    [46]覃建雄,陈洪德,田景春.西南地区二叠系层序格架与烃源岩分布.石油勘探与开发,1998.25(5):21-25.
    [47]卓勤功,宗国洪,郝雪峰等.湖相深水油页岩段层序地层学属性及成油意义-以济阳坳陷为例.油气地质与采收率,2003.10(1):20-22.
    [48]刘洛夫,康永尚,齐雪峰等.准噶尔盆地侏罗系层序地层格架中的烃源岩评价.沉积学报,2002,20(4):687-694.
    [49]PETERSEN H I,ROSENBERG P.ANDSBJ ERGJ.Organicgeochemistry in relation to the depositional environments of middle Jurassic coal seams, Danish central graben, and implication for hydrocarbon generative potential.AAPG Bul letin,1996,80(1):47-62.
    [50]TYSON T V.Sequence-stratigraphical interpretation of organic facies variations in marine siliciclastic system:General principles and application to the onshore Kimmeridge clay formation,U K[A].Sequence Stratigraphy in British Geology[M].[s.l.]:Geology Society Special Publication,1996,103:75-96.
    [51]MANNU, TEINR.Organic facies variations, source rockpotential,and sea level change in Cretaceous black shales oft he Quebrada Ocal,upper Magdalena valley,Colombia.AAPG Bulletin,1996,81(4):556-576.
    [52]RANGEL A,PARRA P,NINO C.The La Luna formation:Chemost ratigraphy and organic facies in the Middle Magdalena Basin. Organic Geochemistry,2000,31:1267-1284.
    [53]刘立,王东坡.湖相油页岩的沉积环境及其层序地层意义.石油实验地质,1996,18(3):311-316.
    [54]杨明慧,夏文臣,张兵山等.非海相盆地准层序级别的有机相变化及其地质意义.沉积学报,2000,18(2):297-301.
    [55]李美俊.大民屯凹陷层序地层有机地球化学及油气成藏特征.北京:中国地质大学,2003:135.
    [56]郝黎明,邵龙义.基于层序地层格架的有机相研究进展.地质科技情报,2000,19(4):60-64.
    [57]郝芳,陈建渝.层序和体系域的有机相构成及其研究意义.地质科技情报,1995,14(3):79-83.
    [58]杨建业,任德贻,邵龙义.沉积有机相在陆相层序地层格架中的分布特征.沉积学报,2000,18(4):585-589.
    [59]赵厚银,王延斌,邵龙义.渤海湾盆地C-P不同体系域有机显微组分与生烃性.中国矿业大学学报,2004,33(1):66-69.
    [60]PASSEY Q R. A practical model for organic richness fromporosity resistance logs. AAPG Bulletin,1990,77(3):1777-1794.
    [61]CREANEY S, PASSEY Q R. Recurring pat terns of total organic carbon and source rock quality within a sequence stratigraphic framework. AAPG Bulletin,1993,77(3):386-401.
    [62]杨长俊,陈发亮,申守广.东濮凹陷下第三系层序地层及深层油气资源潜力分析.中国海上油气(地质),2003,17(6):376-388.
    [63]冯有良.断陷盆地层序格架中岩性地层油气藏分布特征.石油学报,2005,26(4):17-22.
    [64]Passey Q. R., Creaney S., Kulla J. B. A practical model for organic richness from porosity and resistivity logs. AAPG Bulletin, Vol.74, No.12, December 1990,1777-1794.
    [65]许晓宏,黄海平,卢松年.测井资料与烃源岩有机碳含量的定量关系研究.江汉石油学院学报,1998,20(3):8-12.
    [66]张志伟,张龙海.测井评价烃源岩的方法及其应用效果.石油勘探与开发,2000,27(3):84-87.
    [67]运华运,项建新,刘子文.有机碳测井评价方法及在胜利油田的应用.测井技术,2000,24(5):372-381.
    [68]王贵文,朱振宇,朱广宇.烃源岩测井识别与评价方法研究.石油勘探与开发,2002,29(4):50-52.
    [69]岳炳顺,黄华,陈彬等.东濮凹陷测井烃源岩评价方法及应用.石油天然气学报,2005,27(3):351-354.
    [70]王伟峰,辛也.应用测井评价东营凹陷民丰洼陷烃源岩.西部探矿工程,2006,10:99-100.
    [71]秦建中,王静,李欣等.渤海湾盆地饶阳凹陷未熟-低熟油成烃成藏条件研究.石油实验地质,2003,11(1):566-572.
    [72]张文朝,崔周旗,韩春元等.冀中坳陷老第三纪湖盆演化与油气.古地理学报,2001,3(1):45-49.
    [73]纪友亮,杜金虎,赵贤正等.冀中坳陷饶阳凹陷古近系层序地层学及演化模式.古地理学报,2006,8(3):397-406.
    [74]纪友亮,张世奇.层序地层学原理及层序成因机制模式.北京:地质出版社,1998:1-195.
    [75]中国石油天然气集团公司,油气储层重点实验室编.陆相层序地层学应用指南,北京:石油工业出版社,2002:1-82.
    [76]赵霞飞.动力沉积学与陆相沉积.北京:科学出版社,1992:1-135.
    [77]张大智,纪友亮,张瑞峰等.饶阳凹陷古近系层序地层研究.石油勘探与开发.1996.23(5):23-28.
    [78]Cross T A,Lessenger M A.Sediment volume partitioning:rationale for stratigraphic model evaluation and high-Resolution stratigraphic correlation[A].Gradstein F M,Sandvik K O,Milton N J,eds.Sequence Stratigraphy Concepts and Applications[M].NPF Special Publication,1998,8:171-195.
    [79]陈世悦.华北地块南部晚古生代至三叠纪沉积构造演化.中国矿业大学学报,2000.29(5):536-540.
    [80]张世奇,纪友亮.陆相断陷湖盆层序地层学模式探讨.地质调查与研究,2008.31(1):33-42.
    [81]Katz, B. J. Lacustrine basin hydrocarbon exploration-current thoughts. Journal of Paleolimnology,2001, 26(2):161-179.
    [82]Peters, K.E., Walters, C.C. and Moldowan, J.M. The biomarker guild (Second edition). I Biomarkers and Isotpes in the Environment and Human History [M]. Ed. by K.E. Peters, C.C. Walters and J.M. Moldowan, Cambridge university press,2005.
    [83]Peters, K. E., Magoon, L. B., Bird, K. J.,et al. North Slope, Alaska:Source rock distribution, richness.thermal matutity, and petroleum charge. AAPG Bulletin,2006,90(2):261-292.
    [84]Creaney and Passey. Recurring Patterns of Total Organic Carbon and Source Rock Quality within a Sequence Stratigraphic Framework. AAPG Bulletin,1993,77(3):386-401.
    [85]梁狄刚,曾宪章,王雪平等.冀中坳陷油气的生成.北京:石油工业出版社,2001:1-79.
    [86]Dembicki H Jr.Anderson M J.Seconddary migration of oil:Experiments supporting efficient movement of separate,buoyant oil phase along limited conduits.AAPG Bulletin,1989,73(8):1018-1021.
    [87]曾溅辉,王洪玉.输导层和岩性圈闭中石油运移和聚集模拟试验研究.地球科学,1999,24(2):193-196.
    [88]张发强,罗晓容,苗盛等.石油二次运移的模式及其影响因素.石油试验地质,2003,25(1):69-75.
    [89]李铁军,罗晓容.碎屑岩输导层内油气运移聚集非均一性的定量分析.地质科学,2001,36(4):402-413.
    [90]Galeazzi J S.Structural and stratigraphic evolution of the western Malvinas basin, Argentina.AAPG Bulletin,1998,82(4):596-636.
    [91]付广,薛永超,付晓飞.油气运移输导系统及其对成藏的控制.新疆石油地质,2001,22(1):24-26.
    [92]张卫海,查明,曲江秀.油气输导体系的类型及配置关系.新疆石油地质,2003,24(2):118-120.
    [93]Scherer M.Parameters influencing porosity in sandstones:A model for sandstone porosity prediction[J].AAPG Bulletin,1987,71:485-491.
    [94]Allan U S.Model for hydrocarbon migration and entrapment within faulted structures.AAPG Bulletin,1989,73:803-811.
    [95]Knipe R J,Juxtaposition and seal diagrams to help analyze fault seals in hydrocarbon reservoirs.AAPG Bulletin,1997,81:187-495.
    [96]吕延防,李国会,王跃文等.断层封闭性的定量研究方法.石油学报,1996,17(3):39-45.
    [97]高先志.焉耆盆地博湖坳陷断层封闭性与油气藏形成.新疆石油地质,2003,24(1):35-37.
    [98]Roberts S J.,Nunn J A.,Cathles L.et al.Expulsion of abnormally pressured fluids along faults[J]. Journal of Geophysical Research,1996,101:2231-2252.
    [99]李明诚著.石油与天然气运移(第3版)[M].北京:石油工业出版社,2004.
    [100]张守安,杨克明,苟华伟等.塔里木盆地不整合油气藏特征.海洋地质与第四纪地质,1996,23(5):16-19.
    [101]张克银,艾华国,吴亚军.碳酸盐岩顶部不整合面结构层及控油意义.石油勘探与开发,1996,16(3):91-100.
    [102]赵荣,齐景顺,曾庆真.流体势能场分析方法的改进.大庆石油学院学报,2004,28(1):100-102.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700