二连盆地乌里亚斯太凹陷中洼沉积体系及油气成藏条件分析
|
摘要
实践表明,对二连盆地而言,新凹陷的突破所增长的储量远远大于已出油凹陷扩边挖潜所发现的新增储量。乌里亚斯太南洼槽岩性圈闭已经取得突破,乌里亚斯太中洼与南洼相比具有相似的地质结构,应该是进一步扩大勘探成果的重要领域。根据乌里亚斯太凹陷中洼槽钻井资料较少、地震资料上各种反射特征丰富的特点,应用层序地层学建立了等时地层格架;在等时地层格架内对烃源岩、储集层、非构造圈闭等成藏条件进行了分析,建立了成藏模式;在充分分析已钻井成功和失败经验的基础上对有利区带和有利钻探目标进行了预测。
总体上洼槽断层欠发育,为一西断东超的萁状结构,平面上自西向东可进一步划分为陡坡带、中央洼槽带和斜坡带。其中陡坡带范围较小,中央洼槽带和斜坡带范围较大。由于本区断层不发育,导致构造圈闭相对较少。但由于具有比较宽缓的大斜坡,是岩性圈闭发育的有利地区。
从侏罗系到腾一段,本区共识别出12个层序界面和11个洪泛面,由此将中生界划分为11个中期基准面旋回(相当于三级旋回),即11个三级层序。储集岩的成因类型主要有扇三角洲、水下扇和浊积扇等。其中阿尔善组及腾一下段发育4个中期旋回,共发育了33个岩性体。在岩心观察、层序地层学分析和沉积体系分析的基础上建立典型单断萁状“凹陷”结构陡、缓两侧物源、以缓坡物源为主的沉积模式。
对中洼槽的烃源岩、储集岩和岩性圈闭等成藏条件进行了全面的描述和评价,确定阿尔善组和腾一段是本区的有效烃源岩和储集岩发育层段。其中洼槽总生油量为15×10~8t,总聚集量为1-1.4×10~8t。分析认为中洼槽断裂不发育,储层厚度薄、分布范围小,油气运移距离短;储集岩的储集性能为中-低孔、低渗型;以原地生储盖组合为特征;油藏类型应为近源原生油气藏。确定阿尔善组和腾一段是本区最主要的勘探目的层系。在综合各项成藏条件的基础上,建立了成藏模式。中洼槽东部为一大型斜坡,断层不发育,为岩性体的形成提供了良好的条件。斜坡下倾部位发育了大量的扇体,它们位于成熟生油岩和处于生油高峰的生油岩之中,具有良好的油源条件,在一定的构造背景之上的岩性油气藏是洼槽油气勘探的主要领域。
The resource increased in a depression of ErLian basin is greater than those discoveredoil&gas depression in fact. The southern depression of Wuliyastai depression, which has the samegeology buildup as center depression, gets a big discovery in the lithologic trap, it is the mostimportant field to enlarging the exploration outcome. Based on the limited drilling data and thecomplex reflections on seismic profile, the equitime frames were set up by using the theory ofsequence stratigraphy;in these frames, the condition of reservoir such as the initial rock of gasand oil, reservoir and non-structure trap were analyzed. Then the pattern of reservoir was made.Predication for voluble area and voluble drilling target was made based on the analysis of thedrilled wells, success or failure.
Generally, on the upper part of the center depression, faults are not rich. It's a structurelooks like a winnowing fan, breaking in west and overlapping in east, it can be divided into acticregion, middle low-laying land and ramp region, the last two are bigger than first. The shortage offaults caused the lack of big structure trap. Lithologic traps were well developed because of thebig broad slop.
There are 12th sequences and 11 pluvial planes from Jurassic system to Tengyi zone.Mesozoic was divided into 11 middle period basal level cycles, or 11 third sequences. Thereservoir rock has three types: deltaic fan, subsea apron and turbidite fan. 4 middle period cyclesdevelop in Aershan and Tenyixia with 33 lithologic trap in it. A new deposit pattern described as atypical half graben was set up after core research, sequence stratigraphy and deposit systemanalyze. The provenances of the depression come from gentle slope more than steep slope.
Descriptions and evaluations were made to the formation condition of reservoir such assource rock, reservoir rock and lithologic traps in middle low-laying land. Aershan and Tenyiwere confirmed have the valid source rock and reservoir rock. The generation of the low-layingland is 5×10~8t, the accumulation is 1-1.4×10~8t. The features of the middle low-laying land areshort of faults, thin reservoir bed, limited distribution range and closed oil translate distance. Thecharacters of the reservoir rock are middle –low porosity and low permeability, and it is theoriginal place production. Aershan and Tenyi are the most important target layer of exploration inthis area. The pattern of reservoir formation is set up on the generalization of all the factorsaffecting the formation. There is a huge slope at the east of middle law-laying land and less offaults, it is good for develop lithologic trap. Many fans scatters at the far end of the slope, theylocated in mature and high produced generating rock, and got plenty resource;Lithologic traps,above of tectonic setting, will become the main area of exploration in low-laying land.
总体上洼槽断层欠发育,为一西断东超的萁状结构,平面上自西向东可进一步划分为陡坡带、中央洼槽带和斜坡带。其中陡坡带范围较小,中央洼槽带和斜坡带范围较大。由于本区断层不发育,导致构造圈闭相对较少。但由于具有比较宽缓的大斜坡,是岩性圈闭发育的有利地区。
从侏罗系到腾一段,本区共识别出12个层序界面和11个洪泛面,由此将中生界划分为11个中期基准面旋回(相当于三级旋回),即11个三级层序。储集岩的成因类型主要有扇三角洲、水下扇和浊积扇等。其中阿尔善组及腾一下段发育4个中期旋回,共发育了33个岩性体。在岩心观察、层序地层学分析和沉积体系分析的基础上建立典型单断萁状“凹陷”结构陡、缓两侧物源、以缓坡物源为主的沉积模式。
对中洼槽的烃源岩、储集岩和岩性圈闭等成藏条件进行了全面的描述和评价,确定阿尔善组和腾一段是本区的有效烃源岩和储集岩发育层段。其中洼槽总生油量为15×10~8t,总聚集量为1-1.4×10~8t。分析认为中洼槽断裂不发育,储层厚度薄、分布范围小,油气运移距离短;储集岩的储集性能为中-低孔、低渗型;以原地生储盖组合为特征;油藏类型应为近源原生油气藏。确定阿尔善组和腾一段是本区最主要的勘探目的层系。在综合各项成藏条件的基础上,建立了成藏模式。中洼槽东部为一大型斜坡,断层不发育,为岩性体的形成提供了良好的条件。斜坡下倾部位发育了大量的扇体,它们位于成熟生油岩和处于生油高峰的生油岩之中,具有良好的油源条件,在一定的构造背景之上的岩性油气藏是洼槽油气勘探的主要领域。
The resource increased in a depression of ErLian basin is greater than those discoveredoil&gas depression in fact. The southern depression of Wuliyastai depression, which has the samegeology buildup as center depression, gets a big discovery in the lithologic trap, it is the mostimportant field to enlarging the exploration outcome. Based on the limited drilling data and thecomplex reflections on seismic profile, the equitime frames were set up by using the theory ofsequence stratigraphy;in these frames, the condition of reservoir such as the initial rock of gasand oil, reservoir and non-structure trap were analyzed. Then the pattern of reservoir was made.Predication for voluble area and voluble drilling target was made based on the analysis of thedrilled wells, success or failure.
Generally, on the upper part of the center depression, faults are not rich. It's a structurelooks like a winnowing fan, breaking in west and overlapping in east, it can be divided into acticregion, middle low-laying land and ramp region, the last two are bigger than first. The shortage offaults caused the lack of big structure trap. Lithologic traps were well developed because of thebig broad slop.
There are 12th sequences and 11 pluvial planes from Jurassic system to Tengyi zone.Mesozoic was divided into 11 middle period basal level cycles, or 11 third sequences. Thereservoir rock has three types: deltaic fan, subsea apron and turbidite fan. 4 middle period cyclesdevelop in Aershan and Tenyixia with 33 lithologic trap in it. A new deposit pattern described as atypical half graben was set up after core research, sequence stratigraphy and deposit systemanalyze. The provenances of the depression come from gentle slope more than steep slope.
Descriptions and evaluations were made to the formation condition of reservoir such assource rock, reservoir rock and lithologic traps in middle low-laying land. Aershan and Tenyiwere confirmed have the valid source rock and reservoir rock. The generation of the low-layingland is 5×10~8t, the accumulation is 1-1.4×10~8t. The features of the middle low-laying land areshort of faults, thin reservoir bed, limited distribution range and closed oil translate distance. Thecharacters of the reservoir rock are middle –low porosity and low permeability, and it is theoriginal place production. Aershan and Tenyi are the most important target layer of exploration inthis area. The pattern of reservoir formation is set up on the generalization of all the factorsaffecting the formation. There is a huge slope at the east of middle law-laying land and less offaults, it is good for develop lithologic trap. Many fans scatters at the far end of the slope, theylocated in mature and high produced generating rock, and got plenty resource;Lithologic traps,above of tectonic setting, will become the main area of exploration in low-laying land.
引文
1.费宝生等.二连裂谷盆地群油气地质.石油工业出版社.2001.2
2.张文朝、祝玉衡等.二连盆地下白垩统沉积相及含油性.北京.科学出版社,2000
3.张文朝.二连盆地扇三角洲储层沉积特征.断块油气田,1998(3)
4.张文朝、祝玉衡、江东华等.二连盆地“洼槽”控油规律与油气勘探前景.石油学报,1997(4)
5.翟光明等著.中国石油地质志,卷一,总论.北京:石油工业出版社.1996.
6.戴金星.99.海相碳酸盐岩与油气国际研讨会开幕词.海相油气地质.2001.5(l-2).1.
7.邱中建,龚再升主编.中国油气勘探.北京:石油工业出版社,地质出版社.1999.
8.杜金虎等著.二连盆地隐蔽油气藏.石油工业出版社.2003.5.
9.罗立民.河湖沉积体系三维高分辨率层序地层学.地质出版社.
10.徐怀大.层序地层学理论用于我国断陷盆地分析中的问题.石油天然气地质.1991.12(l).
11.L.L.Sloss.Sequence in the cratonic interior of North America. GSA Bulletin,1963,74:93·113.
12.徐怀大.层序地层学原理,译者前言.北京:石油工业出版社.1993.
13.钱凯.层序地层学的产生、发展与应用(代序).见:顾家裕,邓宏文,朱彼敏主编.层序地层学及其在油气勘探开发中的应用.北京:石油工业出版社.l997.14.
14.C.E.佩顿编(1977),牛毓茎等译.地震地层学.北京:石油工业出版社.l980.
15.徐怀大主编.从地震地层学到层序地层学.北京:石油工业出版社.1997.
16.张万选、张厚福、曾洪流等.陆相断陷盆地区域地震地层学研究.山东:石油大学出版社.1988.
17.C.K.Wilgus et a1, eds.Sea-level changes: an integrated approach-SEPM Special Publication42,1988.
18.W.E.Galloway.Genetic stratigraphic sequences in basin analysis I: architecture and genesis of fIooding-surface bounded depostional units.AAPG Bulletin.1989a.73(2).125A42.
19.W.E.Galloway.Genetic stratigraphic sequences in basin analysis II: application to northwest Gu1f of Mexico Cenozoic basin AAPG Bulletin.1989b.73(2).143-154.
20. 邓 宏 文 . 美 国 层 序 地 层 学 研 究 中 的 新 学 派 一 高 分 辨 率 层 序 地 层 学 . 石 油 与 天 然 气 地质 .1995.16(2):89-97.
21.T.A.Cross And M.A.lesssenger Sediment volume partitioning: rational for stratigraphic model evaluation and high-resolution statigraphic correlation. Accepted for publication in Norwegian petroleum-forening conference volume "Predictive High-Resolution Sequence Stratigraphy", July,1996.
22.K.W.Shadey et al. Perspective on the sequence stratigraphy of continental strata. AAPG Bulletin.1994.74(4).544568.
23.J.C.Van Wagoner et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series7.1990.
24.冯增昭、王英华、刘焕杰等.中国沉积学.石油工业出版社.1994
25.赵澄林、刘孟惠.内蒙阿南凹陷中生代储层沉积特征和地质模式.石油大学学报.1991
26.洪庆玉.沉积物重力流地质学.成都科技大学出版社.1992
27.赵澄林等.二连盆地储层沉积学.石油工业出版社.1996
28. 蔡希源等.陆相盆地高精度层序地层学-隐蔽油气藏勘探基础、方法与实践.地质出版社.2003
29.龚再升,李思田等著.南海北部大陆边缘盆地分析与泊气聚集.北京:军斗学出版社.1997.
30.姜在兴、操应长.砂体层序地层及沉积学研究一以山东惠民凹陷为例.地质出版社.2000.6.
31.Xue Liangqing and Galloway W E Genetic sequence stratigraphic framework, depositional style, and hydrocarbon occurrence of the Upper Cretaceous QYN formations in the Songliao lacustrine basin, nortleastern China.AAPG Bulletin,1993,77(10)17924808.
32.王东坡、刘招君、刘立等.松辽盆地演化与海平面升降.北京:地质出版社.1991.
33.魏魁生.非海相层序地层学一以松辽盆地为例.北京:地质出版社.1996.
34.蔡希源、陈章明、王玉华等.松辽两江地区石油地质分析.北京:石油工业出版社.1999.
35.刘招君.湖盆层序地层学术语体系及模式一以松辽盆地西部斜坡区为例.长春地质学院学报.Vol-27.增刊II.1997.10.
36.李思田等著.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.
37.顾家裕等著.塔里木盆地沉积层序特征及其演化.北京:石油工业出版社.1996.
38.顾家裕.陆相盆地层序地层学格架概念及模式.石油勘探与开发.1995.22(4).
39.解习农等.陆相盆地幕式构造旋回与层序构成.地球科学一中国地质大学学报.1996.21(1).27-33.
40.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.
41.郭巍、刘招君.松辽盆地西部斜坡区拗陷期层序地层发育控制因素分析.长春地质学院学报.Vo1.27.N0.3.1997.
42.李增学.含煤盆地层序地层学.地质出版社.2000.9.
43.Hongiiu Zeng ,Milo M.Bachus, Kenneth T.Barrow and Noel Tyler: Stratal slicing, part1: Realistic 3-D seismic model. Geophysics. 1998a. 63(2)502-513.
44.Hongiiu Zeng, Stephen C.Henry,and John P.Riola. Stratal slicing,part2:Realistic LD seismic model.Geopt13sics-1998b.63(2):514 δ 22.
45.Hongliu Zeng ,Tucker F.Hentz, and Lesli J. Wood, Stratal slicing of Miocene-Pliocene sediments in Vermilion Block 50 -Tiger Shoal Area, offshore louisiana,2001,The Leading Edge.
46.Kolla V, Ph Bourges J M Urruty and P Safa ,Evolution of deep water Tertiary sinuous channels offshore Angola (west Africa)and implications for reservoir architecture,2001 AAPG Bulktin,V.85,N08 1373-1405.
47.H.W.Posamentier,Ancient shelf ridges-A potentially significant component of the transgresstive systems tract: Case study from offshore northwest Java,2002AAPG Bulletin, V.86,N0175·106.
48.魏魁生、徐怀大.华北地区典型箕状断陷盆地层序地层学模式及其与油气赋存关系.地球科学.18(2)
49.Ulrik Gregenen, Jarl C.S6ESElsen,Olaf Micklsen,1998,Details of Pliocene sequences resolved on a 3-D data set, central North Sea. Sequence Stratigraphy-Concepts and Applications edited by F M. Gradstin, K.O Sandvik and N J. Milton-NPF Special Publication 8, p.403-412,pubustled by Elsevier Science B.V.,Amsterdam. Norwegian Petroleum Society(NPF) ,1998.
50.N L HaskeIl, S.E.Nissen ,J.A.IDpez,M.S Bahonrich 3-D seismic coherency and the imaging of sedimentological features. Sequence Stratigraphy 一 Concepts and Applications edited by F.M.Gradstin, K.O. Sadvik and N J. MEton-NPF Special Publication 8,pp.197314, Published by Elsevier Science B.V., Amsterdam. Norwgian Petroleum Society(NPF) ,1998.
51.Strven W. Smith, Lazy Danaey. An example of 3D AVO for lithology discrimination in Widuri Field, Asri Basin, Indonesia. The Leading Edge. 1996: 283-288.
52.郑容才、彭军、吴朝容.陆相盆地基准面旋回的级次划分和研究意义.沉积学报.mol.19(2):249-255.
53.The Herbert, Eichenseer, Jean-Pierre Leduc, Automated genetic sequence stratigraphy applied to wireline logs. Bull. centres Rech. Expbr. Prod. Elf aquitaine.1996,20(2)278-307.
54.Xue Liangqing, Chi Yingliu, and Cao Yinghui, Sequence stratigraphic framework and hydrocarbon distribution of the Tertiary nonmarine strata in the Bohai Bay Rift Basin, Scientia Geo1ogica Sinica,2001,10(2).
55.J.A.Howelland J.F. Aitken. High Resolution Sequence Stratigraphy: Innovations and Applications. Geological Society SpeclalPublication.1996.No.104.
56.朱筱敏.层序地层学原理及应用.石油工业出版社,1998.
57.田在艺、常承永、钱绍新.隐蔽油气藏的勘探,大庆石油地质与开发编辑部编.中国隐蔽油气藏勘探论文集.黑龙江科学技术出版社 ,1984.
58.Bergman,K.M. and Walker,R.G.High-resolution sequence stratigrphic analysis of the Shannon Sandstone in Wyoming,using a template for region correlation. Journal of Sedimentary Research,1995,v.b65,No.2:255-264
59.Boyd,R.et al. Relation of sequence stratigrphy to modern sedimentary environments. Geology,1989,V.17:926-92
60.Cross,T.A.Stratigraphicarchitecture,correlation congcepts,volumetricpartitoning,facies differentiation and reservoir commpartmentalization from the perspective of high-resolution sequence stratigraphy.
61.Cross,T.A Application of high-resolution sequence stratigraphy to reservoir analysis. Subsurface Reservoir Characterization from outcrop observation:Proceedings of th 7th Exploration and Production Reserach Conference :Paris,Technip,11-13.
62.Hentz,T.F.Sequence stratigraphy of the Upper Pennsylvannian Cleveland Formation: a major tight-gas sandstone, Western Anadarko basin,Texas Panhandle. AAPG Bulletin, 1994,V.78, No.4:569-595
63.Koss,J.E.et al.An experimental studty of the efficts of base-level Change on fluvial,coastal plain and shef systems.Journal of Sedimenary research,1994,V,B64,No.2:90-98
64.Morton,R.A. and Suter,J.R.Sequence stratigraphy and composition of late Ouaternary shef-Margin deltas, Northern gulf of mexico.AAPG Bullitin,1996,V.80,No.4:505-530
65.Nichol,S.L.et al. Sequence stratigraphy of a coastal-plain incised vally estuary:Lake Calcasieu,Louisiana.Journal of Sedimentary Research,1996,V.66,No.4:847-857
66.Olsen,T.et al. Sequence archtecture in a fluvial succession:sequence stratigraphy in the Upper Cretacious Mesarerde groupe,price Canyon,Utah.Journal of Sedimentary Research, 1995,V.B65,No.2:265-279
67.Rigsby,C.A.Deepening-upward sequences in Oligocence and Lower Miocence fan delta deposits,western Santa Ynez Mountains,california.Journal of Sedimentary Research, 1992, V.B64,No.3:380-391
68.Sun,S.O.and Esteban,M.Paleoclamatic controls on sedimentation,diagenesis,and reservoir quality:Lessons from Miocence carbonates.AAPG bullitin.194,V.78,No.4:519-543
69.Shanley,K.W.and Mccable,P.J. perspectives on the sequence stratigrphy of continental strata.AAPG Bullitin,V.78,no.4:544-568
70.Weller,H.E.Base level,lithosphere surface,and time-stratigraphy.Geological Society of Amarica Bullitin,1964,V.75:599-610
71.Walker,R,G.Facies,dacies model and modern stratigraphic concepts.In Walker,R.G. eds.facies model:Response to ssea level.Geological Association of Canada,1992
72.Vail P.R. Seismic stratigraphy interpretation using sequence stratigraphy ,part 1,Seismic stratigrphy interpretation procedure in A.W.Bally,ed,Atalas of seismic stratigraphy:AAPG studies in geology 27,1987,(1):1-10
73.胡见义,徐树宝,刘淑兰等.非构造油气藏.北京:石油工业出版社,1986:81～83
74.曾溅辉,郑和荣,王宁.东营凹陷岩性油气藏成藏动力学特征.石油与天然气地质,1998,19(4):326～329
75.李丕龙.断陷湖盆油气聚集模式及其动力学特征.石油大学学报,2000,24(4):26～29
76.西门诺维奇BB主编.非背斜油气藏.北京:石油工业出版社,1986:161～224
77.邓宏文、王红亮、祝永军、Cross T A.高分辨率层序地层学――原理及应用.北京.地质出版社. 2002.
78.王捷,关德范.油气生成运移聚集模型研究.北京:石油工业出版社,1999:198～199
79.田世澄.论成藏动力系统.勘探家,1996,1(2):20～25
80.张义纲,陈彦华,陆嘉炎.油气运移及其聚集成藏模式.南京:河海大学出版社,1997
81.张云峰,付广.砂岩透镜体油藏聚油机理及成藏模式.断块油气田,2000,7(2):12～14 1990
82.曹颖辉,池英柳,薛良清,王洪江.沉积基准面在层序划分对比及地层岩性油气藏预测中的应用,石油实验地质,2002,24(1)
83.田在艺,常承永,钱绍新.隐蔽油气藏的勘探[A].大庆石油地质与开发编辑部编.中国隐蔽油气藏勘探论文集[C].哈尔滨:黑龙江科学技术出版社,1984.39-49
84. 林 畅 松 , 张 燕 梅 , 刘 景 彦 , 庞 保 成 . 高 精 度 层 序 地 层 学 与 储 层 预 测 . 地 学 前缘.2000.vol.7.No.3:111-117
85.庞雄奇.岩性油气藏成因机理研究现状及展望.油气地质与采收率.2002,9(5).
86.陈广军等.斜坡带低位扇砂岩体岩性油气藏勘探方法.石油学报.2002,23(3).
87.隋风贵,李洲海,朱明.箕状断陷盆地陡坡带砂砾岩扇体油藏研究.见潘元林主编:中国隐蔽油藏,67-76
88.蒲仁海.断陷湖盆层序地层学的几点进展.石油与天然气地质.23(4):410-414
89.徐怀大、赵政璋、樊太亮.从地震地层学到层序地层学――油气盆地的定性化与定量化描述.石油工业出版社.1997
90.Wheel H E. Base level, lithosphere surface and time-stratigraphy. Bull Geol Soc, 1964. 75:599-610
91.Walkev R. G.(ed). Facies Models Geosci, Can Reprint Ser.,1979, 1 Geol Ass Can Ontario
92.Quirk D C. “Bace level”: a unifying concept in alluvial sequence stratigraphy. In: Howell J A, Aitken J F, eds. High resolution sequence stratigraphy: innovations and applications. Geological Society Special Publication,1996,(104):37-50
93.Ravnas R, Steel R J. Architecture of marine rift-basin successions:1998, AAPG Bulletin, Vol. 82, No. 1:110-146
94.Reading H. G. (ed), Sedimentary Environments: Processes, Facies and Stratigraphy, 1996, Blackwell Sciences, 688P
95.赵文智、何登发、李小弟登.石油地质综合研究导论 1999,石油工业出版社
96.于兴河等,碎屑岩系油气储层沉积学. 2002,地质出版社
97.邓宏文、王红亮、翟爱军等.中国陆源碎屑盆地层序地层于储层展布.1999.石油与天然气地质,20(2),108-114
98.樊太亮、李卫东.层序地层应用于陆相油藏预测的成功实例.1999.石油学报.20(2):12-17
99.樊太亮、吕延仓、丁明华.层序地层体制中的陆相储层发育规律[J].2000.地学前缘.7(4):315-321
100.邓宏文、王红亮、宁宁.沉积物体积分配原理-高分辨率层序地层学的理论基础.2000.地学前缘.7 (4).305-313
101.樊太亮等.沉积基准面变化分析技术及应用.1997.石油与天然气地质.Vol.18.No.2:108-113
102.郑小武、邓宏文等. 测井高分辨率层序地层自动划分技术与应用尝试.1999.石油与天然气地质.20(4).357-360
2.张文朝、祝玉衡等.二连盆地下白垩统沉积相及含油性.北京.科学出版社,2000
3.张文朝.二连盆地扇三角洲储层沉积特征.断块油气田,1998(3)
4.张文朝、祝玉衡、江东华等.二连盆地“洼槽”控油规律与油气勘探前景.石油学报,1997(4)
5.翟光明等著.中国石油地质志,卷一,总论.北京:石油工业出版社.1996.
6.戴金星.99.海相碳酸盐岩与油气国际研讨会开幕词.海相油气地质.2001.5(l-2).1.
7.邱中建,龚再升主编.中国油气勘探.北京:石油工业出版社,地质出版社.1999.
8.杜金虎等著.二连盆地隐蔽油气藏.石油工业出版社.2003.5.
9.罗立民.河湖沉积体系三维高分辨率层序地层学.地质出版社.
10.徐怀大.层序地层学理论用于我国断陷盆地分析中的问题.石油天然气地质.1991.12(l).
11.L.L.Sloss.Sequence in the cratonic interior of North America. GSA Bulletin,1963,74:93·113.
12.徐怀大.层序地层学原理,译者前言.北京:石油工业出版社.1993.
13.钱凯.层序地层学的产生、发展与应用(代序).见:顾家裕,邓宏文,朱彼敏主编.层序地层学及其在油气勘探开发中的应用.北京:石油工业出版社.l997.14.
14.C.E.佩顿编(1977),牛毓茎等译.地震地层学.北京:石油工业出版社.l980.
15.徐怀大主编.从地震地层学到层序地层学.北京:石油工业出版社.1997.
16.张万选、张厚福、曾洪流等.陆相断陷盆地区域地震地层学研究.山东:石油大学出版社.1988.
17.C.K.Wilgus et a1, eds.Sea-level changes: an integrated approach-SEPM Special Publication42,1988.
18.W.E.Galloway.Genetic stratigraphic sequences in basin analysis I: architecture and genesis of fIooding-surface bounded depostional units.AAPG Bulletin.1989a.73(2).125A42.
19.W.E.Galloway.Genetic stratigraphic sequences in basin analysis II: application to northwest Gu1f of Mexico Cenozoic basin AAPG Bulletin.1989b.73(2).143-154.
20. 邓 宏 文 . 美 国 层 序 地 层 学 研 究 中 的 新 学 派 一 高 分 辨 率 层 序 地 层 学 . 石 油 与 天 然 气 地质 .1995.16(2):89-97.
21.T.A.Cross And M.A.lesssenger Sediment volume partitioning: rational for stratigraphic model evaluation and high-resolution statigraphic correlation. Accepted for publication in Norwegian petroleum-forening conference volume "Predictive High-Resolution Sequence Stratigraphy", July,1996.
22.K.W.Shadey et al. Perspective on the sequence stratigraphy of continental strata. AAPG Bulletin.1994.74(4).544568.
23.J.C.Van Wagoner et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series7.1990.
24.冯增昭、王英华、刘焕杰等.中国沉积学.石油工业出版社.1994
25.赵澄林、刘孟惠.内蒙阿南凹陷中生代储层沉积特征和地质模式.石油大学学报.1991
26.洪庆玉.沉积物重力流地质学.成都科技大学出版社.1992
27.赵澄林等.二连盆地储层沉积学.石油工业出版社.1996
28. 蔡希源等.陆相盆地高精度层序地层学-隐蔽油气藏勘探基础、方法与实践.地质出版社.2003
29.龚再升,李思田等著.南海北部大陆边缘盆地分析与泊气聚集.北京:军斗学出版社.1997.
30.姜在兴、操应长.砂体层序地层及沉积学研究一以山东惠民凹陷为例.地质出版社.2000.6.
31.Xue Liangqing and Galloway W E Genetic sequence stratigraphic framework, depositional style, and hydrocarbon occurrence of the Upper Cretaceous QYN formations in the Songliao lacustrine basin, nortleastern China.AAPG Bulletin,1993,77(10)17924808.
32.王东坡、刘招君、刘立等.松辽盆地演化与海平面升降.北京:地质出版社.1991.
33.魏魁生.非海相层序地层学一以松辽盆地为例.北京:地质出版社.1996.
34.蔡希源、陈章明、王玉华等.松辽两江地区石油地质分析.北京:石油工业出版社.1999.
35.刘招君.湖盆层序地层学术语体系及模式一以松辽盆地西部斜坡区为例.长春地质学院学报.Vol-27.增刊II.1997.10.
36.李思田等著.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.
37.顾家裕等著.塔里木盆地沉积层序特征及其演化.北京:石油工业出版社.1996.
38.顾家裕.陆相盆地层序地层学格架概念及模式.石油勘探与开发.1995.22(4).
39.解习农等.陆相盆地幕式构造旋回与层序构成.地球科学一中国地质大学学报.1996.21(1).27-33.
40.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.
41.郭巍、刘招君.松辽盆地西部斜坡区拗陷期层序地层发育控制因素分析.长春地质学院学报.Vo1.27.N0.3.1997.
42.李增学.含煤盆地层序地层学.地质出版社.2000.9.
43.Hongiiu Zeng ,Milo M.Bachus, Kenneth T.Barrow and Noel Tyler: Stratal slicing, part1: Realistic 3-D seismic model. Geophysics. 1998a. 63(2)502-513.
44.Hongiiu Zeng, Stephen C.Henry,and John P.Riola. Stratal slicing,part2:Realistic LD seismic model.Geopt13sics-1998b.63(2):514 δ 22.
45.Hongliu Zeng ,Tucker F.Hentz, and Lesli J. Wood, Stratal slicing of Miocene-Pliocene sediments in Vermilion Block 50 -Tiger Shoal Area, offshore louisiana,2001,The Leading Edge.
46.Kolla V, Ph Bourges J M Urruty and P Safa ,Evolution of deep water Tertiary sinuous channels offshore Angola (west Africa)and implications for reservoir architecture,2001 AAPG Bulktin,V.85,N08 1373-1405.
47.H.W.Posamentier,Ancient shelf ridges-A potentially significant component of the transgresstive systems tract: Case study from offshore northwest Java,2002AAPG Bulletin, V.86,N0175·106.
48.魏魁生、徐怀大.华北地区典型箕状断陷盆地层序地层学模式及其与油气赋存关系.地球科学.18(2)
49.Ulrik Gregenen, Jarl C.S6ESElsen,Olaf Micklsen,1998,Details of Pliocene sequences resolved on a 3-D data set, central North Sea. Sequence Stratigraphy-Concepts and Applications edited by F M. Gradstin, K.O Sandvik and N J. Milton-NPF Special Publication 8, p.403-412,pubustled by Elsevier Science B.V.,Amsterdam. Norwegian Petroleum Society(NPF) ,1998.
50.N L HaskeIl, S.E.Nissen ,J.A.IDpez,M.S Bahonrich 3-D seismic coherency and the imaging of sedimentological features. Sequence Stratigraphy 一 Concepts and Applications edited by F.M.Gradstin, K.O. Sadvik and N J. MEton-NPF Special Publication 8,pp.197314, Published by Elsevier Science B.V., Amsterdam. Norwgian Petroleum Society(NPF) ,1998.
51.Strven W. Smith, Lazy Danaey. An example of 3D AVO for lithology discrimination in Widuri Field, Asri Basin, Indonesia. The Leading Edge. 1996: 283-288.
52.郑容才、彭军、吴朝容.陆相盆地基准面旋回的级次划分和研究意义.沉积学报.mol.19(2):249-255.
53.The Herbert, Eichenseer, Jean-Pierre Leduc, Automated genetic sequence stratigraphy applied to wireline logs. Bull. centres Rech. Expbr. Prod. Elf aquitaine.1996,20(2)278-307.
54.Xue Liangqing, Chi Yingliu, and Cao Yinghui, Sequence stratigraphic framework and hydrocarbon distribution of the Tertiary nonmarine strata in the Bohai Bay Rift Basin, Scientia Geo1ogica Sinica,2001,10(2).
55.J.A.Howelland J.F. Aitken. High Resolution Sequence Stratigraphy: Innovations and Applications. Geological Society SpeclalPublication.1996.No.104.
56.朱筱敏.层序地层学原理及应用.石油工业出版社,1998.
57.田在艺、常承永、钱绍新.隐蔽油气藏的勘探,大庆石油地质与开发编辑部编.中国隐蔽油气藏勘探论文集.黑龙江科学技术出版社 ,1984.
58.Bergman,K.M. and Walker,R.G.High-resolution sequence stratigrphic analysis of the Shannon Sandstone in Wyoming,using a template for region correlation. Journal of Sedimentary Research,1995,v.b65,No.2:255-264
59.Boyd,R.et al. Relation of sequence stratigrphy to modern sedimentary environments. Geology,1989,V.17:926-92
60.Cross,T.A.Stratigraphicarchitecture,correlation congcepts,volumetricpartitoning,facies differentiation and reservoir commpartmentalization from the perspective of high-resolution sequence stratigraphy.
61.Cross,T.A Application of high-resolution sequence stratigraphy to reservoir analysis. Subsurface Reservoir Characterization from outcrop observation:Proceedings of th 7th Exploration and Production Reserach Conference :Paris,Technip,11-13.
62.Hentz,T.F.Sequence stratigraphy of the Upper Pennsylvannian Cleveland Formation: a major tight-gas sandstone, Western Anadarko basin,Texas Panhandle. AAPG Bulletin, 1994,V.78, No.4:569-595
63.Koss,J.E.et al.An experimental studty of the efficts of base-level Change on fluvial,coastal plain and shef systems.Journal of Sedimenary research,1994,V,B64,No.2:90-98
64.Morton,R.A. and Suter,J.R.Sequence stratigraphy and composition of late Ouaternary shef-Margin deltas, Northern gulf of mexico.AAPG Bullitin,1996,V.80,No.4:505-530
65.Nichol,S.L.et al. Sequence stratigraphy of a coastal-plain incised vally estuary:Lake Calcasieu,Louisiana.Journal of Sedimentary Research,1996,V.66,No.4:847-857
66.Olsen,T.et al. Sequence archtecture in a fluvial succession:sequence stratigraphy in the Upper Cretacious Mesarerde groupe,price Canyon,Utah.Journal of Sedimentary Research, 1995,V.B65,No.2:265-279
67.Rigsby,C.A.Deepening-upward sequences in Oligocence and Lower Miocence fan delta deposits,western Santa Ynez Mountains,california.Journal of Sedimentary Research, 1992, V.B64,No.3:380-391
68.Sun,S.O.and Esteban,M.Paleoclamatic controls on sedimentation,diagenesis,and reservoir quality:Lessons from Miocence carbonates.AAPG bullitin.194,V.78,No.4:519-543
69.Shanley,K.W.and Mccable,P.J. perspectives on the sequence stratigrphy of continental strata.AAPG Bullitin,V.78,no.4:544-568
70.Weller,H.E.Base level,lithosphere surface,and time-stratigraphy.Geological Society of Amarica Bullitin,1964,V.75:599-610
71.Walker,R,G.Facies,dacies model and modern stratigraphic concepts.In Walker,R.G. eds.facies model:Response to ssea level.Geological Association of Canada,1992
72.Vail P.R. Seismic stratigraphy interpretation using sequence stratigraphy ,part 1,Seismic stratigrphy interpretation procedure in A.W.Bally,ed,Atalas of seismic stratigraphy:AAPG studies in geology 27,1987,(1):1-10
73.胡见义,徐树宝,刘淑兰等.非构造油气藏.北京:石油工业出版社,1986:81～83
74.曾溅辉,郑和荣,王宁.东营凹陷岩性油气藏成藏动力学特征.石油与天然气地质,1998,19(4):326～329
75.李丕龙.断陷湖盆油气聚集模式及其动力学特征.石油大学学报,2000,24(4):26～29
76.西门诺维奇BB主编.非背斜油气藏.北京:石油工业出版社,1986:161～224
77.邓宏文、王红亮、祝永军、Cross T A.高分辨率层序地层学――原理及应用.北京.地质出版社. 2002.
78.王捷,关德范.油气生成运移聚集模型研究.北京:石油工业出版社,1999:198～199
79.田世澄.论成藏动力系统.勘探家,1996,1(2):20～25
80.张义纲,陈彦华,陆嘉炎.油气运移及其聚集成藏模式.南京:河海大学出版社,1997
81.张云峰,付广.砂岩透镜体油藏聚油机理及成藏模式.断块油气田,2000,7(2):12～14 1990
82.曹颖辉,池英柳,薛良清,王洪江.沉积基准面在层序划分对比及地层岩性油气藏预测中的应用,石油实验地质,2002,24(1)
83.田在艺,常承永,钱绍新.隐蔽油气藏的勘探[A].大庆石油地质与开发编辑部编.中国隐蔽油气藏勘探论文集[C].哈尔滨:黑龙江科学技术出版社,1984.39-49
84. 林 畅 松 , 张 燕 梅 , 刘 景 彦 , 庞 保 成 . 高 精 度 层 序 地 层 学 与 储 层 预 测 . 地 学 前缘.2000.vol.7.No.3:111-117
85.庞雄奇.岩性油气藏成因机理研究现状及展望.油气地质与采收率.2002,9(5).
86.陈广军等.斜坡带低位扇砂岩体岩性油气藏勘探方法.石油学报.2002,23(3).
87.隋风贵,李洲海,朱明.箕状断陷盆地陡坡带砂砾岩扇体油藏研究.见潘元林主编:中国隐蔽油藏,67-76
88.蒲仁海.断陷湖盆层序地层学的几点进展.石油与天然气地质.23(4):410-414
89.徐怀大、赵政璋、樊太亮.从地震地层学到层序地层学――油气盆地的定性化与定量化描述.石油工业出版社.1997
90.Wheel H E. Base level, lithosphere surface and time-stratigraphy. Bull Geol Soc, 1964. 75:599-610
91.Walkev R. G.(ed). Facies Models Geosci, Can Reprint Ser.,1979, 1 Geol Ass Can Ontario
92.Quirk D C. “Bace level”: a unifying concept in alluvial sequence stratigraphy. In: Howell J A, Aitken J F, eds. High resolution sequence stratigraphy: innovations and applications. Geological Society Special Publication,1996,(104):37-50
93.Ravnas R, Steel R J. Architecture of marine rift-basin successions:1998, AAPG Bulletin, Vol. 82, No. 1:110-146
94.Reading H. G. (ed), Sedimentary Environments: Processes, Facies and Stratigraphy, 1996, Blackwell Sciences, 688P
95.赵文智、何登发、李小弟登.石油地质综合研究导论 1999,石油工业出版社
96.于兴河等,碎屑岩系油气储层沉积学. 2002,地质出版社
97.邓宏文、王红亮、翟爱军等.中国陆源碎屑盆地层序地层于储层展布.1999.石油与天然气地质,20(2),108-114
98.樊太亮、李卫东.层序地层应用于陆相油藏预测的成功实例.1999.石油学报.20(2):12-17
99.樊太亮、吕延仓、丁明华.层序地层体制中的陆相储层发育规律[J].2000.地学前缘.7(4):315-321
100.邓宏文、王红亮、宁宁.沉积物体积分配原理-高分辨率层序地层学的理论基础.2000.地学前缘.7 (4).305-313
101.樊太亮等.沉积基准面变化分析技术及应用.1997.石油与天然气地质.Vol.18.No.2:108-113
102.郑小武、邓宏文等. 测井高分辨率层序地层自动划分技术与应用尝试.1999.石油与天然气地质.20(4).357-360