长堤地区下第三系高分辨率层序地层学研究与隐蔽油藏预测
|
摘要
长堤地区位于济阳坳陷沾化凹陷东北部。是在燕山运动末期、在中生代潜山背景上发育起来的北北东走向的下第三系低潜山披覆构造带。针对该区以隐蔽油藏为主要勘探对象、下第三系沉积规律和储层研究中存在的问题，本课题运用以基准面旋回为参考面的高精度层序地层学理论与技术，通过岩芯、钻井、三维地震资料的综合分析，将研究区下第三系划分为沙四段-沙三段和沙二段、沙一段-东营组两个构造基准面旋回；沙三段—东营组划分为三个长期基准面旋回(二级层序)和八个中期基准面旋回(三级层序)。三个长期基准面旋回大致相当于沙三段、沙一段和东营组。其中沙三段由三个中期基准面旋回组成；沙一段由一个中期基准面旋回组成；东营组由四个中期基准面旋回组成。建立起了适应当前隐蔽油藏预测精度要求的研究区下第三系高分辨率层序地层格架。
以中期旋回为单元，分析了该区沉积相的分布与演化规律。本区下第三系发育了近岸水下扇沉积相、滩坝沉积相、扇三角洲沉积相、浊积扇沉积相和河流沉积相等五大类。沉积相纵向演化具有很强的规律性，与区域构造演化及湖平面变化有密切的关系。沙三段主要是在本区西部及南部边缘发育近岸水下扇沉积；沙一段底部主要为生物滩坝沉积，其次为砂坝沉积，之后进入半深湖沉积环境；东营组为前扇三角洲亚相过渡到扇三角洲前缘亚相到扇三角洲平原亚相再到辫状河沉积的递进模式。
长堤潜山披覆构造带四周与生油洼陷相邻，具有优越的成藏条件。下第三系发现的油气藏以构造油气藏和地层油气藏为主。主要含油层位为沙河街组。沙三段的扇中砂体、沙一段底部的生物滩坝、东营组的河流砂体都是优越的储集层。本区油气富集于“两边一隆一斜坡”，富集层位及埋深呈现由南向北依次抬升的趋势。纵向上含油层系多，含油井段长，但富集程度不同。油气富集受构造背景、断裂、岩性、地层不整合、区域盖层等多种因素控制。本区的油气成藏系统可划分为中西部、东部两个成藏系统，各成藏系统具有不同的油气来源、充注因素、封盖条件等，建立了相应的成藏模式。
课题和生产紧密结合，研究成果及时的应用于生产实际中，综合分析了研究区的油气勘探潜力及主要勘探方向，对有利地区及层系作了分析评价，先后在桩47块、桩8-18块及桩1-斜41块获得重大勘探突破，在此基础上提出了八个下一步勘探的有利目标区，提交探井、滚动井10余口，预测石油地质储量1260万吨。
Changdi area lies in the northeast of Zhanhua depression of Jiyang superdepression. It is a NNE-strike low buried-hill draping structural belt on the Mesozoic buried hill at the last phase of Yanshan movement. Aiming at subtle reservoir, this subject applies the theory and technology of high resolution sequence stratigraphy to solve the problems in research of deposition and reservoir of lower Tertiary. By integrative analysis of the cores, drilling and three-dimension seismic interpretation data, the Lower Tertiary of the study area is divided into two cycles of structural base level compsed by Es4-Es3 and Es2-Esl-Ed respectively. Es3-Ed comprises of three long term base-level cycles(secondary sequences ) and eight middle term base-level cycles (tertiary sequences ). The three long term base-level cycles are approximately equivalent to Es3,Esl and Ed, therein Es3 is composed of three middle term base-level cycles, Esl one cycle; and Ed four cycles. Based on the stratigraphic correlation of different order b
ase-level, the sequence stratigraphic framework is built in Changdi area, which can meet the needs of subtle reservoir prediction.
Based on middle-term cycles, the paper discussed the distribution and evolution of the depositional facies in study area. Five types of depositional facies in the Lower Tertiary are recognized. They are offshore subaqueous fan, beach sandbar, fan delta , turbidite fan and fluvial facies. The regularly vertical evolution of depositional facies has close relationship with the regional structure evolution and lake surface
changes. During Es3 period, offshore subaqueous fan mainly developed in the west and south of the area. During Esl, the development of dipositonal facies experienced bioclastic sandbar, beach bar and semi-deep lake deposits was developing. During Ed, there was a progressive model from pre-fan delta, fan delta to fan delta plain and braided river at last.
Being enclosed by hydrocarbon-generating subdepressions, Changdi buried-hill draping structural belt is of excellent conditions of reservoir. The reservoirs found in the Lower Tertiary are mainly structural and stratigraphic type. The main oil-bearing layer is Shahejie Formation. The middle fan sand in Es3, the bioclastic beach bar at the bottom of Esl, the river sand in Ed formed very best reservoir. In the area, oil and gas are enriched in "two side and one bulge and one slope". The rich layer and buried depth have an ascending tendency from south to north. Vertically, there are many thick oil-bearing beds with different enrichment. The enrichment of oil and gas is controlled by many factors including structural background, faults, lithology, stratigraphic unconformity, regional seal bed and so on. The reservoir-generating system in this area can be divided into two systems; the first is in the central west, the second east. Each of them has different sources, different fill factors and conceal conditions.
Consequently, correspondent reservoir-generating models have been established.
To guide the practice of production, the research analyzed the potential in oil and gas exploration, pointed out the main explorative directions, evaluated favorable areas and beds, which have made important explorative breakthroughs in these areas covering Zhuang 47, Zhuang 8-18 and Zhuang l-x41 blocks. At the same time, the study suggests eight favorable targets for next exploration, specifies the location of more than 10 prospective and developing wells with predicted petroleum geologic reserves 12600000 tons.
以中期旋回为单元，分析了该区沉积相的分布与演化规律。本区下第三系发育了近岸水下扇沉积相、滩坝沉积相、扇三角洲沉积相、浊积扇沉积相和河流沉积相等五大类。沉积相纵向演化具有很强的规律性，与区域构造演化及湖平面变化有密切的关系。沙三段主要是在本区西部及南部边缘发育近岸水下扇沉积；沙一段底部主要为生物滩坝沉积，其次为砂坝沉积，之后进入半深湖沉积环境；东营组为前扇三角洲亚相过渡到扇三角洲前缘亚相到扇三角洲平原亚相再到辫状河沉积的递进模式。
长堤潜山披覆构造带四周与生油洼陷相邻，具有优越的成藏条件。下第三系发现的油气藏以构造油气藏和地层油气藏为主。主要含油层位为沙河街组。沙三段的扇中砂体、沙一段底部的生物滩坝、东营组的河流砂体都是优越的储集层。本区油气富集于“两边一隆一斜坡”，富集层位及埋深呈现由南向北依次抬升的趋势。纵向上含油层系多，含油井段长，但富集程度不同。油气富集受构造背景、断裂、岩性、地层不整合、区域盖层等多种因素控制。本区的油气成藏系统可划分为中西部、东部两个成藏系统，各成藏系统具有不同的油气来源、充注因素、封盖条件等，建立了相应的成藏模式。
课题和生产紧密结合，研究成果及时的应用于生产实际中，综合分析了研究区的油气勘探潜力及主要勘探方向，对有利地区及层系作了分析评价，先后在桩47块、桩8-18块及桩1-斜41块获得重大勘探突破，在此基础上提出了八个下一步勘探的有利目标区，提交探井、滚动井10余口，预测石油地质储量1260万吨。
Changdi area lies in the northeast of Zhanhua depression of Jiyang superdepression. It is a NNE-strike low buried-hill draping structural belt on the Mesozoic buried hill at the last phase of Yanshan movement. Aiming at subtle reservoir, this subject applies the theory and technology of high resolution sequence stratigraphy to solve the problems in research of deposition and reservoir of lower Tertiary. By integrative analysis of the cores, drilling and three-dimension seismic interpretation data, the Lower Tertiary of the study area is divided into two cycles of structural base level compsed by Es4-Es3 and Es2-Esl-Ed respectively. Es3-Ed comprises of three long term base-level cycles(secondary sequences ) and eight middle term base-level cycles (tertiary sequences ). The three long term base-level cycles are approximately equivalent to Es3,Esl and Ed, therein Es3 is composed of three middle term base-level cycles, Esl one cycle; and Ed four cycles. Based on the stratigraphic correlation of different order b
ase-level, the sequence stratigraphic framework is built in Changdi area, which can meet the needs of subtle reservoir prediction.
Based on middle-term cycles, the paper discussed the distribution and evolution of the depositional facies in study area. Five types of depositional facies in the Lower Tertiary are recognized. They are offshore subaqueous fan, beach sandbar, fan delta , turbidite fan and fluvial facies. The regularly vertical evolution of depositional facies has close relationship with the regional structure evolution and lake surface
changes. During Es3 period, offshore subaqueous fan mainly developed in the west and south of the area. During Esl, the development of dipositonal facies experienced bioclastic sandbar, beach bar and semi-deep lake deposits was developing. During Ed, there was a progressive model from pre-fan delta, fan delta to fan delta plain and braided river at last.
Being enclosed by hydrocarbon-generating subdepressions, Changdi buried-hill draping structural belt is of excellent conditions of reservoir. The reservoirs found in the Lower Tertiary are mainly structural and stratigraphic type. The main oil-bearing layer is Shahejie Formation. The middle fan sand in Es3, the bioclastic beach bar at the bottom of Esl, the river sand in Ed formed very best reservoir. In the area, oil and gas are enriched in "two side and one bulge and one slope". The rich layer and buried depth have an ascending tendency from south to north. Vertically, there are many thick oil-bearing beds with different enrichment. The enrichment of oil and gas is controlled by many factors including structural background, faults, lithology, stratigraphic unconformity, regional seal bed and so on. The reservoir-generating system in this area can be divided into two systems; the first is in the central west, the second east. Each of them has different sources, different fill factors and conceal conditions.
Consequently, correspondent reservoir-generating models have been established.
To guide the practice of production, the research analyzed the potential in oil and gas exploration, pointed out the main explorative directions, evaluated favorable areas and beds, which have made important explorative breakthroughs in these areas covering Zhuang 47, Zhuang 8-18 and Zhuang l-x41 blocks. At the same time, the study suggests eight favorable targets for next exploration, specifies the location of more than 10 prospective and developing wells with predicted petroleum geologic reserves 12600000 tons.
引文
1．邓宏文 美国层序地层研究中的新学派—高分辨率层序地层学，石油与天然气地质，1995，16(2)89～97
2．邓宏文，王洪亮等，层序地层地层基准面的识别、对比技术及应用，石油与天然气地质，1996，17(3)：P177-184
3．邓宏文，王洪亮等，高分辨率层序地层对比在河流相中的应用，石油天然气地质，1997，18(2)：90-95
4．邓宏文，王红亮等，沉积物体积分配原理—高分辨率层序地层学的理论基础，地学前缘，V．7，No．4，2000
5．樊太亮，吕延仓等，层序地层体制中的陆相储层发育规律，地学前缘，V．7，No．4，2000
6．顾家裕，1995，陆相盆地层序地层学格架概念及模式，石油勘探与开发，22(4)
7．曾允孚，1999，沉积学发展现状与展望，成都理工学院学报，1999(1)
8．顾家裕，邓宏文，朱筱敏，层序地层学及其在油气勘探开发中的应用论文集，北京：石油工业出版社，1997
9．纪友亮，张仕奇等，1996，陆相断陷湖盆层序地层学，北京：石油工业出版社
10．姜在兴，操应长等著，砂体层序地层及沉积学研究——以山东惠民凹陷为例，北京：地质出版社，2000
11．林畅松等，“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，25(3)：260-265，2000
12．王洪亮，邓宏文，地层基准面原理在湖相储层预测中的应用，石油与天然气地质，1997(2)：P96-102
13．王红亮，邓宏文，渤海湾盆地第三系层序地层特征与大中型油气田分布，中国海上油气，V．14，No．2，2000
14．王红亮，邓宏文，东濮凹陷濮卫环洼带层序划分与沉积体系，古地理学报，V．2，No．1，2000
15．吴崇筠，薛叔浩等，中国含油气盆地沉积学，北京：石油工业出版社，1992
16．徐怀大，层序地层学理论用于我国断陷盆地分析中的几个问题，石油与天然气地质12(1)，1997
17．张昌民等，建立储层流动单元模型的新方法，石油与天然气地质，1999，20(2)
18．郑荣才，四川盆地下侏罗统大安寨段高分辨率层序地层学特征，沉积学报，1998，16(2)：42-49
19．郑荣才，吴朝容，郑荣才，尹世民，彭军，基准面旋回结构与叠加样式的沉积动力学分析，沉积学报，2000，18(3)：369-375
20．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，石油与天然气地质，V．20，No．4，1999
21．朱筱敏，层序地层学原理及应用，北京：石油工业出版社，1998
22．Vail，地震地层学于全球海平面变化，1977
23．Wilgus，海平面变化——一种整体性研究，1988
24．Van Wagoner，测井、岩芯、露头研究中的硅质碎屑岩层序地层学，1990
25．Vail，构造、海平面升降和沉积作用的地层标记(综述)，1991
26．陈广军，试论长堤古潜山的含油气性，复式油气田，2000(4)：6～10
27．陈广军，尚延安，庄文山等，关于长堤潜山构造带东翼含油气性的讨论，油气地质与采收率，2001(1)：27～30
28．王离迟，王朝安，史秋贤等，沾化凹陷长堤潜山披覆构造带油气成藏特征，复式油气田，2000(2)：27～30
29．王秉海，钱凯主编．1992．胜利油区地质研究与勘探实践．石油大学出版社．
30．帅德福，王秉海主编．1993．中国石油地质志(第六卷)；胜利油田．石油工业出版社．
31．张义纲等．1997．油气运移及其聚集成藏模式．河海大学出版社．
32．王平等．1994．复杂断块油田详探与开发．石油工业出版社．
33．裘怿楠，薛叔浩．1997．油气储层评价技术．石油工业出版社．
34．刘兴才，帅德福等．1991．济阳断块盆地油气聚集与分布的基本形式．见：中国油气聚集与分布．石油工业出版社．
35．N．J．Milton．圈闭样式—以封堵面为基础的一种新分类．国外油气勘探．1993年第2期．
36．张春荣．1993．济阳坳陷小洼陷资源研究与评价．胜利石油管理局地质科学研究院．
37．杨申镳．1991．济阳坳陷及外围地区油气潜力暨资源评价及附图．胜利石油管理局．
38．宋一涛等．1997．胜海—埕岛地区烃源岩的特征、油源及油气运移聚集研究．胜利石油管理局地质科学研究院．
39．宋一涛等．1997．垦东地区原油的地化特征及油源讨论．胜利石油管理局地质科学研究院．
40．胡朝元．1996．成油系统概念在中国的提出及其应用．石油学报(2)．
41．李明诚．石油与天然气运移研究综述．石油勘探与开发．2000年第4期．
42．张善文．沾化凹陷浅层勘探的思考．复式油气田．1999，3期．P6-7．
43．郝素凤，马立祥．高分辨率层序地层学在油田上的应用．沉积与特提斯地质．2002，22(4)：102-106．
44．许红，李思田等．地层学的发展推动油气地质理论研究的进步．海洋地质动态．2002，18(2)：17-21．
45．孟万斌．从层序地层学到高分辨率层序地层学．成都理工学院学报．2002，29(4)：380-385．
46．周延军，贾云超，焦保富等．高分辨率层序地层特征及其对储层发育的影响：-以胡状集油田胡5块沙三段上、中亚段为例．江汉石油学院学报．2002，24(1)：11-14，29．
47．付明希，朱全胜，段春凤等．基于地层准面原理的高分辨率层序地层学的应用-以华北地区二叠系上石盒子组为例．断块油气田．2002，9(2)：6-10．
48．彭军，陈景山，郑荣才等．百色盆地百岗组高分辨率层序分析及研究意义．地球学报．2002，23(2)：153-158．
49．郑荣才，彭军．陕北志丹三角洲长6油层组高分辨率层序分析与等时对比．沉积学报．2002，20(1)：92-100．
50．胡小强，朱红涛，李梦溪．旋回层序地层学研究及应用．海洋石油．2001，总第100期：48-55．
51．刘豪，王英民，王媛等．用高分辨率层序地层学进行非构造圈闭研究．西安石油学院学报：自然科学版．2001．16(6)：1-4．
52．刘波，赵翰卿，于会宇．储集层的两种精细对比方法讨论．石油勘探与开发．2001，28(6)：94-96．
53．郑荣才，彭军，吴朝荣．陆相盆地基准面旋回的级次划分和研究意义．沉积学报．2001，19(2)：249-255．
54．胡小强，石万忠．渤南凸起浅层高分辨率层序地层学研究．天然气地球科学．2000，11(6)：15-19．
55．瞿辉．层序地展学及其在油气勘探中的运用．地学前缘．2000，7(B08)：257-262．
56．陈建华，田景春．层序地层学的产生、现状与展望．复式油气田．2000，(2)：9-12．
57．蒲仁海，陈振新．高分辨率层序地层学在桩52块近岸浊积扇前积油层对比中的应用．沉积学报．1998．16(4)：21-26．
58．蒲仁海，郑显华．论非构造油气藏综合勘探方法．西北大学学报：自科版．1998，28(6)：522-526．
59. Juan Pablo Milana.Sequence stratigraphy in alluvial setting:a flume-based model with applications to outcrops and seismic data[J].AAPG Bulletin,1998, 82(9):1736—1753.
60. Liangqing Xue and William E.Galloway.High-resolution depositional framework of the paleocene middle Wilcox Strata,Texas coastal plain [J].AAPG Bulletin, 1995, 79(2):205—230.
61. James A M, Brian A Z,Pemberton S G.High-resolution sequence stratigraphy of early transgressive deposits,Viking formation,Joffre Field, Alberta,Canada [J].AAPG Bulletin, 1998, 82(5A):729—756.
62. Alf Ryseth,Hege Fjellbirkeland,Inger Kloster Osmundsen et al.. High-resolution stratigraphy and seismic attribute mapping of a fluvial reservoir:middle Jurassic Ness formation,Oseberg Field [J].AAPG Bulletin,
1998, 82(9):1627—1651.
63. Stephen Flint,Simon Knight,and Andrew Tilbrook.Appliction of high-resolution sequence stratigraphy to Northwest Hutton field, Northern North Sea:implications for management of a Mature Brent Group Field [J]. AAPG Bulletin, 1998, 82(7):1416—1436.
64. Cross, T A., et al.Application of high-resolution sequence stratigraphy to reservoir anyalysis [A].R. Eschard, B. Doligez, eds.Subsurface reservoir characterization from outcrop observations [C].Paris,Editions Technip,1993, 11-33.
65. Bruhn,C. H. L.,and R. G.Walker. High-resolution stratigraphy and sedimentary evolution of coarse-grained canyon-filling turbidities form the Upper Cretaceous transgressive megasequence,Campos Basin,offshore Brazil [J].Journal of Sedimentary Research,1995, B65: 426-442.
66. Henry W Posamentier,Paul Weimer.Siliciclastic sequence stratigraphy and petroleum geology—where to from there?[J].AAPG Bulletin,1993, 77 (5):731—742.
67. Bryant I D.The application of measurements to constrain reservoir-scale sequence stratigraphic models [A].Howell J A,Aitken J F,eds.High-resolution sequence stratigraphy:innovations and applications[C].Geological Society Special Publication,1996, 104: 51—64.
68. Dalrymple R M, Zaitlin B A. High-resolution sequence stratigraphy of a complex, incised valley succession, Clbequid Bay-Salmon River Estuary, Bay of Fundy,Canada [J].Sedimentology, 1995,41(6):1069—1091.
69. Armentrout J M.High resolution sequence biostratigraphy:examples from the Gulf of Mexico Plio-Pleistocene [A].Howell J A,Aitken J F,eds. High-resolution sequence stratigraphy:innovations and applications[C].Geological Society Special Publication,1996, 104: 65—87.
70. Alf R, Hege F, Inger K O, et al.High-Resolution stratigraphy and seismic attribute mapping of a fluvial reservoir:Middle Jurassic Ness Formation,Oseberg Field [J].AAPG Bulletin,1990, 74(3):273—295.
71. Van Waggoner J C. et al.Sliliciclastic sequence stratigraphy in well logs, cores and outcrops:concepts for high-resolutions correlation of time and facies [J].AAPG, Methods in exploration series 7, 1990, 55:1—240.
72. Bowen D W. et al.The relative success of sillciclastic sequence stratigraphic concepts in exploration: examples from incised valley fill and turbidite systems reservoir [A].Weimer P.and Posamentier H W. eds. Siliciclastic sequence stratigraphy:recent developments and applications.AAPG Menoir 58,1994,15—52.
73. Aitken J F, Flint S S.The application of high-resolution sequence stratigraphy to fluvial systems:a case study from the Upper Carboniferous Breathitt Group,eastern Kentucky,USA [J].Sedimenology,1995, 42:3-30.
74. Bruns B A, Heller P L, Marzo M et al.Fluvial response in a sequence stratigraphic framework:example from the Montserrat fan delta, Span [J].Journal of Sedimentary Research,1997, 67:311-321.
75. Shauley,K W, McCabe P J.Perspectives on the sequence stratigraphy of continental strata [J].AAPG Bulletin, 1994,78: 544—568.
76. Magoon L.B,W.G.Dow.1994. The Petroleum System——From Source to Trap. AAPG. Memoir 60.
77. Hunt, J.M. 1990.Generation and migration of petroleum from abnormally pressured fiuid compartments. AAPG Bull.,Vol.74, No.1
78. Hooper E C D, 1991.Fluid migration along growth faults in compacting ediments.Journal of Petroleum geology, 14 (2):161-180.
2．邓宏文，王洪亮等，层序地层地层基准面的识别、对比技术及应用，石油与天然气地质，1996，17(3)：P177-184
3．邓宏文，王洪亮等，高分辨率层序地层对比在河流相中的应用，石油天然气地质，1997，18(2)：90-95
4．邓宏文，王红亮等，沉积物体积分配原理—高分辨率层序地层学的理论基础，地学前缘，V．7，No．4，2000
5．樊太亮，吕延仓等，层序地层体制中的陆相储层发育规律，地学前缘，V．7，No．4，2000
6．顾家裕，1995，陆相盆地层序地层学格架概念及模式，石油勘探与开发，22(4)
7．曾允孚，1999，沉积学发展现状与展望，成都理工学院学报，1999(1)
8．顾家裕，邓宏文，朱筱敏，层序地层学及其在油气勘探开发中的应用论文集，北京：石油工业出版社，1997
9．纪友亮，张仕奇等，1996，陆相断陷湖盆层序地层学，北京：石油工业出版社
10．姜在兴，操应长等著，砂体层序地层及沉积学研究——以山东惠民凹陷为例，北京：地质出版社，2000
11．林畅松等，“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，25(3)：260-265，2000
12．王洪亮，邓宏文，地层基准面原理在湖相储层预测中的应用，石油与天然气地质，1997(2)：P96-102
13．王红亮，邓宏文，渤海湾盆地第三系层序地层特征与大中型油气田分布，中国海上油气，V．14，No．2，2000
14．王红亮，邓宏文，东濮凹陷濮卫环洼带层序划分与沉积体系，古地理学报，V．2，No．1，2000
15．吴崇筠，薛叔浩等，中国含油气盆地沉积学，北京：石油工业出版社，1992
16．徐怀大，层序地层学理论用于我国断陷盆地分析中的几个问题，石油与天然气地质12(1)，1997
17．张昌民等，建立储层流动单元模型的新方法，石油与天然气地质，1999，20(2)
18．郑荣才，四川盆地下侏罗统大安寨段高分辨率层序地层学特征，沉积学报，1998，16(2)：42-49
19．郑荣才，吴朝容，郑荣才，尹世民，彭军，基准面旋回结构与叠加样式的沉积动力学分析，沉积学报，2000，18(3)：369-375
20．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，石油与天然气地质，V．20，No．4，1999
21．朱筱敏，层序地层学原理及应用，北京：石油工业出版社，1998
22．Vail，地震地层学于全球海平面变化，1977
23．Wilgus，海平面变化——一种整体性研究，1988
24．Van Wagoner，测井、岩芯、露头研究中的硅质碎屑岩层序地层学，1990
25．Vail，构造、海平面升降和沉积作用的地层标记(综述)，1991
26．陈广军，试论长堤古潜山的含油气性，复式油气田，2000(4)：6～10
27．陈广军，尚延安，庄文山等，关于长堤潜山构造带东翼含油气性的讨论，油气地质与采收率，2001(1)：27～30
28．王离迟，王朝安，史秋贤等，沾化凹陷长堤潜山披覆构造带油气成藏特征，复式油气田，2000(2)：27～30
29．王秉海，钱凯主编．1992．胜利油区地质研究与勘探实践．石油大学出版社．
30．帅德福，王秉海主编．1993．中国石油地质志(第六卷)；胜利油田．石油工业出版社．
31．张义纲等．1997．油气运移及其聚集成藏模式．河海大学出版社．
32．王平等．1994．复杂断块油田详探与开发．石油工业出版社．
33．裘怿楠，薛叔浩．1997．油气储层评价技术．石油工业出版社．
34．刘兴才，帅德福等．1991．济阳断块盆地油气聚集与分布的基本形式．见：中国油气聚集与分布．石油工业出版社．
35．N．J．Milton．圈闭样式—以封堵面为基础的一种新分类．国外油气勘探．1993年第2期．
36．张春荣．1993．济阳坳陷小洼陷资源研究与评价．胜利石油管理局地质科学研究院．
37．杨申镳．1991．济阳坳陷及外围地区油气潜力暨资源评价及附图．胜利石油管理局．
38．宋一涛等．1997．胜海—埕岛地区烃源岩的特征、油源及油气运移聚集研究．胜利石油管理局地质科学研究院．
39．宋一涛等．1997．垦东地区原油的地化特征及油源讨论．胜利石油管理局地质科学研究院．
40．胡朝元．1996．成油系统概念在中国的提出及其应用．石油学报(2)．
41．李明诚．石油与天然气运移研究综述．石油勘探与开发．2000年第4期．
42．张善文．沾化凹陷浅层勘探的思考．复式油气田．1999，3期．P6-7．
43．郝素凤，马立祥．高分辨率层序地层学在油田上的应用．沉积与特提斯地质．2002，22(4)：102-106．
44．许红，李思田等．地层学的发展推动油气地质理论研究的进步．海洋地质动态．2002，18(2)：17-21．
45．孟万斌．从层序地层学到高分辨率层序地层学．成都理工学院学报．2002，29(4)：380-385．
46．周延军，贾云超，焦保富等．高分辨率层序地层特征及其对储层发育的影响：-以胡状集油田胡5块沙三段上、中亚段为例．江汉石油学院学报．2002，24(1)：11-14，29．
47．付明希，朱全胜，段春凤等．基于地层准面原理的高分辨率层序地层学的应用-以华北地区二叠系上石盒子组为例．断块油气田．2002，9(2)：6-10．
48．彭军，陈景山，郑荣才等．百色盆地百岗组高分辨率层序分析及研究意义．地球学报．2002，23(2)：153-158．
49．郑荣才，彭军．陕北志丹三角洲长6油层组高分辨率层序分析与等时对比．沉积学报．2002，20(1)：92-100．
50．胡小强，朱红涛，李梦溪．旋回层序地层学研究及应用．海洋石油．2001，总第100期：48-55．
51．刘豪，王英民，王媛等．用高分辨率层序地层学进行非构造圈闭研究．西安石油学院学报：自然科学版．2001．16(6)：1-4．
52．刘波，赵翰卿，于会宇．储集层的两种精细对比方法讨论．石油勘探与开发．2001，28(6)：94-96．
53．郑荣才，彭军，吴朝荣．陆相盆地基准面旋回的级次划分和研究意义．沉积学报．2001，19(2)：249-255．
54．胡小强，石万忠．渤南凸起浅层高分辨率层序地层学研究．天然气地球科学．2000，11(6)：15-19．
55．瞿辉．层序地展学及其在油气勘探中的运用．地学前缘．2000，7(B08)：257-262．
56．陈建华，田景春．层序地层学的产生、现状与展望．复式油气田．2000，(2)：9-12．
57．蒲仁海，陈振新．高分辨率层序地层学在桩52块近岸浊积扇前积油层对比中的应用．沉积学报．1998．16(4)：21-26．
58．蒲仁海，郑显华．论非构造油气藏综合勘探方法．西北大学学报：自科版．1998，28(6)：522-526．
59. Juan Pablo Milana.Sequence stratigraphy in alluvial setting:a flume-based model with applications to outcrops and seismic data[J].AAPG Bulletin,1998, 82(9):1736—1753.
60. Liangqing Xue and William E.Galloway.High-resolution depositional framework of the paleocene middle Wilcox Strata,Texas coastal plain [J].AAPG Bulletin, 1995, 79(2):205—230.
61. James A M, Brian A Z,Pemberton S G.High-resolution sequence stratigraphy of early transgressive deposits,Viking formation,Joffre Field, Alberta,Canada [J].AAPG Bulletin, 1998, 82(5A):729—756.
62. Alf Ryseth,Hege Fjellbirkeland,Inger Kloster Osmundsen et al.. High-resolution stratigraphy and seismic attribute mapping of a fluvial reservoir:middle Jurassic Ness formation,Oseberg Field [J].AAPG Bulletin,
1998, 82(9):1627—1651.
63. Stephen Flint,Simon Knight,and Andrew Tilbrook.Appliction of high-resolution sequence stratigraphy to Northwest Hutton field, Northern North Sea:implications for management of a Mature Brent Group Field [J]. AAPG Bulletin, 1998, 82(7):1416—1436.
64. Cross, T A., et al.Application of high-resolution sequence stratigraphy to reservoir anyalysis [A].R. Eschard, B. Doligez, eds.Subsurface reservoir characterization from outcrop observations [C].Paris,Editions Technip,1993, 11-33.
65. Bruhn,C. H. L.,and R. G.Walker. High-resolution stratigraphy and sedimentary evolution of coarse-grained canyon-filling turbidities form the Upper Cretaceous transgressive megasequence,Campos Basin,offshore Brazil [J].Journal of Sedimentary Research,1995, B65: 426-442.
66. Henry W Posamentier,Paul Weimer.Siliciclastic sequence stratigraphy and petroleum geology—where to from there?[J].AAPG Bulletin,1993, 77 (5):731—742.
67. Bryant I D.The application of measurements to constrain reservoir-scale sequence stratigraphic models [A].Howell J A,Aitken J F,eds.High-resolution sequence stratigraphy:innovations and applications[C].Geological Society Special Publication,1996, 104: 51—64.
68. Dalrymple R M, Zaitlin B A. High-resolution sequence stratigraphy of a complex, incised valley succession, Clbequid Bay-Salmon River Estuary, Bay of Fundy,Canada [J].Sedimentology, 1995,41(6):1069—1091.
69. Armentrout J M.High resolution sequence biostratigraphy:examples from the Gulf of Mexico Plio-Pleistocene [A].Howell J A,Aitken J F,eds. High-resolution sequence stratigraphy:innovations and applications[C].Geological Society Special Publication,1996, 104: 65—87.
70. Alf R, Hege F, Inger K O, et al.High-Resolution stratigraphy and seismic attribute mapping of a fluvial reservoir:Middle Jurassic Ness Formation,Oseberg Field [J].AAPG Bulletin,1990, 74(3):273—295.
71. Van Waggoner J C. et al.Sliliciclastic sequence stratigraphy in well logs, cores and outcrops:concepts for high-resolutions correlation of time and facies [J].AAPG, Methods in exploration series 7, 1990, 55:1—240.
72. Bowen D W. et al.The relative success of sillciclastic sequence stratigraphic concepts in exploration: examples from incised valley fill and turbidite systems reservoir [A].Weimer P.and Posamentier H W. eds. Siliciclastic sequence stratigraphy:recent developments and applications.AAPG Menoir 58,1994,15—52.
73. Aitken J F, Flint S S.The application of high-resolution sequence stratigraphy to fluvial systems:a case study from the Upper Carboniferous Breathitt Group,eastern Kentucky,USA [J].Sedimenology,1995, 42:3-30.
74. Bruns B A, Heller P L, Marzo M et al.Fluvial response in a sequence stratigraphic framework:example from the Montserrat fan delta, Span [J].Journal of Sedimentary Research,1997, 67:311-321.
75. Shauley,K W, McCabe P J.Perspectives on the sequence stratigraphy of continental strata [J].AAPG Bulletin, 1994,78: 544—568.
76. Magoon L.B,W.G.Dow.1994. The Petroleum System——From Source to Trap. AAPG. Memoir 60.
77. Hunt, J.M. 1990.Generation and migration of petroleum from abnormally pressured fiuid compartments. AAPG Bull.,Vol.74, No.1
78. Hooper E C D, 1991.Fluid migration along growth faults in compacting ediments.Journal of Petroleum geology, 14 (2):161-180.