牛庄洼陷沙二段高分辨率层序地层学研究与有利砂体预测
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摘要
本文以层序地层学和沉积学理论为基础,通过岩芯观察描述、测井、地震资料综合分析,系统研究了东营凹陷牛庄洼陷沙三上亚段～沙二段层序地层划分与演化、沉积相标志特征、沉积相类型及其时空展布规律。
在层序地层学基本理论的指导下,对研究区探井岩性、测井曲线、地震剖面及其它相关资料进行详细研究,结合小波分析等研究方法,识别出了沙三上亚段～沙二段的层序界面,划分为两个层序,其中沙三上亚段～沙二下亚段为层序S1,沙二上亚段为层序S2。沙三上亚段～沙二段地层内部可以进一步划分为6个准层序组、21个准层序。层序S1是一个二分层序,包含湖进和湖退两个体系域,分为3个准层序组及9个准层序。准层序组自下而上依次命名为S1-1、S1-2和S1-3,准层序包括第13到第21准层序,其中S1-1包含20、21两个准层序,S1-2包含16-19四个准层序,S1-3包含13-15三个准层序。层序S2是一个三分层序,包含低位、湖侵和高位三个体系域。进一步可以划分为3个准层序组和12个准层序。准层序组自下而上依次命名为S2-1、S2-2和S2-3,准层序为第1到第12准层序,其中S2-1包含10-12三个准层序,S2-2包含7-9三个准层序,S2-3包含1-6共六个准层序。S2-1准层序组对应于层序S2的低位体系域,S2-2和S2-3准层序组对应于湖侵体系域。通过单井层序划分、连井剖面追踪对比,建立了牛庄洼陷沙三上亚段～沙二段层序地层格架。
通过对岩芯、测井、录井资料等的沉积相标志研究,在牛庄洼陷沙三上亚段～沙二段地层中识别出三角洲、曲流河、滩坝及湖泊等沉积相类型。其中曲流河河道,三角洲前缘水下分流河道、分流河口砂坝、远砂坝以及滩坝是主要的砂体成因类型。三角洲的物源主要来自洼陷的东部和南坡。砂体的分布平面上受古水深及水动力条件的控制,纵向上演化受湖盆水体变化的影响。
为了能更加真实深入的了解低可容空间下的三角洲沉积特征,本文对东营沉淀池三角洲的现代沉积特点进行了考察和详细解剖,取得了一定的认识,并与牛庄洼陷沙三上亚段～沙二段地层中的三角洲进行了比对,总结出了低可容空间下的三角洲沉积模式,为牛庄洼陷沙二段的油气勘探提供了有效的指导,也为相似沉积环境下三角洲沉积体系的研究提供了帮助。
Through the relevant data such as the core description , well-log and seismic analysis , this paper has studied the sequence division and evolution , the facies marks feature, the facies type and its distribution rules of the upper segment of Es3～Es2 in Niuzhuang sag on the basis of the sequence stratigraphy and sedimentology.
Under the guide of the sequence stratigraphy theory, the sequence boundaries about the upper segment of Es3～Es2 have been recognized and further divide it 2 sequences: the upper segment of Es3-lower segment of Es2 is S1 sequence , the upper segment of Es2 is S2 sequence .The upper segment of Es3～Es2 is divided into 21 parasequence , which include 6 parasequence formation on the studies of the core description , well-log and seismic and the other relevant data , combining with wavelet analysis.
The S1 sequence is a dichotomize sequence,include the TST and the RST, further divided 3 parasequence formations and 9 parasequence. The sequence formations are entitled S1-1 , S1-2 and S1-3 from the bottom to the top, included the 13-21 parasequence: the parasequence 20-21 pertain S1-1, the parasequence 16-19 pertain S1-2, the parasequence 13-15 pertain S1-3. The S2 sequence is a tripartition dichotomize sequence ,include the LST ,TST and HST, further divided 3 parasequence formations and 12 parasequence. The sequence formations are entitled S2-1 , S2-2 and S2-3 from the bottom to the top, included the 1-12 parasequence: the parasequence 10-12 pertain S2-1, the parasequence 7-9 pertain S2-2 , the parasequence 1-6 pertain S2-3. The S2-1 parasequence formation corresponds to the LST of S2, S2-2 and S2-3 correspond to TST. The sequence framework of the upper segment of Es3～Es2 in Niuzhuang sag has been established on the basis of individual well sequence division and well tie section.
There are delta , meandering river , beach bar and lacus facies in upper segment Es3～Es2 of Niuzhuang sag by the relevant data such as the core description , well-log and log data. The channel of meandering river, the distributary channel of delta front ,distributary mouth bar , distal bar and the beach bar are the main sand body types. The provenance of delta is the eastern and south slope of the sag. The sand body distribute is controlled by the palaeobathymetry and hydrodynamic force in plane, and influenced by the change of water of lacus basin in the longitude.
In order to comprehend the feature of delta in lower contained vacuity ,this paper investigate the delta sediment feature of Deposit pool delta in DongYing , then draw certain knowledge , on this basis comparing with the delta of the upper segment of Es3～Es2 in Niuzhuang sag , in the end generalize the model about delta which deposits in lower contained vacuity. The fruit of this paper provides direction for the exploration activity in Es2 of Niuzhuang sag , also is benefit to the study of the delta depositional system in the same deposition condition
在层序地层学基本理论的指导下,对研究区探井岩性、测井曲线、地震剖面及其它相关资料进行详细研究,结合小波分析等研究方法,识别出了沙三上亚段～沙二段的层序界面,划分为两个层序,其中沙三上亚段～沙二下亚段为层序S1,沙二上亚段为层序S2。沙三上亚段～沙二段地层内部可以进一步划分为6个准层序组、21个准层序。层序S1是一个二分层序,包含湖进和湖退两个体系域,分为3个准层序组及9个准层序。准层序组自下而上依次命名为S1-1、S1-2和S1-3,准层序包括第13到第21准层序,其中S1-1包含20、21两个准层序,S1-2包含16-19四个准层序,S1-3包含13-15三个准层序。层序S2是一个三分层序,包含低位、湖侵和高位三个体系域。进一步可以划分为3个准层序组和12个准层序。准层序组自下而上依次命名为S2-1、S2-2和S2-3,准层序为第1到第12准层序,其中S2-1包含10-12三个准层序,S2-2包含7-9三个准层序,S2-3包含1-6共六个准层序。S2-1准层序组对应于层序S2的低位体系域,S2-2和S2-3准层序组对应于湖侵体系域。通过单井层序划分、连井剖面追踪对比,建立了牛庄洼陷沙三上亚段～沙二段层序地层格架。
通过对岩芯、测井、录井资料等的沉积相标志研究,在牛庄洼陷沙三上亚段～沙二段地层中识别出三角洲、曲流河、滩坝及湖泊等沉积相类型。其中曲流河河道,三角洲前缘水下分流河道、分流河口砂坝、远砂坝以及滩坝是主要的砂体成因类型。三角洲的物源主要来自洼陷的东部和南坡。砂体的分布平面上受古水深及水动力条件的控制,纵向上演化受湖盆水体变化的影响。
为了能更加真实深入的了解低可容空间下的三角洲沉积特征,本文对东营沉淀池三角洲的现代沉积特点进行了考察和详细解剖,取得了一定的认识,并与牛庄洼陷沙三上亚段～沙二段地层中的三角洲进行了比对,总结出了低可容空间下的三角洲沉积模式,为牛庄洼陷沙二段的油气勘探提供了有效的指导,也为相似沉积环境下三角洲沉积体系的研究提供了帮助。
Through the relevant data such as the core description , well-log and seismic analysis , this paper has studied the sequence division and evolution , the facies marks feature, the facies type and its distribution rules of the upper segment of Es3～Es2 in Niuzhuang sag on the basis of the sequence stratigraphy and sedimentology.
Under the guide of the sequence stratigraphy theory, the sequence boundaries about the upper segment of Es3～Es2 have been recognized and further divide it 2 sequences: the upper segment of Es3-lower segment of Es2 is S1 sequence , the upper segment of Es2 is S2 sequence .The upper segment of Es3～Es2 is divided into 21 parasequence , which include 6 parasequence formation on the studies of the core description , well-log and seismic and the other relevant data , combining with wavelet analysis.
The S1 sequence is a dichotomize sequence,include the TST and the RST, further divided 3 parasequence formations and 9 parasequence. The sequence formations are entitled S1-1 , S1-2 and S1-3 from the bottom to the top, included the 13-21 parasequence: the parasequence 20-21 pertain S1-1, the parasequence 16-19 pertain S1-2, the parasequence 13-15 pertain S1-3. The S2 sequence is a tripartition dichotomize sequence ,include the LST ,TST and HST, further divided 3 parasequence formations and 12 parasequence. The sequence formations are entitled S2-1 , S2-2 and S2-3 from the bottom to the top, included the 1-12 parasequence: the parasequence 10-12 pertain S2-1, the parasequence 7-9 pertain S2-2 , the parasequence 1-6 pertain S2-3. The S2-1 parasequence formation corresponds to the LST of S2, S2-2 and S2-3 correspond to TST. The sequence framework of the upper segment of Es3～Es2 in Niuzhuang sag has been established on the basis of individual well sequence division and well tie section.
There are delta , meandering river , beach bar and lacus facies in upper segment Es3～Es2 of Niuzhuang sag by the relevant data such as the core description , well-log and log data. The channel of meandering river, the distributary channel of delta front ,distributary mouth bar , distal bar and the beach bar are the main sand body types. The provenance of delta is the eastern and south slope of the sag. The sand body distribute is controlled by the palaeobathymetry and hydrodynamic force in plane, and influenced by the change of water of lacus basin in the longitude.
In order to comprehend the feature of delta in lower contained vacuity ,this paper investigate the delta sediment feature of Deposit pool delta in DongYing , then draw certain knowledge , on this basis comparing with the delta of the upper segment of Es3～Es2 in Niuzhuang sag , in the end generalize the model about delta which deposits in lower contained vacuity. The fruit of this paper provides direction for the exploration activity in Es2 of Niuzhuang sag , also is benefit to the study of the delta depositional system in the same deposition condition
引文
[1]李丕龙,庞雄奇编.隐蔽油气藏形成机理与勘探实践:第三届隐蔽油气藏国际学术研讨会论文集[A].北京:石油工业出版社,2004:1-10
[2]潘元林编.中国隐蔽油气藏[M].北京:地质出版社,1998:2-18
[3]蔡希源,李思田,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[M].北京:地质出版社,2003:3-30
[4]张善文.济阳坳陷第三系隐蔽油气藏勘探理论与实践[J].石油与天然气地质,2006,27(6):731-740
[5]潘元林,李思田等.大型陆相断陷盆地层序地层与隐蔽油气藏研究——以济阳坳陷为例[M].石油工业出版社.2004
[6]王金铎,韩文功,于建国,郑建斌.东营凹陷沙三段浊积岩体系及其油气勘探意义[J].石油学报,2003,24(5),24-29
[7]张宗檩,操应长,高永进等.东营凹陷沙三段-沙一段层序地层与油气[J].石油勘探与开发,2003,30(3),29-31
[8]王秉海,钱凯主编.胜利油区地质研究与勘探实践[M].东营:石油大学出版社,1992
[9]Gino Cantalamessa,Claudio Di Celma,Luca Ragaini. Sequence stratigraphy of the Punta Ballena Member of the Jama Formation( Early Pleistocene,Ecuador):insights from integrated sedimentologic,taphonomic and paleoecologic analysis of molluscan shell concentrations[J]. Palaeogeography,Palaeoclimatology,Palaeoecology 216(2005)1–25
[10]Vail P R. Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure [A].In:Bally A W,ed. Atlas of seismic stratigraphy [C],AAPG,Studies in geology,1987,27
[11]Cross T A,Lessenger M A.Sediment volume partitioning:rationale for stratigraphic model evalution and high-resolution stratigraphic correlation [A],Gradstein F M,Sandvik K O,Milton N J,eds. Sequence statigraphy Concepts and Applications [M],NPF special publication,1998
[12]岳文浙,丁保良,魏乃颐.陆盆层序地层研究的思路[J].地质论评,2000,46(4)347-354
[13]C.K.威尔格斯等编,徐怀大译.层序地层学原理[M].北京:石油工业出版社,1993
[14]纪友亮等编.陆相断陷湖盆层序地层学[M].北京:石油工业出版社,1996
[15]纪友亮,张世奇.层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998
[16]罗立民等编.河湖沉积体系三维高分辨率层序地层学[M].北京:地质出版社,1999
[17]姜在兴等编.层序地层学原理及应用[M].北京:石油工业出版社,1996
[18]魏魁生,徐怀大.华北典型箕状盆地层序地层学模式及油气赋存关系[J].地球科学,1993,18(2),141-149
[19]刘招君,程日辉.层序地层学的概念,进展与争论[J].世界地质,1993,13(3),56-58
[20]胡受权.古气候变迁对泌阳断陷湖盆陆相层序发育的影响[J].江汉石油学院学报,1998,20(1),1-6
[21]操应长.断陷湖盆层序地层学[M].北京:地质出版社,2005
[22]顾家裕,郭彬程,张兴阳.中国陆相盆地层序地层格架及模式[J].石油勘探与开发,2005,32(5),11-15
[23]贾承造,赵文智,邹才能等.岩性地层油气藏勘探研究的两项核心技术[J].石油勘探与开发,2004,31(3):3-9
[24]操应长,姜在兴,夏斌等.声波时差资料识别层序地层单元界面的方法、原理及实例[J].沉积学报,2003,21(2),318-323
[25]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发.2000,27(5),119-121.
[26]苏德晨,李庆谋,罗光文等.Fisher图解在旋回层序地层研究中的应用[J].现代地质,1995,9(3),279-283
[27]朱剑兵,纪友亮,赵培坤等.小波变换在层序地层单元自动划分中的应用[J].石油勘探与开发,2005,32(1),84-86
[28]刘文业.小波分析在高分辨层序地层划分中的应用[J].地质力学学报,2006,12(1),64-70
[29]崔凤林,谢春来,付雷等.小波变缓时频能量谱技术在地震层序划分中的应用[J].长春科技大学学报,2000,30(4),397-400
[30]吴国忱,康仁华,印兴耀.三维时频分席在地震层序分析中的应用[J].石油大学学报(自然科学版),2000,24(1),81-85
[31]Haughton D W,Morton A C,Todd S P.Developments in Sedimentary Provenance Studies[M].London:Oxford University Press,1991
[32]Walker R.G.An introduction to sedimentology[M].London:Academic Press.1982
[33]姜在兴主编.沉积学[M].北京:石油工业出版社,2003
[34]H.G.里丁主编,周明鉴,陈昌明等译.沉积环境和相[M].科学出版社,1991,10-19
[35]安作相.含油气盆地陆相沉积模式的探讨[J].沉积学报,1983,1(4),124-130
[36]吴崇筠.中国含油气盆地沉积学[M].北京:石油工业出版社,1993
[37]王金铎,韩文功,于建国,郑建斌.东营凹陷沙三段浊积岩体系及其油气勘探意义[J].石油学报,2003,24(5),24-29.
[38]田景春,曾允孚,张长俊等.东营凹陷沙河街组层序地层及地层格架研究[J].矿物岩石,1994,14(2):37-46.
[39]武法东,陈建渝,刘从印等.东营凹陷第三纪层序地层格架及沉积体系类型[J].现代地质,1998,12(4):559-566.
[40]冯有良.东营凹陷下第三系层序地层格架及盆地充填模式[J].地球科学,1999,24(6):635-642.
[41]李阳,蔡进功,刘建民.东营凹陷下第三系高分辨率层序地层研究[J].沉积学报,2002,20(2):210-216.
[42]张宗檩,操应长,高永进等.东营凹陷沙三段～沙一段层序地层与油气[J].石油勘探与开发,2003,30(3):29-31.
[43]孙龙德.东营凹陷中央隆起带沉积体系及隐蔽油气藏[J].新疆石油地质,2000,21(2):123-127
[44]于正军,韩宏伟,王福永.东营凹陷滚动勘探开发技术研究与应用[J].石油勘探与开发,2003,30(2):46-48
[45]范代读,丛友滋.东营三角洲的古流向研究[J].石油学报,2000,21(1):29-33
[46]方勇,邓宏文,MassimoSARTI等.东营三角洲演化特征与岩性圈闭分布规律[J].石油勘探与开发,2003,30(5):123-126
[47]Van Wagoner J C,Posamentier H W,Mitchum R M,Vail P R,Sarg J f,Lou-tit TS,Hardenbol J.An overview of the fundamentals of sequence strat-igraphy and key definition.In:Wilgus C K et al.Ed.Sea2level changes:an integrated ap2 proach.SEPM Spec.Pub.,1988,4,39～45
[48]徐怀大.寻找非构造油气藏的新思路[J].勘探家,北京:石油工业出版社,1996,(1),43～47
[49]操应长,姜在兴,王留奇等.陆相断陷湖盆层序地层单元的划分及界面识别标志[J].石油大学学报,1996,20(4),1-4
[50]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发.2000,27(5),119-121
[51]冯有良,邱以钢.高精度层序地层学在济阳坳陷下第三系隐蔽油气藏勘探中的应用[J].石油学报,2003,24(1),49-52
[52]侯遵泽.小波分析及其在勘查地球物理中的应用[J].物探与化探,1998,22(1):71～75
[53]飞思科技产品研发中心.MATLAB6.5辅助小波分析与应用[M],北京:电子工业出版社,2003
[54]胡昌华,张军波,夏军等.基于MATLAB的系统分析与设计——小波分析[M].陕西西安:西安电子科技大学出版社,1999
[55]董长虹主编.Matlab小波分析工具箱与应用[M].北京:国防工业出版社,2004:20
[56]王志坤,王多云,宋广寿等.测井信号小波分析在高分辨率层序地层划分中的应用[J].大庆石油学院学报,2005,29(6):17-20
[57]李江涛,余继峰,李增学.基于测井数据小波变换的层序划分[J].煤田地质与勘探,2004,30(2):48-50
[58]朱剑兵,纪友亮,赵培坤等.小波变换在层序地层单元自动划分中的应用[J].石油勘探与开发,2005,32(1):84-86
[59]苏德辰,李庆谋,罗光文,等.Fischer图解及其在旋回层序研究中的应用-以北京西山张夏组为例[J].现代地质,1995,9(3):279-283
[60]张世奇,宁学功.东营凹陷下第三系湖相密集段特征[J].石油大学学报:自然科学版,1997,21(2):4-7
[61]李丕龙等著.陆相断陷盆地油气地质与勘探[M].北京:石油工业出版
[2]潘元林编.中国隐蔽油气藏[M].北京:地质出版社,1998:2-18
[3]蔡希源,李思田,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[M].北京:地质出版社,2003:3-30
[4]张善文.济阳坳陷第三系隐蔽油气藏勘探理论与实践[J].石油与天然气地质,2006,27(6):731-740
[5]潘元林,李思田等.大型陆相断陷盆地层序地层与隐蔽油气藏研究——以济阳坳陷为例[M].石油工业出版社.2004
[6]王金铎,韩文功,于建国,郑建斌.东营凹陷沙三段浊积岩体系及其油气勘探意义[J].石油学报,2003,24(5),24-29
[7]张宗檩,操应长,高永进等.东营凹陷沙三段-沙一段层序地层与油气[J].石油勘探与开发,2003,30(3),29-31
[8]王秉海,钱凯主编.胜利油区地质研究与勘探实践[M].东营:石油大学出版社,1992
[9]Gino Cantalamessa,Claudio Di Celma,Luca Ragaini. Sequence stratigraphy of the Punta Ballena Member of the Jama Formation( Early Pleistocene,Ecuador):insights from integrated sedimentologic,taphonomic and paleoecologic analysis of molluscan shell concentrations[J]. Palaeogeography,Palaeoclimatology,Palaeoecology 216(2005)1–25
[10]Vail P R. Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure [A].In:Bally A W,ed. Atlas of seismic stratigraphy [C],AAPG,Studies in geology,1987,27
[11]Cross T A,Lessenger M A.Sediment volume partitioning:rationale for stratigraphic model evalution and high-resolution stratigraphic correlation [A],Gradstein F M,Sandvik K O,Milton N J,eds. Sequence statigraphy Concepts and Applications [M],NPF special publication,1998
[12]岳文浙,丁保良,魏乃颐.陆盆层序地层研究的思路[J].地质论评,2000,46(4)347-354
[13]C.K.威尔格斯等编,徐怀大译.层序地层学原理[M].北京:石油工业出版社,1993
[14]纪友亮等编.陆相断陷湖盆层序地层学[M].北京:石油工业出版社,1996
[15]纪友亮,张世奇.层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998
[16]罗立民等编.河湖沉积体系三维高分辨率层序地层学[M].北京:地质出版社,1999
[17]姜在兴等编.层序地层学原理及应用[M].北京:石油工业出版社,1996
[18]魏魁生,徐怀大.华北典型箕状盆地层序地层学模式及油气赋存关系[J].地球科学,1993,18(2),141-149
[19]刘招君,程日辉.层序地层学的概念,进展与争论[J].世界地质,1993,13(3),56-58
[20]胡受权.古气候变迁对泌阳断陷湖盆陆相层序发育的影响[J].江汉石油学院学报,1998,20(1),1-6
[21]操应长.断陷湖盆层序地层学[M].北京:地质出版社,2005
[22]顾家裕,郭彬程,张兴阳.中国陆相盆地层序地层格架及模式[J].石油勘探与开发,2005,32(5),11-15
[23]贾承造,赵文智,邹才能等.岩性地层油气藏勘探研究的两项核心技术[J].石油勘探与开发,2004,31(3):3-9
[24]操应长,姜在兴,夏斌等.声波时差资料识别层序地层单元界面的方法、原理及实例[J].沉积学报,2003,21(2),318-323
[25]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发.2000,27(5),119-121.
[26]苏德晨,李庆谋,罗光文等.Fisher图解在旋回层序地层研究中的应用[J].现代地质,1995,9(3),279-283
[27]朱剑兵,纪友亮,赵培坤等.小波变换在层序地层单元自动划分中的应用[J].石油勘探与开发,2005,32(1),84-86
[28]刘文业.小波分析在高分辨层序地层划分中的应用[J].地质力学学报,2006,12(1),64-70
[29]崔凤林,谢春来,付雷等.小波变缓时频能量谱技术在地震层序划分中的应用[J].长春科技大学学报,2000,30(4),397-400
[30]吴国忱,康仁华,印兴耀.三维时频分席在地震层序分析中的应用[J].石油大学学报(自然科学版),2000,24(1),81-85
[31]Haughton D W,Morton A C,Todd S P.Developments in Sedimentary Provenance Studies[M].London:Oxford University Press,1991
[32]Walker R.G.An introduction to sedimentology[M].London:Academic Press.1982
[33]姜在兴主编.沉积学[M].北京:石油工业出版社,2003
[34]H.G.里丁主编,周明鉴,陈昌明等译.沉积环境和相[M].科学出版社,1991,10-19
[35]安作相.含油气盆地陆相沉积模式的探讨[J].沉积学报,1983,1(4),124-130
[36]吴崇筠.中国含油气盆地沉积学[M].北京:石油工业出版社,1993
[37]王金铎,韩文功,于建国,郑建斌.东营凹陷沙三段浊积岩体系及其油气勘探意义[J].石油学报,2003,24(5),24-29.
[38]田景春,曾允孚,张长俊等.东营凹陷沙河街组层序地层及地层格架研究[J].矿物岩石,1994,14(2):37-46.
[39]武法东,陈建渝,刘从印等.东营凹陷第三纪层序地层格架及沉积体系类型[J].现代地质,1998,12(4):559-566.
[40]冯有良.东营凹陷下第三系层序地层格架及盆地充填模式[J].地球科学,1999,24(6):635-642.
[41]李阳,蔡进功,刘建民.东营凹陷下第三系高分辨率层序地层研究[J].沉积学报,2002,20(2):210-216.
[42]张宗檩,操应长,高永进等.东营凹陷沙三段～沙一段层序地层与油气[J].石油勘探与开发,2003,30(3):29-31.
[43]孙龙德.东营凹陷中央隆起带沉积体系及隐蔽油气藏[J].新疆石油地质,2000,21(2):123-127
[44]于正军,韩宏伟,王福永.东营凹陷滚动勘探开发技术研究与应用[J].石油勘探与开发,2003,30(2):46-48
[45]范代读,丛友滋.东营三角洲的古流向研究[J].石油学报,2000,21(1):29-33
[46]方勇,邓宏文,MassimoSARTI等.东营三角洲演化特征与岩性圈闭分布规律[J].石油勘探与开发,2003,30(5):123-126
[47]Van Wagoner J C,Posamentier H W,Mitchum R M,Vail P R,Sarg J f,Lou-tit TS,Hardenbol J.An overview of the fundamentals of sequence strat-igraphy and key definition.In:Wilgus C K et al.Ed.Sea2level changes:an integrated ap2 proach.SEPM Spec.Pub.,1988,4,39～45
[48]徐怀大.寻找非构造油气藏的新思路[J].勘探家,北京:石油工业出版社,1996,(1),43～47
[49]操应长,姜在兴,王留奇等.陆相断陷湖盆层序地层单元的划分及界面识别标志[J].石油大学学报,1996,20(4),1-4
[50]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发.2000,27(5),119-121
[51]冯有良,邱以钢.高精度层序地层学在济阳坳陷下第三系隐蔽油气藏勘探中的应用[J].石油学报,2003,24(1),49-52
[52]侯遵泽.小波分析及其在勘查地球物理中的应用[J].物探与化探,1998,22(1):71～75
[53]飞思科技产品研发中心.MATLAB6.5辅助小波分析与应用[M],北京:电子工业出版社,2003
[54]胡昌华,张军波,夏军等.基于MATLAB的系统分析与设计——小波分析[M].陕西西安:西安电子科技大学出版社,1999
[55]董长虹主编.Matlab小波分析工具箱与应用[M].北京:国防工业出版社,2004:20
[56]王志坤,王多云,宋广寿等.测井信号小波分析在高分辨率层序地层划分中的应用[J].大庆石油学院学报,2005,29(6):17-20
[57]李江涛,余继峰,李增学.基于测井数据小波变换的层序划分[J].煤田地质与勘探,2004,30(2):48-50
[58]朱剑兵,纪友亮,赵培坤等.小波变换在层序地层单元自动划分中的应用[J].石油勘探与开发,2005,32(1):84-86
[59]苏德辰,李庆谋,罗光文,等.Fischer图解及其在旋回层序研究中的应用-以北京西山张夏组为例[J].现代地质,1995,9(3):279-283
[60]张世奇,宁学功.东营凹陷下第三系湖相密集段特征[J].石油大学学报:自然科学版,1997,21(2):4-7
[61]李丕龙等著.陆相断陷盆地油气地质与勘探[M].北京:石油工业出版