曲堤油田西区古近系沙河街组沉积相研究
|
摘要
惠民凹陷是渤海湾盆地内重要的含油气单元,本文主要是对位于惠民凹陷南斜坡上的曲堤油田西区古近系沙河街组沉积相及砂体展布规律进行研究。经过多年的勘探与研究,曲堤油田已发现一批以构造油气藏为主的油气田。但近年来随着岩性油气藏、古潜山油气藏等隐蔽油气藏的相继发现,认为研究区仍有很大的勘探潜力,这对于曲堤油田的增储上产具有重要意义。
在系统研究了曲堤地垒带的基本特征、形成及演化的基础上,以岩心资料、测井资料为主,结合地震资料,根据不同断块的特征各自建立标准井,并以标准井为中心,结合邻井进行追踪和对比,将该区200余口井的目标层位进行了系统的地层划分与对比,将沙河街组自上而下划分为沙一段、沙二段、沙三段、沙四上、中、下亚段。
通过对该区沉积岩的矿物组成、沉积构造、古生物学特征以及地球物理特征等沉积相标志的综合研究判断,认为研本区沙河街组主要发育冲积扇、河流、三角洲、湖泊四种沉积体系。识别出研究区沙四下亚段主要发育扇中—扇端亚相;沙四上、中亚段主要发育曲流河亚相,局部受断层控制而发育小型冲积扇;沙三、沙二段主要发育三角洲前缘亚相;沙一段主要发育浅湖亚相。
利用阴极发光、轻重矿物分析、岩屑分析、砂砾岩百分含量分析等方法确定了研究区物源主要来自于东南方向鲁西隆起的前寒武纪片麻岩和古、中生代以及新生代的花岗岩。并在此基础上,以石油地质学、沉积学等理论为指导,结合单井、连井沉积学分析,利用单优势相作图的方法,编制沙一至沙四段(包括沙四上、中、下亚段)的岩相古地理图,并结合沉积相联井剖面对比图详细研究了各层段的沉积相与砂体展布特征。
Huimin depression is important oil and gas bearing basin in Bohai Bay Basin. Sedimentary facies and distribution of sand bodies of the Shahejie formation in the west Qudi oil field, that is located in the south slope of Huimin depression, were systematieally studied. After many years of exploration and research, many oil and gas fields based on structural reservoir have been diseovered. In recent years, with many sequent discoveriesof elusive reservoir, such as stratigraphic reservoir and ancient buried hill hydrocarbon reservoir, we believe there is still much potential for exploration in Qudi oil field, and these discoveries will exert a profound enfluence on the output of reserves.
Based on the comprehensive research of basic characteristics, formation and evolution in Qudi oil field, from studying some data of well drilling, logging and seismic, the typical well depending on the characteristics of fault-block has been set up, and 200 wells' stratum in the study area have been divided and compared. Shahejie formation has been divided into Es1, Es2, Es3 Es4S, Es4Z, Es4X.
Based on the study of facies indicators of sedimentary structure, Biological characteristics and geophysical signature, 4 depositional system including alluvial fan , fluvial, delta, lacustrine developed in Shahejie formation, and the mid-fan,end-fan, mainly developed during the depositional Period of Es4X, meandering river- Miniature alluvial fan mainly developed during the depositional Period of Es4S- Es4Z,delta front developed during the depositional Period of Es3- Es2, shallow lake mainly developed during the depositional Period of Es1.
From analyses of cathodeluminescence, light mineral, heavy mineral and cuttings, the provenance system that mainly comes from west Shandong uplift and mainly direction is south-east trending has been comfirmed. On the basis of provenance system, under the guidance of Petroleum Geology and Sedimentology theory, according to the sand content chorisopleth and the distribution of sand thickness, lithofacies paleogeography maps of Es1-Es4(including ESsS,Es4Z,Es4X) have been drawn, and sedimentary facies, unfold characters of sandstones have been detailly study.
在系统研究了曲堤地垒带的基本特征、形成及演化的基础上,以岩心资料、测井资料为主,结合地震资料,根据不同断块的特征各自建立标准井,并以标准井为中心,结合邻井进行追踪和对比,将该区200余口井的目标层位进行了系统的地层划分与对比,将沙河街组自上而下划分为沙一段、沙二段、沙三段、沙四上、中、下亚段。
通过对该区沉积岩的矿物组成、沉积构造、古生物学特征以及地球物理特征等沉积相标志的综合研究判断,认为研本区沙河街组主要发育冲积扇、河流、三角洲、湖泊四种沉积体系。识别出研究区沙四下亚段主要发育扇中—扇端亚相;沙四上、中亚段主要发育曲流河亚相,局部受断层控制而发育小型冲积扇;沙三、沙二段主要发育三角洲前缘亚相;沙一段主要发育浅湖亚相。
利用阴极发光、轻重矿物分析、岩屑分析、砂砾岩百分含量分析等方法确定了研究区物源主要来自于东南方向鲁西隆起的前寒武纪片麻岩和古、中生代以及新生代的花岗岩。并在此基础上,以石油地质学、沉积学等理论为指导,结合单井、连井沉积学分析,利用单优势相作图的方法,编制沙一至沙四段(包括沙四上、中、下亚段)的岩相古地理图,并结合沉积相联井剖面对比图详细研究了各层段的沉积相与砂体展布特征。
Huimin depression is important oil and gas bearing basin in Bohai Bay Basin. Sedimentary facies and distribution of sand bodies of the Shahejie formation in the west Qudi oil field, that is located in the south slope of Huimin depression, were systematieally studied. After many years of exploration and research, many oil and gas fields based on structural reservoir have been diseovered. In recent years, with many sequent discoveriesof elusive reservoir, such as stratigraphic reservoir and ancient buried hill hydrocarbon reservoir, we believe there is still much potential for exploration in Qudi oil field, and these discoveries will exert a profound enfluence on the output of reserves.
Based on the comprehensive research of basic characteristics, formation and evolution in Qudi oil field, from studying some data of well drilling, logging and seismic, the typical well depending on the characteristics of fault-block has been set up, and 200 wells' stratum in the study area have been divided and compared. Shahejie formation has been divided into Es1, Es2, Es3 Es4S, Es4Z, Es4X.
Based on the study of facies indicators of sedimentary structure, Biological characteristics and geophysical signature, 4 depositional system including alluvial fan , fluvial, delta, lacustrine developed in Shahejie formation, and the mid-fan,end-fan, mainly developed during the depositional Period of Es4X, meandering river- Miniature alluvial fan mainly developed during the depositional Period of Es4S- Es4Z,delta front developed during the depositional Period of Es3- Es2, shallow lake mainly developed during the depositional Period of Es1.
From analyses of cathodeluminescence, light mineral, heavy mineral and cuttings, the provenance system that mainly comes from west Shandong uplift and mainly direction is south-east trending has been comfirmed. On the basis of provenance system, under the guidance of Petroleum Geology and Sedimentology theory, according to the sand content chorisopleth and the distribution of sand thickness, lithofacies paleogeography maps of Es1-Es4(including ESsS,Es4Z,Es4X) have been drawn, and sedimentary facies, unfold characters of sandstones have been detailly study.
引文
[1]Borowski W.S.,Paull C.K.,Usslerll I.W..Marine pore-water sulfate profiles indicate in situ methane flux from underlying gas hydrate[J].Geology,1996,24(7):655-658
[2]Brijraj K.D.,Al-Mikhlafi A.S.,Kaur P..Geochemistry of Mansar Lake sediments,Jammu,India:Implication for source-area weathering,provenance,and tectonic setting[J].Journal of Asian Earth Sciences,2006,26:649-668.
[3]Bruhn F.,Veizer J.,Buhl D.,et al.,Diagenetic history of the Korallenoolith(Malm) of northwestern Germany.Implications from insitu trace element and isotopic studies[J].Nuclear Instruments and Methods in Physics Research B,2005,231:518-523.
[4]Hanson A.D..Evidence for Cenozoic erosional unroofing adjacent to the Norhtern Qaidam Basin,NW China,Preserved within basin margin strata[J].Abstracts with Programs-Geological Society of American,1999,6:143
[5]Kwon Y.H.,Park K.S.,Yu K.M..Detrital heavy-mineral Charactetisfies of rift-related sediments from the Dragon-1 Well in the Cheju Basin(NE East China Sea),Korea[J].Geoscience Journal (Seoul),1999,3:115-121
[6]Mclennan S.M.,Bock B.,Comptton W.,et al.Detrital zeroon geochronology of Taconian and Acadian foreland sedimentary rocks in New England[J].Journal of Sedimentary.Rearch,2001,71(2):305-317
[7]Morton A.C.,Hallsworth C.R..Processes controlling the composition of heavy mineral assemblages in sandstones[J].Sedimentary Geology,1999,124:3-29
[8]Sambridge M.S.Compston W..Mixture modeling of Multi-component data sets with application to ion-probe zircon ages[J].Earth and Planetary Science Letters,1994,18:373-390.
[9]She Zhenbing,Ma Changqian,Mason R.,et al.Provenance of the Triassic Songpan-Ganzi flysch,West China[J].Chemical Geology,2006,231:159-175
[10]Van Wagoner,J.C.Siliciclastic sequence stratigraphy in well logs,cores and outcrops:concepts for high-resolution correlation of time and faces[J].AAPG.Bulletin,1990,74(1):126-139
[11]陈发景等.中国东部中、新生代伸展构造特征及地球动力学背景[J].地球:科学(中国地质大学学报),1996,21(4):357-365
[12]陈洁,张学才.渤海湾盆地构造圈闭类型与勘探方向—以济阳坳陷为例[J].地球物理学进展.2006,21(3):872-878
[13]陈洁.济阳坳陷第三系构造层序及其演化[J].地球物理学进展,2003,18(4):700-706
[14]陈书平,戴俊生,李理.惠民—东营盆地构造特征及控油作用[J].石油与天然气地质,1999,20(4):344-348
[15]池英柳,赵文智.渤海湾盆地油气富集带的形成与分布[J].勘探家,2000,5(11):9-16
[16]丁增勇,王良书,张鹏.济阳坳陷及鲁西隆起区中、新生代伸展与断裂活动特征[J].石油与天然气地质,2008,29(1):107-112
[17]杜玉民.夏口断层对临南斜坡区油气分布及运移方向的影响[J].新疆石油地质,2005,26(5):525-528
[18]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003,21(1):137-141
[19]郭龙.曲堤复杂断块油气田的特点及开发技术政策研究[J].特种油气藏,2003,10(3):65-69
[20]郭兴伟,施小斌,丘学林,等.渤海湾盆地新生代沉降特征及其动力学机制探讨[J].中国石油大学学报,2006,30(3):6-11
[21]何起祥.沉积地球科学的历史回顾与展望[J].沉积学报,2003,23(1):10-18
[22]何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32
[23]胡宗全,周新科,张玉兰.济阳坳陷前第三系油气勘探前景[J].石油与天然气地质,2005,26(5):655-660
[24]黄思静,佟宏鹏,黄可可.阴极发光分析在恢复砂岩碎屑长石含量中的应用—鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J].地球科学进展,2008,23(10):1013-1019
[25]贾志斌,田新琦.渤海湾盆地成因机制与油气评价[J].石油地球物理勘探,2003,38(1):62-66
[26]李惠玲,李红梅.惠民凹陷南坡天然气藏形成条件及勘探方向[J].2008,24(7-8):47-50
[27]李军,王培.渤海湾盆地构造格架及演化[J].石油与天然气地质,1998,19(1):63-67
[28]李丕龙,金之钧,张善文,等.济阳坳陷油气勘探现状及主要研究进展[J].油勘探与开发,2003,30(3):1-4
[29]李思田.沉积盆地动力学分析—盆地研究领域的主要趋向[J].地学前缘.1995,2(3-4):1-7
[30]梁生正,杨国奇,田建章,等.渤海湾叠合盆地大中型天然气田的勘探方向[J].石油学报,2001,22(6):1-4
[31]梁生正,张以明.渤海湾盆地油气地质与勘探[J].中国石油勘探,2006,11(2):1-7
[32]刘宝珺,韩作振,杨仁超.当代沉积学研究进展、前瞻与思考[J].特种油气藏,2006,13(5):1-9
[33]刘宝珺,李廷栋.地质学的若干问题[J].地球科学进展,2001,16(5):607-616
[34]刘宝珺,王剑,谢渊,等.当代沉积学研究的新进展与发展趋势—来自第三十一届国际地质大会的信息[J].沉积与特堤斯地质,2002,22(1):1-6
[35]刘宝珺,中国沉积学的回顾和展望[J].矿物岩石,2001,21(3):1-7
[36]刘光鼎.前新生代海相残留盆地[J].地球物理学进展,2001,16(2):1-7
[37]梅志超.沉积相与古地理重建[M].西安:西北大学出版社.1994:30-55
[38]潘元林,李思川.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].北京:石油工业出版社,2004,24-81
[39]漆家福等.渤海湾新生代裂陷盆地的伸展模式及其动力学过程[J].石油实验地质,1995,17(4):316-323
[40]秦永霞,姜素华,王永诗.斜坡带油气成藏特征与勘探方法[J].复式油气田,1999,5(3):10-14
[41]邵磊,李文厚,袁明生.吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析[J].沉积学报,1999, 17(3):435-442
[42]胜利油田石油地质志编写组.中国石油地质志(卷六):胜利油田分卷[M].北京:石油工业出版社,1998:32-50
[43]苏向光,邱楠生.济阳坳陷惠民凹陷热演化史分析[J].天然气工业,2006,26(10):15-17
[44]孙枢.中国沉积学的今后发展:若干思考与建议[J].地学前缘,2005,12(2):3-10
[45]覃建雄,等.现代沉积学理论的重大进展[J].地质科技情报,1995,14(3):5-16
[46]覃克,赵密福.惠民凹陷临南斜坡带油气成藏模式[J].石油大学学报,2002,26(2):21-32
[47]汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000,20(4):104-110
[48]王秉海,钱凯.胜利油区地质研究与勘探实践[M].山东东营:石油大学出皈社,1992,23-52
[49]王光付,战春光,刘显太.精细地层对比技术在油藏挖潜中的应用[J].石油勘探与开发,2002,27(6):56-621
[50]王俊玲,郑和荣.中国东部成熟探区剩余油气资源潜力及重点勘探领域[J].石油与天然气地质,2003,24(3):296-300
[51]王世虎,夏斌,陈根文,等.济阳坳陷构造特征及形成机制讨论[J].大地构造与成矿学,2004,28(4):428-434
[52]王英华,张绍平,潘荣胜.阴极发光技术在地质学中的应用[M].北京:地质出版社,1990:10-34
[53]王颖,高锡奎,高博禹.济阳坳陷构造演化特征[J].成都理工学院学报,2002.29(2):181-189
[54]王毓俊,田在艺.华北东部盆地油气勘探潜力与发展方向[J].石油学报,2003,24(7):7-12
[55]吴兴宁,周建勋.渤海湾盆地构造成因观点剖析[J].地球物理学进展,2000,15(1):98-107
[56]鲜本忠,姜在兴.环境沉积学的兴起[J].沉积学报,2005,23(4):677-682
[57]谢锐杰,漆家福,王永诗,等.海湾盆地东营凹陷北部地区新生代构造演化特征研究[J].石油实验地质,2004,26(5):427-431
[58]徐强,刘宝,朱同兴,等.中国沉积学研究的现状和发展方向[J].西南石油学院学报,2000,22(3):1-4
[59]闫义,林舸,王岳军,等.盆地陆源碎屑沉积物对源区构造背景的指示意[J].地球科学进展,2002,17(1):85-90
[60]杨俊生,樊太亮.惠民凹陷古近系沙河街组三段沉积体系[J].新疆石油地质,2007,28(4):457-461
[61]于兴河,郑秀娟.沉积学的发展历程与未来展望[J].地球科学进展,2004,19(2):173-182
[62]余素玉.沉积学紧张中的若干主要方向[J].地学前缘,1994,1(1-2):170-183
[63]袁选俊,谯汉生.渤海湾盆地富油气凹陷隐蔽油气藏勘探[J].石油与天然气地质,2002,23(2):130-133
[64]越俊生,陆克政,漆家福,等.渤海湾盆地早第三纪构造样式的演化[J].石油学报,1998,19(4):16-20
[65]曾允孚,覃建雄.沉积学发展现状与前瞻[J].成都理工学院学报,1999,26(1):1-7
[66]翟光明,何文渊.渤海湾盆地勘探策略探讨[J].石油勘探与开发,2003,30(6):1-4
[67]翟光明,何文渊.渤海湾盆地资源潜力和进一步勘探方向的探讨[J].石油学报,2002,23(1):1-5
[68]翟中喜,白振瑞,渤海湾盆地石油储量增长规律及潜力分析[J].石油与天然气地质,2008,29(1):88-94
[69]张本琪,余宏忠,姜在兴.应用阴极发光技术研究母岩性质及成岩环境[J].石油勘探与开发,2003,30(3):117-118.
[70]赵澄林,朱筱敏.沉积岩石学[M].第三版,北京:石油工业出版社.2001:91-92
[71]赵红格,刘池阳.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415
[72]赵密福,刘泽容,信荃麟,等.惠民凹陷临南地区断层活动特征及控油作用[J].石油勘探与开发,2000,27(6):9-11
[73]郑秀娟,于兴河,李胜利.环境沉积学及其发展趋势[J].海洋地质动态,2003,19(10):8-11
[74]朱光有,金强,张永昌.惠民断陷湖盆演化过程与油气生成[J].新疆石油地质,2006,27(1):27-31
[75]朱筱敏,信荃麟,张晋仁.断陷湖盆滩坝储集体沉积特征及沉积模式[J].沉积学报,1994,12(2):20-28
[76]宗国洪,肖焕钦,李长宝,等.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282
[2]Brijraj K.D.,Al-Mikhlafi A.S.,Kaur P..Geochemistry of Mansar Lake sediments,Jammu,India:Implication for source-area weathering,provenance,and tectonic setting[J].Journal of Asian Earth Sciences,2006,26:649-668.
[3]Bruhn F.,Veizer J.,Buhl D.,et al.,Diagenetic history of the Korallenoolith(Malm) of northwestern Germany.Implications from insitu trace element and isotopic studies[J].Nuclear Instruments and Methods in Physics Research B,2005,231:518-523.
[4]Hanson A.D..Evidence for Cenozoic erosional unroofing adjacent to the Norhtern Qaidam Basin,NW China,Preserved within basin margin strata[J].Abstracts with Programs-Geological Society of American,1999,6:143
[5]Kwon Y.H.,Park K.S.,Yu K.M..Detrital heavy-mineral Charactetisfies of rift-related sediments from the Dragon-1 Well in the Cheju Basin(NE East China Sea),Korea[J].Geoscience Journal (Seoul),1999,3:115-121
[6]Mclennan S.M.,Bock B.,Comptton W.,et al.Detrital zeroon geochronology of Taconian and Acadian foreland sedimentary rocks in New England[J].Journal of Sedimentary.Rearch,2001,71(2):305-317
[7]Morton A.C.,Hallsworth C.R..Processes controlling the composition of heavy mineral assemblages in sandstones[J].Sedimentary Geology,1999,124:3-29
[8]Sambridge M.S.Compston W..Mixture modeling of Multi-component data sets with application to ion-probe zircon ages[J].Earth and Planetary Science Letters,1994,18:373-390.
[9]She Zhenbing,Ma Changqian,Mason R.,et al.Provenance of the Triassic Songpan-Ganzi flysch,West China[J].Chemical Geology,2006,231:159-175
[10]Van Wagoner,J.C.Siliciclastic sequence stratigraphy in well logs,cores and outcrops:concepts for high-resolution correlation of time and faces[J].AAPG.Bulletin,1990,74(1):126-139
[11]陈发景等.中国东部中、新生代伸展构造特征及地球动力学背景[J].地球:科学(中国地质大学学报),1996,21(4):357-365
[12]陈洁,张学才.渤海湾盆地构造圈闭类型与勘探方向—以济阳坳陷为例[J].地球物理学进展.2006,21(3):872-878
[13]陈洁.济阳坳陷第三系构造层序及其演化[J].地球物理学进展,2003,18(4):700-706
[14]陈书平,戴俊生,李理.惠民—东营盆地构造特征及控油作用[J].石油与天然气地质,1999,20(4):344-348
[15]池英柳,赵文智.渤海湾盆地油气富集带的形成与分布[J].勘探家,2000,5(11):9-16
[16]丁增勇,王良书,张鹏.济阳坳陷及鲁西隆起区中、新生代伸展与断裂活动特征[J].石油与天然气地质,2008,29(1):107-112
[17]杜玉民.夏口断层对临南斜坡区油气分布及运移方向的影响[J].新疆石油地质,2005,26(5):525-528
[18]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003,21(1):137-141
[19]郭龙.曲堤复杂断块油气田的特点及开发技术政策研究[J].特种油气藏,2003,10(3):65-69
[20]郭兴伟,施小斌,丘学林,等.渤海湾盆地新生代沉降特征及其动力学机制探讨[J].中国石油大学学报,2006,30(3):6-11
[21]何起祥.沉积地球科学的历史回顾与展望[J].沉积学报,2003,23(1):10-18
[22]何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32
[23]胡宗全,周新科,张玉兰.济阳坳陷前第三系油气勘探前景[J].石油与天然气地质,2005,26(5):655-660
[24]黄思静,佟宏鹏,黄可可.阴极发光分析在恢复砂岩碎屑长石含量中的应用—鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J].地球科学进展,2008,23(10):1013-1019
[25]贾志斌,田新琦.渤海湾盆地成因机制与油气评价[J].石油地球物理勘探,2003,38(1):62-66
[26]李惠玲,李红梅.惠民凹陷南坡天然气藏形成条件及勘探方向[J].2008,24(7-8):47-50
[27]李军,王培.渤海湾盆地构造格架及演化[J].石油与天然气地质,1998,19(1):63-67
[28]李丕龙,金之钧,张善文,等.济阳坳陷油气勘探现状及主要研究进展[J].油勘探与开发,2003,30(3):1-4
[29]李思田.沉积盆地动力学分析—盆地研究领域的主要趋向[J].地学前缘.1995,2(3-4):1-7
[30]梁生正,杨国奇,田建章,等.渤海湾叠合盆地大中型天然气田的勘探方向[J].石油学报,2001,22(6):1-4
[31]梁生正,张以明.渤海湾盆地油气地质与勘探[J].中国石油勘探,2006,11(2):1-7
[32]刘宝珺,韩作振,杨仁超.当代沉积学研究进展、前瞻与思考[J].特种油气藏,2006,13(5):1-9
[33]刘宝珺,李廷栋.地质学的若干问题[J].地球科学进展,2001,16(5):607-616
[34]刘宝珺,王剑,谢渊,等.当代沉积学研究的新进展与发展趋势—来自第三十一届国际地质大会的信息[J].沉积与特堤斯地质,2002,22(1):1-6
[35]刘宝珺,中国沉积学的回顾和展望[J].矿物岩石,2001,21(3):1-7
[36]刘光鼎.前新生代海相残留盆地[J].地球物理学进展,2001,16(2):1-7
[37]梅志超.沉积相与古地理重建[M].西安:西北大学出版社.1994:30-55
[38]潘元林,李思川.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].北京:石油工业出版社,2004,24-81
[39]漆家福等.渤海湾新生代裂陷盆地的伸展模式及其动力学过程[J].石油实验地质,1995,17(4):316-323
[40]秦永霞,姜素华,王永诗.斜坡带油气成藏特征与勘探方法[J].复式油气田,1999,5(3):10-14
[41]邵磊,李文厚,袁明生.吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析[J].沉积学报,1999, 17(3):435-442
[42]胜利油田石油地质志编写组.中国石油地质志(卷六):胜利油田分卷[M].北京:石油工业出版社,1998:32-50
[43]苏向光,邱楠生.济阳坳陷惠民凹陷热演化史分析[J].天然气工业,2006,26(10):15-17
[44]孙枢.中国沉积学的今后发展:若干思考与建议[J].地学前缘,2005,12(2):3-10
[45]覃建雄,等.现代沉积学理论的重大进展[J].地质科技情报,1995,14(3):5-16
[46]覃克,赵密福.惠民凹陷临南斜坡带油气成藏模式[J].石油大学学报,2002,26(2):21-32
[47]汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000,20(4):104-110
[48]王秉海,钱凯.胜利油区地质研究与勘探实践[M].山东东营:石油大学出皈社,1992,23-52
[49]王光付,战春光,刘显太.精细地层对比技术在油藏挖潜中的应用[J].石油勘探与开发,2002,27(6):56-621
[50]王俊玲,郑和荣.中国东部成熟探区剩余油气资源潜力及重点勘探领域[J].石油与天然气地质,2003,24(3):296-300
[51]王世虎,夏斌,陈根文,等.济阳坳陷构造特征及形成机制讨论[J].大地构造与成矿学,2004,28(4):428-434
[52]王英华,张绍平,潘荣胜.阴极发光技术在地质学中的应用[M].北京:地质出版社,1990:10-34
[53]王颖,高锡奎,高博禹.济阳坳陷构造演化特征[J].成都理工学院学报,2002.29(2):181-189
[54]王毓俊,田在艺.华北东部盆地油气勘探潜力与发展方向[J].石油学报,2003,24(7):7-12
[55]吴兴宁,周建勋.渤海湾盆地构造成因观点剖析[J].地球物理学进展,2000,15(1):98-107
[56]鲜本忠,姜在兴.环境沉积学的兴起[J].沉积学报,2005,23(4):677-682
[57]谢锐杰,漆家福,王永诗,等.海湾盆地东营凹陷北部地区新生代构造演化特征研究[J].石油实验地质,2004,26(5):427-431
[58]徐强,刘宝,朱同兴,等.中国沉积学研究的现状和发展方向[J].西南石油学院学报,2000,22(3):1-4
[59]闫义,林舸,王岳军,等.盆地陆源碎屑沉积物对源区构造背景的指示意[J].地球科学进展,2002,17(1):85-90
[60]杨俊生,樊太亮.惠民凹陷古近系沙河街组三段沉积体系[J].新疆石油地质,2007,28(4):457-461
[61]于兴河,郑秀娟.沉积学的发展历程与未来展望[J].地球科学进展,2004,19(2):173-182
[62]余素玉.沉积学紧张中的若干主要方向[J].地学前缘,1994,1(1-2):170-183
[63]袁选俊,谯汉生.渤海湾盆地富油气凹陷隐蔽油气藏勘探[J].石油与天然气地质,2002,23(2):130-133
[64]越俊生,陆克政,漆家福,等.渤海湾盆地早第三纪构造样式的演化[J].石油学报,1998,19(4):16-20
[65]曾允孚,覃建雄.沉积学发展现状与前瞻[J].成都理工学院学报,1999,26(1):1-7
[66]翟光明,何文渊.渤海湾盆地勘探策略探讨[J].石油勘探与开发,2003,30(6):1-4
[67]翟光明,何文渊.渤海湾盆地资源潜力和进一步勘探方向的探讨[J].石油学报,2002,23(1):1-5
[68]翟中喜,白振瑞,渤海湾盆地石油储量增长规律及潜力分析[J].石油与天然气地质,2008,29(1):88-94
[69]张本琪,余宏忠,姜在兴.应用阴极发光技术研究母岩性质及成岩环境[J].石油勘探与开发,2003,30(3):117-118.
[70]赵澄林,朱筱敏.沉积岩石学[M].第三版,北京:石油工业出版社.2001:91-92
[71]赵红格,刘池阳.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415
[72]赵密福,刘泽容,信荃麟,等.惠民凹陷临南地区断层活动特征及控油作用[J].石油勘探与开发,2000,27(6):9-11
[73]郑秀娟,于兴河,李胜利.环境沉积学及其发展趋势[J].海洋地质动态,2003,19(10):8-11
[74]朱光有,金强,张永昌.惠民断陷湖盆演化过程与油气生成[J].新疆石油地质,2006,27(1):27-31
[75]朱筱敏,信荃麟,张晋仁.断陷湖盆滩坝储集体沉积特征及沉积模式[J].沉积学报,1994,12(2):20-28
[76]宗国洪,肖焕钦,李长宝,等.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282