陇东地区侏罗系沉积体系及成藏潜力研究
|
摘要
鄂尔多斯盆地陇东地区富县组、延10-延6油层组是该地区侏罗系的主要产油层,发育河流、曲流河三角洲沉积,属特低孔~低孔、特低渗~低渗储层。本次研究综合应用了地质、钻井、测井及地震等资料,在层序地层学、储层沉积学、地球物理测井等理论的基础上,进行了多学科、一体化的综合分析。建立了目的层段的层序地层格架,开展了物源与沉积相研究,恢复了研究区前侏罗纪古地貌特征,并对储层特征进行了分析。同时,在储层研究的基础上划分出油藏的成藏模式。
本次研究取得的主要成果与认识有：
1、研究区古地貌划分为侵蚀河谷、古高地、古隆起斜坡带、古阶地、河间丘。具体划分为4条古河：甘陕一级古河谷、庆西二级古河谷及贺旗支河、庆合支河两支三级支河谷；3个高地：演武高地、姬塬高地及子午岭高地；3个斜坡：演武北坡、姬塬南坡及子午岭斜坡；6个河间丘及阶地。
2、研究区岩石的结构成熟度和成分成熟度均较低。物源方向主要为北和北西、南和南西；侏罗系富县组及延安组延10~延6油层组自下而上构成了河流相-曲流河三角洲相沉积体系,其中富县组、延10段主要发育辫状河沉积,自延9段逐渐向上过渡为曲流河三角洲沉积。
3、研究区油气成藏的地质条件为烃源岩、油气运移、储盖组合及成藏等；将研究区油藏类型分为岩性油藏及复合圈闭油藏,其中岩性油藏在研究区多见,而复合圈闭油藏主要发育于研究区北部。
4、结合研究区构造、沉积相及储层特征等多种因素,划分出研究区古地貌油藏成藏模式分别为河间丘式、坡咀式、斜坡式及高地式。
Fuxian formation and Yan10～Yan6oil formation are the major oil producing zone of Longdong area in Odors basin. They are river and meandering delta sedimentary and are ultra-low porosity-low porosity and ultra-low permeability-low permeability reservoir. Geology, drilling, well logging, seismic data and so on were used in the study. On the basic of the theory of sequence stratigraphy, reservoir sedimentology, geophysical logging, the reserch was multi-disciplinary and integrated systematic analyed. We studyed on the sequence stratigraphy, source, reservoir, pre-Jurassic paleogeomorphological feature of research area and reservoir feature. At the same time, we divided accumulation model in research are.
There are some main results and understanding:
1. The palaogeomorphology was divided into erode-valley, ancient-upland, ancient uplift slope band, ancient terrace and mound; There are four ancient rivers:the first of Ganshan, the second of Qingxi, the third of Heqi and Qinghe; three ancient-upland: Yanwu, Jiyuan and Ziwuling ancient-upland. Six mounds and terraces.
2. The structue maturity and component maturity are poor. Moreover, The direction of provenance are north and northwest, south and southwest. The Fuxian formation and Yan10～Yan6formations of Jurassic are river-meandering river delta deposits from below to above. And Fuxian Group and YanlO formation are the braid river sedimentary reservoir, Yan9formation and other formations which is above Yan9gradually become meandering river delta reservoir.
3. The geological condition and factors of oil reservoir formation in research area are source rocks, hydrocarbon migration, reservoir seal assemblage and reservoir formation. The types of reservoir in area are devided into lithologic reservoir which is more in research area and complex reservoir which is distributed in north of area.
4. According to Structure, sedimentary facies, reservoir characteristics and so on in the study area, we summarized that there are four oil reservoir formation models, mound model, uplift model, slope model and upland model.
本次研究取得的主要成果与认识有：
1、研究区古地貌划分为侵蚀河谷、古高地、古隆起斜坡带、古阶地、河间丘。具体划分为4条古河：甘陕一级古河谷、庆西二级古河谷及贺旗支河、庆合支河两支三级支河谷；3个高地：演武高地、姬塬高地及子午岭高地；3个斜坡：演武北坡、姬塬南坡及子午岭斜坡；6个河间丘及阶地。
2、研究区岩石的结构成熟度和成分成熟度均较低。物源方向主要为北和北西、南和南西；侏罗系富县组及延安组延10~延6油层组自下而上构成了河流相-曲流河三角洲相沉积体系,其中富县组、延10段主要发育辫状河沉积,自延9段逐渐向上过渡为曲流河三角洲沉积。
3、研究区油气成藏的地质条件为烃源岩、油气运移、储盖组合及成藏等；将研究区油藏类型分为岩性油藏及复合圈闭油藏,其中岩性油藏在研究区多见,而复合圈闭油藏主要发育于研究区北部。
4、结合研究区构造、沉积相及储层特征等多种因素,划分出研究区古地貌油藏成藏模式分别为河间丘式、坡咀式、斜坡式及高地式。
Fuxian formation and Yan10～Yan6oil formation are the major oil producing zone of Longdong area in Odors basin. They are river and meandering delta sedimentary and are ultra-low porosity-low porosity and ultra-low permeability-low permeability reservoir. Geology, drilling, well logging, seismic data and so on were used in the study. On the basic of the theory of sequence stratigraphy, reservoir sedimentology, geophysical logging, the reserch was multi-disciplinary and integrated systematic analyed. We studyed on the sequence stratigraphy, source, reservoir, pre-Jurassic paleogeomorphological feature of research area and reservoir feature. At the same time, we divided accumulation model in research are.
There are some main results and understanding:
1. The palaogeomorphology was divided into erode-valley, ancient-upland, ancient uplift slope band, ancient terrace and mound; There are four ancient rivers:the first of Ganshan, the second of Qingxi, the third of Heqi and Qinghe; three ancient-upland: Yanwu, Jiyuan and Ziwuling ancient-upland. Six mounds and terraces.
2. The structue maturity and component maturity are poor. Moreover, The direction of provenance are north and northwest, south and southwest. The Fuxian formation and Yan10～Yan6formations of Jurassic are river-meandering river delta deposits from below to above. And Fuxian Group and YanlO formation are the braid river sedimentary reservoir, Yan9formation and other formations which is above Yan9gradually become meandering river delta reservoir.
3. The geological condition and factors of oil reservoir formation in research area are source rocks, hydrocarbon migration, reservoir seal assemblage and reservoir formation. The types of reservoir in area are devided into lithologic reservoir which is more in research area and complex reservoir which is distributed in north of area.
4. According to Structure, sedimentary facies, reservoir characteristics and so on in the study area, we summarized that there are four oil reservoir formation models, mound model, uplift model, slope model and upland model.
引文
[1]Bathurst R.G.C.Carbonate sediments and their diagenesis[J].Developments in sediment-tology,Amsterdam:Elsevier,1971:620
[2]Cross T. A., Lessenger M. A.The scientific basis for stratigraphic inversion[J].Geological Society of America Bulletin,1993:7-10
[3]Cross T. A.. High-resolution stratigraphic correlation from the Perspeetive of base level cycles and sediment accommodation[J].In:Proeeedings of Northwestern European Sequence Stratigraphy Congress.1994:205-123
[4]Curtis C.D.. Link between aluminum mobility and destruction of secondary porosity[J]. AAPG Bulletin,1983,67:380-393
[5]Fyfe W.S.. Towards the wide use of planet earth:the challenge to world society[J]. J Geol Soc Japan, 1993,9(1):173-190
[6]Galloway W. E., Hobday D.K. Terrigenous Clastic Depositional Systems:applications to fossil fuel and groundwater resources[M]. Springer Verlag,1996:5-10
[7]Jervey M. T.. Quantitative geological modeling of siliciclasticrock sequences and their seismic expression[A]. Wilgus CK. Sea-Level Changes:an Integrated Approach[C]. Soc E-con Palaeontol Mineral Spec Publ,1988,42:47-69
[8]Miall A.D.. Architectural-elementanalysis:A newmethod of facies analysis applied to fluvial deposits[J]. Earth Science Reviews,1985,(22):261-308
[9]Miall A.D.. Reconstructing the architecture and sequence stratigraphy of the preserved fluvial record as a tool for reservoir development: A reality check [J]. AAPG Bulletin,2006,90(7):989-1002
[10]Mitehum R.M.. Seismie stratigraphy and gobal changes of seal evel,Part2:the depositional sequence as abasic unit for stratigriaphy analysis[M]. AAPG,Memoir 26,1977
[11]Oliver J. Solid earth science during the 21th century[J].EOS,1991,72(11):172-190
[12]Pettijohn F.J., Potter P.E, Siever R. Sand and sandstone[M]. Berlin: Springer-Verlag,1973
[13]Posamenter H. W., JerveyM. T.,Vail P. R. Eustatic Controls on ClasticDeposition II:conceptual framework[J]. SEPM SepicalPublication,1988,42:109-125
[14]Posamentier H.W., Weimer P. Siliciclastic sequence stratigraphy and petroleum geology:where to from here [J]. AAPG Bulletin,1993,77 (5):731-742
[15]Sloss L.L.. Paleozoic stratigraphy in the Montana area[J]. AAPG Bull,1950,34:423-451
[16]Sloss L.L.. Sequences in the crationic interior of North America[J]. Geologica Society of Ameirica Bulletin,1963,46:1050-1057
[17]Schmidt V., McDonald D.A., Platt R L. Pore geometry and reservoiraspects of secondary porosity in sandstones [J]. Bulletin of Canada Petroleum Geology,1977,25:271-290
[18]Taylor J.C.M.. Sandstone as reservoir rocks[J].Developments in Petroleum Geology,1977:147-196
[19]Tillman R.W.. Reservoir sedimentology[J]. SEPMSpec.Pub,1987,2-23
[20]Vail P.R. Seismic stratigraphy and global changes of sea level In: Seismic stratigraphy application to hydrocarbon exploration[J].Pettol Geol 1987,26(3):99-116
[21]Van Wagoner, Mitchum J.C., Campion R.M., et al. Siliciclastic sequence stratigraphy in welllogs, cores and outcrops[J]. AAPG, Methods in Exploration,1990,755
[22]Wheeler R. J., Baselevel. lithosphere surface and time-stratigraphy. Bull. Geol. Soc. America,1964, 75:599-610
[23]Wolf K.H.,Chilingar G.V.,eds. Diagenesis Ⅳ [M]. Amsterdam:Elsevier,1994:519
[24]Zenger D.H.,Dunham J.B.,Ethington R.L.. Concep ts and models of dolomitization[J].SEPM Special Publication,1980,28:426
[25]蔡希源,李思田.陆相盆地高精度层序地层学[M].北京：地质出版社,2003：68-75
[26]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
[27]戴启德,纪有亮.油气储层地质学[M].北京：石油大学出版社,1996：120-145
[28]邓宏文,王红亮,李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2)：90-95
[29]邓宏文,王红亮,王敦则.吉地貌对陆相裂谷盆地层序充填特征的控制一以渤中凹陷西斜坡区下第三系为例.石油与天然气地质,2001,22(4)：294-296
[30]邓宏文,王洪亮,祝永军.高分辨率层序地层学一原理及应用[M].北京：地质出版社,2002：3-13
[31]邓宏文.沉积物体积分配原理一高分辨率层序地层学的理论基础[J].地学前缘,2000,7(4)：305-310
[32]邓宏文.美国层序地层研究中的新学派一高分辨率层序地层学[J].石油与天然气地质,1995,16(2)：89-97
[33]樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2)：12-17
[34]顾家裕,范土芝.层序地层学回顾与展望[J].海相油气地质,2001,6(4)：15-17
[35]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)：137-140
[36]顾家裕.陆相盆地层序地层学格架概念及模式[J]。石油勘探与开发,1995,22(4)：25-30
[37]郭正权,张立荣,楚美娟,等。鄂尔多斯盆地南部前侏罗纪古地貌对延安组下部油藏的控制作用[J].古地理学报,2008(10)：63-71
[38]何起祥.沉积地球科学的历史回顾与展望[J].沉积学报,2003,21(1)：10-18
[39]侯洪斌,牟泽辉,朱宏权,等.鄂尔多斯盆地北部上古生界天然气成藏条件与勘探方向[M].北京：石油工业出版社,2004：1
[40]侯明才,陈洪德,田景春.层序地层学的研究进展[J].矿物岩石,2001,21(3)：128-134
[41]黄子齐.层序地层学研究现状和发展方向[J].勘探家,1998,3(3)：28-30
[42]姜正龙,邓宏文,林会喜,等.古地貌恢复方法及应用一以济阳坳陷桩西地区沙二段为例.现代地质,2009：23(5)：865-871
[43]李凤杰,王多云.鄂尔多斯盆地西峰油田延长组高分辨率层序地层学研究[J].天然气地球科学,2006,17(3)：339-343
[44]李书舜.层序地层学的发展与应用[J].地球科学进展,1992,7(2)：24-29
[45]李树同,张海峰,王多云,等.聚油古地貌成因类型及其有利成藏条件分析一以鄂尔多斯盆地上里 塬地区前侏罗纪古地貌为例[J].沉积学报,2011,29(5)：962-967
[46]廖远涛.层序地层学的研究现状及发展方向[J].重庆石油高等专科学校学报,2002,4(2)：9-10
[47]刘宝瑁,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)：1-8
[48]刘博.鄂尔多斯盆地陇东地区长8段储层物性及演化研究[D].西安：西北大学,2008.赵俊兴.鄂尔多斯盆地侏罗纪早中期甘陕古河的演化变迁[J].石油与天然气地质,2006,2
[49]刘春慧,金振奎,张鑫,等.高分辨率层序地层学理论在准噶尔盆地勘探中的应用[J].沉积学报,2008,26(2)：248-254
[50]刘林玉,曲志浩,孙卫,等.新疆鄯善油田碎屑岩中的粘土矿物特征[J].西北大学学报(自然科学版)1998,28(5)：443-446
[51]刘泽容,信荃麟,王伟锋,等.油藏描述原理与方法技术[M].北京：石油工业出版社,1993
[52]柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3)：87-95
[53]孟万斌.从层序地层学到高分辨率层序地层学[J].成都理工学院学报,2000,29(4)：380-385
[54]苗庆梅.安塞地区三叠系延长组层序地层学研究[D].西安：西安石油大学,2007
[55]裘亦楠.中国陆相碎屑岩储层沉积学的进展[J].沉积学报,1992,10(3)：16-20
[56]裘怿楠,薛叔浩.中国陆相油气储集层[M].北京：石油工业出版社,1997：15-17
[57]裘怿楠.油田地质研究的几个基本问题[C].裘怿楠石油开发地质文集.北京：石油工业出版社,1997
[58]任纪舜.中国油气勘探和开发战略[c].21世纪中国石油天然气资源战略研讨会论文.北京：石油工业出版社,2000
[59]邵世忠.鄂尔多斯盆地榆林一延安地区侏罗系沉积体系与主要砂体研究[D].北京：中国地质大学,2005
[60]宋凯,吕剑文,凌升阶,等.鄂尔多斯盆地定边一吴旗地区前侏罗纪古地貌与油藏.古地理学报,2003,5(4)：497-504
[61]宋凯,吕剑文,凌升阶,等.鄂尔多斯盆地定边一吴旗地区前侏罗纪古地貌与油藏[J].古地理学报,2003,5(4)：497-505
[62]孙枢.中国沉积学的今后发展：若干思考与建议[J].地学前缘,200512(2)：3·10
[63]田纳新,徐国强.塔中地区早海西期风化壳古岩溶控制因素分析[J].江汉石油学院学报,2004,26(2)：61-63
[64]田在艺,张庆春中国含油气沉积盆地论[M].北京：石油工业出版社,1996
[65]汪泽成,刘焕杰,张林,等.鄂尔多斯含油气区构造层序地层研究[J].中国矿业大学学报,2000,29(4)：433-436
[66]吴丽艳,樊太亮,张淑品,等.济阳蚴陷上第三系层序地层及沉积体系研究.石油天然气学报(江汉石油学院学报),200527(4)：413-415
[67]吴丽艳,陈春强,江春明,等.浅谈我国油气勘探中的古地貌恢复技术[J].石油天然气学报(江汉石 油学院学报),2005,27(4)：559-561
[68]吴贤顺,樊太亮.从古地貌谈层序格架中储层的发育规律[J].地球学报,2002,23(3)：259-262
[69]武文慧.鄂尔多斯盆地上古生界储层砂岩特征及成岩作用研究[D].成都：成都理工大学,2011
[70]夏锦芬,胡明毅.高分辨率层序地层学的研究现状及发展趋势[J].内蒙古石油化工,2008,第3期：26-28
[71]谢又予.沉积地貌分析[M]北京：海洋出版社,2000：11-18
[72]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)：1-3
[73]徐伟.东营凹陷西部地区滨浅湖滩坝砂岩储层预测及描述技术研究[D].山东：中国海洋大学,2009
[74]许仕策,杨少坤,黄丽芬.层序地层学在地层对比中的应用[J].地学前缘,1995,2(3)115-118
[75]薛良清.层序地层学研究现状、方法与前景[J].石油勘探与开发,1995,22(5)：1-8
[76]杨县超.鄂尔多斯盆地吴定地区晚三叠世早期的沉积环境与古地理演化[D].西安：西北大学,2009
[77]杨小萍,刘桂侠,马文杰.层序地层学研究现状及发展趋势[J].西北地质,2001,43(2)：16-20
[78]于兴河,李胜利.碎屑岩系油气储层沉积学的发展历程与热点问题思考[J].沉积学报,2009,27(5)：880-89 1
[79]于兴河,李胜利.碎屑岩系油气储层沉积学的发展历程与热点问题思考[J].沉积学报,2009,27(5)：880-891
[80]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004
[81]张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学咖.北京：科学出版社,2001
[82]张振晗,辛初波.沉积学研究的新进展与发展趋势[J].山西建筑,2006,32(6)：91
[83]赵重远.鄂尔多斯盆地的演化历史、形成机制和含油气有利地区[A].西安：西北大学出版社,1990
[84]赵国连.层序地层学的研究现状[J].沉积与特提斯地质,2000,20(3)：97-103
[85]赵俊兴,陈洪德,时志强.古地貌恢复技术方法及其研究意义一以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例[J].成都理工学院学报,2001,28(3)：260-265
[86]赵俊兴,陈洪德,时志强.古地貌恢复技术方法及其研究意义一以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例[J].成都理工学院学报,2001,3(28)：260-266
[87]赵俊兴,陈洪德,向芳.高分辨率层序地层学方法在沉积前古地貌恢复中的应用.成都理工大学学报(自然科学版),2003,30(1)：76-81
[88]郑荣才,彭军,吴朝容.陆相盆地基准面旋回的级次划分和研究意义[J].沉积学报,2001,19(2)：302-308
[89]周川,王英民,黄志超,等.澳大利亚北波拿巴盆地北部侏罗纪古地貌特征与演化[J].海洋地质动态,2008,25(10)：14-19
[90]邹德江,于兴河,李胜利,等.古地貌对储层沉积体系控制作用分析一以冀中油田马西地区为例[J].石油天然气学报.2008,30(2)：175-177
[91]翟光叽杨俊杰中国石油地质志：卷十二[M].北京：石油工业出版社,1992.3
[92]赵杏嫒.粘土矿物在油气初次运移中作用的探讨[J].沉积学报.1990,8(27)：67-73
[93]焦养泉,等.曲流河与湖泊三角洲沉积体系及典型骨架砂体内部构成分析[M].武汉：中国地质大学出版社,1995
[94]杨小萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发.2001,28(4)：38-40
[95]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京：石油工业出版社,2002,104-105
[96]钟广法,杜社卿,侯方浩.泌阳凹陷核三下亚段砂岩成岩作用及初级性[J]。矿物岩石,1996,16(2)：40-46
[2]Cross T. A., Lessenger M. A.The scientific basis for stratigraphic inversion[J].Geological Society of America Bulletin,1993:7-10
[3]Cross T. A.. High-resolution stratigraphic correlation from the Perspeetive of base level cycles and sediment accommodation[J].In:Proeeedings of Northwestern European Sequence Stratigraphy Congress.1994:205-123
[4]Curtis C.D.. Link between aluminum mobility and destruction of secondary porosity[J]. AAPG Bulletin,1983,67:380-393
[5]Fyfe W.S.. Towards the wide use of planet earth:the challenge to world society[J]. J Geol Soc Japan, 1993,9(1):173-190
[6]Galloway W. E., Hobday D.K. Terrigenous Clastic Depositional Systems:applications to fossil fuel and groundwater resources[M]. Springer Verlag,1996:5-10
[7]Jervey M. T.. Quantitative geological modeling of siliciclasticrock sequences and their seismic expression[A]. Wilgus CK. Sea-Level Changes:an Integrated Approach[C]. Soc E-con Palaeontol Mineral Spec Publ,1988,42:47-69
[8]Miall A.D.. Architectural-elementanalysis:A newmethod of facies analysis applied to fluvial deposits[J]. Earth Science Reviews,1985,(22):261-308
[9]Miall A.D.. Reconstructing the architecture and sequence stratigraphy of the preserved fluvial record as a tool for reservoir development: A reality check [J]. AAPG Bulletin,2006,90(7):989-1002
[10]Mitehum R.M.. Seismie stratigraphy and gobal changes of seal evel,Part2:the depositional sequence as abasic unit for stratigriaphy analysis[M]. AAPG,Memoir 26,1977
[11]Oliver J. Solid earth science during the 21th century[J].EOS,1991,72(11):172-190
[12]Pettijohn F.J., Potter P.E, Siever R. Sand and sandstone[M]. Berlin: Springer-Verlag,1973
[13]Posamenter H. W., JerveyM. T.,Vail P. R. Eustatic Controls on ClasticDeposition II:conceptual framework[J]. SEPM SepicalPublication,1988,42:109-125
[14]Posamentier H.W., Weimer P. Siliciclastic sequence stratigraphy and petroleum geology:where to from here [J]. AAPG Bulletin,1993,77 (5):731-742
[15]Sloss L.L.. Paleozoic stratigraphy in the Montana area[J]. AAPG Bull,1950,34:423-451
[16]Sloss L.L.. Sequences in the crationic interior of North America[J]. Geologica Society of Ameirica Bulletin,1963,46:1050-1057
[17]Schmidt V., McDonald D.A., Platt R L. Pore geometry and reservoiraspects of secondary porosity in sandstones [J]. Bulletin of Canada Petroleum Geology,1977,25:271-290
[18]Taylor J.C.M.. Sandstone as reservoir rocks[J].Developments in Petroleum Geology,1977:147-196
[19]Tillman R.W.. Reservoir sedimentology[J]. SEPMSpec.Pub,1987,2-23
[20]Vail P.R. Seismic stratigraphy and global changes of sea level In: Seismic stratigraphy application to hydrocarbon exploration[J].Pettol Geol 1987,26(3):99-116
[21]Van Wagoner, Mitchum J.C., Campion R.M., et al. Siliciclastic sequence stratigraphy in welllogs, cores and outcrops[J]. AAPG, Methods in Exploration,1990,755
[22]Wheeler R. J., Baselevel. lithosphere surface and time-stratigraphy. Bull. Geol. Soc. America,1964, 75:599-610
[23]Wolf K.H.,Chilingar G.V.,eds. Diagenesis Ⅳ [M]. Amsterdam:Elsevier,1994:519
[24]Zenger D.H.,Dunham J.B.,Ethington R.L.. Concep ts and models of dolomitization[J].SEPM Special Publication,1980,28:426
[25]蔡希源,李思田.陆相盆地高精度层序地层学[M].北京：地质出版社,2003：68-75
[26]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
[27]戴启德,纪有亮.油气储层地质学[M].北京：石油大学出版社,1996：120-145
[28]邓宏文,王红亮,李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2)：90-95
[29]邓宏文,王红亮,王敦则.吉地貌对陆相裂谷盆地层序充填特征的控制一以渤中凹陷西斜坡区下第三系为例.石油与天然气地质,2001,22(4)：294-296
[30]邓宏文,王洪亮,祝永军.高分辨率层序地层学一原理及应用[M].北京：地质出版社,2002：3-13
[31]邓宏文.沉积物体积分配原理一高分辨率层序地层学的理论基础[J].地学前缘,2000,7(4)：305-310
[32]邓宏文.美国层序地层研究中的新学派一高分辨率层序地层学[J].石油与天然气地质,1995,16(2)：89-97
[33]樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2)：12-17
[34]顾家裕,范土芝.层序地层学回顾与展望[J].海相油气地质,2001,6(4)：15-17
[35]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)：137-140
[36]顾家裕.陆相盆地层序地层学格架概念及模式[J]。石油勘探与开发,1995,22(4)：25-30
[37]郭正权,张立荣,楚美娟,等。鄂尔多斯盆地南部前侏罗纪古地貌对延安组下部油藏的控制作用[J].古地理学报,2008(10)：63-71
[38]何起祥.沉积地球科学的历史回顾与展望[J].沉积学报,2003,21(1)：10-18
[39]侯洪斌,牟泽辉,朱宏权,等.鄂尔多斯盆地北部上古生界天然气成藏条件与勘探方向[M].北京：石油工业出版社,2004：1
[40]侯明才,陈洪德,田景春.层序地层学的研究进展[J].矿物岩石,2001,21(3)：128-134
[41]黄子齐.层序地层学研究现状和发展方向[J].勘探家,1998,3(3)：28-30
[42]姜正龙,邓宏文,林会喜,等.古地貌恢复方法及应用一以济阳坳陷桩西地区沙二段为例.现代地质,2009：23(5)：865-871
[43]李凤杰,王多云.鄂尔多斯盆地西峰油田延长组高分辨率层序地层学研究[J].天然气地球科学,2006,17(3)：339-343
[44]李书舜.层序地层学的发展与应用[J].地球科学进展,1992,7(2)：24-29
[45]李树同,张海峰,王多云,等.聚油古地貌成因类型及其有利成藏条件分析一以鄂尔多斯盆地上里 塬地区前侏罗纪古地貌为例[J].沉积学报,2011,29(5)：962-967
[46]廖远涛.层序地层学的研究现状及发展方向[J].重庆石油高等专科学校学报,2002,4(2)：9-10
[47]刘宝瑁,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)：1-8
[48]刘博.鄂尔多斯盆地陇东地区长8段储层物性及演化研究[D].西安：西北大学,2008.赵俊兴.鄂尔多斯盆地侏罗纪早中期甘陕古河的演化变迁[J].石油与天然气地质,2006,2
[49]刘春慧,金振奎,张鑫,等.高分辨率层序地层学理论在准噶尔盆地勘探中的应用[J].沉积学报,2008,26(2)：248-254
[50]刘林玉,曲志浩,孙卫,等.新疆鄯善油田碎屑岩中的粘土矿物特征[J].西北大学学报(自然科学版)1998,28(5)：443-446
[51]刘泽容,信荃麟,王伟锋,等.油藏描述原理与方法技术[M].北京：石油工业出版社,1993
[52]柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3)：87-95
[53]孟万斌.从层序地层学到高分辨率层序地层学[J].成都理工学院学报,2000,29(4)：380-385
[54]苗庆梅.安塞地区三叠系延长组层序地层学研究[D].西安：西安石油大学,2007
[55]裘亦楠.中国陆相碎屑岩储层沉积学的进展[J].沉积学报,1992,10(3)：16-20
[56]裘怿楠,薛叔浩.中国陆相油气储集层[M].北京：石油工业出版社,1997：15-17
[57]裘怿楠.油田地质研究的几个基本问题[C].裘怿楠石油开发地质文集.北京：石油工业出版社,1997
[58]任纪舜.中国油气勘探和开发战略[c].21世纪中国石油天然气资源战略研讨会论文.北京：石油工业出版社,2000
[59]邵世忠.鄂尔多斯盆地榆林一延安地区侏罗系沉积体系与主要砂体研究[D].北京：中国地质大学,2005
[60]宋凯,吕剑文,凌升阶,等.鄂尔多斯盆地定边一吴旗地区前侏罗纪古地貌与油藏.古地理学报,2003,5(4)：497-504
[61]宋凯,吕剑文,凌升阶,等.鄂尔多斯盆地定边一吴旗地区前侏罗纪古地貌与油藏[J].古地理学报,2003,5(4)：497-505
[62]孙枢.中国沉积学的今后发展：若干思考与建议[J].地学前缘,200512(2)：3·10
[63]田纳新,徐国强.塔中地区早海西期风化壳古岩溶控制因素分析[J].江汉石油学院学报,2004,26(2)：61-63
[64]田在艺,张庆春中国含油气沉积盆地论[M].北京：石油工业出版社,1996
[65]汪泽成,刘焕杰,张林,等.鄂尔多斯含油气区构造层序地层研究[J].中国矿业大学学报,2000,29(4)：433-436
[66]吴丽艳,樊太亮,张淑品,等.济阳蚴陷上第三系层序地层及沉积体系研究.石油天然气学报(江汉石油学院学报),200527(4)：413-415
[67]吴丽艳,陈春强,江春明,等.浅谈我国油气勘探中的古地貌恢复技术[J].石油天然气学报(江汉石 油学院学报),2005,27(4)：559-561
[68]吴贤顺,樊太亮.从古地貌谈层序格架中储层的发育规律[J].地球学报,2002,23(3)：259-262
[69]武文慧.鄂尔多斯盆地上古生界储层砂岩特征及成岩作用研究[D].成都：成都理工大学,2011
[70]夏锦芬,胡明毅.高分辨率层序地层学的研究现状及发展趋势[J].内蒙古石油化工,2008,第3期：26-28
[71]谢又予.沉积地貌分析[M]北京：海洋出版社,2000：11-18
[72]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)：1-3
[73]徐伟.东营凹陷西部地区滨浅湖滩坝砂岩储层预测及描述技术研究[D].山东：中国海洋大学,2009
[74]许仕策,杨少坤,黄丽芬.层序地层学在地层对比中的应用[J].地学前缘,1995,2(3)115-118
[75]薛良清.层序地层学研究现状、方法与前景[J].石油勘探与开发,1995,22(5)：1-8
[76]杨县超.鄂尔多斯盆地吴定地区晚三叠世早期的沉积环境与古地理演化[D].西安：西北大学,2009
[77]杨小萍,刘桂侠,马文杰.层序地层学研究现状及发展趋势[J].西北地质,2001,43(2)：16-20
[78]于兴河,李胜利.碎屑岩系油气储层沉积学的发展历程与热点问题思考[J].沉积学报,2009,27(5)：880-89 1
[79]于兴河,李胜利.碎屑岩系油气储层沉积学的发展历程与热点问题思考[J].沉积学报,2009,27(5)：880-891
[80]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004
[81]张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学咖.北京：科学出版社,2001
[82]张振晗,辛初波.沉积学研究的新进展与发展趋势[J].山西建筑,2006,32(6)：91
[83]赵重远.鄂尔多斯盆地的演化历史、形成机制和含油气有利地区[A].西安：西北大学出版社,1990
[84]赵国连.层序地层学的研究现状[J].沉积与特提斯地质,2000,20(3)：97-103
[85]赵俊兴,陈洪德,时志强.古地貌恢复技术方法及其研究意义一以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例[J].成都理工学院学报,2001,28(3)：260-265
[86]赵俊兴,陈洪德,时志强.古地貌恢复技术方法及其研究意义一以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例[J].成都理工学院学报,2001,3(28)：260-266
[87]赵俊兴,陈洪德,向芳.高分辨率层序地层学方法在沉积前古地貌恢复中的应用.成都理工大学学报(自然科学版),2003,30(1)：76-81
[88]郑荣才,彭军,吴朝容.陆相盆地基准面旋回的级次划分和研究意义[J].沉积学报,2001,19(2)：302-308
[89]周川,王英民,黄志超,等.澳大利亚北波拿巴盆地北部侏罗纪古地貌特征与演化[J].海洋地质动态,2008,25(10)：14-19
[90]邹德江,于兴河,李胜利,等.古地貌对储层沉积体系控制作用分析一以冀中油田马西地区为例[J].石油天然气学报.2008,30(2)：175-177
[91]翟光叽杨俊杰中国石油地质志：卷十二[M].北京：石油工业出版社,1992.3
[92]赵杏嫒.粘土矿物在油气初次运移中作用的探讨[J].沉积学报.1990,8(27)：67-73
[93]焦养泉,等.曲流河与湖泊三角洲沉积体系及典型骨架砂体内部构成分析[M].武汉：中国地质大学出版社,1995
[94]杨小萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发.2001,28(4)：38-40
[95]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京：石油工业出版社,2002,104-105
[96]钟广法,杜社卿,侯方浩.泌阳凹陷核三下亚段砂岩成岩作用及初级性[J]。矿物岩石,1996,16(2)：40-46