鄂尔多斯盆地中西部延长组下组合油藏控制因素研究
|
摘要
近年来,鄂尔多斯盆地中西部延长组下组合油层组勘探取得了重大突破,显示出较好的勘探前景。许多学者对该区延长组下组合油层进行了构造单元、地层格架、沉积展布等方面的研究,但对该区延长组下组合油藏的分布规律以及成藏控制因素等方面的问题认识还不够明晰。这些问题的解决不仅能够进一步完善对鄂尔多斯盆地中生界湖盆油气成藏规律的认识,而且对于鄂尔多斯盆地中西部下组合油藏的勘探也具有指导意义。
本次研究充分利用最新的录井、测井、化验分析等资料,对鄂尔多斯盆地中西部延长组下组合油藏的主控因素进行了系统研究,从控制储层形成的沉积相、储层特征等静态要素和影响油藏形成的成岩作用过程、油气运聚成藏过程、圈闭形成过程等动态过程两个方面进行综合研究。
在静态要素研究方面,利用层序地层学方法对鄂尔多斯盆地延长组地层沉积旋回进行划分,确立了该区延长组下组合地层三维地质模型。通过研究区下组合储层砂岩的轻重矿物组合特征、微量元素配分模式、成像测井古水流分析等资料对研究区物源进行分析,认为该区受西北、东北两个方向的物源控制,其主要受西北物源的控制。本文结合鄂尔多斯盆地中生界湖盆演化过程和沉积相标志综合研究,认为晚三叠世早期湖盆基底处于沉降阶段,研究区距离物源较近,长9期发育辫状河三角洲沉积体系,辫状河三角洲平原为主要的沉积亚相,长8期发育浅水三角洲沉积体系,浅水三角洲平原和浅水三角洲前缘沉积为主要的沉积亚相。本文在对铸体薄片、扫描电镜等相关分析化验资料统计的基础上,分析得出延长组下组合储层砂体主要为岩屑长石砂岩、长石岩屑砂岩,长9储层砂岩粒度较粗,粒间孔发育,平均孔隙度11.27%,平均渗透率3.80mmD。长8储层砂岩以细砂岩为主,粒间孔、长石溶孔发育,平均孔隙度8.5%,平均渗透率0.61mD。
在动态过程研究方面,盆地中西部延长组下组合油藏储层砂岩的成岩作用过程的研究结果表明延长组下组合油层储层砂岩经历了压实作用、胶结作用、交代作用和溶蚀作用等成岩作用,储层砂岩已进入晚成岩A期。利用单因素分析多因素综合的方法进行成岩相分析,将研究区延长组下组合油层成岩相划分为长石溶蚀成岩相、绿泥石膜-粒间孔成岩相、碳酸盐胶结成岩相、压实成岩相等四种类型；长石溶蚀成岩相和绿泥石膜-粒间孔成岩相为建设性成岩相,有利于储集空间的形成。根据包裹体镜下观察和均一温度频率分布特征,结合盆地中生界构造演化史的综合分析,发现盆地中西部延长期发育两期包裹体,分别代表了晚侏罗世-早白垩世、白垩世末的两次构造抬升过程中的油气成藏事件。在研究区延长组下组合地层砂岩裂缝的发育特征和平面分布规律研究的基础上,本文认为研究区主要发育E-W、NE-SW向裂缝,在天环坳陷轴部裂缝走向为NE-SW:天环坳陷东西两侧和邻近伊陕斜坡区为E-W向。受NEE-SWW向现今应力场的影响,NE-SW向裂缝为主要的渗流方向。鄂尔多斯盆地延长组长7烃源岩的生烃增压作用产生的过剩压力是石油横向、纵向运移的动力,过剩压力从高值区向低值区聚集,过剩压力低值区是油气聚集的场所。与油藏伴生的地层水水型、矿化度、物化参数的平面分布规律反映了油藏保存条件,研究区延长组下组合油藏伴生的地层水平面分布受燕山期构造运动的影响较大,不同区域地层水的化学性质明显不同,天环坳陷东侧靠近伊陕斜坡、三角洲河道砂体发育区地层水矿化度高、钠氯系数、脱硫系数低,油藏保存条件好；天环坳陷轴部、靠近西缘冲断带断层、裂缝发育区,由于受后期构造运动改造封闭性变差,地层水矿化度低,钠氯系数、脱硫系数都偏高,油藏保存条件相对较差。
本文在对鄂尔多斯盆地中西部延长组下组合油藏形成的静态要素和动态过程系统研究的基础上,根据油藏的分布规律和主控因素,在研究区延长组长8油层优选了四个有利目标区。
In recent years, the lower Yanchang formation exploration in the middle of west Ordos basin is making a breakthrough and displaying preferable prospect. Many scholars studied the lower formation of Yanchang formation reservoir of the area tectonic units, stratigraphic framework, sand spread characteristic, but the less study of the distributive regularity and control factors of the lower formation of Yanchang formation reservoir and which restricts the exploration process. The results of these programs improve the understanding of Ordos Basin in Mesozoic accumulation theories, but also direct the exploration of the area.
Utilizing the latest drilling data, the research analyses the main controlling factors the lower formation of Yanchang formation reservoir in the middle of west Ordos basin. The comprehensive research includes two aspects which were static elements controlling reservoir formed and dynamic elements which destructed and transformed reservoir. Static elements are formed by deposition phase, characteristics and source rock conditions. These dynamic elements are consist of diagenesis, hydrocarbon migration, accumulation reservoir, trap formation, and the reservoir destruction and transformation.
Static factor analysis, the sequence stratigraphy method is used to divide Yanchang formation reservoir into sedimentary cycles, establish the lower Yanchang formation reservoir3D geological model. Used light and heavy mineral assemblages, trace elements, imaging logging paleocurrent direction to analysis provenance direction. The conclusion is that the provenance direction of in the middle of west Ordos basin subject to the control of the direction of the northwest and northeast provenance, and the northwest provenance is the mainly control. Combination the basin evolution and sedimentary facies characteristic comprehensive analysis that early Late Triassic lake basin base was in descending stage. The middle of west Ordos basin is closer to provenance, Chang9was developed braided river delta sedimentary system, and Chang8was developed shallow water delta. Analysis of the statistics shows that the lower Yanchang formation mainly sandstone is Lithic arkose, feldspathic lithic sandstone. The Grain Size of Chang9sandstone is coarse, the average porosity of the sandstone is11.27%, and the average permeability is3.8OmD. Chang8sandstone is fine sandstone, The dominating pore type of Chang8reservoirs is intergranular pore and feldspar dissolved pore, the average porosity is8.5%, and the average permeability is0.61mD.
Dynamic factor analysis, the lower Yanchang formation sandstones are in the A period of the late diagenetic stage. This set of sandstone experienced compaction, cementation, metasomatism and dissolution diagenesis. Used the single factor analysis and multifactor comprehensive method to analysis diagenetic facies zone of the area. The result is that the feldspar dissolution diagenetic facies, chlorite intergranular pore diagenetic facies is a constructive diagenetic facies. Two different phases of hydrocarbon inclusions have been identified according to the microscopic characteristics of sandstone type U-deposit and homogeneous temperature distribution characteristics and referring to the tectonic evolution history of the Ordos Basin. It represents Late Jurassic and end of the Cretaceous tectonic uplift process hydrocarbon accumulation event. Based on the characteristics of tectonics evolution, the well drilling, log information and microscopic, high resolution boreholemicro resistivity image logs were used to investigate the flat distribution regulation and genesis of the fractures.The research shows that the E-W and NW-SE regional fractures are developping well. It is found that E-W fractures developed well where closed to Yishan Slope, and NW-SE fractures developed well neared Tianhuan depression or faults.The directions of the present tectonic stress fields in the basin were NEE-SWW which controlled the fractures expanded and permeability. Hydrocarbon source rocks of Chang7increased pressure from hydrocarbon generation expanding which was the dynamic force for the oil transverse and vertical migration.The oil migrated from higher pressure area to lower pressure area and accumulated in lower pressure area. Chemical characteristics of formation water were used to study the condition about the oil and gas migration and preservation of the lower Yanchang formation in the middle of west Ordos Basin. It is found that the formation water type is CaCb, the formation water salinity is high, ratio of Na+and Cl-and coefficient of desulphuration is low where develop shallow-water deltas in sandstones and closed to Yishan Slope. The formation water salinity is low, ratio of Na+and Cl-and coefficient of desulphuration is high where neared Tianhuan depression or faults. Conclusion The formation water distribution was influenced by Yanshan movements, closed geological environment is good for oil to be preserved where the formation water salinity is high, ratio of Na+and Cl-and coefficient of desulphuration is low.
Analysing those static elements and dynamic elements of the controlling factors of the lower assemblage of Yanchang formation reservoir, four targets were selected in Chang8reservoir to provide the orientations of exploration.
本次研究充分利用最新的录井、测井、化验分析等资料,对鄂尔多斯盆地中西部延长组下组合油藏的主控因素进行了系统研究,从控制储层形成的沉积相、储层特征等静态要素和影响油藏形成的成岩作用过程、油气运聚成藏过程、圈闭形成过程等动态过程两个方面进行综合研究。
在静态要素研究方面,利用层序地层学方法对鄂尔多斯盆地延长组地层沉积旋回进行划分,确立了该区延长组下组合地层三维地质模型。通过研究区下组合储层砂岩的轻重矿物组合特征、微量元素配分模式、成像测井古水流分析等资料对研究区物源进行分析,认为该区受西北、东北两个方向的物源控制,其主要受西北物源的控制。本文结合鄂尔多斯盆地中生界湖盆演化过程和沉积相标志综合研究,认为晚三叠世早期湖盆基底处于沉降阶段,研究区距离物源较近,长9期发育辫状河三角洲沉积体系,辫状河三角洲平原为主要的沉积亚相,长8期发育浅水三角洲沉积体系,浅水三角洲平原和浅水三角洲前缘沉积为主要的沉积亚相。本文在对铸体薄片、扫描电镜等相关分析化验资料统计的基础上,分析得出延长组下组合储层砂体主要为岩屑长石砂岩、长石岩屑砂岩,长9储层砂岩粒度较粗,粒间孔发育,平均孔隙度11.27%,平均渗透率3.80mmD。长8储层砂岩以细砂岩为主,粒间孔、长石溶孔发育,平均孔隙度8.5%,平均渗透率0.61mD。
在动态过程研究方面,盆地中西部延长组下组合油藏储层砂岩的成岩作用过程的研究结果表明延长组下组合油层储层砂岩经历了压实作用、胶结作用、交代作用和溶蚀作用等成岩作用,储层砂岩已进入晚成岩A期。利用单因素分析多因素综合的方法进行成岩相分析,将研究区延长组下组合油层成岩相划分为长石溶蚀成岩相、绿泥石膜-粒间孔成岩相、碳酸盐胶结成岩相、压实成岩相等四种类型；长石溶蚀成岩相和绿泥石膜-粒间孔成岩相为建设性成岩相,有利于储集空间的形成。根据包裹体镜下观察和均一温度频率分布特征,结合盆地中生界构造演化史的综合分析,发现盆地中西部延长期发育两期包裹体,分别代表了晚侏罗世-早白垩世、白垩世末的两次构造抬升过程中的油气成藏事件。在研究区延长组下组合地层砂岩裂缝的发育特征和平面分布规律研究的基础上,本文认为研究区主要发育E-W、NE-SW向裂缝,在天环坳陷轴部裂缝走向为NE-SW:天环坳陷东西两侧和邻近伊陕斜坡区为E-W向。受NEE-SWW向现今应力场的影响,NE-SW向裂缝为主要的渗流方向。鄂尔多斯盆地延长组长7烃源岩的生烃增压作用产生的过剩压力是石油横向、纵向运移的动力,过剩压力从高值区向低值区聚集,过剩压力低值区是油气聚集的场所。与油藏伴生的地层水水型、矿化度、物化参数的平面分布规律反映了油藏保存条件,研究区延长组下组合油藏伴生的地层水平面分布受燕山期构造运动的影响较大,不同区域地层水的化学性质明显不同,天环坳陷东侧靠近伊陕斜坡、三角洲河道砂体发育区地层水矿化度高、钠氯系数、脱硫系数低,油藏保存条件好；天环坳陷轴部、靠近西缘冲断带断层、裂缝发育区,由于受后期构造运动改造封闭性变差,地层水矿化度低,钠氯系数、脱硫系数都偏高,油藏保存条件相对较差。
本文在对鄂尔多斯盆地中西部延长组下组合油藏形成的静态要素和动态过程系统研究的基础上,根据油藏的分布规律和主控因素,在研究区延长组长8油层优选了四个有利目标区。
In recent years, the lower Yanchang formation exploration in the middle of west Ordos basin is making a breakthrough and displaying preferable prospect. Many scholars studied the lower formation of Yanchang formation reservoir of the area tectonic units, stratigraphic framework, sand spread characteristic, but the less study of the distributive regularity and control factors of the lower formation of Yanchang formation reservoir and which restricts the exploration process. The results of these programs improve the understanding of Ordos Basin in Mesozoic accumulation theories, but also direct the exploration of the area.
Utilizing the latest drilling data, the research analyses the main controlling factors the lower formation of Yanchang formation reservoir in the middle of west Ordos basin. The comprehensive research includes two aspects which were static elements controlling reservoir formed and dynamic elements which destructed and transformed reservoir. Static elements are formed by deposition phase, characteristics and source rock conditions. These dynamic elements are consist of diagenesis, hydrocarbon migration, accumulation reservoir, trap formation, and the reservoir destruction and transformation.
Static factor analysis, the sequence stratigraphy method is used to divide Yanchang formation reservoir into sedimentary cycles, establish the lower Yanchang formation reservoir3D geological model. Used light and heavy mineral assemblages, trace elements, imaging logging paleocurrent direction to analysis provenance direction. The conclusion is that the provenance direction of in the middle of west Ordos basin subject to the control of the direction of the northwest and northeast provenance, and the northwest provenance is the mainly control. Combination the basin evolution and sedimentary facies characteristic comprehensive analysis that early Late Triassic lake basin base was in descending stage. The middle of west Ordos basin is closer to provenance, Chang9was developed braided river delta sedimentary system, and Chang8was developed shallow water delta. Analysis of the statistics shows that the lower Yanchang formation mainly sandstone is Lithic arkose, feldspathic lithic sandstone. The Grain Size of Chang9sandstone is coarse, the average porosity of the sandstone is11.27%, and the average permeability is3.8OmD. Chang8sandstone is fine sandstone, The dominating pore type of Chang8reservoirs is intergranular pore and feldspar dissolved pore, the average porosity is8.5%, and the average permeability is0.61mD.
Dynamic factor analysis, the lower Yanchang formation sandstones are in the A period of the late diagenetic stage. This set of sandstone experienced compaction, cementation, metasomatism and dissolution diagenesis. Used the single factor analysis and multifactor comprehensive method to analysis diagenetic facies zone of the area. The result is that the feldspar dissolution diagenetic facies, chlorite intergranular pore diagenetic facies is a constructive diagenetic facies. Two different phases of hydrocarbon inclusions have been identified according to the microscopic characteristics of sandstone type U-deposit and homogeneous temperature distribution characteristics and referring to the tectonic evolution history of the Ordos Basin. It represents Late Jurassic and end of the Cretaceous tectonic uplift process hydrocarbon accumulation event. Based on the characteristics of tectonics evolution, the well drilling, log information and microscopic, high resolution boreholemicro resistivity image logs were used to investigate the flat distribution regulation and genesis of the fractures.The research shows that the E-W and NW-SE regional fractures are developping well. It is found that E-W fractures developed well where closed to Yishan Slope, and NW-SE fractures developed well neared Tianhuan depression or faults.The directions of the present tectonic stress fields in the basin were NEE-SWW which controlled the fractures expanded and permeability. Hydrocarbon source rocks of Chang7increased pressure from hydrocarbon generation expanding which was the dynamic force for the oil transverse and vertical migration.The oil migrated from higher pressure area to lower pressure area and accumulated in lower pressure area. Chemical characteristics of formation water were used to study the condition about the oil and gas migration and preservation of the lower Yanchang formation in the middle of west Ordos Basin. It is found that the formation water type is CaCb, the formation water salinity is high, ratio of Na+and Cl-and coefficient of desulphuration is low where develop shallow-water deltas in sandstones and closed to Yishan Slope. The formation water salinity is low, ratio of Na+and Cl-and coefficient of desulphuration is high where neared Tianhuan depression or faults. Conclusion The formation water distribution was influenced by Yanshan movements, closed geological environment is good for oil to be preserved where the formation water salinity is high, ratio of Na+and Cl-and coefficient of desulphuration is low.
Analysing those static elements and dynamic elements of the controlling factors of the lower assemblage of Yanchang formation reservoir, four targets were selected in Chang8reservoir to provide the orientations of exploration.
引文
[1]Alaa M,Salem S,Morad S,Luiz F,Mato,Al-Aasm I S. Diagenesis and reservoir-quality evolution of fluvial sandstones during progressive burial and uplift:evidence from the Upper Jurassic Boipeba Member,Reconcavo Basin, Northeastern Brazil[J]. AAPG Bulletin,2000,84(7):1015-1040
[2]Barker C E.A fluid inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer.Geology,1991,18:1003-1006.
[3]Barth T, Bjorlykke K. Organic acids from source rock maturation:generation potentials,transport mechanisms and relevance for mineral diagenesis[J].AppIied Geochemistry,1993,8:325-337.
[4]Bloch S, Franks S G. Preservation of shallow plagioclase dissolution porosity during burial:implications for porosity prediction and aluminium mass balance[J].AAPG Bulletin,1993,77:1488-1501.
[5]Brendow K. Global oil shale issues and perspectives[J].Oil Shale,2003,20(1):81-92.
[6]Carr A D. Suppression and retardation of vitrinite reflectance, Part 1. Formation and significance for hydrocarbon generation[J] Journal of Petroleum Geology,2000,23:313-343.
[7]Carr A D. Suppression and retardation of vitrinite reflectance, Part 2. Derivation and testing of a kinetic model for suppression [J]. Journal of Petroleum Geology,2000,23:475-496.
[8]Chad A,Underwood ML,Cooke JA,et al.Stratigraphic controls on vertical fracture patterns in Silarian dolomite, northeastern Wisconsin. AAPG Bulletin,2003,87(1):121-142.
[9]Cross TA and Lessenger MA.1996. Sediment volume partitioning:Rationale for stratigraphic model evaluation and high-resolution stratigraphic correlation. Accepted for Publication in Norwegian Petroleums-Forening Conference Volume July,1-24.
[10]Cross TA. Controls on coal distribution intransgressive 2 regressive cycle, Upper Cretaceous, Western Interior, USA [M] WilgausC K. Sea Level Change:An Integrated Approach. NewYork:SEPM SpecialPublication,1998:371-380.
[11]GALEAZZI J S. Structural and stratigraphic evolution of the western Malvinas Basin, Argentina[J]. AAPG Bul,1998,82(4):596-636.
[12]Ganil M R, Bhattacharya J P. Basic building blocks and process variability of a Cretaceous delta: Internal facies architecture reveals a more dynamic interaction of river, wave, and tidal processes than is indicated by external shape[J]. Journal of Sedimentary Research,2007,77(4):284-302.
[13]Guiton Martin LE, Sassi W, Leroy YM, et al. Mechanical constraints on the chronology of fracture activation in folded Devonian sandstone of the western Moroccan Anti-Atlas. Journal of Structural Geology,2003,25(8):1317-1330.
[14]Helgeson H C,Knox A M,Owens C E, et al.Petroleum,oil field brines.and authigenic mineral assemblages:are they in metastable equilibrium in hydrocarbon reservoirs [J].Geochimica et Cosmochimica Acta,1993,57:3295-3340.
[15]Hillier S.Pore-lining chlorites in siliciclastic reservoir sandstones:Electron microprobe, SEM and XRD data, and implications for their rigin [J].Clay Minerals,1994,29(4):665-679.
[16]Karlsen D A, Nedkvitne T, Larter S R and Bjurlykke K. Hydrocarbon composition of authigenic inclusions:Application to elucidation of petroleum reservoir filling history. Geochimica et Cosmochimica Acta,1993,57:3641-3659.
[17]Knutson C F. Developments in oil shale in 1985[J].AAPG,1990,69(10):882-889.
[18]Land L S. Na-Ca-Cl saline formation water, Frio Formation (Oligocene),South Texas,USA:products of diagenesis[J]. Geochimica et Cosmochimica Acta,1995,59(11):2163-2174.
[19]Marchant M E.Smaijjey P C,Haszeldine R S,et al.Note on the importance of hydrocarbon fill for reservoir quality prediction in sandstones[J].AAPG Bulletin,2002,86(9):1561-1571.
[20]Meissen F F. Petroleum geology of the bakken formation, Wiliston Basin, North Dakota and Montana[C] Proceedings of Williston Basin Symposium. September 24-27,Montana Geological Society.Billings,1978:207-227.
[21]MichalK and BachuS. Fluids and pressure distribution in the foreland basin succession in the west-central part of the Albert basin.Canada:evidence for permeability barriers and hydrocarbon generation andmigration. AAPG Bulletin,2001,85:1231-1252
[22]Nedkvitne T, Karlsen D A, Bjurlykke K and Larter S R. Relationship Between Reservoir Diagenetic evolution and petroleum emplacement in Ula Field. North Sea, Marine and Petroleum Geology, 1993,255-270.
[23]Oelkers E H, Bjorkum P A, Murphy W M. A petrographic and computational investigation of quartz cementation and porosity reduction in North Sea sandstones[J]. American Journal of Science, 1996,296:420-452.
[24]Ortoleva P J.Basin Compartmentation:Definitions and Mecanisms[J].AAPG Memoir,1994,61:39-50.
[25]Parnell J, Carey P, Duncan W. History of hydrocarbon chargeon the Atlantic margin:Evidence from fluid-inclusion studies,west of Shetland[J].Geology,1998,26(9):807-810.
[26]Roberts S J, Nunn J A. Episodic fluid expulsion from geop ressured sediments [J].Marine and Petroleum Geology,1995,12:195-204.
[27]Schmid S,Worden R H,Fisher Q J.Diagenesis and reservoir quality of the Sherwood Sandstone(Triassic),Corrib Field,Slyne Basin,west of Ireland[J]. Marine and Petroleum Geology,2004,21(3):299-315.
[28]Shedid AS.Influences of fracture orientation on oil recovery by water and polymer flooding processes: An experimental approach. Journal of Petroleum Science and Engineering,2006,50:285-292.
[29]Spencer C W. Hydrocarbon generation as a mechanism for over pressuring in Rocky Mountain region[J].AAPG Bulletin,1987:368-388.
[30]Surdam R C, Jiao Z S,MacGowen D B.1993. Redox rreaction involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstones. AAPG Bulletin, 77(9):1509-1518.
[31]Ungerer P,Burrus J,Doligez B,et al. Basin evaluation by integrated two-dimensional modeling of heat transfer,fluid flow, hydrocarbon generation and migration [J].AAPG Bulletin,1990,74:309-335.
[32]Villegas M E, Bachu S, Ramon JC, andUnderschultz JR. Flow of formation waters in the Cretaceous-Miocene succession of the Llanos basin, Colombia. AAPG Bulletin,1994,78: 1843-1862.
[33]Wilkinson M D, Darby R S, Haszeldine,et al.Secondary porosity generation during deep burial associated with overpres sure leak-off, Fulmar formation,U K Central Graben[J].AAPG Bulletin,1997,81:803-813.
[34]YahiN, SchaeferR G and Littke R. Petroleum generation and accumulation in the Berkine basin, Eastern Algeria. AAPG Bulletin,2001,85:1439-1467.
[35]安志渊,邢凤存,李群星,王昌勇,等.成像测井在沉积相研究中的应用—以克拉玛依油田八区下乌尔禾组为例[J].石油地质与工程,2007,21(1)：21-24.
[36]曹华,龚晶晶,汪贵锋.超压的成因及其与油气成藏的关系[J].天然气地球科学,2006,17(3)：422-425.
[37]陈荷立,罗晓容.砂泥岩中异常高流体压力的定量计算及其地质应用[J].地质论评,1988,34(1)：54-63.
[38]陈荷立.油气运移研究的有效途径[J].石油与天然气地质,1995,16(2)：123-131.
[39]陈红汉,孙永传,李思田.沉积盆地异常超压与岩石破裂祸合动力学模型综述[J].地质科技情报,1994,13(4)：65-70.
[40]陈全红,王文武,韩文哲,等.鄂尔多斯盆地南部上三叠统层序地层学研究[J].西北地质,2003,36(4)：35-38.
[41]陈瑞银,罗晓容,陈占坤,等.鄂尔多斯盆地埋藏演化史恢复[J].石油学报,2006,27(2)：42-47.
[42]陈瑞银,罗晓容,赵文智,等.鄂尔多斯盆地中生代热异常及烃源岩热演化特征[J].石油勘探与开发,2007,34(6)：658-663.
[43]陈彦华,刘莺.成岩相-储集体预测的新途径[J].石油实验地质,1997,16(3)：274-281.
[44]陈中红,查明,曲江秀.沉积盆地超压体系油气成藏条件及机理[J].天然气地球科学,2003,14(2)：97-102.
[45]崔金栋,郭建华,朱美衡.塔中地区石炭系生屑灰岩段成岩层序地层学[J].地质科技情报,2011,30(5)：23-28.
[46]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[J].石油与天然气地质,1995,16(2)：89-97.
[47]邓秀芹,刘新社,李士祥.鄂尔多斯盆地三叠系延长组超低渗透储层致密史与油藏成藏史[J].石油与天然气,2009,30(2)：156-161.
[48]邓秀芹.鄂尔多斯盆地三叠系延长组超低渗透大型岩性油藏成藏机理研究[D].西安：西北大学博士论文.2011.
[49]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2)：34-37.
[50]邸世祥.油田水文地质学[M].西安：西北大学出版社,1991.
[51]杜业波,季汉成,吴因业,等.前陆层序致密储层的单因素成岩相分析[J].石油学报,2006,27(2)：48-52.
[52]傅强,李益.鄂尔多斯盆地三叠系延长组长8-长7油层组高分辨率层序地层格架及其地质意义.现代地质,2006,20(4)：579-584.
[53]高福红,于均民.流体包裹体在成岩作用研究中的应用[J].世界地质,2000,19(4)：320-323.
[54]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.
[55]国吉安,庞军刚,王桂成,等.鄂尔多斯盆地晚三叠世延长组湖盆演化及石油聚集规律[J].世界地质,2010,29(2)：277-291.
[56]韩永林,王成玉,王海红,等.姬塬地区长8油层组浅水三角洲沉积特征[J].沉积学报,2009,27(6)：1057-1064.
[57]郝芳,邹华耀,倪建华.沉积盆地超压系统演化与深层油气成藏条件[J].地球科学-中国地质大学学报,2002,27(5)：610-614.
[58]郝芳.超压盆地生烃作用动力学与油气成藏机理[M].北京：科学出版社,2005.
[59]何自新.鄂尔多斯盆地演化与油气[M].北京：石油工业出版社.2003.
[60]侯林慧,彭平安,于赤灵等.鄂尔多斯盆地姬塬西峰地区原油地球化学特征及油源分析[J].地球化学,2007,36(5)：497-506.
[61]黄思静,黄培培,王庆东等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3)：7-13.
[62]黄思静,谢连文,张萌,等.中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J].成都理工大学学报(自然科学版),2004,31(3)：273-281.
[63]姜向强,柳广弟,张年富等.准噶尔盆地克百断裂封闭性研究及其对成藏的控制作用[J].高校地质学报,2008,14(2)：243-249.
[64]蒋凌志,顾家裕,郭彬程.中国含油气盆地碎屑岩低渗透储层的特征及形成机理[J].沉积学报,2004,22(1)：13-18.
[65]康锐.鄂尔多斯盆地延长组长9、长10油层组沉积体系研究[D].西安：长安大学硕士论文,2007.
[66]李传亮.地层异常压力原因分析[J].新疆石油地质,2004,25(4)：443-445.
[67]李凤杰,王多云,张庆龙,徐旭辉.鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析.沉积学报,2006,24(4)：549-554.
[68]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)：339-344.
[69]李明诚,单秀琴,马成华.油气成藏期探讨[J].新疆石油地质,2005,26(5)：587-591.
[70]李明诚.石油与天然气运移(第二版)[M].北京：石油工业出版社,1994.
[71]李明诚.石油与天然气运移研究综述[J].石油勘探与开发,2000,27(4)：3-10.
[72]李珊珊.鄂尔多斯盆地西北部延长组长9-10油层组沉积体系研究[D].北京：中国石油大学硕士论文.2010.
[73]李士祥,邓秀芹,庞锦莲等.鄂尔多斯盆地中生界油气成藏与构造运动的关系[J].沉积学报,2010,28(4)：798-807.
[74]李英华.油田水地化指标研究的新认识[J].中国海上油气(地质),1998,12(1)：1-23.
[75]李元昊,刘池洋,独育国,等.鄂尔多斯盆地西北部上三叠统延长组长8油层组浅水三角洲沉积特征及湖岸线控砂[J].古地理学报,2009,11(3)：265-274.
[76]梁积伟,肖丽,高小林,等.鄂尔多斯盆地晚三叠世早期物源分析[J].西北地质,2008,41(2)：81-86.
[77]梁晓伟,韩永林,王海红,等.鄂尔多斯盆地姬塬地区上三叠统延长组裂缝特征及其地质意义.岩性油气藏,2009,21(1)：49-53.
[78]廖朋,唐俊,庞国印,等.鄂尔多斯盆地姬塬地区延长组长81段储层特征及控制因素分析[J].矿物岩石,2012,32(2)：97-104.
[79]廖一,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8油层组高分辨率层序分析[J].沉积学报,2010,28(3)：481-488.
[80]刘宝珺,张锦泉.沉积成岩作用[M].北京：科学出版社,1992.
[81]刘池洋,赵红格,王锋,等.鄂尔多斯盆地西缘(部)中生代构造属性[J].地质学报,2005,79(6)：737-747.
[82]刘德良,谈迎,孙先如,等.鄂尔多斯古生界流体包裹体特征及其与油气演化关系[J].沉积学报,2002,20(4)：695-704.
[83]刘显阳,惠潇,李士祥.鄂尔多斯盆地中生界低渗透岩性油藏形成规律综述[J].沉积学报,2012,30(5)：965-972.
[84]刘小洪,罗静兰,郭彦如,等.鄂尔多斯盆地陕北地区上三叠统延长组长6油层组的成岩相与储层分布[J].地质通报,2008,27(5)：626-632.
[85]刘小琦,邓宏文,李青斌,等.鄂尔多斯盆地延长组剩余压力分布及油气运聚条件[J].新疆石油地质,2007,28(2)：143-145.
[86]柳少波,顾家裕.流体包裹体成分研究方法及其在油气研究中的应用[J].石油勘探与开发,1999,24(3)：29-33.
[87]柳少波,顾家裕.包裹体在石油地质研究中的应用与问题讨论[J].石油与天然气地质,1997,18(4)：326-331.
[88]柳益群,李文厚.陕甘宁盆地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)：87-96.
[89]隆昊,田景春,苏楠,等.鄂尔多斯盆地姬塬地区三叠系延长组长9油层组沉积体系特征[J].沉积与特提斯地质,2010,30(4)：79-85.
[90]隆昊,田景春,苏楠,等.鄂尔多斯盆地姬塬地区三叠系延长组长9油层组砂体储集性研究[J].中国西部科技,2011,10(5)：12-14.
[91]楼章华,兰翔,卢庆梅,等.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用—以松辽盆地北部东区葡萄花油层为例[J].地质学报,1999,73(1)：83-92.
[92]楼章华,卢庆梅,蔡希源,等.湖平面升降对浅水三角洲前缘砂体形态的影响[J].沉积学报,1998,16(4)：27-31.
[93]楼章华,袁笛,金爱民.松辽盆地北部浅水三角洲前缘砂体类型、特征与沉积动力学过程分析[J].浙江大学学报(理学版),2004,31(2)：211-215.
[94]卢焕章,郭迪江.流体包裹体研究进展与方向.地质论评,2000,46(4)：385-392.
[95]卢进才,李玉宏,魏仙样.鄂尔多斯盆地三叠系延长组长7油层组油页岩沉积环境与资源潜力研究[J].吉林大学学报(地球科学版),2006,36(6)：928-932.
[96]吕晓光,李长山,蔡希源,等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型[J].沉积学报,1999,17(4)：572-577.
[97]罗静兰,J.Marcelo Keter,李文厚,等.延长油区侏罗系上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4)：337-342.
[98]罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报.2006,80(5)：664-673.
[99]罗静兰,张立成,阎世可,等.盆地埋藏史及其对砂岩储层物性演化的影响-以陕北延长油区砂岩储层为例[J].石油与天然气地质,2001,22(2)：123-127.
[100]罗静兰,张晓莉,张云翔,等.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4)：541-547.
[101]罗群，孙宏志.断裂活动与油气藏保存关系研究[J].石油实验地质,2000,22(3)：225-231.
[102]罗顺社,银晓.鄂尔多斯盆地姬塬地区延长组长8沉积相的研究[J].石油天然气学报,2008,30(4)：5-9.
[103]苗建宇,赵建设,李文厚等.鄂尔多斯盆地南部烃源岩沉积环境研究[J].西北大学学报(自然科学版),2005,35(6)：771-776.
[104]南珺祥,王素荣,姚卫华.鄂尔多斯盆地陇东地区延长组长6-8特低渗透储层微裂缝研究[J].岩性油气藏,2007,19(4)：40-44.
[105]聂永生,田景春,夏青松.鄂尔多斯盆地白豹-姬塬地区上三叠统延长组物源分析[J].油气地质与采收率,2004,11(5)：4-7.
[106]潘长春,周中毅,解启来.油气和含油气包裹体及其在油气地质地球化学研究中的意义[J].沉积学报,1996,14(4)：15-22.
[107]庞军刚.鄂尔多斯盆地子长史家畔地区延长组储层特征研究[D].西安：西北大学博士论文.2010.
[108]裘怿楠,薛叔浩.油气储层评价技术[M].北京：石油工业出版社,1994.
[109]屈红军,李文厚,梅志超,等.论层序地层学与含油气系统在油气勘探中的联系—以鄂尔多斯中生代盆地为例[J].地质论评,2003,49(5)：495-500.
[110]任战利,张盛,高胜利,等.鄂尔多斯盆地热演化程度异常分布区及形成时期探讨[J].地质学报,2006,80(5)：674-684.
[111]石玉江,肖亮,毛志,等.低渗透砂岩储层成岩相测井识别方法及其地质意义-以鄂尔多斯盆地姬塬地区长8段储层为例[J].石油学报,2011,32(5)：820-828.
[112]宋凯,吕剑文,杜金良等.鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系[J].古地理学报,2002,4(3)：59-66.
[113]孙少华,李小明,龚革联.鄂尔多斯盆地构造热事件研究[J].科学通报,1997,42(3)：306-309.
[114]孙向阳.沉积盆地中地层水化学特征及其地质意义[J].天然气勘探与开发,2001,24(4)：47-53.
[115]万天丰,王明明,殷秀兰等.渤海湾地区不同方向断裂带的封闭[J].现代地质,2004,18(2)：157-163.
[116]万志峰,夏斌,何家雄.沉积盆地超压形成机制及其对油气运聚成藏过程的影响[J].天然气地球科学,2007,18(2)：219-223.
[117]王昌勇,郑荣才,李忠权,等.鄂尔多斯盆地姬塬油田长8油层组岩性油藏特征[J].地质科技情报,2010,29(3)：69-74.
[118]王传远,段毅,杜建国,等.鄂尔多斯盆地长9油层组流体包裹体特征与油气成藏期次分析[J].地质科技情报,2009,28(4)：47-58.
[119]王峰,田景春,张锦泉,等.鄂尔多斯盆地姬塬-胡尖山地区长6油层组的物源和优质储层分布[J].天然气地球科学,2006,17(6)：783-788.
[120]王峰.鄂尔多斯盆地三叠系延长组沉积、层序演化及岩性油藏特征研究[D].成都：成都理工大学博士论文.2007.
[121]王宏波,郑希民,冯明.鄂尔多斯盆地三叠系延长组层序地层与生储盖组合特征.天然气地球科学,2006,17(5)：678-681.
[122]王居峰,郭彦如,张延玲,等.鄂尔多斯盆地三叠系延长组层序地层格架与沉积相构成[J].现代地质,2009,23(5)：803-808.
[123]王鹏,金卫东,高会军,等.声、电成像测井资料裂缝识别技术及其应用.北京：石油工业出版社,2004.
[124]王琪,禚喜准,陈国俊,等.鄂尔多斯西部长6砂岩成岩演化与优质储层[J].石油学报,2005,26(5)：17-23.
[125]王启宇,郑荣才,梁晓伟,等.鄂尔多斯盆地姬塬地区延长组裂缝特征及成因[J].成都理工大学学报(自然科学版),2011,38(2)：220-228.
[126]王瑞飞,孙卫.鄂尔多斯盆地姬塬油田上三叠统延长组超低渗透砂岩储层微裂缝研究.地质论评,2009,55(3)：444-448.
[127]王瑞飞.低渗砂岩储层微观特征及物性演化研究[D].西安：西北大学博士论文.2004.
[128]王若谷,李文厚,廖友运,等.鄂尔多斯盆地胡尖山地区长9-长8油层组物源及沉积体系分析[J].西 安石油大学学报(自然科学版),2010,25(5)：10-15.
[129]王纹婷,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8油层组物源分析[J].岩性油气藏,2009,21(4)：41-46.
[130]王允诚.裂缝性致密储集层[M].北京：地质出版社,1992.
[131]王兆文,赵文智,何海清.超压与烃类生成相互作用及对油气运聚成藏的影响[J].石油勘探与开发,2002,29(4)：12-15.
[132]魏斌,魏红红,陈全红,等.鄂尔多斯盆地上三叠统延长组物源分析[J].西北大学学报,2003,33(4)：447-450.
[133]武富礼,李文厚,李玉宏,等.鄂尔多斯盆地上三叠统延长组三角洲沉积及演化[J].古地理学报,2004,6(3)：307-315.
[134]席胜利,刘新社,王涛.鄂尔多斯盆地中生界石油运移特征分析[J].石油实验地质,2004,26(3)：229-235.
[135]席胜利,刘新社.鄂尔多斯盆地中生界石油二次运移通道研究[J].西北大学学报,2005,35(5)：628-632.
[136]肖丽.鄂尔多斯盆地晚三叠世早期沉积体系与沉积演化规律[D].西安：西北大学硕士论文.2008.
[137]肖七林,孙永革.沉积盆地超压系统内油气的生成与保存[J].地球化学,2007,36(4)：375-382.
[138]徐黎明,周立发,张义楷等.鄂尔多斯盆地构造应力场特征及其构造背景.大地构造与成矿学,2006,30(4)：455-462.
[139]杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用：地质地球化学特征[J].地球化学,2005,34(5)：147-154.
[140]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.
[141]杨雷,梅志超,熊伟.陕北地区延长组层序地层划分与含油气性[J].古地理学报,2001,3(3)：83-88.
[142]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：西北大学博士论文.2009.
[143]杨飏.鄂尔多斯盆地延长组沉积作用与构造变动的关系[D].西安：西北大学硕士论文.2006.
[144]杨友运.鄂尔多斯盆地南部延长组沉积体系和层序特征.地质通报,2005,24(4)：369-372.
[145]银晓,罗顺社,李鑫,等.鄂尔多斯盆地姬塬地区延长组长8时期物源分析[J].岩性油气藏,2008,20(3)：59-63.
[146]于翠玲,曾溅辉,林承焰等.断裂带流体活动证据的确定—以东营凹陷胜北断裂带为例[J].石油学报,2005,26(4)：34-38.
[147]于雷,陈建文,李元,等.姬塬油田堡子湾南长4+5储层裂缝特征及其影响因素分析[J].岩性油气藏,2011,23(6)：69-72.
[148]曾联波,李忠兴,史成恩,等.鄂尔多斯盆地上三叠统延长组特低渗砂岩储层裂缝特征及成因.地质学报,2007,81(2)：174-180.
[149]曾联波,漆家福,王永秀.低渗透储层构造裂缝的成因类型及形成地质条件.石油学报,2007,28(4)：52-56.
[150]曾联波,赵继勇,朱圣举,等.岩层非均质性对裂缝发育的影响研究.自然科学进展,2008,18(2)：216-220.
[151]曾联波.陕甘宁盆地延长统区域裂缝的形成及其油气地质意义.中国区域地质,1999,18(4)：391-396.
[152]曾联波.2008.低渗透砂岩储层裂缝的形成与分布.北京：科学出版社.
[153]曾治平,王敏芳,倪建华.油气成藏期次研究中有机包裹体方法存在问题探讨[J].天然气地球科学,2002,13(3)：55-59.
[154]张凤奎,张忠义,张林.鄂尔多斯盆地三叠系延长组层序地层特征新认识[J].地层学杂志,2008,32(1)：99-195.
[155]张泓.鄂尔多斯盆地中新生代构造应力场.华北地质矿产杂志,1996,11(1)：87-92.
[156]张杰,赵玉华.鄂尔多斯盆地三叠系延长组地震层序地层研究[J].岩性油气藏,2007,19(4)：71-74.
[157]张磊,龚福华,任瑞清,等.鄂尔多斯盆地胡尖山-王洼子地区长4+5储层成岩作用及成岩相研究[J].特种油气藏,2009,16(5)：40-47.
[158]张莉.陕甘宁盆地储层裂缝特征及形成的构造应力场分析.地质科技情报,2003,22(2)：21-24.
[159]张世广,柳成志,卢双舫,等.高分辨率层序地层学在河、湖、三角洲复合沉积体系的应用—以朝阳沟油田扶余油层开发区块为例[J].吉林大学学报(地球科学版),2009,39(3)：361-368.
[160]张文正,李剑峰.鄂尔多斯盆地油气源研究[J].中国石油勘探,2001,6(4)：28-36.
[161]张文正,杨华,傅锁堂.鄂尔多斯盆地长91湖相优质烃源岩的发育机制探讨[J].中国科学(D辑)：地球科学,2007,37(增刊)：33-38
[162]张文王,杨华,李剑锋,等.2006.论鄂尔多斯盆地长7段优质烃源岩在低渗透油气成藏富集中的主导作用-强生排烃特征及机理分析[J].石油勘探与开发,33(3)：289-293.
[163]张文正,杨华,李剑锋等.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用[J].石油勘探与开发,2006,33(3)：497-506.
[164]张义楷,周立发,党犇,等.鄂尔多斯盆地中新生代构造应力场与油气聚集.石油实验地质, 2006,28(3)：215-219.
[165]张照录,王华,杨红.含油气盆地输导体系研究[J].石油与天然气地质,2000,21(2)：133-135.
[166]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.
[167]赵靖周.油气包裹体在成藏年代学研究中的应用实例分析[J].地质地球化学,2002,30(2)：83-87.
[168]赵俊兴,申赵军,李良等.大型内陆拗陷湖盆层序结构充填特征及其分布规律——以鄂尔多斯盆地延长组为例[J].岩石学报,2011,27(8)：147-154.
[169]赵力彬,黄志龙,高岗,等.关于用包裹体研究油气成藏期次问题的探讨[J].油气地质与采收率,2005,12(6)：6-18.
[170]赵孟为,Behr H J.鄂尔多斯盆地三叠系镜质体反射率与地热史[J].石油学报,1996,17(2)：15-23.
[171]赵文智,胡树云,汪泽成,等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用[J].石油勘探与开发,2003,30(5)：1-5.
[172]赵文智,王新民,郭彦如,等.鄂尔多斯盆地西部晚三叠世原型盆地恢复及其改造演化[J].石油勘探与开发,2006,33(1)：6-13.
[173]赵云翔,王建峰,丁熊,等.鄂尔多斯盆地上三叠统长9油层组物源分析[J].石油天然气学报,2012,34(4)：7-13.
[174]郑荣才,耿威,周刚,等.鄂尔多斯盆地白豹地区长6砂岩成岩作用与成岩相研究[J].岩性油气藏,2007,19(2)：1-8.
[175]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[J].沉积学报,2001,19(2)：249-255.
[176]郑荣才,尹世名,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3)：369-375.
[177]郑荣才,赵俊兴,李永军,等.鄂尔多斯盆地环县地区延安组高分辨率层序地层学特征[J].中国矿业大学学报,2009,34(3)：394-399.
[178]郑荣才等.高分辨率层序地层学[M].北京：地质出版社.2010.
[179]郑有业,王思源,等.有机包裹体研究在石油地质领域中的应用现状[J].地质地球化学,1998,26(2)：72-76.
[180]钟广法,祁兴中,马勇,等.电成像测井资料在裂缝成因分析中的应用.物探与化探,2005,29(2)：116-118.
[181]周伦先.成像测井技术在研究砂砾岩沉积构造中的应用[J].新疆石油地质,2008,29(5)：654-667.
[182]朱伟林,李建平,周心怀,等.渤海新近系浅水三角洲沉积体系与大型油气田勘探[J].沉积学 报,2008,26(4)：575-582.
[183]朱玉双,王震亮,高红,等.油气水物化性质与油气运移及保存[J].西北大学学报(自然科学版),2000,30(5)：415-418.
[184]邹才能,陶士振,薛叔浩.“相控论”的内涵及其勘探意义[J].石油勘探与开发,2005,32(6)：7-12.
[185]邹才能,陶士振,周慧,等.成岩相的形成、分类与定量评价方法[J].石油勘探与开发,2008,35(5)：526-540.
[186]邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布[J].地质学报,2008,82(6)：813-825.
[2]Barker C E.A fluid inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer.Geology,1991,18:1003-1006.
[3]Barth T, Bjorlykke K. Organic acids from source rock maturation:generation potentials,transport mechanisms and relevance for mineral diagenesis[J].AppIied Geochemistry,1993,8:325-337.
[4]Bloch S, Franks S G. Preservation of shallow plagioclase dissolution porosity during burial:implications for porosity prediction and aluminium mass balance[J].AAPG Bulletin,1993,77:1488-1501.
[5]Brendow K. Global oil shale issues and perspectives[J].Oil Shale,2003,20(1):81-92.
[6]Carr A D. Suppression and retardation of vitrinite reflectance, Part 1. Formation and significance for hydrocarbon generation[J] Journal of Petroleum Geology,2000,23:313-343.
[7]Carr A D. Suppression and retardation of vitrinite reflectance, Part 2. Derivation and testing of a kinetic model for suppression [J]. Journal of Petroleum Geology,2000,23:475-496.
[8]Chad A,Underwood ML,Cooke JA,et al.Stratigraphic controls on vertical fracture patterns in Silarian dolomite, northeastern Wisconsin. AAPG Bulletin,2003,87(1):121-142.
[9]Cross TA and Lessenger MA.1996. Sediment volume partitioning:Rationale for stratigraphic model evaluation and high-resolution stratigraphic correlation. Accepted for Publication in Norwegian Petroleums-Forening Conference Volume July,1-24.
[10]Cross TA. Controls on coal distribution intransgressive 2 regressive cycle, Upper Cretaceous, Western Interior, USA [M] WilgausC K. Sea Level Change:An Integrated Approach. NewYork:SEPM SpecialPublication,1998:371-380.
[11]GALEAZZI J S. Structural and stratigraphic evolution of the western Malvinas Basin, Argentina[J]. AAPG Bul,1998,82(4):596-636.
[12]Ganil M R, Bhattacharya J P. Basic building blocks and process variability of a Cretaceous delta: Internal facies architecture reveals a more dynamic interaction of river, wave, and tidal processes than is indicated by external shape[J]. Journal of Sedimentary Research,2007,77(4):284-302.
[13]Guiton Martin LE, Sassi W, Leroy YM, et al. Mechanical constraints on the chronology of fracture activation in folded Devonian sandstone of the western Moroccan Anti-Atlas. Journal of Structural Geology,2003,25(8):1317-1330.
[14]Helgeson H C,Knox A M,Owens C E, et al.Petroleum,oil field brines.and authigenic mineral assemblages:are they in metastable equilibrium in hydrocarbon reservoirs [J].Geochimica et Cosmochimica Acta,1993,57:3295-3340.
[15]Hillier S.Pore-lining chlorites in siliciclastic reservoir sandstones:Electron microprobe, SEM and XRD data, and implications for their rigin [J].Clay Minerals,1994,29(4):665-679.
[16]Karlsen D A, Nedkvitne T, Larter S R and Bjurlykke K. Hydrocarbon composition of authigenic inclusions:Application to elucidation of petroleum reservoir filling history. Geochimica et Cosmochimica Acta,1993,57:3641-3659.
[17]Knutson C F. Developments in oil shale in 1985[J].AAPG,1990,69(10):882-889.
[18]Land L S. Na-Ca-Cl saline formation water, Frio Formation (Oligocene),South Texas,USA:products of diagenesis[J]. Geochimica et Cosmochimica Acta,1995,59(11):2163-2174.
[19]Marchant M E.Smaijjey P C,Haszeldine R S,et al.Note on the importance of hydrocarbon fill for reservoir quality prediction in sandstones[J].AAPG Bulletin,2002,86(9):1561-1571.
[20]Meissen F F. Petroleum geology of the bakken formation, Wiliston Basin, North Dakota and Montana[C] Proceedings of Williston Basin Symposium. September 24-27,Montana Geological Society.Billings,1978:207-227.
[21]MichalK and BachuS. Fluids and pressure distribution in the foreland basin succession in the west-central part of the Albert basin.Canada:evidence for permeability barriers and hydrocarbon generation andmigration. AAPG Bulletin,2001,85:1231-1252
[22]Nedkvitne T, Karlsen D A, Bjurlykke K and Larter S R. Relationship Between Reservoir Diagenetic evolution and petroleum emplacement in Ula Field. North Sea, Marine and Petroleum Geology, 1993,255-270.
[23]Oelkers E H, Bjorkum P A, Murphy W M. A petrographic and computational investigation of quartz cementation and porosity reduction in North Sea sandstones[J]. American Journal of Science, 1996,296:420-452.
[24]Ortoleva P J.Basin Compartmentation:Definitions and Mecanisms[J].AAPG Memoir,1994,61:39-50.
[25]Parnell J, Carey P, Duncan W. History of hydrocarbon chargeon the Atlantic margin:Evidence from fluid-inclusion studies,west of Shetland[J].Geology,1998,26(9):807-810.
[26]Roberts S J, Nunn J A. Episodic fluid expulsion from geop ressured sediments [J].Marine and Petroleum Geology,1995,12:195-204.
[27]Schmid S,Worden R H,Fisher Q J.Diagenesis and reservoir quality of the Sherwood Sandstone(Triassic),Corrib Field,Slyne Basin,west of Ireland[J]. Marine and Petroleum Geology,2004,21(3):299-315.
[28]Shedid AS.Influences of fracture orientation on oil recovery by water and polymer flooding processes: An experimental approach. Journal of Petroleum Science and Engineering,2006,50:285-292.
[29]Spencer C W. Hydrocarbon generation as a mechanism for over pressuring in Rocky Mountain region[J].AAPG Bulletin,1987:368-388.
[30]Surdam R C, Jiao Z S,MacGowen D B.1993. Redox rreaction involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstones. AAPG Bulletin, 77(9):1509-1518.
[31]Ungerer P,Burrus J,Doligez B,et al. Basin evaluation by integrated two-dimensional modeling of heat transfer,fluid flow, hydrocarbon generation and migration [J].AAPG Bulletin,1990,74:309-335.
[32]Villegas M E, Bachu S, Ramon JC, andUnderschultz JR. Flow of formation waters in the Cretaceous-Miocene succession of the Llanos basin, Colombia. AAPG Bulletin,1994,78: 1843-1862.
[33]Wilkinson M D, Darby R S, Haszeldine,et al.Secondary porosity generation during deep burial associated with overpres sure leak-off, Fulmar formation,U K Central Graben[J].AAPG Bulletin,1997,81:803-813.
[34]YahiN, SchaeferR G and Littke R. Petroleum generation and accumulation in the Berkine basin, Eastern Algeria. AAPG Bulletin,2001,85:1439-1467.
[35]安志渊,邢凤存,李群星,王昌勇,等.成像测井在沉积相研究中的应用—以克拉玛依油田八区下乌尔禾组为例[J].石油地质与工程,2007,21(1)：21-24.
[36]曹华,龚晶晶,汪贵锋.超压的成因及其与油气成藏的关系[J].天然气地球科学,2006,17(3)：422-425.
[37]陈荷立,罗晓容.砂泥岩中异常高流体压力的定量计算及其地质应用[J].地质论评,1988,34(1)：54-63.
[38]陈荷立.油气运移研究的有效途径[J].石油与天然气地质,1995,16(2)：123-131.
[39]陈红汉,孙永传,李思田.沉积盆地异常超压与岩石破裂祸合动力学模型综述[J].地质科技情报,1994,13(4)：65-70.
[40]陈全红,王文武,韩文哲,等.鄂尔多斯盆地南部上三叠统层序地层学研究[J].西北地质,2003,36(4)：35-38.
[41]陈瑞银,罗晓容,陈占坤,等.鄂尔多斯盆地埋藏演化史恢复[J].石油学报,2006,27(2)：42-47.
[42]陈瑞银,罗晓容,赵文智,等.鄂尔多斯盆地中生代热异常及烃源岩热演化特征[J].石油勘探与开发,2007,34(6)：658-663.
[43]陈彦华,刘莺.成岩相-储集体预测的新途径[J].石油实验地质,1997,16(3)：274-281.
[44]陈中红,查明,曲江秀.沉积盆地超压体系油气成藏条件及机理[J].天然气地球科学,2003,14(2)：97-102.
[45]崔金栋,郭建华,朱美衡.塔中地区石炭系生屑灰岩段成岩层序地层学[J].地质科技情报,2011,30(5)：23-28.
[46]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[J].石油与天然气地质,1995,16(2)：89-97.
[47]邓秀芹,刘新社,李士祥.鄂尔多斯盆地三叠系延长组超低渗透储层致密史与油藏成藏史[J].石油与天然气,2009,30(2)：156-161.
[48]邓秀芹.鄂尔多斯盆地三叠系延长组超低渗透大型岩性油藏成藏机理研究[D].西安：西北大学博士论文.2011.
[49]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2)：34-37.
[50]邸世祥.油田水文地质学[M].西安：西北大学出版社,1991.
[51]杜业波,季汉成,吴因业,等.前陆层序致密储层的单因素成岩相分析[J].石油学报,2006,27(2)：48-52.
[52]傅强,李益.鄂尔多斯盆地三叠系延长组长8-长7油层组高分辨率层序地层格架及其地质意义.现代地质,2006,20(4)：579-584.
[53]高福红,于均民.流体包裹体在成岩作用研究中的应用[J].世界地质,2000,19(4)：320-323.
[54]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.
[55]国吉安,庞军刚,王桂成,等.鄂尔多斯盆地晚三叠世延长组湖盆演化及石油聚集规律[J].世界地质,2010,29(2)：277-291.
[56]韩永林,王成玉,王海红,等.姬塬地区长8油层组浅水三角洲沉积特征[J].沉积学报,2009,27(6)：1057-1064.
[57]郝芳,邹华耀,倪建华.沉积盆地超压系统演化与深层油气成藏条件[J].地球科学-中国地质大学学报,2002,27(5)：610-614.
[58]郝芳.超压盆地生烃作用动力学与油气成藏机理[M].北京：科学出版社,2005.
[59]何自新.鄂尔多斯盆地演化与油气[M].北京：石油工业出版社.2003.
[60]侯林慧,彭平安,于赤灵等.鄂尔多斯盆地姬塬西峰地区原油地球化学特征及油源分析[J].地球化学,2007,36(5)：497-506.
[61]黄思静,黄培培,王庆东等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3)：7-13.
[62]黄思静,谢连文,张萌,等.中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J].成都理工大学学报(自然科学版),2004,31(3)：273-281.
[63]姜向强,柳广弟,张年富等.准噶尔盆地克百断裂封闭性研究及其对成藏的控制作用[J].高校地质学报,2008,14(2)：243-249.
[64]蒋凌志,顾家裕,郭彬程.中国含油气盆地碎屑岩低渗透储层的特征及形成机理[J].沉积学报,2004,22(1)：13-18.
[65]康锐.鄂尔多斯盆地延长组长9、长10油层组沉积体系研究[D].西安：长安大学硕士论文,2007.
[66]李传亮.地层异常压力原因分析[J].新疆石油地质,2004,25(4)：443-445.
[67]李凤杰,王多云,张庆龙,徐旭辉.鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析.沉积学报,2006,24(4)：549-554.
[68]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)：339-344.
[69]李明诚,单秀琴,马成华.油气成藏期探讨[J].新疆石油地质,2005,26(5)：587-591.
[70]李明诚.石油与天然气运移(第二版)[M].北京：石油工业出版社,1994.
[71]李明诚.石油与天然气运移研究综述[J].石油勘探与开发,2000,27(4)：3-10.
[72]李珊珊.鄂尔多斯盆地西北部延长组长9-10油层组沉积体系研究[D].北京：中国石油大学硕士论文.2010.
[73]李士祥,邓秀芹,庞锦莲等.鄂尔多斯盆地中生界油气成藏与构造运动的关系[J].沉积学报,2010,28(4)：798-807.
[74]李英华.油田水地化指标研究的新认识[J].中国海上油气(地质),1998,12(1)：1-23.
[75]李元昊,刘池洋,独育国,等.鄂尔多斯盆地西北部上三叠统延长组长8油层组浅水三角洲沉积特征及湖岸线控砂[J].古地理学报,2009,11(3)：265-274.
[76]梁积伟,肖丽,高小林,等.鄂尔多斯盆地晚三叠世早期物源分析[J].西北地质,2008,41(2)：81-86.
[77]梁晓伟,韩永林,王海红,等.鄂尔多斯盆地姬塬地区上三叠统延长组裂缝特征及其地质意义.岩性油气藏,2009,21(1)：49-53.
[78]廖朋,唐俊,庞国印,等.鄂尔多斯盆地姬塬地区延长组长81段储层特征及控制因素分析[J].矿物岩石,2012,32(2)：97-104.
[79]廖一,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8油层组高分辨率层序分析[J].沉积学报,2010,28(3)：481-488.
[80]刘宝珺,张锦泉.沉积成岩作用[M].北京：科学出版社,1992.
[81]刘池洋,赵红格,王锋,等.鄂尔多斯盆地西缘(部)中生代构造属性[J].地质学报,2005,79(6)：737-747.
[82]刘德良,谈迎,孙先如,等.鄂尔多斯古生界流体包裹体特征及其与油气演化关系[J].沉积学报,2002,20(4)：695-704.
[83]刘显阳,惠潇,李士祥.鄂尔多斯盆地中生界低渗透岩性油藏形成规律综述[J].沉积学报,2012,30(5)：965-972.
[84]刘小洪,罗静兰,郭彦如,等.鄂尔多斯盆地陕北地区上三叠统延长组长6油层组的成岩相与储层分布[J].地质通报,2008,27(5)：626-632.
[85]刘小琦,邓宏文,李青斌,等.鄂尔多斯盆地延长组剩余压力分布及油气运聚条件[J].新疆石油地质,2007,28(2)：143-145.
[86]柳少波,顾家裕.流体包裹体成分研究方法及其在油气研究中的应用[J].石油勘探与开发,1999,24(3)：29-33.
[87]柳少波,顾家裕.包裹体在石油地质研究中的应用与问题讨论[J].石油与天然气地质,1997,18(4)：326-331.
[88]柳益群,李文厚.陕甘宁盆地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)：87-96.
[89]隆昊,田景春,苏楠,等.鄂尔多斯盆地姬塬地区三叠系延长组长9油层组沉积体系特征[J].沉积与特提斯地质,2010,30(4)：79-85.
[90]隆昊,田景春,苏楠,等.鄂尔多斯盆地姬塬地区三叠系延长组长9油层组砂体储集性研究[J].中国西部科技,2011,10(5)：12-14.
[91]楼章华,兰翔,卢庆梅,等.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用—以松辽盆地北部东区葡萄花油层为例[J].地质学报,1999,73(1)：83-92.
[92]楼章华,卢庆梅,蔡希源,等.湖平面升降对浅水三角洲前缘砂体形态的影响[J].沉积学报,1998,16(4)：27-31.
[93]楼章华,袁笛,金爱民.松辽盆地北部浅水三角洲前缘砂体类型、特征与沉积动力学过程分析[J].浙江大学学报(理学版),2004,31(2)：211-215.
[94]卢焕章,郭迪江.流体包裹体研究进展与方向.地质论评,2000,46(4)：385-392.
[95]卢进才,李玉宏,魏仙样.鄂尔多斯盆地三叠系延长组长7油层组油页岩沉积环境与资源潜力研究[J].吉林大学学报(地球科学版),2006,36(6)：928-932.
[96]吕晓光,李长山,蔡希源,等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型[J].沉积学报,1999,17(4)：572-577.
[97]罗静兰,J.Marcelo Keter,李文厚,等.延长油区侏罗系上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4)：337-342.
[98]罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报.2006,80(5)：664-673.
[99]罗静兰,张立成,阎世可,等.盆地埋藏史及其对砂岩储层物性演化的影响-以陕北延长油区砂岩储层为例[J].石油与天然气地质,2001,22(2)：123-127.
[100]罗静兰,张晓莉,张云翔,等.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4)：541-547.
[101]罗群，孙宏志.断裂活动与油气藏保存关系研究[J].石油实验地质,2000,22(3)：225-231.
[102]罗顺社,银晓.鄂尔多斯盆地姬塬地区延长组长8沉积相的研究[J].石油天然气学报,2008,30(4)：5-9.
[103]苗建宇,赵建设,李文厚等.鄂尔多斯盆地南部烃源岩沉积环境研究[J].西北大学学报(自然科学版),2005,35(6)：771-776.
[104]南珺祥,王素荣,姚卫华.鄂尔多斯盆地陇东地区延长组长6-8特低渗透储层微裂缝研究[J].岩性油气藏,2007,19(4)：40-44.
[105]聂永生,田景春,夏青松.鄂尔多斯盆地白豹-姬塬地区上三叠统延长组物源分析[J].油气地质与采收率,2004,11(5)：4-7.
[106]潘长春,周中毅,解启来.油气和含油气包裹体及其在油气地质地球化学研究中的意义[J].沉积学报,1996,14(4)：15-22.
[107]庞军刚.鄂尔多斯盆地子长史家畔地区延长组储层特征研究[D].西安：西北大学博士论文.2010.
[108]裘怿楠,薛叔浩.油气储层评价技术[M].北京：石油工业出版社,1994.
[109]屈红军,李文厚,梅志超,等.论层序地层学与含油气系统在油气勘探中的联系—以鄂尔多斯中生代盆地为例[J].地质论评,2003,49(5)：495-500.
[110]任战利,张盛,高胜利,等.鄂尔多斯盆地热演化程度异常分布区及形成时期探讨[J].地质学报,2006,80(5)：674-684.
[111]石玉江,肖亮,毛志,等.低渗透砂岩储层成岩相测井识别方法及其地质意义-以鄂尔多斯盆地姬塬地区长8段储层为例[J].石油学报,2011,32(5)：820-828.
[112]宋凯,吕剑文,杜金良等.鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系[J].古地理学报,2002,4(3)：59-66.
[113]孙少华,李小明,龚革联.鄂尔多斯盆地构造热事件研究[J].科学通报,1997,42(3)：306-309.
[114]孙向阳.沉积盆地中地层水化学特征及其地质意义[J].天然气勘探与开发,2001,24(4)：47-53.
[115]万天丰,王明明,殷秀兰等.渤海湾地区不同方向断裂带的封闭[J].现代地质,2004,18(2)：157-163.
[116]万志峰,夏斌,何家雄.沉积盆地超压形成机制及其对油气运聚成藏过程的影响[J].天然气地球科学,2007,18(2)：219-223.
[117]王昌勇,郑荣才,李忠权,等.鄂尔多斯盆地姬塬油田长8油层组岩性油藏特征[J].地质科技情报,2010,29(3)：69-74.
[118]王传远,段毅,杜建国,等.鄂尔多斯盆地长9油层组流体包裹体特征与油气成藏期次分析[J].地质科技情报,2009,28(4)：47-58.
[119]王峰,田景春,张锦泉,等.鄂尔多斯盆地姬塬-胡尖山地区长6油层组的物源和优质储层分布[J].天然气地球科学,2006,17(6)：783-788.
[120]王峰.鄂尔多斯盆地三叠系延长组沉积、层序演化及岩性油藏特征研究[D].成都：成都理工大学博士论文.2007.
[121]王宏波,郑希民,冯明.鄂尔多斯盆地三叠系延长组层序地层与生储盖组合特征.天然气地球科学,2006,17(5)：678-681.
[122]王居峰,郭彦如,张延玲,等.鄂尔多斯盆地三叠系延长组层序地层格架与沉积相构成[J].现代地质,2009,23(5)：803-808.
[123]王鹏,金卫东,高会军,等.声、电成像测井资料裂缝识别技术及其应用.北京：石油工业出版社,2004.
[124]王琪,禚喜准,陈国俊,等.鄂尔多斯西部长6砂岩成岩演化与优质储层[J].石油学报,2005,26(5)：17-23.
[125]王启宇,郑荣才,梁晓伟,等.鄂尔多斯盆地姬塬地区延长组裂缝特征及成因[J].成都理工大学学报(自然科学版),2011,38(2)：220-228.
[126]王瑞飞,孙卫.鄂尔多斯盆地姬塬油田上三叠统延长组超低渗透砂岩储层微裂缝研究.地质论评,2009,55(3)：444-448.
[127]王瑞飞.低渗砂岩储层微观特征及物性演化研究[D].西安：西北大学博士论文.2004.
[128]王若谷,李文厚,廖友运,等.鄂尔多斯盆地胡尖山地区长9-长8油层组物源及沉积体系分析[J].西 安石油大学学报(自然科学版),2010,25(5)：10-15.
[129]王纹婷,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8油层组物源分析[J].岩性油气藏,2009,21(4)：41-46.
[130]王允诚.裂缝性致密储集层[M].北京：地质出版社,1992.
[131]王兆文,赵文智,何海清.超压与烃类生成相互作用及对油气运聚成藏的影响[J].石油勘探与开发,2002,29(4)：12-15.
[132]魏斌,魏红红,陈全红,等.鄂尔多斯盆地上三叠统延长组物源分析[J].西北大学学报,2003,33(4)：447-450.
[133]武富礼,李文厚,李玉宏,等.鄂尔多斯盆地上三叠统延长组三角洲沉积及演化[J].古地理学报,2004,6(3)：307-315.
[134]席胜利,刘新社,王涛.鄂尔多斯盆地中生界石油运移特征分析[J].石油实验地质,2004,26(3)：229-235.
[135]席胜利,刘新社.鄂尔多斯盆地中生界石油二次运移通道研究[J].西北大学学报,2005,35(5)：628-632.
[136]肖丽.鄂尔多斯盆地晚三叠世早期沉积体系与沉积演化规律[D].西安：西北大学硕士论文.2008.
[137]肖七林,孙永革.沉积盆地超压系统内油气的生成与保存[J].地球化学,2007,36(4)：375-382.
[138]徐黎明,周立发,张义楷等.鄂尔多斯盆地构造应力场特征及其构造背景.大地构造与成矿学,2006,30(4)：455-462.
[139]杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用：地质地球化学特征[J].地球化学,2005,34(5)：147-154.
[140]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.
[141]杨雷,梅志超,熊伟.陕北地区延长组层序地层划分与含油气性[J].古地理学报,2001,3(3)：83-88.
[142]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：西北大学博士论文.2009.
[143]杨飏.鄂尔多斯盆地延长组沉积作用与构造变动的关系[D].西安：西北大学硕士论文.2006.
[144]杨友运.鄂尔多斯盆地南部延长组沉积体系和层序特征.地质通报,2005,24(4)：369-372.
[145]银晓,罗顺社,李鑫,等.鄂尔多斯盆地姬塬地区延长组长8时期物源分析[J].岩性油气藏,2008,20(3)：59-63.
[146]于翠玲,曾溅辉,林承焰等.断裂带流体活动证据的确定—以东营凹陷胜北断裂带为例[J].石油学报,2005,26(4)：34-38.
[147]于雷,陈建文,李元,等.姬塬油田堡子湾南长4+5储层裂缝特征及其影响因素分析[J].岩性油气藏,2011,23(6)：69-72.
[148]曾联波,李忠兴,史成恩,等.鄂尔多斯盆地上三叠统延长组特低渗砂岩储层裂缝特征及成因.地质学报,2007,81(2)：174-180.
[149]曾联波,漆家福,王永秀.低渗透储层构造裂缝的成因类型及形成地质条件.石油学报,2007,28(4)：52-56.
[150]曾联波,赵继勇,朱圣举,等.岩层非均质性对裂缝发育的影响研究.自然科学进展,2008,18(2)：216-220.
[151]曾联波.陕甘宁盆地延长统区域裂缝的形成及其油气地质意义.中国区域地质,1999,18(4)：391-396.
[152]曾联波.2008.低渗透砂岩储层裂缝的形成与分布.北京：科学出版社.
[153]曾治平,王敏芳,倪建华.油气成藏期次研究中有机包裹体方法存在问题探讨[J].天然气地球科学,2002,13(3)：55-59.
[154]张凤奎,张忠义,张林.鄂尔多斯盆地三叠系延长组层序地层特征新认识[J].地层学杂志,2008,32(1)：99-195.
[155]张泓.鄂尔多斯盆地中新生代构造应力场.华北地质矿产杂志,1996,11(1)：87-92.
[156]张杰,赵玉华.鄂尔多斯盆地三叠系延长组地震层序地层研究[J].岩性油气藏,2007,19(4)：71-74.
[157]张磊,龚福华,任瑞清,等.鄂尔多斯盆地胡尖山-王洼子地区长4+5储层成岩作用及成岩相研究[J].特种油气藏,2009,16(5)：40-47.
[158]张莉.陕甘宁盆地储层裂缝特征及形成的构造应力场分析.地质科技情报,2003,22(2)：21-24.
[159]张世广,柳成志,卢双舫,等.高分辨率层序地层学在河、湖、三角洲复合沉积体系的应用—以朝阳沟油田扶余油层开发区块为例[J].吉林大学学报(地球科学版),2009,39(3)：361-368.
[160]张文正,李剑峰.鄂尔多斯盆地油气源研究[J].中国石油勘探,2001,6(4)：28-36.
[161]张文正,杨华,傅锁堂.鄂尔多斯盆地长91湖相优质烃源岩的发育机制探讨[J].中国科学(D辑)：地球科学,2007,37(增刊)：33-38
[162]张文王,杨华,李剑锋,等.2006.论鄂尔多斯盆地长7段优质烃源岩在低渗透油气成藏富集中的主导作用-强生排烃特征及机理分析[J].石油勘探与开发,33(3)：289-293.
[163]张文正,杨华,李剑锋等.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用[J].石油勘探与开发,2006,33(3)：497-506.
[164]张义楷,周立发,党犇,等.鄂尔多斯盆地中新生代构造应力场与油气聚集.石油实验地质, 2006,28(3)：215-219.
[165]张照录,王华,杨红.含油气盆地输导体系研究[J].石油与天然气地质,2000,21(2)：133-135.
[166]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.
[167]赵靖周.油气包裹体在成藏年代学研究中的应用实例分析[J].地质地球化学,2002,30(2)：83-87.
[168]赵俊兴,申赵军,李良等.大型内陆拗陷湖盆层序结构充填特征及其分布规律——以鄂尔多斯盆地延长组为例[J].岩石学报,2011,27(8)：147-154.
[169]赵力彬,黄志龙,高岗,等.关于用包裹体研究油气成藏期次问题的探讨[J].油气地质与采收率,2005,12(6)：6-18.
[170]赵孟为,Behr H J.鄂尔多斯盆地三叠系镜质体反射率与地热史[J].石油学报,1996,17(2)：15-23.
[171]赵文智,胡树云,汪泽成,等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用[J].石油勘探与开发,2003,30(5)：1-5.
[172]赵文智,王新民,郭彦如,等.鄂尔多斯盆地西部晚三叠世原型盆地恢复及其改造演化[J].石油勘探与开发,2006,33(1)：6-13.
[173]赵云翔,王建峰,丁熊,等.鄂尔多斯盆地上三叠统长9油层组物源分析[J].石油天然气学报,2012,34(4)：7-13.
[174]郑荣才,耿威,周刚,等.鄂尔多斯盆地白豹地区长6砂岩成岩作用与成岩相研究[J].岩性油气藏,2007,19(2)：1-8.
[175]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[J].沉积学报,2001,19(2)：249-255.
[176]郑荣才,尹世名,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3)：369-375.
[177]郑荣才,赵俊兴,李永军,等.鄂尔多斯盆地环县地区延安组高分辨率层序地层学特征[J].中国矿业大学学报,2009,34(3)：394-399.
[178]郑荣才等.高分辨率层序地层学[M].北京：地质出版社.2010.
[179]郑有业,王思源,等.有机包裹体研究在石油地质领域中的应用现状[J].地质地球化学,1998,26(2)：72-76.
[180]钟广法,祁兴中,马勇,等.电成像测井资料在裂缝成因分析中的应用.物探与化探,2005,29(2)：116-118.
[181]周伦先.成像测井技术在研究砂砾岩沉积构造中的应用[J].新疆石油地质,2008,29(5)：654-667.
[182]朱伟林,李建平,周心怀,等.渤海新近系浅水三角洲沉积体系与大型油气田勘探[J].沉积学 报,2008,26(4)：575-582.
[183]朱玉双,王震亮,高红,等.油气水物化性质与油气运移及保存[J].西北大学学报(自然科学版),2000,30(5)：415-418.
[184]邹才能,陶士振,薛叔浩.“相控论”的内涵及其勘探意义[J].石油勘探与开发,2005,32(6)：7-12.
[185]邹才能,陶士振,周慧,等.成岩相的形成、分类与定量评价方法[J].石油勘探与开发,2008,35(5)：526-540.
[186]邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布[J].地质学报,2008,82(6)：813-825.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |