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尚家鼻状构造区油气运聚机制研究
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摘要
在充分利用研究区现有资料的基础上,对尚家地区构造及断裂发育、演化特征进行了系统研究,得到尚家鼻状构造是一个长期继承性发育的古构造,断裂主要有断陷期形成坳陷期继续活动的断裂、坳陷期形成的断裂、断陷期生成坳陷期和构造反转期继续活动的断裂、坳陷期形成构造反转期活动的断裂4种类型。通过油气藏解剖得到,尚家油田扶杨油层油气藏类型主要有断块、断层遮挡、断层—岩性3种类型。其中以断层—岩性油气藏最多,其次是断层遮挡油气藏,最少是断块油气藏,油气分布在平面上主要在尚家鼻状构造的鼻尖部位及其附近,油水分布关系复杂,主要受砂体与断裂沟通情况及砂体分布连续性的控制。通过油源对比得到:尚家地区扶杨油层原油主要来自三肇凹陷青一段源岩,其次为青二三段源岩;通过源岩发育及其地化特征研究得到,三肇坳凹陷青山口组源岩向尚家地区的供油量约为1.1×108t。通过油气成藏条件、时空匹配关系研究得到:尚家地区扶杨油层油气运聚成藏模式是三肇凹陷青山口组源岩生成的油气在超压作用下通过T2-T22断裂向下伏扶杨油层中倒灌运移,然后在浮力作用下沿着被断裂沟通的砂体进行侧向运移至尚家鼻状构造的断块、断层遮挡和断层岩性圈闭中聚集成藏;尚家地区葡萄花油层中油气运聚成藏模式应是尚家地区扶杨油层中的油在浮力作用下通过T2-T11断裂向上运移至葡萄花油层,再沿砂体短距离侧向运移至断块、断层遮挡和断层—岩性圈闭中聚集成藏;尚家地区泉二段油气运聚成藏模式应是沿着扶杨油层油气运移至尚家地区的油进入与其沟通的泉二段高断块圈闭中聚集成藏;尚家地区杨一组中的天然气成藏模式应为沙河子组源岩生成的天然气在浮力作用下沿着T5-T2或T4-T2断裂向上运移至杨一组中的断层圈闭中聚集成藏。通过油气分布与成藏条件时空匹配关系研究得到,尚家油田扶杨油层油成藏主要受圈闭是否发育,圈闭是否位于油气运移路径上和圈闭内砂体是否发育3个因素控制;葡萄花油层油成藏主要受圈闭发育、圈闭位于扶杨油区上方、过T2-T11(反转期活动)断裂连通和圈闭内砂体发育4个因素控制,泉二段油成藏主要受圈闭发育,高断块圈闭与扶杨油气运移路径对接和圈闭内砂体发育3个因素控制,杨大城子天然气成藏主要受圈闭发育、圈闭之下有沙河子组源岩发育、有过T5或T4至T2断裂连通和圈闭内砂体发育4个因素控制。通过实测样品数据得到,尚家地区扶杨油层储层样品流体包裹体均一温度主要分布在115-120℃,结合该区地层埋藏史、热史、源岩生排烃史和断裂活动史恢复结果得到,尚家地区扶杨油层、葡萄花油层和泉二段油气成藏的主要时期应为明水组沉积末期,杨大城子油层天然气成藏的主要时期为泉头组—青山口组沉积时期。综合油气成藏主控因素得到,尚家地区扶杨油层Ⅰ类有利区3个,面积52.2Km2,油资源量1507×104t,Ⅱ类有利区5个,面积13.3 Km2,油资源量267×104t。葡萄花油层Ⅰ类有利区4个,面积9.5 Km2,油资源量113×104t,Ⅱ类有利区3个,面积12.5Km2,油资源量149×104t。泉二段地层Ⅰ类有利区2个,面积3.7 Km2,油资源量107×104t,Ⅱ类有利区1个,面积3.0 Km2,油资源量43×104t。杨大城子组天然气有利区1个,面积2.2 Km2。
With the detailed application of the available datas in working area ,systematically study and the research of the stucture and fault development、evolution features of Shangjia region, the conclusion of Shangjia nose structure is a long-term inherited development paleostructure and the faults of it have four types ( generated in rift stage and still activing in depression stage、generated in depression stage、generated in rift stage and still activing in structure reversal stage、generated in depression and still activing in structrue reversal stage ) has been come up with .
     With the target reservoirs researched , Fuyang Oil Layer Reservoir types mainly have three types,they are: fault、fracture、fault-lithology reservoir in Shangjia Oilfield. Among them the fault-lithology reservoir type is the most ,second is fracture reservoir,the least is fault reservoir,oil and gas distribution is mainly situated near or tip of the nose of Shangjia nosing structure. The relationship of oil and gas distribution is complex, dominately controled by sandbody and fault connection and the continuity of sandstone .
     Through oil sources comparison we abtain that crude oil of Fuyang oil layer in Shangjia region chiefly stem from k1q1 in Sanzhao Sag, secondly stem from k1q2; By means of distribution and geochemical features of sources we abtain that Qingshankou Formation source rock in Sanzhao provide hydrocarbon amount to Shangjia Region about 1.1×103t. Through the research of the relationship of time and space configuration , oil &gas migration and accumulation models of Fuyang oil layer in Shangjia Region are that oil and gas generated by Qingshankou Formation source rock in Sanzhao Sag through T2-T22 fault migrate downward to Fuyang reservoir by overpressure action. Then migrate laterally through sands connected by fault by buoyancy action to fault、fracture、fault-lithology trap of Shangjia nosing structure and accumulate reservoir; migration and accumulation models of Putaohua oil layer in Shangjia Region are that oil-gas of Fuyang oil layer in Shangjia region migrate upward through T2-T11 fault by buoyancy action to Putaohua oil layer, then migrate laterally through sands by short distance to fault、fracture、fault-lithology trap of Shangjia nosing structure and accumulate reservoir; migration and accumulation model of k1q2 in Shangjia region is that migrate through Fuyang oil layer to Shangjia region into connected with k1q2 high block trap and accumulate reservoir; Natural gas migration and accumulation model of Yang1 Formation in Shangjia region is that gas generated by Shahezi group sourcerock action migrate upward through T5-T2 or T4-T2 fault by buoyancy to fault trap of Yang1 group and accumulate reservoir. Through the study of the relations between the distribution of oil and gas and reservoir conditions, the accumulation of Fuyang oil layer in Shangjia Oil field was controled by 3 factors what are that whether the traps were development, whether the traps were located in the path of oil and gas migration and whether the sand was rich in the traps. The accumulation of Putaohua oil layer was controlled by 4 factors, what were that traps were development, the traps were located above the F oil region, the faults of between T2 and T11 (reversal stage activities) were connectivity and the sand was rich in the traps. The accumulation of K1q2 oil was controlled by 3 factors, what were that the traps were development, high block traps and the oil and gas of Fuyang oil layer migration ways were connectivity, and the sand was rich in the traps.
     The accumulation of the gas of Yangdachengzi oil layer was controlled by 4 factors, what were that the traps were development, the development Shahezi Formation source rock was under the traps, there were faults which connected T5 or T4 and T2, and the sand was rich in the traps.Through actual measurement, reservoil samples fluid inclusion homogenizaion temperature of Fuyang oil layer in Shangjia Region mainly distribute 115-120℃, mainly paticular period of reservoir forming of Fuyang oil layer、Putaohua oil layer and k1q2 in Shangjia Region is the end of Mingshui group sedimentation period, mainly paticular period of gas reservoir forming of Yangdachengzi oil layer is the end of Quantou group-Qingshaokou Formation sedimentation period. Synthesize main controlling factors,we obtain thatⅠt ype range of profitability of Fuyang oil layer in Shangjia region has three, that area is 52.2Km2,resources amount is 1507×104t,Ⅱtype range of profitability has five, that area is 13.3Km2,resources amount is 267×104t.Ⅰtype range of profitability of Putaohua oil layer has four, that area is 9.5Km2,resources amount is 113×104t,Ⅱtype range of profitability has three, that area is 12.5Km2,resources amount is 149×104t.Ⅰtype range of profitability of k1q2 layer has two, that area is 3.7Km2,resources amount is 107×104t,Ⅱtype range of profitability has one, that area is 3.0Km2,resources amount is 43×104t.Gas range of profitability of Yangdachengzi group has one, that area is 2.2Km2.
引文
[1] Welte D H and Yukler M A. Petroleum origin and accumulation in basin evolution-A quantitative model[J]. AAPG Bullet in, 1981,66:1387-1396.
    [2] Lerche I, Yarzab K F and Kendall C G S C. Determination of paleoheat flux from vitrinite reflectance data[J]. AAPG Bullet in. 1984,68: 1704-1717.
    [3]李德生.李德生石油地质论文集[M].北京:石油工业出版社,1992.
    [4]田在艺.田在艺石油地质论文集[M].北京:石油工业出版社,1997.
    [5]胡见义,黄第藩,徐树宝等.中国陆相石油地质理论基础[M].北京:石油工业出版社,1991.
    [6]张厚福,张万选.石油地质学(第二版)[M].北京:石油工业出版社,1990.
    [7]郝石生,陈章明等著.天然气藏的形成和保存[M].北京:石油工业出版社,1995.
    [8]陈发景,田世澄主编.压实油气运移[M].北京:石油工业出版社,1989.
    [9]陈荷立等译.石油地质论文集.油气运移(2)[M].北京:石油工业出版社,1987.
    [10]李明诚.石油和天然气运移、聚集的特征[J].地球物理学进展,1994,9(1):122-123.
    [11]陶一川.石油地质流体力学分析基础[M].武汉:中国地质大学出版社,1993.
    [12]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.
    [13] Ortoleva P J. Compartmentation: definition and mechanisms[J]. AAPG Memoir 1994,61, 39-52.
    [14]李明诚.油气运移研究的现状与发展[J].石油勘探与开发,1994,21(2):1-6
    [15]张义纲.天然气生成聚集与保存[M].南京:海河大学出版社,1991.
    [16]张新民等.中国的煤层甲烷[M].西安:陕西科学技术出版社,1991.
    [17]骆祖红.煤层甲烷数值模拟[J].煤田地质勘探,1997,25(2):28-30.
    [18] Lenormand R, Touboul E, Zarcooe C. Numerical models and experiments on immiscible displacements in porous media[J]. Journal of Fluid Mechanics,1988,189:165-187.
    [19] Dembicki H J, Anderson M J. secondary migration of oil: experiments supporting efficient movement of separate, buoyant oil phase along Limited conduits[J]. AAPG Bull, 1989, 73(8):1018-1021.
    [20] Catalan L, Xiaowen F, Chatais I. An experimental study of secondary oil migration[J]. AAPG Bull, 1992, 76(5):638-650.
    [21] Gussow. Differential entrapment of oil and gas: a fundamental principle[J]. AAPGBull. 1954, 38:816-853.
    [22] Tissot B. Migration of hydrocarbons in sedimentary basin: a geological geochemical and historical perspective, and IFP Exploration Research Conference. 1987.
    [23] Hindle A D. Petroleum migration pathways and charge concentration:A three dimensional model[J]. AAPG Bulletin, 1997, 81:1451-1481.
    [24] Knipe R J. The influence of fault zone processes and diagenesis on fluid flow[J] .AAPG Tulsa,Stud. Geol. 1993,36,135-151.
    [25] Aydin A. Fractures faults and hydrocarbon entrapment migration and flow[J]. Marine and petroleum geology. 2000,17:797-814.
    [26] Nuun J A and Meulbroek P. Kilometer-scale upward migration of hydrocarbons in geopressured sediments by buoyancy-driven propagation of methane-filled fractures[J]. AAPG Bulletin, 2002,86(5):907-918.
    [27]潘钟祥.不整合对油气运移聚集的重要性及寻找不整合面下的某些油气藏[J].地质论评,1983,29(4):374-381.
    [28] Bethke C M, Reed J D and Oitz D F. Long-range petroleum migration in the lllinois basin[J]. AAPG Bulletin, 1991, 75(5):925-945.
    [29]吕修祥.塔里木盆地不整合面石油运移散失量的实验研究[J].石油大学学报(自然科学版).2000,24(4):112-114.
    [30] Nie F J, Li S T,Wang H, et al. Lateral migration pathways of petroleum in theⅢsubbasin, Pearl river mouth basin, South China Sea[J]. Marine and petroleum geology, 2001, 18:561-575.
    [31]向才富,夏斌,谢习农,冯志强.松辽盆地西部斜坡带油气运移主输导通道[J].石油与天然气地质. 2004,25(2):204-208.
    [32] Dreyer T, Scheie A and Walderhung O. Minipermeter-based study of permeability trends in channel sandbodies[J]. AAPG Bulletin, 1990,74:359-374.
    [33] Doyel J D and Sweet M L. Three dimensional distribution of lithofacies, bounding surfaces, porosity and permeability in a fluvial sandstone Gypsy sandstone of North Oklahoma[J]. AAPG, Bulletin, 1995,79:70-96.
    [34] Hindle A D. Petroleum migration pathways and charge concentration. A three dimensional model[J]. AAPG Bulletin, 1999,83:1020-1023.
    [35] Bekele E, Person M and Marsily G. Petroleum migration pathways and charge conceration: A three dimensional model: Discussion[J]. AAPG Bulletin, 1999, 83:1015-1019.
    [36]龚再生,杨甲明.油气成藏动力学及油气运移模式[J].中国海上油气(地质). 1999,13(4):235-239.
    [37]雷茂盛,林铁峰.松辽盆地断层纵向导流性浅析[J].石油勘探与开发, 1999,26(1):32-35.
    [38]王震亮,陈荷立.有效运聚通道的提出与确定初探[J].石油实验地质, 1999,21(1):71-75.
    [39]张照录,王华,杨红等.含油气盆地的输导体系研究[J].石油与天然气地质, 2000, 21(2):133-135.
    [40]谢泰俊.琼东南盆地天然气运移输导体系及成藏模式[J].勘探家,5(1):17-21.
    [41]付广,薛永超,付晓飞.油气运移输导体系及对成藏的控制[J].新疆石油地质, 2001,22(1):24-26.
    [42]赵忠新,王华,郭奇军等.油气输导体系的类型及其输导性能在时空上的演化分析[J].石油实验地质.2002,24(6):527-532. [43 Galeazzi J S. Structural and stratigraphic evolution of the westem Maivinas basin,Argentina[J]. AAPG Bulletin,1998,82(4):596-636.
    [44]卓勤功,宁万兴,荣娜.断陷盆地输导体系类型及控制机制[J].地质论评.2005,51(4):416-422.
    [45]梁书义,刘克奇,蔡忠贤.油气成藏体系及油气输导子系统研究[J].石油实验地质. 2005,27(4):327-332.
    [46]张发强,罗晓容等.石油二次运移优势路径形成过程实验及机理分析[J].地质科学.2004,39(2):159-176.
    [47] Ungerer P,Bessis F,Chent Y, et al. Geological and geochemical models in exploration: principles and practical examples, In: Demaison G ed. Petroleum geochemistry and basin evaluation[J]. AAPG Memoir, 1984, 35:53-57.
    [48] Ungerer P et al. Basin evaluation by integrater two-demensional modeling of heat transfer,fluid flow,hudrocarbon generation and migration[J]. AAPG Bull, 1990,74(3):1578-1583.
    [49] England W A et al. The movement and entrapment of petroleum fluids in the subsurface. Jour[J]. Of the Geol. Soci., London, 1987,144:327-347
    [50] Braester C. et al. Hydrocarbon Accumulation of the dead sea Graben. A simulation Approach[J]. Jour of Petrol Geo. 1991,14(2):72-75.
    [51] Selle O M , et al. Experimental Verification of Low-dip, Low-rate Two-phase(Secondary) Migration By Means ofγ-ray Absorbtion[J]. In: Geofluids`93(Ed, by J. Parnell,A H Ruffell and N R Moles):72-75.
    [52] Thomas M M, Ciouse J A. Scaled Physical Model of Seconday Oil Migration[J]. AAPG Bull,1995,79(1):19-29.
    [53] Hirsch L M and Thompson A H. Minimum saturations and buoyancy in secondary migration[J]. AAPG Bull.1995,79:696-710.
    [54]曲志浩,王菁.卡断现象与油气二次运移形式.见:碎屑岩储层的孔隙结构与成因及其对油气运移的控制[M].西安:西北大学出版社,1991.
    [55]郭尚平,黄延章,周娟等.物理化学渗流微观机理[M].北京:科学出版社.6-18,1990.
    [56]张义纲,陈彦华,陆嘉炎.油气运移及其聚集成藏模式[M].南京:河海大学出版社,1997.
    [57] Scheidegger A E. The physics of flow through porous media[M]. Toronto, Canada: Univ of Toronto Press, 1974. 20-240.
    [58] Dembicki H J, Anderson M J. secondary migration of oil: experiments supporting efficient movement of separate, buoyant oil phase along Limited conduits[J]. AAPG Bull, 1989, 73(8):1018-1021.
    [59]陈章明,张云峰,韩有信,等.凸镜状砂体聚油模拟实验及其机理分布[J].石油实验地质,1998,25(1):166-170.
    [60]曾溅辉,金之钧.油气二次运移和聚集物理模拟[M].北京:石油工业出版社. .2000
    [61]张发强,罗晓容,苗盛等,等.石油二次运移的模式及其影响因素[J].石油实验地质,2003,25(1)69-75.
    [62] Ungerer P,Bessis F,Chent Y, et al. 1984, Geological and geochemical models in exploration: principles and practical examples, In: Demaison G ed. Petroleum geochemistry and basin evaluation[J]. AAPG Memoir, 35:53-57.
    [63] Bethke C.M,Reed J D and Oitz D F. long-range petroleum migration in the lllinois basin 1991[J], AAPG Bulletin,75(5):925-945.
    [64]石广仁.油气盆地数值模拟方法[M].北京:石油工业出版社,1994.1-172.
    [65]刘伊克,常旭.盆地模拟水动力油气二次运移隐式多重网络法[J].地球物理学报,1998,342-347.
    [66]金之钧,张发强.油气运移研究现状及主要进展[J].石油与天然气地质.2005,26(3):263-270.
    [67]李明诚. 2004石油与天然气运移(第三版)[M].北京:石油工业出版社.
    [68] England W A et al. The movement and entrapment of petroleum fluids in the subsurface. Jour[J]. Of the Geol. Soci., London. 1987,144:327-347.
    [69] Lythaeuser D and Ruckheim J. Heterogeneity of oil composition within a reservoir as a reflectance of accumulation history[J]. Geochimica et Cosmochimica Acta,1989,53:2119-2123.
    [70] Lartter S R and Alpin A C. Reservoir geochemistry: methods, applications and opportunities. Ln: The Geochemistry of Reservoir(sCubitt, J. M. and, W. A. eds)[J]. Geol. Soc. London,159-183.
    [71] Haszeldine R S,Samson I M and Cornfort C. Dating diagenesis and convective fluid movement[J], Beatrice Oil-field. Nature, 1984,307:354-357.
    [72] Horsfield B and Mclimans S R. Geothermometry and geochemistry aqueous and oil-bearing fluid inclusions from Fatch Field[J], Dubai. Org. geochem,1984,6:733-740.
    [73] Burrus R, Cercone K R and Harris P M. Timing of hydrocarbon migration: evidenced from fluid inclusions in calcite cerments, tectonics and burial history. In: Carbonate cements(Schneidermann,N.and Harris,P.M.eds.) [J].Soc Econ Paleontol Mineral, Tula,1985,277-289.
    [74] MacLimans R K. The application of fluid inclusions to migration of oil and diagenesis in petroleum reservois[J].App.Geochem.1987,(2):585-603.
    [75]施继锡,李本超,傅家谟等.有机包裹体及其与油气关系[J].中国科学(B辑),1987,3:318-326.
    [76] Hulen J B, Bereskin S R and Lemieux M. 1990. Timing and temperature of petroleum entrapment in the Grant Canyon Oilfield, Nevada[J]. AAPG Bullrtin,1990,74(8):1328.
    [77]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,1997,8(4):326-331.
    [78]郑有业,王思源,李小菊等.有机包裹体在石油地质领域中的应用现状[J].地质地球科学,1998,26(2):72-76.
    [79]赵靖舟.油气流体包裹体分析在成藏年代学研究中的应用[J].地质地球化学,2002,30(2):83-89.
    [80]赵靖舟.流体包裹体与塔里木盆地油气成藏年代分析[J].石油勘探与开发,2002,29(4):21-25.
    [81] Eadington P J, Hamilton P J. Bai G P. Fluid history analysis-a new concept for prospect evaluation[J]. The APPEA Joumal, 1991,31(1):282-294.
    [82] Lee M,Aronson J L and Savin S.M. K-Ar dating of gas emplacement in Rotliegendes sandstone, Netherlands[J]. AAPG. Bulletin, 69:1381-1385.
    [83]王飞宇,何萍,张水昌等.利用自生伊利石K-Ar定年分析烃类进入储集层的时间[J].地质论评,1997,43(5):540-546
    [84]王飞宇,郝石生,雷加锦. 1998,砂岩储层中自生伊利石定年分析油气藏形成期[J].石油学报,19(2):40-43
    [85]姜振学,庞雄奇,黄志龙.叠合盆地油气运聚期次研究方法及应用[J].石油勘探与开发.2000,27(4):22-25.
    [86]辛仁臣,田春志,窦同君.油藏成藏年代学分析[J].地学前缘,2000,7(3):48-53.
    [87]赵靖舟,罗继红,时保宏等.塔里木盆地油气成藏系统分析[J].石油实验地质,2002,24(4):311-316.
    [88] Hamilton P J, et al Isotopic tracing of the province and diagenesis of Lower Brent Group Sand, North Sea. In: Petroleum Geology of Northwest Europe (Eds. J. Brooks and K.W Glennie) [J]. Graham and Trotman, London, 1987, 939-949.
    [89] Hamilton P J, Kelly S and Fallick A E. Isotopic constraints on diagentic processes[J]. 1.Radiometric dating of illite in hydrocarbon reservoirs, Clay Miner,1989,24:215-231.
    [90] Saigai G, Bjorlykke K and later S. The effect of oil emplacement on diagenic process-examples from the Fu;mar reservoir sandstone, central North Sea[J]. AAPG Bulltin,1993,77(1):68-80.
    [91] Karlsen D A, Nedkvitne T, Larter S R et al. Hydrocarbon composition of authigenic inclusions: application to elucidation of petroleum reservoir filling[J]. Geochimica et Comochimica Acta, 1993,57(15):3641-3659.
    [92] Jacob H. Disperse solid bitumen as an indicator for migration and maturity in prospecting for oil and gas[J]. Erdol und Kohle, 1985,38:364-366.
    [93]肖贤明,刘汉德,傅家谟,等应用沥青反射率推算油气生成与运移的地质时间[J].科学通报,.2000,45(19):2123-2127.
    [94]邓良全,刘胜,杨海军.塔中隆起石炭系油气成藏研究[J].新疆石油地质,2000,21(1):23-27.
    [95]赵靖舟.油水界面追溯法与塔里木盆地海相油气成藏期分析[J].石油勘探与开发,2000,28(4):53-56.
    [96]赵靖舟.油气水界面追溯法—研究烃类流体运聚成藏史的一种重要方法[J].地学前缘. 2001,8(4):373-378.
    [97]赵靖舟.前陆盆地天然气成藏理论及应用[M].北京:石油工业出版社,2003,48-88.
    [98]马安来,张水昌,张大江等[J].油气成藏期研究新进展.石油与天然气地质. 2005,26(3):271-276.
    [99]曾国寿,徐梦虹.石油地球化学[M].北京:石油工业出版社。1990
    [100]李振广,李景坤等.多元统计分析在油源对比中的应用[J].新疆石油地质,2004,25(3): 262-263
    [101]卢鸿,冯小杰.油源对比常规方法的使用误区[J].西安工程学院学报,2000,22(2):56-59
    [102]陈建平,赵长毅,王兆云等.西北地区侏罗纪煤系烃源岩和油气地球化学特征.地质论评[J],1998,44(49):149-158.
    [103]陈建平,何忠华等.银额盆地查干凹陷原油地化特征及油源对比[J].沉积学报第19卷第2期,2001年6月
    [104]霍秋立,冯子辉.三肇凹陷低成熟原油地球化学特征及成因探讨[J].大庆石油地质与开发,1995,14(4):6-11
    [105]霍秋立,李振广等.三肇凹陷低熟原油13C-NMR谱特征[J].大庆石油地质与开发,1997,16(3):26-30
    [106] K.E.彼得斯, J.M.莫尔多万著.生物标记化合物指南[M].石油工业出版社,1995:79-187
    [107]曾宪章,梁狄刚等编著.中国陆相原油和生油岩中的生物标志物[M].甘肃科学技术出版社,1989:101-225.
    [108]王铁冠.陆相烃源岩有机质丰度评价指标(SY/T 5735-1995).石油工业出版社.1999.
    [109]戴金星,陈践发,钟宁宁等,中国大气田及其气源[M],北京:石油工业出版社,2003
    [110]庞雄奇,陈章明,陈发景.含油气盆地地史、热史、生留排烃史数值模拟研究与烃源岩定量评价[M].北京:地质出版社,1993.
    [111]中国石油天然气总公司勘探局编.油气资源评价技术[M].石油工业出版社,1999:35-48
    [112]达江,宋岩等.沉积盆地流体势的研究[J].中国西部油气地质,2006,2(4):385-389
    [113]刘晓冬,徐景祯等.流体势场中油气运移分隔槽的自动识别及运聚单元的划分[J].地质科学2002:295-301
    [114]朱红涛.流体势分析研究及应用[J].新疆石油学院学报,2001,13(3):9-14
    [115]柳广弟,赵文智等.油气运聚单元石油运聚系数的预测模型[J].石油勘探与开2003,30(5):53-55
    [116]邹才能,贾承造,赵文智等。松辽盆地南部岩性—地层油气成藏动力和分布规律[J].石油勘探与开发,2005,32(4):125-130
    [117]付广,王兴涛,方纯昌.利用声波时差资料研究欠压实浓度盖层抑制浓度封闭作用形成时期及其研究意义[J].石油地球物理勘探,2001,36(3):279-284
    [118]刘德来,陈发景,温祥泉.松辽盆地坳陷期T2断层成因机制分析[J].大庆石油学院学报,1996,20(1)23-27.
    [119]胡望水.松辽盆地T2断层系及青山口组早期伸展裂陷[J].石油勘探与开发,1995,22(2):8-12
    [120]胡望水,吕炳全,张文军,等.松辽盆地构造演化及成盆动力学探讨[J].地质科学,2005,40(1):16-31.
    [121]迟元林,云金表,蒙启安.松辽盆地深部结构及成盆动力学与油气聚集[M].北京:石油工业出版社,2002,10-80.
    [122]迟元林,萧德铭,殷进垠.松辽盆地三肇地区上生下储“注入式”成藏机制[J].地质学报,2000,74(4):371-377
    [123]蔡希源,陈章明,王玉华等.松辽盆地两江地区石油地质分析[M].北京:石油工业出版社,1999,117-141
    [124]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].北京:石油工业出版社,1997,104-180.
    [125]彭秀美.1993.用岩石力学实验研究区域盖层的埋深和厚度标值[A].石宝珩,周堃,关德范等.1993.扬子海相地质与油气[M].北京:石油工业出版社,262-269
    [126]吕延防,付广.断层封闭研究[M].北京:石油工业出版社,2002,132-141
    [127]吕延防,李国会,王跃文.断层封闭性的定量研究方法[J].石油学报,1996,17(3):39-45
    [128]吕延防,陈章明,陈发景.非线性映射分析断层封闭性[J].石油学报,1995,16(2):36-41.
    [129]付广,李玉喜,张云峰等.断层垂向封闭油气性研究方法及其应用[J].天然气工业,1997,17(6):22-25
    [130]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性[J].现代地质,2004,18(2):157-162.
    [131]付广,孟庆芬.断层封闭性影响因素的理论分析[J].天然气地球科学,2002,13(3-4):40-44.
    [132]刘德汉.包裹体研究—盆地流体追踪的有利工具[J].地学前缘.1995,2(3-4):149-154.
    [133]付广,李凤君,白明轩.断层垂向侧向封闭性与垂向封闭性关系分析[J].大庆石油地质与开发.1998,17(2):6-10.
    [134] Gibson R G. Fault-zone Seals in Siliciclastic Strata of the Columbus Basin, Offshore Trinidad[J], AAPG Bulletin,1995,78(9):1372-1385.

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