东濮凹陷濮卫洼陷区古近系油气成藏机理研究
|
摘要
在前人成果的基础上,以现代油气成藏理论为指导,对濮卫洼陷区的烃源岩特征、油气来源、输导体系及油气运移路径进行了分析,并通过研究烃源岩生排烃史、成藏期次及成藏动力条件明确了濮卫洼陷区油气运聚成藏过程,划分了油气成藏系统,建立了成藏模式。
通过对烃源岩和原油系统取样与地化分析,剖析了烃源岩与原油的地球化学特征,建立了源-藏空间对应关系。研究区内已发现的油气主要富集于濮卫洼陷区及相邻构造带,根据原油地化及分布特征,可将其划分为濮卫洼陷型、相邻洼陷型及混合型三种成因类型:洼陷西翼、古云集斜坡带和洼陷东翼沙三段油气为濮卫洼陷型;濮城断背斜东翼、濮城南构造文北断块区沙三中、下亚段油气为相邻洼陷型,来自于濮城-前梨园洼陷;卫城地垒-文明寨、濮城断背斜轴部沙三中原油、濮城断背斜构造沙三上及全区沙二-沙一段为混和型,洼陷西部油气来自于濮卫洼陷和马寨洼陷,洼陷东南部油气来自于濮卫洼陷和濮城-前梨园洼陷。
通过对濮卫洼陷区砂体特征、断层特征及断层和砂体配置关系进行全面分析,明确了砂体型、断层型和断-砂型三种输导体系类型及其空间分布规律,并根据油源对比及源-藏空间对应关系,综合利用生物标志化合物、含氮化合物等指标对濮卫洼陷区油气运移路径进行了追踪。油气由濮卫洼陷向西和西北方向沿砂体型和断-砂型输导体系运移,向东则沿断-砂型输导体系直接充注,由沙三段向沙二段-沙一段沿断层型输导体系垂向运移。
分析了濮卫洼陷区成藏期次及成藏动力条件,利用盆地模拟技术进行了烃源岩生排烃史和油气运聚史模拟,根据流线特征,将研究区划分为五个成藏系统,各成藏系统的主要运聚期为古近纪末期,此时烃源岩生排烃量大,在洼陷中心异常高压力驱动下,油气沿砂体向斜坡区剩余压力过渡带运移,部分油气在断层和盐岩遮挡下形成岩性及构造-岩性油气藏,部分油气继续沿断层-砂体向地垒带及断背斜构造带等剩余压力低值区运移形成构造油气藏,在构造应力与地层压力作用下油气由沙三段沿油源断层及其次生断层向浅层运聚,油气充注基本定型;新近纪晚期-第四纪烃源岩存在二次生烃,但生排烃量小,以洼陷区本层系成藏为主。
On the basis of previous results, directed by the hydrocarbon accumulation theory, the characteristics of source rock, oil-source correlation, the migration sysytem and the direction of oil migration in Puwei sag is researched. And the petroleum accumulation process is recovered by simulating the hydrocarbon generation and expulsion histories associated with the analysis of the stages of hydrocarbon accumulation and the reservoir forming dynamic. The reservoir forming systems of Puwei sag are divided and the dynamic hydrocarbon accumulation models are set up in this paper.
Through systematic sampling and geochemical analysis the geochemical characteristics of source rock and oil are clearly and the spatial relationship between them has been established. The oil and gas discovered mainly distributes in Puwei sag area and adjacent structure zones. The oil can be divided into three types of Puwei sag, neighboring sags and mixed type based on the characteristics of geochemist and distribution. The oil of Es3 distributed in the west wing of Puwei sag, Guyunji slope and the east wing of Puwei sag is Puwei sag type. The oil of middle and lower Es3 distributed in the east wing of Pucheng faulted anticline and Pucheng-nan structure Wenbei fault block zone is neighboring sags type and comes from Pucheng-Qianliyuan sag. The oil distributed from Weicheng horst to Wenmingzhai area is mixed type. The oil from Es2 to Es1 in whole area, the oil of middle Es3 distributed in Pucheng faulted anticline axis part and upper Es3 in Pucheng faulted anticline zone are mixed type too. The mixed oil of west comes from Puwei and Mazhai sag. The mixed oil of east and east-south comes from Puwei and Pucheng-Qianliyuan sag.
By means of comprehensively analyzing the characteristics of sand bodies, faults and the disposition relationship between them, three kinds of migration system of sand body, fault and fault-sand are found and their distribution law is described. According to oil-source correlation and the spatial relationship between oil and source rock, in the distribution area of the same oil, the oil migration paths are analyzed by the indexes of biomarker and nitrogen compounds. The oil and gas migrated from Puwei sag to the west and north-west area along sand type and fault-sand type migration systems, charged to the east zone along fault-sand type migration system. The active periods of main faults are match with the hydrocarbon migration times and the oil and gas migrated to the upper Es2 and Es1 strata along fault type migration system.
The stages of hydrocarbon accumulation and the reservoir forming dynamic are clearly. The hydrocarbon generation, expulsion, and migration histories of Puwei sag are studied using simulation technology. Based on the flow-path characteristics, the Puwei sag areas are divided into five accumulation systems. To every system, the main time of hydrocarbon migration is terminal of paleogene. During this time, the amount of hydrocarbon generated and expulsed from source rocks is large. The hydrocarbon migrated from sag area to the pressure transitional zone of slopes along the sand driven by abnormal high pressure of central sag. Some oil and gas accumulated formed lithologic or structural-lithologic reservoirs. Some continuing migrated to the low pressure zone of horst belts and faulted anticline areas formed structural reservoirs. Also the oil and gas of Es3 migrated to Es2 to Es1 along source faults and secondary faults driven by tectonic stress and formation pressure and the hydrocarbon charging terminated basically. From Quaternary period to now, there is hydrocarbon generated for the second time in source rocks, but the amount of hydrocarbon generated and expulsed is little, mainly charging to source rock layer in sag area.
通过对烃源岩和原油系统取样与地化分析,剖析了烃源岩与原油的地球化学特征,建立了源-藏空间对应关系。研究区内已发现的油气主要富集于濮卫洼陷区及相邻构造带,根据原油地化及分布特征,可将其划分为濮卫洼陷型、相邻洼陷型及混合型三种成因类型:洼陷西翼、古云集斜坡带和洼陷东翼沙三段油气为濮卫洼陷型;濮城断背斜东翼、濮城南构造文北断块区沙三中、下亚段油气为相邻洼陷型,来自于濮城-前梨园洼陷;卫城地垒-文明寨、濮城断背斜轴部沙三中原油、濮城断背斜构造沙三上及全区沙二-沙一段为混和型,洼陷西部油气来自于濮卫洼陷和马寨洼陷,洼陷东南部油气来自于濮卫洼陷和濮城-前梨园洼陷。
通过对濮卫洼陷区砂体特征、断层特征及断层和砂体配置关系进行全面分析,明确了砂体型、断层型和断-砂型三种输导体系类型及其空间分布规律,并根据油源对比及源-藏空间对应关系,综合利用生物标志化合物、含氮化合物等指标对濮卫洼陷区油气运移路径进行了追踪。油气由濮卫洼陷向西和西北方向沿砂体型和断-砂型输导体系运移,向东则沿断-砂型输导体系直接充注,由沙三段向沙二段-沙一段沿断层型输导体系垂向运移。
分析了濮卫洼陷区成藏期次及成藏动力条件,利用盆地模拟技术进行了烃源岩生排烃史和油气运聚史模拟,根据流线特征,将研究区划分为五个成藏系统,各成藏系统的主要运聚期为古近纪末期,此时烃源岩生排烃量大,在洼陷中心异常高压力驱动下,油气沿砂体向斜坡区剩余压力过渡带运移,部分油气在断层和盐岩遮挡下形成岩性及构造-岩性油气藏,部分油气继续沿断层-砂体向地垒带及断背斜构造带等剩余压力低值区运移形成构造油气藏,在构造应力与地层压力作用下油气由沙三段沿油源断层及其次生断层向浅层运聚,油气充注基本定型;新近纪晚期-第四纪烃源岩存在二次生烃,但生排烃量小,以洼陷区本层系成藏为主。
On the basis of previous results, directed by the hydrocarbon accumulation theory, the characteristics of source rock, oil-source correlation, the migration sysytem and the direction of oil migration in Puwei sag is researched. And the petroleum accumulation process is recovered by simulating the hydrocarbon generation and expulsion histories associated with the analysis of the stages of hydrocarbon accumulation and the reservoir forming dynamic. The reservoir forming systems of Puwei sag are divided and the dynamic hydrocarbon accumulation models are set up in this paper.
Through systematic sampling and geochemical analysis the geochemical characteristics of source rock and oil are clearly and the spatial relationship between them has been established. The oil and gas discovered mainly distributes in Puwei sag area and adjacent structure zones. The oil can be divided into three types of Puwei sag, neighboring sags and mixed type based on the characteristics of geochemist and distribution. The oil of Es3 distributed in the west wing of Puwei sag, Guyunji slope and the east wing of Puwei sag is Puwei sag type. The oil of middle and lower Es3 distributed in the east wing of Pucheng faulted anticline and Pucheng-nan structure Wenbei fault block zone is neighboring sags type and comes from Pucheng-Qianliyuan sag. The oil distributed from Weicheng horst to Wenmingzhai area is mixed type. The oil from Es2 to Es1 in whole area, the oil of middle Es3 distributed in Pucheng faulted anticline axis part and upper Es3 in Pucheng faulted anticline zone are mixed type too. The mixed oil of west comes from Puwei and Mazhai sag. The mixed oil of east and east-south comes from Puwei and Pucheng-Qianliyuan sag.
By means of comprehensively analyzing the characteristics of sand bodies, faults and the disposition relationship between them, three kinds of migration system of sand body, fault and fault-sand are found and their distribution law is described. According to oil-source correlation and the spatial relationship between oil and source rock, in the distribution area of the same oil, the oil migration paths are analyzed by the indexes of biomarker and nitrogen compounds. The oil and gas migrated from Puwei sag to the west and north-west area along sand type and fault-sand type migration systems, charged to the east zone along fault-sand type migration system. The active periods of main faults are match with the hydrocarbon migration times and the oil and gas migrated to the upper Es2 and Es1 strata along fault type migration system.
The stages of hydrocarbon accumulation and the reservoir forming dynamic are clearly. The hydrocarbon generation, expulsion, and migration histories of Puwei sag are studied using simulation technology. Based on the flow-path characteristics, the Puwei sag areas are divided into five accumulation systems. To every system, the main time of hydrocarbon migration is terminal of paleogene. During this time, the amount of hydrocarbon generated and expulsed from source rocks is large. The hydrocarbon migrated from sag area to the pressure transitional zone of slopes along the sand driven by abnormal high pressure of central sag. Some oil and gas accumulated formed lithologic or structural-lithologic reservoirs. Some continuing migrated to the low pressure zone of horst belts and faulted anticline areas formed structural reservoirs. Also the oil and gas of Es3 migrated to Es2 to Es1 along source faults and secondary faults driven by tectonic stress and formation pressure and the hydrocarbon charging terminated basically. From Quaternary period to now, there is hydrocarbon generated for the second time in source rocks, but the amount of hydrocarbon generated and expulsed is little, mainly charging to source rock layer in sag area.
引文
[1]郝芳,邹华耀,王敏芳,等.油气成藏机理研究进展和前沿研究领域[J].地质科技情报,2002,21(4):7-14.
[2]胡朝元.生油区控制油气田分布——中国东部陆相盆地进行区域勘探的有效理论(源控论)[J].石油学报,1982,3(2).
[3]蒋有录,查明.石油天然气地质与勘探[M].北京:石油工业出版社,2006.
[4]梅玲,张枝焕,王旭东,等.渤海湾盆地南堡凹陷原油地球化学特征及油源对比[J].中国石油大学学报(自然科学版),2008,32(6):40-46.
[5]罗家群.泌阳凹陷核桃园组未熟—低熟油地球化学特征及精细油源对比[J].地质科技与情报,2008,27(5):77-86.
[6]徐冠军,王培荣,刘建宪,等.烃源岩中C5—C13分析新方法及在油源对比中的应用[J]. 2008,35(6):710-714.
[7]申家年,邓冰,卢双舫.齐家古龙凹陷凝析油气的地球化学剖析与油源对比及其启示[J].地球化学,2007,36(6):633-637.
[8]罗宪婴,赵宗举,孟元林.正构烷烃奇偶优势在油源对比中的应用———以塔里木盆地下古生界为例[J].石油实验地质,2007,29(1):74-77.
[9]揭异新,袁月琴,王斌.海拉尔盆地乌尔逊—贝尔凹陷白垩系原油地球化学特征及油源对比[J].石油实验地质,2007,29(1):82-87.
[10]郭艳琴,李文厚,陈全红,等.鄂尔多斯盆地安塞-富县地区延长组-延安组原油地球化学特征及油源对比[J].石油与天然气地质,2006,27(2):218-224.
[11]赵鹏,陈世加,李丽萍,等.酒东盆地营尔凹陷下白垩统油源对比[J].天然气地球科学,2006,17(2):192-195.
[12]马安来,金之钧,王毅.塔里木盆地台盆区海相油源对比存在的问题及进一步工作方向[J].石油与天然气地质,2006,27(3):356-362.
[13]郑冰,高仁祥.塔里木盆地原油碳硫同位素特征及油源对比[J].石油实验地质,2006,28(3):281-285.
[14]严永新,袁光喜,马蓉芳,等.焉耆盆地原油物理化学特征及油源对比研究[J].石油实验地质,2006,28(5):467-471.
[15]彼得斯K E,莫尔多万J M.生物标记化合物指南———古代沉积物和石油中分子化石的解释[M].姜乃煌,张永昌,林永汉,等译.北京:石油工业出版社, 2001.
[16]刘华,蒋有录,陈涛.东营凹陷辛东地区有效输导体系及成藏模式[J].中国石油大学学报(自然科学版). 2008,32(4):13-18.
[17]吕双兵,高先志,何万军,等.阿克库勒凸起输导体系对油气分布的控制效应[J].西南石油大学学报. 2007,29(4):49-52.
[18]卓勤功,宁方兴,荣娜.断陷盆地输导体系类型及控藏机制[J].地质论评. 2005,51(4):416-422.
[19]杜学斌,解习农,任建业.济阳坳陷中生界古潜山油藏输导体系及成藏模式[J].地质科技情报. 2005,24(2):22-26.
[20]冷济高,解习农,刘晓峰.秦皇岛32-6地区油气运移输导体系及成藏模式研究[J].西安石油大学学报(自然科学版). 2008,23(3):22-26.
[21]尹微,樊太亮,曾清波.塔里木盆地巴楚地区输导体系类型及油气成藏[J].石油实验地质. 2006,28(4):340-344.:
[22]魏福军,高志前,樊太亮.塔里木盆地塔中地区输导体系及成藏效应[J].石油与天然气地质.2007,28(2):266-273.
[23]龚再升,杨甲明.油气成藏动力学及油气运移模型[J].中国海上油气(地质), 1999, 13(4): 235-239.
[24]谢泰俊,潘祖荫,杨学昌.油气运移动力及通道体系.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997:385-405
[25] Galeazzi J S.Structral and stratigraphic evolution of the western Malvinas basin.Argentina[J].AAPG Bulletin,1998;82(4):596-636.
[26]陈建平,查明,柳广弟等.准噶尔盆地西北缘斜坡区不整合面在油气成藏中的作用[J].石油大学学报(自然科学版),2000;24(4):75-79
[27]李铁军,罗晓容.碎屑岩输导层内油气运聚非均一性的定量分析[J].地质科学, 2001, 36(4): 402-413.
[28]杜春国,郝芳,邹华耀.断裂输导体系研究现状及存在的问题[J].地质科技情报,2007,26(1):51-56.
[29]郝芳,邹华耀,姜建群.油气成藏动力学及其研究进展[J].地学前沿, 2000, 7(3): 11-21.
[30] Allan U S. Model for hydrocarbon migration and entrapment within faulted structures [J]. AAPG Bulletin, 1989, 73(7):803-811.
[31]高君,吕延防,田庆丰.断裂带内部结构与油气运移及封闭[J].大庆石油学院学,2007,31(2):4-7.
[32]金博,刘震,李绪深.莺东斜坡带上第三系天然气输导系统研究[J].天然气地球科学,2004;15(5):498-502.
[33]曾溅辉、王捷等著.油气运移机理及物理模拟[M].北京:石油工业出版社,2002:137-158.
[34]姜振学,庞雄奇,曾溅辉.油气优势运移通道的类型及其物理模拟实验研究[J].地学前缘,2005,12(4):507-516.
[35] O'Brien G W., Lisk M, Duddy I R., et al. Plate convergence, foreland development and fault reactivation; primary controls on brine migration, thermal histories and trap breach in the Timor Sea, Australia[J]. Marine and Petroleum Geology, 1999, 16(6):533-560.
[36]罗群,庞雄奇,姜振学.一种有效追踪油气运移轨迹的新方法——断面优势运移通道的提出及其应用[J].地质论评, 2005, 51(2):156-162.
[37]李明诚.石油与天然气运移(第三版)[M].北京:石油工业出版社,2004.
[38]张厚福,金之钧.我国油气运移的研究现状与展望[J].石油大学学报,2000,24(4):1~4.
[39]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
[40]王捷,关德范.油气生成运移聚集模型研究[M].北京:石油工业出版社,1999.
[41]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):126~130.
[42]吴冲龙,刘海滨,毛小平,等.油气运移和聚集的人工神经网络模拟.石油实验地质[J]. 2001, 23(2):203~212.
[43]郝芳,邹华耀,方勇,等.断-压双控流体流动与油气幕式快速成藏.石油学报,2004,25(6):38-47.
[44]郝芳,邹华耀,杨旭升,等.油气幕式成藏及其驱动机制和识别标志[J].地质科学,2003,38(3):413-424.
[45]胡文瑄,金之钧,张义杰.油气幕式成藏的矿物学和地球化学记录———以准噶尔盆地西北缘油藏为例[J].石油与天然气地质,2006,27(4):442-450.
[46]陈中红,查明,金强.东营凹陷超压系统的幕式排烃[J].石油与天然气地质,2004,25(4):444-454.
[47]华保钦.构造应力场、地震泵和油气运移[J].沉积学报, 1995,13(2):77-85.
[48]孙雄,洪汉净.构造应力场对油气运移的影响[J].石油勘探与开发,1988,25(1):1-6.
[49]邱楠生,方家虎.热作为油运移动力的物理模拟实验[J].石油与天然气地质,2003,24(3):210-214.
[50]邱楠生,胡圣标,何丽娟.沉积盆地热体制研究的理论与应用[M].北京:石油工业出版社,2004:45-50.
[51]李多丽,关平.中国油气二次运移的研究现状及展望[J].北京大学学报(自然科学版),2004,40(4):658-668.
[52]邱楠生,金之钧.油气成藏的脉动式探讨[J].地学前缘,2000,7(4):561-567.
[53]赵靖舟.幕式成藏的机理和规律探讨[J].天然气工业,2006,26(3):9-11.
[54] Hillebrand T, Leythaeuser D. Reservoir geochemistry of Stock-stadt Oilfield: Compositional heterogeneities reflecting accumulation history and multiple source input[J]. Organic Geochemistry, 1992,19:119-131.
[55]张枝焕,杨永才,李伟.油藏地球化学原理及其在油气勘探与油藏评价中的应用[J].海相油气地质,2006,11(4):39-47.
[56] Christine A. H, Ryan P. R, Alan G. M, et al. Acidic and neutral polar NSO compounds in Smackover oils of different thermal maturity revealed by electrospray high field Fourier transform ion cyclotron resonance mass spectrometry[J]. Organic Geochemistry.2002, 33(7):743-759.
[57] Mohamed M. Y. B , Heinz Wilkes. The influence of facies and depositional environment on the occurrence and distribution of carbazoles and benzocarbazoles in crude oils; a case study from the Gulf of Suez, Egypt[J]. Organic Geochemistry. 2002,33(5):561-580.
[58] Bennett. B, Olsen. S.D. The influence of source depositional conditions on the hydrocarbon and nitrogen compounds in petroleum from central Montana, USA[J]. Organic Geochemistry. 2007, 38(6):935-956.
[59]李素梅,张爱云,王铁冠.朝长地区原油中的有机含氮化合物及其应用[J].现代地质,1999,13(4):444-449.
[60]王铁冠,李素梅,张爱云.利用原油含氮化合物研究油气运移[J].石油大学学报(自然科学版),2000,24(4):83-86.
[61]李素梅,庞雄奇,黎茂稳.低熟油、烃源岩中含氮化合物分布规律及其地球化学意义[J].地球化学,2002,31(1):1-6.
[62]李素梅,曾凡刚,庞雄奇.金湖凹陷西斜坡油气运移分子地球化学研究[J].沉积学报,2001,19(3):459-464.
[63]段毅,张辉,吴保祥.鄂尔多斯盆地西峰油田原油含氮化合物分布特征与油气运移[J].石油勘探与开发,2004,31(5):17-20.
[64]张敏,龙长河,张俊.塔北地区三叠系油藏原油中性含氮化合物和烷基苯酚的运移分馏作用[J].沉积学报,2001,19(1):150-155.
[65]王铁冠,朱丹,卢鸿,等.千米桥古潜山高蜡凝析油的高分子量(C35+)正烷烃分布及其烃源灶方位[J].中国科学:D辑地球科学,2003,33(5):401-410.
[66] Hillebrand T, Leythaeuser D. Reservoir geochemistry of Stock-stadt Oilfield: Compositional heterogeneities reflecting accumulation history and multiple source input[J]. Organic Geochemistry, 1992,19:119-131.
[67] Hwang R J, Moldowan J M. Oil composition variation and reservoir continuity: Unity field, Sudan[J]. Organic Geochemistry,1994,21:171-188.
[68] Later S R, Aplin A C. Reservoir geochemistry: methods, applications and opportunities.// Cubitt J M, England W A[J]. The Geochemistry of Reservoirs. Geological Society Special Publication, 1995,86:5-32.
[69] Horstad I, Larter S R, Dypvik H, et al. Degradation and maturity controls on oil field petroleum column heterogeneity in the Gullfaks Field,Norwegian North Sea[J].Organic Geochemistry,1990,16:497-510.
[70]韩立国,张枝焕,李伟.准噶尔盆地中部Ⅰ区块现今油气运移方向研究[J].地球学报. 2006, 27(4):335-340.
[71]常象春,林玉祥,郭海花,等.混合原油的地球化学特征及成藏贡献率[J].地质科技情报,2007,26(2):75-80.
[72]赵永军,李汉林.石油数学地质[M].山东东营:石油大学出版社, 1998.
[73]金之钧,张一伟,王捷.油气成藏机理与分布规律[M].北京:石油工业出版社,2003.
[74] Lee M, Aronson J L, SAVIN S M. K-Ar dating of time of gas emplacement in Rotliegendes sandstone, Netherlands[J].AAPG Bulletin,1985,69:1381-1385.
[75] Hamilton P J, Kelley S, Fallick A E. K-Ar dating of illite in hydrocarbon reservoirs[J]. Clay Minerals,1989,24:215-231.
[76]王飞宇.利用自生伊利石K-Ar定年分析烃类进入储层的时间[J].地质论评,1997,43(5):540-545.
[77]白国平.伊利石K-Ar测年在确定油气成藏期中的应用[J].石油大学学报:自然科学版,2000,24(4):100-103.
[78]陈建平,查明,周瑶琪.有机包裹体在油气运移研究中的综述[J].地质科技情报,2000,19(1):62-64.
[79]杨惠民.包裹体类型和成分特征在油气运移研究和油气储层评价中的应用—以赤水气田为例[J].海相油气地质,1997(3):16-21.
[80]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):326-331,342.
[81]张金亮.利用流体包裹体研究油藏注入史[J].西安石油学院学报:自然科学版,1998,13(4):1-4.
[82] Hao Fang,Li Sitian,Zhang Qiming,et al.Geology,compositional heterogeneities and geochemical origin of theYacheng Gas Field in the Qiongdongnan basin, South China Sea[J]. AAPG Bulletin,1998,82:1372-1384.
[83]马立祥.烃类聚集系统的层次分析思路及其应用[M].武汉:中国地质大学出版社,2001.
[84]胡朝元,孔志平,廖曦.油气成藏原理[M].北京:石油工业出版社,2002.
[85]田世澄,陈建渝,张树林,等.论成藏动力学系统[J].中国石油勘探,1996,1(2):20-25.
[86]岳伏生,郭彦如,马龙.成藏动力学系统的研究现状及发展趋向[J].地球科学进展,2003,18(1):122-126.
[87]杨瑞召,郑水吉.国外含油气系统研究现状及研究方法综述[J].国外油气勘探, 1992, 4(6): 77-84
[88]辛仁臣.油气成藏系统一概念、分类和应用[J].地球科学进展, 1997, 12(3):265-269.
[89]赵靖舟.油气系统理论及中国西北含油气系统划分[J].西安石油学院学报,1997, 12(5):14-18.
[90]伍涛,陈建渝,田世澄.济阳坳陷孤南洼陷油气成藏系统[J].石油与然气地质,1999, 20(4): 326-329.
[91]赵文智,何登发,瞿辉,等.复合含油气系统中油气运移流向研究的意义[J].石油学报, 2001, 22 (4): 7-12.
[92]柳广弟,高先志.油气运聚单元分析:油气勘探评价的有效途径[J].地质科学, 2003, 8(3): 307-314.
[93]宋国奇.含油气盆地成藏组合体理论初步探讨[J].油气地质与采收率, 2002, 9(5):4-7.
[94]蒋有录,谭丽娟,荣启宏,等.油气成藏系统的概念及其在东营凹陷博兴地区的应用[J].石油大学学报(自然科学版), 2002, 26(6):12-16.
[95]周东延,李洪辉.油气运移动态富集概念及其在塔里木台盆区油气勘探中的应用[J].石油勘探与开发, 2000, 27(1):2-6.
[96]赵万优,王振升,苏俊青.黄骅坳陷埕北断阶带油气成藏系统[J].石油勘探与开发,2008,35(1):34-39.
[97]朱振宇,裴江云,刘洪.库车坳陷侏罗系—第三系天然气成藏系统定量评价[J].大庆石油地质与开发,2005,24(1):27-30.
[98]陈中红,查明.准噶尔盆地陆梁地区复式油气成藏系统初探[J].地质科学,2006,41(3):455—464.
[99]达江,宋岩,洪峰.准噶尔盆地南缘前陆盆地油气成藏系统划分研究[J].天然气地球科学,2006,17(4):452-455.
[100]田波,冯斌,纪友亮.长堤地区油气成藏系统及成藏模式[J].油气地质与采收率, 2005,12(5):24-26.
[101]陈发亮.东濮凹陷盐湖盆地油气成藏规律及预测技术研究[D].北京:中国科学院,2006.
[102]屈红军,李文厚,苗建宇,等.东濮凹陷濮卫环洼带沙三段沉积体系及储层发育规律[J].沉积学报,2003,21(4):601-606.
[103]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.
[104]刘洛夫,妥进才,陈践发.烃源岩的研究现状[J].勘探家,1997,2(3):62-65.
[105]张志伟,张龙海.测井评价烃源岩的方法及其应用效果[J].石油勘探与开发,2000,27(3):84-87.
[106]岳炳顺,黄华,陈彬,等.东濮凹陷测井烃源岩评价方法及应用[J].石油天然气学报,2005,27(3):351-354.
[107]中原石油勘探局.东濮凹陷油气生成地球化学研究[M].北京:石油工业出版社,1991.
[108]李守军.正烷烃、姥鲛烷与植烷对沉积环境的指示意义-以山东济阳坳陷下第三系为例[J].石油大学学报(自然科学版),1999,23(5):14-16.
[109]孟仟祥,房嬛,徐永昌,等.柴达木盆地石炭系烃源岩和煤岩生物标志物特征及其地球化学意义[J].沉积学报,2001,22(4):729-736.
[110]侯读杰,王铁冠.陆相油气地球化学研究[M].武汉:中国地质大学出版社,1995.
[111]梅博文,刘希江.我国原油中异戊间二烯烃的分布及其与地质环境的关系[J].石油与天然气地质,1980,1(2):99-115.
[112]李任伟,李哲,王志珍,等.分子化石指标在中国东部盆地古环境分析中的应用[J].沉积学报,1988,6(4):108-119.
[113]翟慎德,任拥军,查明.胶莱盆地白垩系烃源岩生物标志物[J].新疆石油地质,2003,24(5):392-395.
[114]张水昌.南方海相地层中生物标志物———细菌和藻类生物的贡献[M].北京:石油工业出版社, 1993.
[115] Mackenzie A S, Hoffmann C F, Maxwell J R. Molecular parameters of maturation in the Toarcian shales, Paris Basin, France[J]. Changes in aromatic steroid hydrocarbons. Geochimica et Cosmochimica Acta, 1981, 45: 1345-1355.
[116]常振恒,陈中红,王兴武.东濮凹陷濮城地区沙一段盐湖相原油地球化学特征[J].中国石油大学学报(自然科学版),2007,31(3):22-27.
[117]常振恒,陈中红,张玉体.东濮凹陷卫城—文明寨地区原油地球化学特征[J].断块油气田, 2007,14(4):1-3.
[118] Hindle A D. Petroleum migration pathways and charge concentration; a three-dimensional model[J]. AAPG Bulletin, Sep 1997; 81: 1451 - 1481.
[119]姜素华,曾溅辉,李涛.断层面形态对中浅层石油运移影响的模拟实验研究[J].中国海洋大学学报,2005,35(2):245-248.
[2]胡朝元.生油区控制油气田分布——中国东部陆相盆地进行区域勘探的有效理论(源控论)[J].石油学报,1982,3(2).
[3]蒋有录,查明.石油天然气地质与勘探[M].北京:石油工业出版社,2006.
[4]梅玲,张枝焕,王旭东,等.渤海湾盆地南堡凹陷原油地球化学特征及油源对比[J].中国石油大学学报(自然科学版),2008,32(6):40-46.
[5]罗家群.泌阳凹陷核桃园组未熟—低熟油地球化学特征及精细油源对比[J].地质科技与情报,2008,27(5):77-86.
[6]徐冠军,王培荣,刘建宪,等.烃源岩中C5—C13分析新方法及在油源对比中的应用[J]. 2008,35(6):710-714.
[7]申家年,邓冰,卢双舫.齐家古龙凹陷凝析油气的地球化学剖析与油源对比及其启示[J].地球化学,2007,36(6):633-637.
[8]罗宪婴,赵宗举,孟元林.正构烷烃奇偶优势在油源对比中的应用———以塔里木盆地下古生界为例[J].石油实验地质,2007,29(1):74-77.
[9]揭异新,袁月琴,王斌.海拉尔盆地乌尔逊—贝尔凹陷白垩系原油地球化学特征及油源对比[J].石油实验地质,2007,29(1):82-87.
[10]郭艳琴,李文厚,陈全红,等.鄂尔多斯盆地安塞-富县地区延长组-延安组原油地球化学特征及油源对比[J].石油与天然气地质,2006,27(2):218-224.
[11]赵鹏,陈世加,李丽萍,等.酒东盆地营尔凹陷下白垩统油源对比[J].天然气地球科学,2006,17(2):192-195.
[12]马安来,金之钧,王毅.塔里木盆地台盆区海相油源对比存在的问题及进一步工作方向[J].石油与天然气地质,2006,27(3):356-362.
[13]郑冰,高仁祥.塔里木盆地原油碳硫同位素特征及油源对比[J].石油实验地质,2006,28(3):281-285.
[14]严永新,袁光喜,马蓉芳,等.焉耆盆地原油物理化学特征及油源对比研究[J].石油实验地质,2006,28(5):467-471.
[15]彼得斯K E,莫尔多万J M.生物标记化合物指南———古代沉积物和石油中分子化石的解释[M].姜乃煌,张永昌,林永汉,等译.北京:石油工业出版社, 2001.
[16]刘华,蒋有录,陈涛.东营凹陷辛东地区有效输导体系及成藏模式[J].中国石油大学学报(自然科学版). 2008,32(4):13-18.
[17]吕双兵,高先志,何万军,等.阿克库勒凸起输导体系对油气分布的控制效应[J].西南石油大学学报. 2007,29(4):49-52.
[18]卓勤功,宁方兴,荣娜.断陷盆地输导体系类型及控藏机制[J].地质论评. 2005,51(4):416-422.
[19]杜学斌,解习农,任建业.济阳坳陷中生界古潜山油藏输导体系及成藏模式[J].地质科技情报. 2005,24(2):22-26.
[20]冷济高,解习农,刘晓峰.秦皇岛32-6地区油气运移输导体系及成藏模式研究[J].西安石油大学学报(自然科学版). 2008,23(3):22-26.
[21]尹微,樊太亮,曾清波.塔里木盆地巴楚地区输导体系类型及油气成藏[J].石油实验地质. 2006,28(4):340-344.:
[22]魏福军,高志前,樊太亮.塔里木盆地塔中地区输导体系及成藏效应[J].石油与天然气地质.2007,28(2):266-273.
[23]龚再升,杨甲明.油气成藏动力学及油气运移模型[J].中国海上油气(地质), 1999, 13(4): 235-239.
[24]谢泰俊,潘祖荫,杨学昌.油气运移动力及通道体系.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997:385-405
[25] Galeazzi J S.Structral and stratigraphic evolution of the western Malvinas basin.Argentina[J].AAPG Bulletin,1998;82(4):596-636.
[26]陈建平,查明,柳广弟等.准噶尔盆地西北缘斜坡区不整合面在油气成藏中的作用[J].石油大学学报(自然科学版),2000;24(4):75-79
[27]李铁军,罗晓容.碎屑岩输导层内油气运聚非均一性的定量分析[J].地质科学, 2001, 36(4): 402-413.
[28]杜春国,郝芳,邹华耀.断裂输导体系研究现状及存在的问题[J].地质科技情报,2007,26(1):51-56.
[29]郝芳,邹华耀,姜建群.油气成藏动力学及其研究进展[J].地学前沿, 2000, 7(3): 11-21.
[30] Allan U S. Model for hydrocarbon migration and entrapment within faulted structures [J]. AAPG Bulletin, 1989, 73(7):803-811.
[31]高君,吕延防,田庆丰.断裂带内部结构与油气运移及封闭[J].大庆石油学院学,2007,31(2):4-7.
[32]金博,刘震,李绪深.莺东斜坡带上第三系天然气输导系统研究[J].天然气地球科学,2004;15(5):498-502.
[33]曾溅辉、王捷等著.油气运移机理及物理模拟[M].北京:石油工业出版社,2002:137-158.
[34]姜振学,庞雄奇,曾溅辉.油气优势运移通道的类型及其物理模拟实验研究[J].地学前缘,2005,12(4):507-516.
[35] O'Brien G W., Lisk M, Duddy I R., et al. Plate convergence, foreland development and fault reactivation; primary controls on brine migration, thermal histories and trap breach in the Timor Sea, Australia[J]. Marine and Petroleum Geology, 1999, 16(6):533-560.
[36]罗群,庞雄奇,姜振学.一种有效追踪油气运移轨迹的新方法——断面优势运移通道的提出及其应用[J].地质论评, 2005, 51(2):156-162.
[37]李明诚.石油与天然气运移(第三版)[M].北京:石油工业出版社,2004.
[38]张厚福,金之钧.我国油气运移的研究现状与展望[J].石油大学学报,2000,24(4):1~4.
[39]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
[40]王捷,关德范.油气生成运移聚集模型研究[M].北京:石油工业出版社,1999.
[41]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):126~130.
[42]吴冲龙,刘海滨,毛小平,等.油气运移和聚集的人工神经网络模拟.石油实验地质[J]. 2001, 23(2):203~212.
[43]郝芳,邹华耀,方勇,等.断-压双控流体流动与油气幕式快速成藏.石油学报,2004,25(6):38-47.
[44]郝芳,邹华耀,杨旭升,等.油气幕式成藏及其驱动机制和识别标志[J].地质科学,2003,38(3):413-424.
[45]胡文瑄,金之钧,张义杰.油气幕式成藏的矿物学和地球化学记录———以准噶尔盆地西北缘油藏为例[J].石油与天然气地质,2006,27(4):442-450.
[46]陈中红,查明,金强.东营凹陷超压系统的幕式排烃[J].石油与天然气地质,2004,25(4):444-454.
[47]华保钦.构造应力场、地震泵和油气运移[J].沉积学报, 1995,13(2):77-85.
[48]孙雄,洪汉净.构造应力场对油气运移的影响[J].石油勘探与开发,1988,25(1):1-6.
[49]邱楠生,方家虎.热作为油运移动力的物理模拟实验[J].石油与天然气地质,2003,24(3):210-214.
[50]邱楠生,胡圣标,何丽娟.沉积盆地热体制研究的理论与应用[M].北京:石油工业出版社,2004:45-50.
[51]李多丽,关平.中国油气二次运移的研究现状及展望[J].北京大学学报(自然科学版),2004,40(4):658-668.
[52]邱楠生,金之钧.油气成藏的脉动式探讨[J].地学前缘,2000,7(4):561-567.
[53]赵靖舟.幕式成藏的机理和规律探讨[J].天然气工业,2006,26(3):9-11.
[54] Hillebrand T, Leythaeuser D. Reservoir geochemistry of Stock-stadt Oilfield: Compositional heterogeneities reflecting accumulation history and multiple source input[J]. Organic Geochemistry, 1992,19:119-131.
[55]张枝焕,杨永才,李伟.油藏地球化学原理及其在油气勘探与油藏评价中的应用[J].海相油气地质,2006,11(4):39-47.
[56] Christine A. H, Ryan P. R, Alan G. M, et al. Acidic and neutral polar NSO compounds in Smackover oils of different thermal maturity revealed by electrospray high field Fourier transform ion cyclotron resonance mass spectrometry[J]. Organic Geochemistry.2002, 33(7):743-759.
[57] Mohamed M. Y. B , Heinz Wilkes. The influence of facies and depositional environment on the occurrence and distribution of carbazoles and benzocarbazoles in crude oils; a case study from the Gulf of Suez, Egypt[J]. Organic Geochemistry. 2002,33(5):561-580.
[58] Bennett. B, Olsen. S.D. The influence of source depositional conditions on the hydrocarbon and nitrogen compounds in petroleum from central Montana, USA[J]. Organic Geochemistry. 2007, 38(6):935-956.
[59]李素梅,张爱云,王铁冠.朝长地区原油中的有机含氮化合物及其应用[J].现代地质,1999,13(4):444-449.
[60]王铁冠,李素梅,张爱云.利用原油含氮化合物研究油气运移[J].石油大学学报(自然科学版),2000,24(4):83-86.
[61]李素梅,庞雄奇,黎茂稳.低熟油、烃源岩中含氮化合物分布规律及其地球化学意义[J].地球化学,2002,31(1):1-6.
[62]李素梅,曾凡刚,庞雄奇.金湖凹陷西斜坡油气运移分子地球化学研究[J].沉积学报,2001,19(3):459-464.
[63]段毅,张辉,吴保祥.鄂尔多斯盆地西峰油田原油含氮化合物分布特征与油气运移[J].石油勘探与开发,2004,31(5):17-20.
[64]张敏,龙长河,张俊.塔北地区三叠系油藏原油中性含氮化合物和烷基苯酚的运移分馏作用[J].沉积学报,2001,19(1):150-155.
[65]王铁冠,朱丹,卢鸿,等.千米桥古潜山高蜡凝析油的高分子量(C35+)正烷烃分布及其烃源灶方位[J].中国科学:D辑地球科学,2003,33(5):401-410.
[66] Hillebrand T, Leythaeuser D. Reservoir geochemistry of Stock-stadt Oilfield: Compositional heterogeneities reflecting accumulation history and multiple source input[J]. Organic Geochemistry, 1992,19:119-131.
[67] Hwang R J, Moldowan J M. Oil composition variation and reservoir continuity: Unity field, Sudan[J]. Organic Geochemistry,1994,21:171-188.
[68] Later S R, Aplin A C. Reservoir geochemistry: methods, applications and opportunities.// Cubitt J M, England W A[J]. The Geochemistry of Reservoirs. Geological Society Special Publication, 1995,86:5-32.
[69] Horstad I, Larter S R, Dypvik H, et al. Degradation and maturity controls on oil field petroleum column heterogeneity in the Gullfaks Field,Norwegian North Sea[J].Organic Geochemistry,1990,16:497-510.
[70]韩立国,张枝焕,李伟.准噶尔盆地中部Ⅰ区块现今油气运移方向研究[J].地球学报. 2006, 27(4):335-340.
[71]常象春,林玉祥,郭海花,等.混合原油的地球化学特征及成藏贡献率[J].地质科技情报,2007,26(2):75-80.
[72]赵永军,李汉林.石油数学地质[M].山东东营:石油大学出版社, 1998.
[73]金之钧,张一伟,王捷.油气成藏机理与分布规律[M].北京:石油工业出版社,2003.
[74] Lee M, Aronson J L, SAVIN S M. K-Ar dating of time of gas emplacement in Rotliegendes sandstone, Netherlands[J].AAPG Bulletin,1985,69:1381-1385.
[75] Hamilton P J, Kelley S, Fallick A E. K-Ar dating of illite in hydrocarbon reservoirs[J]. Clay Minerals,1989,24:215-231.
[76]王飞宇.利用自生伊利石K-Ar定年分析烃类进入储层的时间[J].地质论评,1997,43(5):540-545.
[77]白国平.伊利石K-Ar测年在确定油气成藏期中的应用[J].石油大学学报:自然科学版,2000,24(4):100-103.
[78]陈建平,查明,周瑶琪.有机包裹体在油气运移研究中的综述[J].地质科技情报,2000,19(1):62-64.
[79]杨惠民.包裹体类型和成分特征在油气运移研究和油气储层评价中的应用—以赤水气田为例[J].海相油气地质,1997(3):16-21.
[80]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):326-331,342.
[81]张金亮.利用流体包裹体研究油藏注入史[J].西安石油学院学报:自然科学版,1998,13(4):1-4.
[82] Hao Fang,Li Sitian,Zhang Qiming,et al.Geology,compositional heterogeneities and geochemical origin of theYacheng Gas Field in the Qiongdongnan basin, South China Sea[J]. AAPG Bulletin,1998,82:1372-1384.
[83]马立祥.烃类聚集系统的层次分析思路及其应用[M].武汉:中国地质大学出版社,2001.
[84]胡朝元,孔志平,廖曦.油气成藏原理[M].北京:石油工业出版社,2002.
[85]田世澄,陈建渝,张树林,等.论成藏动力学系统[J].中国石油勘探,1996,1(2):20-25.
[86]岳伏生,郭彦如,马龙.成藏动力学系统的研究现状及发展趋向[J].地球科学进展,2003,18(1):122-126.
[87]杨瑞召,郑水吉.国外含油气系统研究现状及研究方法综述[J].国外油气勘探, 1992, 4(6): 77-84
[88]辛仁臣.油气成藏系统一概念、分类和应用[J].地球科学进展, 1997, 12(3):265-269.
[89]赵靖舟.油气系统理论及中国西北含油气系统划分[J].西安石油学院学报,1997, 12(5):14-18.
[90]伍涛,陈建渝,田世澄.济阳坳陷孤南洼陷油气成藏系统[J].石油与然气地质,1999, 20(4): 326-329.
[91]赵文智,何登发,瞿辉,等.复合含油气系统中油气运移流向研究的意义[J].石油学报, 2001, 22 (4): 7-12.
[92]柳广弟,高先志.油气运聚单元分析:油气勘探评价的有效途径[J].地质科学, 2003, 8(3): 307-314.
[93]宋国奇.含油气盆地成藏组合体理论初步探讨[J].油气地质与采收率, 2002, 9(5):4-7.
[94]蒋有录,谭丽娟,荣启宏,等.油气成藏系统的概念及其在东营凹陷博兴地区的应用[J].石油大学学报(自然科学版), 2002, 26(6):12-16.
[95]周东延,李洪辉.油气运移动态富集概念及其在塔里木台盆区油气勘探中的应用[J].石油勘探与开发, 2000, 27(1):2-6.
[96]赵万优,王振升,苏俊青.黄骅坳陷埕北断阶带油气成藏系统[J].石油勘探与开发,2008,35(1):34-39.
[97]朱振宇,裴江云,刘洪.库车坳陷侏罗系—第三系天然气成藏系统定量评价[J].大庆石油地质与开发,2005,24(1):27-30.
[98]陈中红,查明.准噶尔盆地陆梁地区复式油气成藏系统初探[J].地质科学,2006,41(3):455—464.
[99]达江,宋岩,洪峰.准噶尔盆地南缘前陆盆地油气成藏系统划分研究[J].天然气地球科学,2006,17(4):452-455.
[100]田波,冯斌,纪友亮.长堤地区油气成藏系统及成藏模式[J].油气地质与采收率, 2005,12(5):24-26.
[101]陈发亮.东濮凹陷盐湖盆地油气成藏规律及预测技术研究[D].北京:中国科学院,2006.
[102]屈红军,李文厚,苗建宇,等.东濮凹陷濮卫环洼带沙三段沉积体系及储层发育规律[J].沉积学报,2003,21(4):601-606.
[103]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.
[104]刘洛夫,妥进才,陈践发.烃源岩的研究现状[J].勘探家,1997,2(3):62-65.
[105]张志伟,张龙海.测井评价烃源岩的方法及其应用效果[J].石油勘探与开发,2000,27(3):84-87.
[106]岳炳顺,黄华,陈彬,等.东濮凹陷测井烃源岩评价方法及应用[J].石油天然气学报,2005,27(3):351-354.
[107]中原石油勘探局.东濮凹陷油气生成地球化学研究[M].北京:石油工业出版社,1991.
[108]李守军.正烷烃、姥鲛烷与植烷对沉积环境的指示意义-以山东济阳坳陷下第三系为例[J].石油大学学报(自然科学版),1999,23(5):14-16.
[109]孟仟祥,房嬛,徐永昌,等.柴达木盆地石炭系烃源岩和煤岩生物标志物特征及其地球化学意义[J].沉积学报,2001,22(4):729-736.
[110]侯读杰,王铁冠.陆相油气地球化学研究[M].武汉:中国地质大学出版社,1995.
[111]梅博文,刘希江.我国原油中异戊间二烯烃的分布及其与地质环境的关系[J].石油与天然气地质,1980,1(2):99-115.
[112]李任伟,李哲,王志珍,等.分子化石指标在中国东部盆地古环境分析中的应用[J].沉积学报,1988,6(4):108-119.
[113]翟慎德,任拥军,查明.胶莱盆地白垩系烃源岩生物标志物[J].新疆石油地质,2003,24(5):392-395.
[114]张水昌.南方海相地层中生物标志物———细菌和藻类生物的贡献[M].北京:石油工业出版社, 1993.
[115] Mackenzie A S, Hoffmann C F, Maxwell J R. Molecular parameters of maturation in the Toarcian shales, Paris Basin, France[J]. Changes in aromatic steroid hydrocarbons. Geochimica et Cosmochimica Acta, 1981, 45: 1345-1355.
[116]常振恒,陈中红,王兴武.东濮凹陷濮城地区沙一段盐湖相原油地球化学特征[J].中国石油大学学报(自然科学版),2007,31(3):22-27.
[117]常振恒,陈中红,张玉体.东濮凹陷卫城—文明寨地区原油地球化学特征[J].断块油气田, 2007,14(4):1-3.
[118] Hindle A D. Petroleum migration pathways and charge concentration; a three-dimensional model[J]. AAPG Bulletin, Sep 1997; 81: 1451 - 1481.
[119]姜素华,曾溅辉,李涛.断层面形态对中浅层石油运移影响的模拟实验研究[J].中国海洋大学学报,2005,35(2):245-248.
© 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 |