松辽盆地肇41-州58区块葡萄花油层油成藏规律研究
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摘要
本文介绍了松辽盆地肇41—州58区块葡萄花油层的区域地质概况、油藏类型及油气分布特征,通过分析研究区的源岩、储层以及油源断裂等成藏条件,总结出本研究区油气成藏的控制因素。指出断层、砂体控制了圈闭的形成和油气运移状态,为本区油气成藏模式的主控因素。通过对肇41-州58区块葡萄花油层沉积、源岩、盖层、断层、运移路径和圈闭条件与油气藏的叠合的研究,分析了肇41-州58区块葡萄花油层油气成藏与分布的控制因素主要为下伏有无油源供给,有无源断裂发育,有无砂体发育,并且断裂密集带内的地垒、断阶构造有利油聚集成藏。在典型油气成藏或井解剖的基础上,总结出研究区有3种成藏模式,即源内垂向运移成藏模式,源内先垂向再侧向运移成藏模式,源外垂向运移成藏模式。
This article describes the regional geology state, reservoir types and distribution characteristics of oil and gas of P oil layer in Zhao 41-58 block in Songliao basin. Through analyzing the accumulation condition such as the source rock, reservoir and oil source fault of the study area, summarized the controlling factors of hydrocarbon accumulation in the study area. Pointed out that the trap formation and the oil and gas migration state are controlled by the fault and sand, and the fault and sand are the main control factors in this zone. Through the study of superimposed with source rock, seal rock, faults, migration paths, trap conditions and reservoir, we have analyzed whether the supply of oil sources in the underlying ,whether the growth of the oil source fault, whether the growth of sand, they are the main controlling factors of hydrocarbon accumulation and distribution of P oil layer in Zhao 41-58 block, and the horst in the fault condensed belts and fault stage construction are benefit for the oil accumulation. Based on the Dissection of the typical oil and gas reservoirs or wells, concluded that there are 3 kinds of accumulation mode in study area, namely, the vertical migration and accumulation mode within the source, the first vertical and then lateral migration and accumulation mode within the source, the vertical migration and accumulation mode outside the source.
This article describes the regional geology state, reservoir types and distribution characteristics of oil and gas of P oil layer in Zhao 41-58 block in Songliao basin. Through analyzing the accumulation condition such as the source rock, reservoir and oil source fault of the study area, summarized the controlling factors of hydrocarbon accumulation in the study area. Pointed out that the trap formation and the oil and gas migration state are controlled by the fault and sand, and the fault and sand are the main control factors in this zone. Through the study of superimposed with source rock, seal rock, faults, migration paths, trap conditions and reservoir, we have analyzed whether the supply of oil sources in the underlying ,whether the growth of the oil source fault, whether the growth of sand, they are the main controlling factors of hydrocarbon accumulation and distribution of P oil layer in Zhao 41-58 block, and the horst in the fault condensed belts and fault stage construction are benefit for the oil accumulation. Based on the Dissection of the typical oil and gas reservoirs or wells, concluded that there are 3 kinds of accumulation mode in study area, namely, the vertical migration and accumulation mode within the source, the first vertical and then lateral migration and accumulation mode within the source, the vertical migration and accumulation mode outside the source.
引文
[1]胡朝元,廖曦.成油系统概念在中国的提出和应用[J].石油学报,1996,17(1):10-16.
[2]崔可.源控论的广泛适用性——从油气运移距离频率直方图上解读[J].海相油气地质,2003,8(1-2):108.
[3] Dow W.G Application of oil correlation and source rock data to exploration in Willinston basin[J].AAPG.1972,12(6):56-615.
[4]程克明,王铁冠,钟宁宁等.烃源岩地球化学[M].北京:科学出版社,1992,12-18.
[5]林畅松,潘元林,肖建新,等.“构造坡折带”—断陷盆地层序分析和油气预测的重要概念[J].地球科学,2000,25(3):260-26.
[6]李树同,王多云,王彬,等.坳陷型湖盆缓坡边缘沉积坡折带的识别——以鄂尔多斯盆地三叠纪延长期沉积坡折带为例[J].天然气地球科学,2008,19(1) : 83-88.
[7]陈发景,田世澄.压实与油气运移[M].武汉:中国地质大学出版社,1989,156~160.
[8] Hindle A D. Petroleum migration pathways and charge concentration: a three Dimensional Model [J]. AAPG Bulletin, 1997, 81: 1451~1481.
[9]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.
[10]胡望水,王燮培.松辽盆地北部变换构造及其石油地质意义[J].石油与天然气地质,1994,15(2):164-172.
[11]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[J].石油学报,1982,12(4):9-13.
[12] Antonellini M,Aydin A.Efect of Faulting on Fluid Flaw in Porous Sandstones Petrophysical Properties[J].AAPG,1994,78(2):355-377.
[13]蔡希源,陈章明,王玉华等.松辽盆地两江地区石油地质分析.北京:石油工业出版社,1999,117-141
[14]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律.北京:石油工业出版社,1997,104-180.
[15]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.
[16]卢双舫,薛海涛,钟宁宁.地史过程中烃源岩有机质丰度和生烃潜力变化的模拟计算[J].地质论评,2003,49(3):292-296.
[17]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.北京:石油工业出版社,2002,10-80.
[18]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.北京:地质出版社,1993.
[19]中国石油天然气总公司勘探局编.油气资源评价技术.石油工业出版社,1999:35-48.
[20]Vail P R, AudeIIlard F, BowmanSA, et al. The stratigraphic signatures of tectonics, eustasy and sedimentology: an overview [A]. In:Einsele G, RickenW, Seilacher A. Cycles and events instratigraphy[C]. Berlin: Springer-Verlag, 1991, 53:617-659.
[21]林景晔,门广田,黄薇.砂岩透镜体岩性油气藏成藏机理与成藏模式探讨[J].大庆石油地质与开发,2004,23(2):5-7.
[22]樊太亮,等.层序地层学体制中的陆相储层发育规律[J].地学前缘,2000,7(4):32-36.
[23]顾家裕,张兴阳.陆相层序地层学进展与在油气勘探开发中的应用[J].石油与天然气地质, 2004, 25 (5):484-485.
[24]于兴河.碎屑岩系油气储层沉积学[M].北京:石油工业出版社,2008,85-86.
[25]庞雄奇,陈冬霞,李丕龙,等.砂岩透镜体成藏门限及控油气作用机理[J].石油学报,2003,24(3):38-41.
[26]刘志宏,任延广,李春柏,等.海拉尔盆地乌尔逊一贝尔凹陷的构造特征及其对油气成藏的影响[J].大地构造与成矿学,2007,31(2):151-156.
[27] Richard P. Experiments on faulting in a two-layer cover sequence overlying a reactivated basement fault with oblique-slip[J]. Journal of Structural Geology,1991,13(4):459-469.
[28] Yossi Mart,Olivier Dauteuil. Analogue Experiments of Propagation of Oblique Rifts[J]. Tectonophysics,2000,316:121-132.
[29]Barclay S A, Worden R H, Parnell J, et al. Assessment of fluid inclusions: an example from the Magnus oil field, North Sea[J]. AAPG Bulletin, 2000,84(4):489-504
[30]吕延防,姜贵周.延吉盆地断裂特征及对油气分布的控制[J].断块油气田,1997,4(2):1-4.
[31] Van der Zee W,Urai J L,Wibberley C,et al. The Evolution of Fault Zones in Layered Sequences: American Geophysical Union Abstracts FallMeeting[J],1999,80:740.
[32] Shipton, Cowie. A Conceptual Model for the Origin of Fault Damage Zone Structures in High-porosity Sandston [J]. Journal of Structural Geology, 2003, 25: 333~344.
[33] Childs C,Walsh J J,Watterson J. Complexity in Fault Zone Structure and Implications for Fault Seal Prediction. In:Moller-Pedersen P, Koestler A G (Eds), Hydrocarbon Seals:Importance for Exploration and Production, Norwegian Petroleum Society.1998,7:61-72.
[34]付广,黄劲松,康德江,等.源断裂在油气成藏与分布中的作用研究——以贝尔凹陷布达特群潜山为例[J].石油物探,2006,45(5):459-463.
[35]徐忠美,龙胜祥.叠合盆地油气成藏体系研究方法探讨[J].重庆科技学院学报(自然科学版),2010,12(6):9-12.
[36]付广,吕延防,于丹.我国不同类型盆地高效大中型气田形成的主控因素[J].地球科学-中国地质大学学报,2007,32(1):82-88.
[37]梁书义,刘克奇,蔡忠贤.油气成藏体系及油气输导子体系研究[J].石油实验地质,2005,27(4):327-330.
[38]Allan U S. Model for hydrocarbon migration and entrapment within faulted structures. AAPG, 1989, 73(7): 803~811.
[39]林畅松.沉积盆地的层序和沉积充填结构及过程响应[J].沉积学报,2009,27(5):849-861.
[40]Miall A D. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis and Petroleum Geology[M]. Berlin, Heidelberg. New York: Spinger-Verlag. 1996:57-98.
[41]王宝清,徐文发,徐站立,等.三肇地区扶余和杨大城子油层储集岩的成岩作用[J].石油与天然气地质,2001,22(1):82-87.
[42]张革,林景晔,杨庆杰等.松辽盆地西部扶杨油层成藏条件和勘探潜力[J].大庆石油地质与开发,2002,21(5):5-7.
[43]付晓飞,王朋岩,吕延防等.松辽盆地西部斜坡构造特征及对油气成藏的控制[J].地质科学,2007,42(2):209-222.
[44]金之钧.中国典型叠合盆地油气形成富集与分布预测[M].北京:科学出版社,2007,236-237.
[45]叶徳燎.松了盆地东南隆起区下白垩统层序地层格架及油气成藏规律[J].地质科学,2005,40(2):227-236.
[2]崔可.源控论的广泛适用性——从油气运移距离频率直方图上解读[J].海相油气地质,2003,8(1-2):108.
[3] Dow W.G Application of oil correlation and source rock data to exploration in Willinston basin[J].AAPG.1972,12(6):56-615.
[4]程克明,王铁冠,钟宁宁等.烃源岩地球化学[M].北京:科学出版社,1992,12-18.
[5]林畅松,潘元林,肖建新,等.“构造坡折带”—断陷盆地层序分析和油气预测的重要概念[J].地球科学,2000,25(3):260-26.
[6]李树同,王多云,王彬,等.坳陷型湖盆缓坡边缘沉积坡折带的识别——以鄂尔多斯盆地三叠纪延长期沉积坡折带为例[J].天然气地球科学,2008,19(1) : 83-88.
[7]陈发景,田世澄.压实与油气运移[M].武汉:中国地质大学出版社,1989,156~160.
[8] Hindle A D. Petroleum migration pathways and charge concentration: a three Dimensional Model [J]. AAPG Bulletin, 1997, 81: 1451~1481.
[9]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.
[10]胡望水,王燮培.松辽盆地北部变换构造及其石油地质意义[J].石油与天然气地质,1994,15(2):164-172.
[11]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[J].石油学报,1982,12(4):9-13.
[12] Antonellini M,Aydin A.Efect of Faulting on Fluid Flaw in Porous Sandstones Petrophysical Properties[J].AAPG,1994,78(2):355-377.
[13]蔡希源,陈章明,王玉华等.松辽盆地两江地区石油地质分析.北京:石油工业出版社,1999,117-141
[14]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律.北京:石油工业出版社,1997,104-180.
[15]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.
[16]卢双舫,薛海涛,钟宁宁.地史过程中烃源岩有机质丰度和生烃潜力变化的模拟计算[J].地质论评,2003,49(3):292-296.
[17]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.北京:石油工业出版社,2002,10-80.
[18]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.北京:地质出版社,1993.
[19]中国石油天然气总公司勘探局编.油气资源评价技术.石油工业出版社,1999:35-48.
[20]Vail P R, AudeIIlard F, BowmanSA, et al. The stratigraphic signatures of tectonics, eustasy and sedimentology: an overview [A]. In:Einsele G, RickenW, Seilacher A. Cycles and events instratigraphy[C]. Berlin: Springer-Verlag, 1991, 53:617-659.
[21]林景晔,门广田,黄薇.砂岩透镜体岩性油气藏成藏机理与成藏模式探讨[J].大庆石油地质与开发,2004,23(2):5-7.
[22]樊太亮,等.层序地层学体制中的陆相储层发育规律[J].地学前缘,2000,7(4):32-36.
[23]顾家裕,张兴阳.陆相层序地层学进展与在油气勘探开发中的应用[J].石油与天然气地质, 2004, 25 (5):484-485.
[24]于兴河.碎屑岩系油气储层沉积学[M].北京:石油工业出版社,2008,85-86.
[25]庞雄奇,陈冬霞,李丕龙,等.砂岩透镜体成藏门限及控油气作用机理[J].石油学报,2003,24(3):38-41.
[26]刘志宏,任延广,李春柏,等.海拉尔盆地乌尔逊一贝尔凹陷的构造特征及其对油气成藏的影响[J].大地构造与成矿学,2007,31(2):151-156.
[27] Richard P. Experiments on faulting in a two-layer cover sequence overlying a reactivated basement fault with oblique-slip[J]. Journal of Structural Geology,1991,13(4):459-469.
[28] Yossi Mart,Olivier Dauteuil. Analogue Experiments of Propagation of Oblique Rifts[J]. Tectonophysics,2000,316:121-132.
[29]Barclay S A, Worden R H, Parnell J, et al. Assessment of fluid inclusions: an example from the Magnus oil field, North Sea[J]. AAPG Bulletin, 2000,84(4):489-504
[30]吕延防,姜贵周.延吉盆地断裂特征及对油气分布的控制[J].断块油气田,1997,4(2):1-4.
[31] Van der Zee W,Urai J L,Wibberley C,et al. The Evolution of Fault Zones in Layered Sequences: American Geophysical Union Abstracts FallMeeting[J],1999,80:740.
[32] Shipton, Cowie. A Conceptual Model for the Origin of Fault Damage Zone Structures in High-porosity Sandston [J]. Journal of Structural Geology, 2003, 25: 333~344.
[33] Childs C,Walsh J J,Watterson J. Complexity in Fault Zone Structure and Implications for Fault Seal Prediction. In:Moller-Pedersen P, Koestler A G (Eds), Hydrocarbon Seals:Importance for Exploration and Production, Norwegian Petroleum Society.1998,7:61-72.
[34]付广,黄劲松,康德江,等.源断裂在油气成藏与分布中的作用研究——以贝尔凹陷布达特群潜山为例[J].石油物探,2006,45(5):459-463.
[35]徐忠美,龙胜祥.叠合盆地油气成藏体系研究方法探讨[J].重庆科技学院学报(自然科学版),2010,12(6):9-12.
[36]付广,吕延防,于丹.我国不同类型盆地高效大中型气田形成的主控因素[J].地球科学-中国地质大学学报,2007,32(1):82-88.
[37]梁书义,刘克奇,蔡忠贤.油气成藏体系及油气输导子体系研究[J].石油实验地质,2005,27(4):327-330.
[38]Allan U S. Model for hydrocarbon migration and entrapment within faulted structures. AAPG, 1989, 73(7): 803~811.
[39]林畅松.沉积盆地的层序和沉积充填结构及过程响应[J].沉积学报,2009,27(5):849-861.
[40]Miall A D. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis and Petroleum Geology[M]. Berlin, Heidelberg. New York: Spinger-Verlag. 1996:57-98.
[41]王宝清,徐文发,徐站立,等.三肇地区扶余和杨大城子油层储集岩的成岩作用[J].石油与天然气地质,2001,22(1):82-87.
[42]张革,林景晔,杨庆杰等.松辽盆地西部扶杨油层成藏条件和勘探潜力[J].大庆石油地质与开发,2002,21(5):5-7.
[43]付晓飞,王朋岩,吕延防等.松辽盆地西部斜坡构造特征及对油气成藏的控制[J].地质科学,2007,42(2):209-222.
[44]金之钧.中国典型叠合盆地油气形成富集与分布预测[M].北京:科学出版社,2007,236-237.
[45]叶徳燎.松了盆地东南隆起区下白垩统层序地层格架及油气成藏规律[J].地质科学,2005,40(2):227-236.