三肇凹陷断层垂向分段生长与扶杨油层油源断层的厘定
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
野外观察、典型地震解剖和物理模拟证实,只要岩石存在能干性差,断层具有典型垂向分段生长特征.岩石能干性差异决定断层演化历经3个阶段:下部断层形成、断裂上下分段和贯通性断裂形成.以三肇凹陷为例,应用岩石力学特征和断层相关褶皱理论,证实扶杨油层砂岩层段普遍形成断裂,青一段泥岩阻止下部断层向上传播,从而形成断层垂向分段生长现象.结合油藏精细解剖表明,三肇凹陷扶杨油层"倒灌"运移的主要油源断层是成藏期活动、沟通源储且垂向分段生长的断裂.
It is proved that fault possesses a typical characteristic of vertical segmentation growth if there is competent difference by field observation,typical seismic analysis and physical modeling.Fault evolution can be divided into three stages by competent difference:formation of lower fault,segmentation of upper and lower faults and formation of throughgoing fault.Taking Sanzhao depression as an example,rock mechanical properties and fault related fold theories prove that there widely exist faults in sandstone layer of Fuyang oil layer,whose propagation is stopped by mudstone in Qingshankou FormationⅠ member,leading to the vertical segmentation growth of fault.Combining fine reservoir anatomy,it can be concluded that the main oil source faults of the"reversed"migration in Fuyang oil layer must have been active in hydrocarbon migration and accumulation period,connecting oil source and reservoirs,and featuring vertical segmentation growth in Sanzhao depression.
引文
Chi,Y.L.,Xiao,D.M.,Yin,J.Y.,2000.The Injection Pattern of Oil and Gas Migration and Accumulation in theSanzhao Area of Songliao Basin.Acta Geologica Sinica,74(4):371-377(in Chinese with English abstract).
    Chi,Y.L.,Yun,J.B.,Meng,Q.A.,et al.,2002.Deep Structure and Dynamics and Its Relation to Hydrocarbon Accumulation of Songliao Basin.Petroleum IndustryPress,Beijing,10-80(in Chinese).
    Egholm,D.L.,Clausen,O.R.,Sandiford,M.,et al.,2008.The Mechanics of Clay Smearing along Faults.Geology,36(10):787-790.doi:10.1130/G24975A.1
    Faerseth,R.B.,2006.Shale Smear along Large Faults:Continuity of Smear and the Fault Seal Capacity.Journalof the Geological Society,163(5):741-751.doi:10.1144/0016-76492005-162
    Faerseth,R.B.,Johnsen,E.,Sperrevik,S.,2007.Methodology for Risking Fault Seal Capacity:Implications ofFault Zone Architecture.AAPG Bulletin,91(9):1231-1246.doi:10.1306/03080706051
    Fu,G.,Wang,Y.G.,2008.Oil Migration TransportingPathways in Nose Structure Region Outside Oil SourceArea and Their Controlling on Oil Accumulation—Example of Shangjia Region in the Songliao Basin.Geological Review,54(5):646-652(in Chinese with English abstract).
    Fu,G.,Wang,Y.G.,Yuan,D.W.,2010.Source Faults ofFuyang Oil Layer in Sanzhao Depression and Its Controlto Oil Accumulation.Acta Petrolei Sinica,31(5):762-766,773(in Chinese with English abstract).
    Fu,X.F.,Guo,X.,Zhu,L.X.,et al.,2012.Formation andEvolution of Clay Smear and Hydrocarbon Migrationand Sealing.Journal of China University of Mining&Technology,41(1):52-63(in Chinese with Englishabstract).
    Fu,X.F.,Chen,Z.,Yan,B.Q.,et al.,2013.Analysis ofMain Controlling Factors for Hydrocarbon Accumulation in Central Rift Zones of the Hailar-Tamtsag BasinUsing a Fault-Caprock Dual Control Mode.Science inChina(Series D),56(8):1357-1370.doi:10.1007/s11430-013-4622-5
    Fu,X.F.,Ping,G.D.,Fan,R.D.,et al.,2009.Research onMigration and Accumulation Mechanism of Hydrocarbon“Reversed Migration”in Fuyu and YangdachengziFormation in Sanzhao Depression.Acta Sedimentologica Sinica,27(3):558-566(in Chinese with Englishabstract).
    Grieser,W.V.,Bray,J.M.,2007.Identification of Production Potential in Unconventional Reservoirs.Society ofPetroleum Engineers,106623:1-6.doi:10.2118/106623-MS
    Gudehus,G.,Karcher,C.,2007.Hypoplastic Simulation ofNormal Faults without and with Clay Smears.Journalof Structural Geology,29(3):530-540.doi:10.1016/j.jsg.2006.09.011
    Gupta,A.,Scholz,C.H.,2000.A Model of Normal Fault Interaction Based on Observations and Theory.Journalof Structural Geology,22(7):865-879.doi:10.1016/s0191-8141(00)00011-0
    Hao,F.,Jiang,J.Q.,Zou,H.Y.,et al.,2004.Overpressureand the Level Difference of the Thermal Evolution ofOrganic Matter.Sciences in China(Series D),34(5):443-451(in Chinese).
    Hu,W.S.,Lü,B.Q.,Zhang,W.J.,et al.,2005.An Approach to Tectonic Evolution and Dynamics of theSongliao Basin.Chinese Journal of Geology,40(1):16-31(in Chinese with English abstract).
    Huo,Q.L.,Feng,Z.H.,Fu,L.,et al.,1999.The MigrationModel of Oil in Fuyu-Yangdachengzi Reservoir ofSanzhao Depression,Songliao Basin.Petroleum Exploration and Development,26(3):25-27(in Chinesewith English abstract).
    Koledoye,A.B.,Aydin,A.,May,E.,2000.ThreeDimensional Visualization of Normal Fault Segmentation and Its Implication for Fault Growth.The LeadingEdge,19(7):692-701.doi:10.1190/1.1438692
    Li,J.Z.,Zhao,W.Z.,Hu,S.Y.,et al.,2007.Principal Features of Stratigraphic-Lithological Hydrocarbon Accumulation Zone.Acta Petrolei Sinica,28(1):14-19(inChinese with English abstract).
    Li,M.C.,2004.Oil and Gas Migration(Fourth Edition).Petroleum Industry Press,Beijing,15-80(in Chinese).
    Lin,J.Y.,Zhang,G.,Yang,Q.J.,et al.,2003.Analysis onExploration Potential of Fuyang Reservoir in DaqingPlacanticline.Petroleum Geology&Oilfield Development in Daqing,22(3):16-18(in Chinese with English abstract).
    Meng,Y.L.,Gao,Y.T.,Wu,H.Y.,et al.,2010.RegionalDiagenetic Regularity and Controlling Factors ofMiddle-Shallow Horizons in the Northern Songliao Basin.Journal of Palaeogeography,12(1):97-106(inChinese with English abstract).
    Ramsay,J.G.,1982.Rock Ductility and Its Influence on theDevelopment of Tectonic Structures in Mountain BeltsIn:Hsu,K.J.,et al.,Mountain Building Processes.Academic Press,London,111-127.
    Rickman,R.,Mullen,M.J.,Petre,J.E.,et al.,2008.APractical Use of Shale Petrophysics for Stimulation Design Optimization:All Shale Plays are not Clones of theBarnett Shale.SPE Annual Technical Conference andExhibition.Society of Petroleum Engineers,1-11.doi:10.2118/115258-ms
    Rykkelid,E.,Fossen,H.,2002.Layer Rotation around Vertical Fault Overlap Zones:Observations from SeismicData,Field Examples and Physical Experiments.Marineand Petroleum Geology,19(2):181-192.doi:10.1016/80264-8172(02)00007-7
    Shi,L.Z.,Wu,H.Y.,Lin,T.F.,et al.,2007.Characteristics of Hydrocarbon Migration in Fuyang Oil Layer inDaqing Placanticline and Its Western Area in SongliaoBasin.Acta Petrolei Sinica,28(6):21-26(in Chinesewith English abstract).
    Schlische,R.W.,1995.Geometry and Origin of FaultRelated Folds in Extensional Settings.AAPG Bulletin,79(11):1661-1678.
    Schpfer,M.P.J.,Childs,C.,Walsh,J.J.,2006.Localisation of Normal Faults in Multilayer Sequences.Journalof Structural Geology,28(5):816-833.doi:10.1016/j.jsg.2006.02.003
    Sperrevik,S.,Faerseth,R.B.,Gabrielsen,R.H.,2000.Experiments on Clay Smear Formation along Faults.Petroleum Geoscience,6(2):113-123.doi:10.1144/petgeo.6.2.113
    Sun,T.W.,Lü,Y.F.,Liu,Z.B.,et al.,2011.HydrocarbonMigration and Enrichment Features of the Fuyu OilLayer to the East of the Daqing Placanticline.PetroleumExploration and Development,38(6):700-707(inChinese with English abstract).
    Wang,Y.C.,Wang,S.N.,2009.Controlling of the Match ofSource Rock,Overpressure and Fault on Oil Accumulation of Fuyang Oil Layer in Sanzhao Depression.Journal of Jilin University(Earth Science Edition),39(4):656-661(in Chinese with English abstract).
    Withjack,M.O.,Olson,J.,Peterson,E.,1990.ExperimentalModels of Extensional Forced Folds.AAPG Bulletin,74(7):1038-1054.
    Yun,J.B.,Jin,Z.J.,Yin,J.Y.,2002.Characteristic of Inherited Fault Belts and Their Effect on HydrocarbonAccumulation.Geotectonica et Metallogenia,26(4):379-385(in Chinese with English abstract).
    Zou,C.N.,Jia,C.Z.,Zhao,W.Z.,et al.,2005.Accumulation Dynamics and Distribution of Litho-StratigraphicReservoirs in South Songliao Basin.Petroleum Exploration and Development,32(4):125-130(in Chinesewith English abstract).
    迟元林,萧德铭,殷进垠,2000.松辽盆地三肇地区上生下储“注入式”成藏机制.地质学报,74(4):371-377.
    迟元林,云金表,蒙启安,等,2002.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,10-80.
    付广,王有功,2008.源外鼻状构造区油运移输导通道及对成藏的作用———以松辽盆地尚家地区为例.地质论评,54(5):646-652.
    付广,王有功,袁大伟,2010.三肇凹陷扶杨油层源断裂的再认识及其对成藏的控制作用.石油学报,31(5):762-766,773.
    付晓飞,郭雪,朱丽旭,等,2012.泥岩涂抹形成演化与油气运移及封闭.中国矿业大学学报,41(1):52-63.
    付晓飞,平贵东,范瑞东,等,2009.三肇凹陷扶杨油层油气“倒灌”运聚成藏规律研究.沉积学报,27(3):558-566.
    郝芳,姜建群,邹华耀,等,2004.超压对有机质热演化的差异抑制作用及层次.中国科学(D辑),34(5):443-451.
    胡望水,吕炳全,张文军,等,2005.松辽盆地构造演化及成盆动力学探讨.地质科学,40(1):16-31.
    霍秋立,冯子辉,付丽,等,1999.松辽盆地三肇凹陷扶杨油层石油运移方式.石油勘探与开发,26(3):25-27.
    李建忠,赵文智,胡素云,等,2007.岩性地层型油气聚集区带的基本特征.石油学报,28(1):14-19.
    李明诚,2004.石油与天然气运移(第四版).北京:石油工业出版社,15-80.
    林景晔,张革,杨庆杰,等,2003.大庆长垣扶余杨大城子油层勘探潜力分析.大庆石油地质与开发,22(3):16-18.
    孟元林,高煜婷,吴河勇,等,2010.松辽盆地北部中浅层区域成岩规律及影响因素.古地理学报,12(1):97-106.
    施立志,吴河勇,林铁锋,等,2007.松辽盆地大庆长垣及其以西地区扶杨油层油气运移特征.石油学报,28(6):21-26.
    孙同文,吕延防,刘宗堡,等,2011.大庆长垣以东地区扶余油层油气运移与富集.石油勘探与开发,38(6):700-707.
    王雅春,王胜男,2009.源岩、超压和断裂空间匹配对三肇凹陷扶杨油层油成藏的控制作用.吉林大学学报(地球科学版),39(4):656-661.
    云金表,金之钧,殷进垠,2002.松辽盆地继承性断裂带特征及其在油气聚集中的作用.大地构造与成矿学,26(4):379-385.
    邹才能,贾承造,赵文智,等,2005.松辽盆地南部岩性-地层油气藏成藏动力和分布规律.石油勘探与开发,32(4):125-130.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心