松辽盆地T11界面的地质属性及其形成机制
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摘要
以地震剖面的精细构造解释和钻井资料分析为基础,对松辽盆地姚家组毒山口组的底界面T11特征展开详细研究.研究表明:在该界面之下地层内发育了4组微幅隆起褶皱带,且沿该界面发育了的红色古土壤层.这些特征揭示了T11界面是发育在盆地裂后热沉降期内的一个具有挤压背景的区域性角度不整合面.该界面的形成发育与周缘板块重组事件在时间上具有一致性,在成因上具有耦合性.因此,松辽盆地T11界面是晚白垩纪太平洋板块与欧亚板块构造重组事件在松辽盆地内的响应界面.
Based on interpretation and analysis of seismic and well drilling data in Songliao Basin,the characteristics of T11 and the bottom boundary of Yaojia Formation are elaborately described and studied.The four fold belts(large-scale,broad,low-relief,north-east-north-trending) and thrust systems are distinguished through the analysis.It is indicated through these characteristics that the regional angular unconformity T11 was formed in a compressional regime during the post-rift thermal subsidence of Songliao Basin.T11 boundary was formed during the period of late Cretaceous(about 88.5Ma).This is in consistence with the time of a great reorganization of plate tectonic in the Mesozoic time.It is therefore argued that the T11 bottom boundary of Yaojia Formation in Songliao Basin is the responding surface to interaction between Pacific plate and Eurasian plate in late Mesozoic.
Based on interpretation and analysis of seismic and well drilling data in Songliao Basin,the characteristics of T11 and the bottom boundary of Yaojia Formation are elaborately described and studied.The four fold belts(large-scale,broad,low-relief,north-east-north-trending) and thrust systems are distinguished through the analysis.It is indicated through these characteristics that the regional angular unconformity T11 was formed in a compressional regime during the post-rift thermal subsidence of Songliao Basin.T11 boundary was formed during the period of late Cretaceous(about 88.5Ma).This is in consistence with the time of a great reorganization of plate tectonic in the Mesozoic time.It is therefore argued that the T11 bottom boundary of Yaojia Formation in Songliao Basin is the responding surface to interaction between Pacific plate and Eurasian plate in late Mesozoic.
引文
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[32]Skelton P W.The Cretaceous World[M].London:Cambridge University Press,2003:1-350.
[33]陈刚,孙建博,周立发,等.鄂尔多斯盆地西南缘中生代构造事件的裂变径迹年龄记录[J].中国科学(D辑:地球科学),2007,37(增刊):110-118.
[34]任凤楼,张岳桥,邱连贵,等.胶莱盆地白垩纪构造应力场与转换机制[J].大地构造与成矿学,2007,31(2):157-167.
[2]高瑞祺,张莹,崔同翠.松辽盆地白垩纪石油地层[M].北京:石油工业出版社,1985:1-234.
[3]叶得泉,黄清华,张莹,等.松辽盆地白垩纪介形类生物地层学[M].北京:石油工业出版社,2002:53-98.
[4]迟元林,云金表,蒙启安,等.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,2002:1-112.
[5]魏魁生,徐怀大,雷怀玉.非海相层序地层学—以松辽盆地为例[M].北京:地质出版社,1996:46-94.
[6]王东坡,刘招君,刘立.松辽盆地演化与海平面升降[M].北京:地质出版社,1994:79-149.
[7]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,1997:47-103.
[8]任延广,王稚峰,王占国,等.松辽盆地北部葡萄花油层高频层序地层特征[J].石油学报,2006,27(增刊):25-30.
[9]卓弘春,林春明,李艳丽,等.松辽盆地北部上白垩统青山口-姚家组沉积相及层序地层界面特征[J].沉积学报,2007,25(1):30-38.
[10]高瑞棋,赵传本,乔秀云,等.松辽盆地白垩纪石油地层孢粉学[M].北京:地质出版社,1999:55-103.
[11]刘招君,董清水,王嗣敏,等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002:46-94.
[12]崔莹.大庆油田徐22井青山口组-姚家组界线地层及古气候记录[D].北京:中国地质大学,2006.
[13]万天丰.中国东部中—新生代板内变形构造应力场及其应用[M].北京:地质出版社,1993:12-83.
[14]谢鸣谦.拼贴板块及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社,2000:5-248.
[15]Twc Hilde,Uyeda S,Kroenke L.Evolution of the Western Pacific and its Margin[J].Tectonophysics,1977,38:145-152.
[16]Sharman GF,Risch DL.Northwest Pacific Tectonic Evolution in the Middle Mesozoic[J].Tectonophysics,1988,155:331-344.
[17]Ren J Y,Tamaki K,Li S T,et al.Late Mesozoic and Cenozoic Rifting and its Dynamic Eetting in Eastern China and AdjacentAreas[J].Tectonophysics,2002,344:175-205.
[18]任建业.渤海湾盆地东营凹陷S6′界面的构造变革意义[J].地球科学—中国地质大学学报,2004,29(1):69-76.
[19]Larson RL.Latest Pulse of Earth:Evidence for a Mid-Cretaceous Superplume[J].Geology,1991,19:547-550.
[20]王成善,胡修棉.白垩纪世界与大洋红层[J].地学前缘,2005,12(2):11-21.
[21]高瑞祺.松辽盆地白垩纪被子植物花粉的演化[J].古生物学报,1982,21(2):217-222
[22]叶得泉.松辽盆地白垩系介形类生物地层和磁性地层学意义[J].大庆石油地质与开发,1991,10(4):1-12.
[23]方大钧,王兆樑,金国海,等.中国松辽盆地白垩系磁性地层[J].中国科学(B辑),1989,10:1084-1091.
[24]王璞裙,杜小弟,王俊,等.松辽盆地白垩纪年代地层研究及地层时代划分[J].地质学报,1995,69(4):372-379.
[25]黄清华,谭伟,杨会臣.松辽盆地白垩纪地层序列与年代地层[J].大庆石油地质与开发,1999,18(6):15-17.
[26]Stepashko A A.The Cretaceous Dynamics of the Pacific Plate and Stages of Magmatic Activity in Northeastern Asia[J].Geo-tectonics,2006,40(3):225?235.
[27]Stepashko A A..Spreading Cycles in the Pacific Ocean[J].Oceanology,2008,48(3):401-408.
[28]Alexey Soloviev,John Garver,Galina Ledneva.Cretaceous Accretionary Complex Related to Okhotsk-Chukotka Subduction,Omgon Range,Western Kamchatka,Russian Far East[J].Journal of Asian Earth Sciences,2006,27:437-453.
[29]Wilgus C K,Hastings B S,Kendall CG,et al.SeaLevel Changes—A Integrated Approach[M].SEPM Special Publication(No.42),1988:71-108.
[30]辛仁臣,蔡希源,王英民.松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,2004,22(3):387-392.
[31]Huber B T,Hodell D A,Hamilton CP.Middle-Late Cretaceous Climate of the Southern High Latitudes:Stable Isotopic Evi-dence for Minimal Equator-to-Pole Thermal Gradients[J].Geological Society American,1995,107:1161-1191.
[32]Skelton P W.The Cretaceous World[M].London:Cambridge University Press,2003:1-350.
[33]陈刚,孙建博,周立发,等.鄂尔多斯盆地西南缘中生代构造事件的裂变径迹年龄记录[J].中国科学(D辑:地球科学),2007,37(增刊):110-118.
[34]任凤楼,张岳桥,邱连贵,等.胶莱盆地白垩纪构造应力场与转换机制[J].大地构造与成矿学,2007,31(2):157-167.
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