引文
[1]翟光明,王志武.中国石油地质志:卷2[M].北京:石油工业出版社,1993:55-305.Zhai Guangming,Wang Zhi wu.Petroleumgeology of China:Vol.2[M].Beijing:PetroleumIndustry Press,1993:55-305.
[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.Gao Ruiqi,Zhang Ying,Cui Tongcui.Cretaceous oil and gas stra-ta of Songliao Basin[M].Beijing:Petroleum Industry Press,1994:1-234.
[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.Ye Dequan,Huang Qinghua,Zhang Ying,et al.Cretaceous ostra-coda biostratigraphy in Songliao Basin[M].Beijing:PetroleumIndustry Press,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.Chi Yuanlin,Yun Jinbiao,Meng Qi’an,et al.Deep structure anddynamics of Songliao Basin and hydrocarbon accumulation[M].Beijing:PetroleumIndustry Press,2002:1-112.
[5]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.Wang Dongpo,Liu Zhaojun,Liu Li.Evolution of Songliao Basinand global eustacy[M].Beijing:Geological Publishing House,1994:79-149.
[6]任延广,王雅峰,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.Ren Yanguang,Wang Yafeng,Wang Zhanguo,et al.Features ofhigh-resolution sequence stratigraphy of Putaohua reservoir innorthern Songliao Basin[J].Acta Petrolei Sinica,2006,27(Sup-plement):25-30.
[7]李家强.层拉平方法在沉积前古地貌恢复中的应用——以济阳坳陷东营三角洲发育区为例[J].油气地球物理,2008,6(2):46-49.Li Jiaqiang.Application of beddingflatteninginthe process of re-building paleogeomorphology before basin deposition:A casestudy in Dongying Sag,Jiyang Depression[J].Petroleum Geo-physics,2008,6(2):46-49.
[8]蔡希源,辛仁臣.松辽坳陷深水湖盆层序构成模式对岩性圈闭分布的控制[J].石油学报,2004,25(5):6-10.Cai Xiyuan,Xin Renchen.Architectural model of sequence stra-tigraphy controlling the distribution of litho-trap in deep-waterlake of Songliao depressive basin[J].Acta Petrolei Sinica,2004,25(5):6-10.
[9]高瑞祺,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.Gao Ruiqi,Zhao Chuanben,Qiao Xiuyun,et al.Cretaceous oilstrata palynology from Songliao Basin[M].Beijing:GeologicalPublishing House,1999:55-103.
[10]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):29-38.Zhuo Hongchun,Lin Chunming,Li Yanli,et al.Characteristics ofsedi mentary facies and sequence boundary in Upper CretaceousQingshankou-Yaojia Formation of northern Songliao Basin[J].Acta Sedi mentologica Sinica,2007,25(1):29-38.
[11]Cloetingh S,Kooi H.Intraplate stresses and dynamical aspects ofrifted basins[J].Tectonophysics,1992,215(1/2):167-185.
[12]Ziegler P A,Van Wees J D,Cloetingh S,et al.Mechanical con-trols on collision-related compressional intraplate deformation[J].Tectonophysics,1998,300(1/4):103-129.
[13]何登发,李德生,童晓光,等.多期叠加盆地古隆起控油规律[J].石油学报,2008,29(4):475-488.He Dengfa,Li Desheng,Tong Xiaoguang,et al.Accumulationand distribution of oil and gas controlled by paleo-uplift in poly-history superi mposed basin[J].Acta Petrolei Sinica,2008,29(4):475-488.
[14]Dyksterhuis S,Müller R D.Cause and evolution of intraplate o-rogeny in Australia[J].Geology,2008,36(6):495-498.
[15]Kley J,Voigt T.Late Cretaceous intraplate thrusting in centralEurope:Effect of Africa-Iberia-Europe convergence,not Alpinecollision[J].Geology,2008,36(11):839-842.
[16]Hilde T WC,Uyeda S,Kroenke L.Evolution of the western pa-cific andits margin[J].Tectonophysics,1977,38(1/2):145-152.
[17]Müller R D,Sdrolias M,Gaina C,et al.Age,spreading rates,andspreading symmetry of the world’s ocean crust[J].Geochemis-try,Geophysics,Geosystems,2008,9(4):1-19.
[18]Clark R,Müller R D.Convection modelsinthe Kamchatka regionusingi mposed plate motion and thermal histories[J].Journal ofGeodynamics,2008,46(1/2):1-9.
[19]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.Wan Tianfeng.Intraplate deformation,tectonic stress field andtheir application for eastern China in Meso-Cenozoic[M].Bei-jing:Geological Publishing House,1993:12-83.
[20]谢鸣谦.拼贴板块构造及其驱动机理: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.Xie Mingqian.Piece together the slab structure and its drivingmechanisms for the evolution of the geotectonicsinthe northeastof China and adjacent area[M].Beijing:Science Press,2000:5-248.
[21]Maruyama S,Send T.Orogeny and relative plate motions:Exam-ple of the Japanese islands[J].Tectonophysics,1986,127(3/4):305-329.
[22]Stepashko A A.The Cretaceous dynamics of the pacific plate andstages of magmatic activity in northeastern Asia[J].Geotecton-ics,2006,40(3):225-235.
[23]Maruyama S,Isozaki Y,Ki mura G,et al.Paleogeographic mapsof the Japanese Islands:Plate tectonic synthesis from750Ma tothe present[J].Island Arc,1997,6(1):121-142.
[24]Ren Jianye,Tamaki K,Li Sitian,et al.Late Mesozoic and Ceno-zoic rifting andits dynamic settingin Eastern China and adjacentareas[J].Tectonophysics,2002,344(3/4):175-205.
[25]任建业.渤海湾盆地东营凹陷S′6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.Ren Jianye.Tectonic significance of S′6boundaryin Dongying De-pression,Bohai Gulf Basin[J].Earth Science:Journal of China U-niversity of Ceosciences,2004,29(1):69-76.
[26]宋建国,窦立荣,李建忠.中国东北区晚中生代盆地构造与含油气系统[J].石油学报,1996,17(4):1-7Song Jianguo,Dou Lirong,Li Jianzhong.Tectonics and petrolifer-ous systems of Late Mesozoic basins in NE China[J].Acta Pe-trolei Sinica,1996,17(4):1-7.
[27]谭试典,王冰,黄子齐,等.中国中、新生代沉积盆地类型与演化[J].石油学报,1990,11(3):1-11.Tan Shidian,Wang Bing,Huang Ziqi,et al.The types and evolu-tion of Mesozoic-Cenozoic sedi mentary basins in China[J].ActaPetrolei Sinica,1990,11(3):1-11.
[28]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,1989,8(10):1084-1091.Fang Dajun,Wang Zhaoliang,Jin Guohai,et al.Cretaceous mag-netostratigraphy in the Songliao Basin,China[J].Science in Chi-na:Series B,1989,8(10):1084-1091.
[29]王璞?,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):372-381.Wang Pujun,Du Xiaodi,Wang Jun,et al.The chronostratigraphyand stratigraphic classification of the Cretaceous of the SongliaoBasin[J].Acta Geologica Sinica,1995,69(4):372-381.
[30]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.Huang Qinghua,Tan Wei,Yang Huichen.Stratigraphic succes-sion and chronostrata of Cretaceous in Songliao Basin[J].Petro-leum Geology&Oilfield Development in Daqing,1999,18(6):15-17.
[31]Skelton P W,Spicer R A,Kelley S P,et al.The Cretaceous world[M].Cambridge,New York,Melbourne:Cambridge UniversityPress,2003:1-350.
[32]Stepashko A A.Spreading cycles in the Pacific Ocean[J].Ocean-ology,2008,48(3):401-408.
[33]Müller R D,Sdrolias M,Gaina C,et al.Long-termsea-level fluc-tuations driven by ocean basin dynamics[J].Science,2008,319:1357-1362.
[34]袁选俊,薛良清,池英柳,等.坳陷型湖盆层序地层特征与隐蔽油气藏勘探——以松辽盆地为例[J].石油学报,2003,24(3):11-15.Yuan Xuanjun,Xue Liangqing,Chi Yingliu,et al.Sequence stra-tigraphic and subtle-trap characteristics of lacustrine depressionbasin[J].Acta Petrolei Sinica,2003,24(3):11-15.
[35]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.Ren Fenglou,Zhang Yueqiao,Qiu Liangui,et al.Evolution of thestructural stress field in Jiaolai Basin in Cretaceous[J].Geotec-tonica et Metallogenia,2007,31(2):157-167.
[36]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,2007,37(增刊):110-118.Chen Gang,Sun Jianbo,Zhou Lifa,et al.Tectonic events insouthwestern margin of Ordos Basin in Mesozoic using fissiontrack dating[J].Science in China:Series D,2007,37(Supple-ment):110-118.
[37]张功成,徐宏,刘和甫,等.松辽盆地反转构造与油气田分布[J].石油学报,1996,17(2):9-14.Zhang Gongcheng,Xu Hong,Liu Hefu,et al.Inversion struc-tures in relation to oil and gas field distributionin Songliao basin[J].Acta Petrolei Sinica,1996,17(2):9-14.
[38]侯读杰,黄清华,黄福堂,等.松辽盆地海侵地层的分子地球化学特征[J].石油学报,1999,20(2):30-34Hou Dujie,Huang Qinghua,Huang Futang,et al.The character-istics of molecular geochemistry of marine transgression stratainSongliao Basin[J].Acta Petrolei Sinica,1999,20(2):30-34.
[39]向才富,冯志强,庞雄奇,等.松辽盆地晚期热历史及其构造意义:磷灰石裂变径迹(AFT)证据[J].中国科学:D辑,2007,37(8):1024-1031.Xiang Caifu,Feng Zhiqiang,Pang Xiongqi,et al.Late stage ther-mal history of the Songliao Basin and its tectonic i mplications:Evidence fromapatite fissiontrack(AFT)analyses[J].ScienceinChina:Series D,2007,37(8):1024-1031.