松辽盆地坡折带研究及岩性油气藏预测
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摘要
松辽盆地是中国东部中新生代具有断坳双重结构的大型复合型沉积盆地,目前,以泉头组、青山口组、姚家组为主的坳陷期含油层系的勘探逐步由“构造油气藏的勘探”转向“岩性油气藏的勘探”为重点。由于岩性地层油气藏具有多样性、复杂性和隐蔽性特点,因此如何预测岩性油气藏分布规律、研究岩性油气藏形成的控制因素对于松辽盆地坳陷期开展岩性油气藏勘探具有重要的指导意义。
通过松辽盆地坳陷期构造特征、古地理特征及沉积体系分布特征、论述了松辽盆地坳陷期坡折带-“挠曲坡折带”的成因机制和分布特征,论述了挠曲坡折带对高频层序构型、挠曲坡折带对沉积相带分异、砂体类型分布特征的控制,论述了挠曲坡折带对岩性油气藏类型分布、岩性油气藏分布规律和分布规模的控制。
论述了松辽盆地坳陷期葡萄花油层“浅水湖泊三角洲”沉积的形成条件,论述了浅水湖泊三角洲沉积相带的分布特征,总结了各沉积相带不同的沉积微相类型,论述了高频层序序约束下的沉积相和沉积环境的演变特征,最后总结了葡萄花油层浅水湖泊三角洲的沉积模式及对岩性地层油气藏分布规律的控制。
应用波阻抗反演和测井多参数信息反演、地震属性提取及优化、地震属性透视技术、地震波形分类、三维可视化、相干体、频谱分解技术等,在坳陷湖盆“坡折带”和“浅水三角洲”形成岩性油气藏的地质背景下,根据不同储层类型的特点(厚层高孔高渗砂体和薄互层低孔低渗砂体)采用不同的地球物理预测技术,有效地开展岩性圈闭识别和岩性油气藏预测取得卓有成效的预测效果。
通过对松辽盆地坳陷期挠曲坡折带和浅水湖泊三角洲对岩性油气藏分布规律的控制作用研究,结合地球物理预测方法,对松辽盆地挠曲坡折带发育区和葡萄花油层浅水湖泊三角洲前缘相带,预测了岩性油气藏形成的有利区带、指出了岩性油气藏勘探的目标。
Songliao basin is largely composite Meso-cenozoic petroleum basin with fault anddepression architecture in east china. Recently, The exploration of Quantouzu,Qingshankou and yaojia formation gradually is charging from structure reservior tolithological reservoir. Because of multiplicity, complexity and subtle, Witch how toforecast lithological reservoir is difficulty. The highlight of this paper is carrying outthat the research of genesis and characteristic of slope break, of sedimentary modeland characteristic of shallow lacustrine. Accoding to the guide of sequencestratagrapgy theory , this paper systematically research the slope break and shallowlacustrine delta of depression controlling the distribution of lithological reservoir,using of approaches of high resolution sequence strata correlation, wave impedanceinversion, multiple logging parameter inversion, seismic property extracting andoptimizing, 3dimention visualization, seismic perspectivity and hydrocarbon detect,and identified lithological traps and forecasted lithological reservoir. Forecastingeffect was successful.
According to the characteristics of structure, palaeography and depositionalsystem, in depression of Songliao basin, this paper talked about the flexure breakslope controlling the oil & gas distribution. The main research content included in thegenesis and the characteristics of flexure break slope, included in the flexure breakslope controlling the architecture of high resolution sequence strata, controlling thedifferentiation of sedimentation facies , controlling the distribution of sandstone styles,controlling the distribution of lithological reservoir, during depression of Songliaobasin.
This paper talked about the genetic condition of shallow lacustrine delta ofPutaohua formation, talked about the sedimentary facies belt distribution of shallowlacustrine delta, generalized the distribution of sedimentary micro-facies styles andevolution characteristics of sedimentary environment during the depression stage ofSongliao basin. In the end, this paper generalized the sedimentary model of theshallow water lacustrine delta of Putaohua formation and distribution of litholgicalreservoir.
This paper used new technique and new approaches of physics, included in thehigh resolution seismic data process approaches, high seismic amplitude, high realimagery, included in seismic wave impedance inversion and logging parameterinversion, included in the extracting and optimizing of seismic property, fluoroscopytechnique of seismic property, classification of seismic wave pattern, visualization ofthree dimention seismic data, cohere seismic data body, disintegration of seismicfrequency spectrum. According to different genetic condition of lithological reservoirand different styles reservoir characteristics, this paper carried out the identification oflithological traps and forecast the lithological reservoirs using the different physicalforecast techniques.
Through research of flexure slope break and shallow lacustrine controlling thedistribution of lithological reservoir, integrating of geophysical forecasting approach,this paper forecasted the beneficial block and pointed out the exploration target of the
flexure slope break and fore-delta of shallow lacustrine, in the depression of Songliaobasin.
通过松辽盆地坳陷期构造特征、古地理特征及沉积体系分布特征、论述了松辽盆地坳陷期坡折带-“挠曲坡折带”的成因机制和分布特征,论述了挠曲坡折带对高频层序构型、挠曲坡折带对沉积相带分异、砂体类型分布特征的控制,论述了挠曲坡折带对岩性油气藏类型分布、岩性油气藏分布规律和分布规模的控制。
论述了松辽盆地坳陷期葡萄花油层“浅水湖泊三角洲”沉积的形成条件,论述了浅水湖泊三角洲沉积相带的分布特征,总结了各沉积相带不同的沉积微相类型,论述了高频层序序约束下的沉积相和沉积环境的演变特征,最后总结了葡萄花油层浅水湖泊三角洲的沉积模式及对岩性地层油气藏分布规律的控制。
应用波阻抗反演和测井多参数信息反演、地震属性提取及优化、地震属性透视技术、地震波形分类、三维可视化、相干体、频谱分解技术等,在坳陷湖盆“坡折带”和“浅水三角洲”形成岩性油气藏的地质背景下,根据不同储层类型的特点(厚层高孔高渗砂体和薄互层低孔低渗砂体)采用不同的地球物理预测技术,有效地开展岩性圈闭识别和岩性油气藏预测取得卓有成效的预测效果。
通过对松辽盆地坳陷期挠曲坡折带和浅水湖泊三角洲对岩性油气藏分布规律的控制作用研究,结合地球物理预测方法,对松辽盆地挠曲坡折带发育区和葡萄花油层浅水湖泊三角洲前缘相带,预测了岩性油气藏形成的有利区带、指出了岩性油气藏勘探的目标。
Songliao basin is largely composite Meso-cenozoic petroleum basin with fault anddepression architecture in east china. Recently, The exploration of Quantouzu,Qingshankou and yaojia formation gradually is charging from structure reservior tolithological reservoir. Because of multiplicity, complexity and subtle, Witch how toforecast lithological reservoir is difficulty. The highlight of this paper is carrying outthat the research of genesis and characteristic of slope break, of sedimentary modeland characteristic of shallow lacustrine. Accoding to the guide of sequencestratagrapgy theory , this paper systematically research the slope break and shallowlacustrine delta of depression controlling the distribution of lithological reservoir,using of approaches of high resolution sequence strata correlation, wave impedanceinversion, multiple logging parameter inversion, seismic property extracting andoptimizing, 3dimention visualization, seismic perspectivity and hydrocarbon detect,and identified lithological traps and forecasted lithological reservoir. Forecastingeffect was successful.
According to the characteristics of structure, palaeography and depositionalsystem, in depression of Songliao basin, this paper talked about the flexure breakslope controlling the oil & gas distribution. The main research content included in thegenesis and the characteristics of flexure break slope, included in the flexure breakslope controlling the architecture of high resolution sequence strata, controlling thedifferentiation of sedimentation facies , controlling the distribution of sandstone styles,controlling the distribution of lithological reservoir, during depression of Songliaobasin.
This paper talked about the genetic condition of shallow lacustrine delta ofPutaohua formation, talked about the sedimentary facies belt distribution of shallowlacustrine delta, generalized the distribution of sedimentary micro-facies styles andevolution characteristics of sedimentary environment during the depression stage ofSongliao basin. In the end, this paper generalized the sedimentary model of theshallow water lacustrine delta of Putaohua formation and distribution of litholgicalreservoir.
This paper used new technique and new approaches of physics, included in thehigh resolution seismic data process approaches, high seismic amplitude, high realimagery, included in seismic wave impedance inversion and logging parameterinversion, included in the extracting and optimizing of seismic property, fluoroscopytechnique of seismic property, classification of seismic wave pattern, visualization ofthree dimention seismic data, cohere seismic data body, disintegration of seismicfrequency spectrum. According to different genetic condition of lithological reservoirand different styles reservoir characteristics, this paper carried out the identification oflithological traps and forecast the lithological reservoirs using the different physicalforecast techniques.
Through research of flexure slope break and shallow lacustrine controlling thedistribution of lithological reservoir, integrating of geophysical forecasting approach,this paper forecasted the beneficial block and pointed out the exploration target of the
flexure slope break and fore-delta of shallow lacustrine, in the depression of Songliaobasin.
引文
[1] 蔡希源;陈章明等.松辽两江地区石油地质分析. 北京:石油工业出版社,1999
[2] 陈广军,宋国奇,王永诗,等.斜坡扇低位域砂岩体岩性油气藏勘探方法-以埕岛潜山披覆构造东部斜坡带为例. 石油学报,2002,23(3):34-38.
[3] 程学儒.松辽盆地北部油气聚集地基本特征和勘探方向.见:徐数宝,胡见义.中国油气聚集与分布 .北京:石油工业出版社,1991.24～38
[4] 程学儒.松辽盆地北部油气聚集地基本特征和勘探方向.徐数宝,胡见义.中国油气聚集与分布.北京:石油工业出版社,1991.
[5] 迟元林,云金表等.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
[6] 邓宏文,王红亮,王居峰,等. 层序地层构成与层序控砂、控藏的自相似性特征-以三角洲-浊积扇为例.石油与天然气地质,2004,25(5):491-495.
[7] 丁正言,韩广玲,张 惠,等.松辽盆地南部油气聚集的成因类型和分部模式. 见:徐数宝,胡见义.中国油气聚集与分布 .北京:石油工业出版社,1991.38～48
[8] 高 山,金振民等.拆沉作用及其壳—幔演化动力学意义.地质科技情报,1997,16(1):1～9
[9] 高瑞琪,赵传本,乔秀云,郑玉龙,闫凤云,万传彪.松辽盆地白垩纪石油地层孢粉学.北京:地质出版社,1999
[10] 高瑞琪,赵传本,乔秀云,郑玉龙,闫凤云,万传彪.松辽盆地白垩纪石油地层孢粉学.北京:地质出版社,1999
[11] 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.
[12] 高瑞祺,赵政璋.中国油气新区勘探(第二卷)—中国陆上天然气勘探新领域.290～315.北京:石油工业出版社,2001
[13] 高山林,陈海泓,窦伟坦,等. 鄂尔多斯盆地延长组的湖泊风暴沉积.沉积学报,1999,17(增刊):758-763.
[14] 韩晓东,楼章华,姚炎明,杨卫东,蔡希源.松辽盆地湖泊浅水三角洲沉积动力学研究. 矿物学报,2000,20(3):305-314
[15] 候贵廷,冯大晨,等.松辽盆地的反转构造作用及其对油气成藏的影响.石油与天然气地质.2004,25(1):49～57
[16] 胡见义,王明明等.含油气地质单元序列中含油气系统的研究与应用.中国含油气系统的应用与进展.北京:石油工业出版社,2001.3～8
[17] 胡明毅,贺 萍. 潮坪风暴沉积特征及其研究意义.地球科学进展,2002,17(3):391-396.
[18] 胡望水.正反转构造与油气聚集.北京:石油工业出版社,2000.
[19] 胡望水.正反转构造与油气聚集.北京:石油工业出版社,2000.
[20] 黄福堂.松辽盆地油气水地球化学.北京:石油工业出版社,1999
[21] 贾承造.前陆冲断带油气勘探.北京:石油工业出版社,2000.
[22] 李德生.中国含油气盆地构造学.北京:石油工业出版社,2002.
[23] 李冬旭.旋钮构造动力学—理论、方法及应用. 北京:地质出版社,2003.
[24] 李丕龙,张善文,宋国奇,肖焕钦,等.济阳成熟区非构造油气藏深化勘探.石油学报,2003,24(5):10-15
[25] 李思田,路凤香,林畅松,等.中国东部及邻区中、新生代盆地演化及地球动力学背景.北京:中国地质大学出版社,1997
[26] 李思田,潘元林,陆永潮,等. 断陷湖盆隐蔽性油气藏预测及勘探的关键技术—高精度地震探测基础上的层序地层学研究. 地球科学—中国地质大学学报,2002,27(5):592-598.
[27] 林畅松,潘元林,肖建新,等.构造坡折带断陷湖盆层序和油气预测的重要概念.地球科学-中国地质大学学报,2000,25(3):260-267.
[28] 刘和甫;梁慧社,等.中国东部新生代裂陷盆地与伸展山岭耦合机制.地学前缘.2000,7(4):477～487
[29] 刘招君;董清水等.陆相层序地层学导轮与应用.北京:石油工业出版社,2002.
[30] 马宗晋,杜品仁,洪汉净.地球构造与动力学.广州:广东科技出版社,2003.
[31] 马宗晋,杜品仁,洪汉净.地球构造与动力学.广州:广东科技出版社,2003.
[32] 牛数银,孙爱群等.造山带与盆地间物质的横向迁移.地学前缘.1995,2(1～2):85～93
[33] 潘元林,宋国洪,郭玉新,等.济阳断陷湖盆层序地层学及砂砾岩油气藏群.石油学报,2003,24(3):16-23.
[34] 潘元林等. 1998. 中国隐蔽油气藏. 地质出版社
[35] 宋国洪,冯有良,刘承华,李传华,等.同沉积断裂带砂砾岩隐蔽性油藏研究-以东营凹陷胜北断裂带为例.石油试验地质,2003,25(3):274～281
[36] 隋淑玲,赵开连等.断裂构造在油气成藏中的作用-以齐阳坳陷曲堤油田为例.石油地球物理勘探.2003,38(6):666～670
[37] 万天丰;朱 鸿等.中国大陆及邻区中生代—新生代大地构造与环境变迁.现代地质.2002,16(2):107～121
[38] 王春鹏,马玉龙,时庚戊.辽河油区油田开发实践.北京:石油工业出版社,2002.
[39] 王东坡等. 沉积盆地地球动力学系统的研究—以辽西、辽北、松辽盆地为例.石油与天然气地质.1999,20(4):273～279
[40] 王建功,王天琦,粱苏娟,等. 松辽盆地北部葡萄花油层事件沉积.石油学报,2005,26(6):20～24
[41] 王建功,王天琦,粱苏娟,等. 松辽盆地北部葡萄花油层事件沉积.石油学报,2005,26(6):20～24
[42] 王建功,卫平生,贺顺义,王斌婷.松辽盆地南部大麻苏—大情字井区低阻油层识别.西北油气勘探,2004,16(4):27～33.
[43] 王建功,卫平生,史永苏,王斌婷,潘树新.松辽盆地南部西部斜坡区大规模岩性油气藏和地层超覆油气藏成藏条件.中国石油勘探,2003,8(3):27～30.
[44] 王建功,卫平生,杨建礼.松辽盆地南部青山口组三段底界不整合面与油气分布.地质论评,2005,26(2):26～29
[45] 王建功,卫平生,赵占银,潘树新,赵志魁,等.松南西部勘探领域及前景.中国石油勘探,2005,10(3):8～15
[46] 王建功,卫平生,郑浚茂,等.挠曲坡折带特征与油气勘探-以松辽盆地南部为例.石油学报,2005,26(2):1～5
[47] 王建功,吴克平,卫平生,赵占银,潘树新,赵志魁.松辽盆地南部西区断裂体系与油气分布.新疆石油地质,2005,26(1):29～32.
[48] 王涛.中国东部裂谷盆地油气藏地质.北京:石油工业出版社,1997.
[49] 王燮培;费 琪等.石油勘探构造分析.北京:中国地质大学出版社,1992
[50] 王训练. 露头层序地层学研究中定义和识别不同级别沉积层序的标准.中国科学(D 辑),2003,33(11):1057-1068.
[51] 王英民,金武弟等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义.石油与天然气地质,2003,24(3):199-203.
[52] 王英民,刘豪等.准噶尔大型坳陷湖盆坡折带的类型和分布特征.地球科学,2002,27(5):683-688.
[53] 王永春.松辽盆地南部岩性油藏的形成和分布. 北京:地质出版社,2001.
[54] 卫平生,李天顺,李安春,王建功.巴彦浩特盆地石炭系沉积相及沉积演化. 沉积学报,2005,23(2).
[55] 卫平生,王建功,潘树新,王斌婷.河口坝、沿岸坝的形成及成藏机制-以松辽盆地西、南沉积体系为例,新 疆石油地质,2004,25(6)592-595
[56] 魏魁生. 非海相层序地层学.北京:地质出版社,1996.
[57] 吴孔友,查 明,柳广弟.2002.准噶尔盆地二叠系不整合面及其油气运聚特征.石油勘探与开发,29(2):53～58.
[58] 吴永平,杨池银,王喜双.2000.渤海湾盆地北部奥陶系潜山油气藏成藏组合及勘探技术.石油勘探与开发,27(5):1-6.
[59] 许怀大,王世凤,陈开远.地震地层学解释基础.武汉:中国地质大学出版社,1990.
[60] 许世远,邵虚生. 杭州湾北部滨岸的风暴沉积.中国科学(B),1984(12):1136-1143.
[61] 许世远. 长江三角洲地区风暴沉积研究.北京:科学出版社,1997.
[62] 严钦尚. 论滨岸浅海的风暴沉积.海洋与沼泽,1984,15(1):14-19.
[63] 杨万里,高瑞琪,郭庆福,刘耀光. 松辽盆地陆相油气生成运移和聚集.哈尔滨:黑龙江科学技术出版社,1985.
[64] 叶德泉,黄清华,张 莹,陈春瑞. 松辽盆地白垩纪介形类生物地层学学. 北京:石油工业出版社,2002,56-74.
[65] 于文卿,松 希,于恩君,屈旭钧.1999.松辽盆地白垩系地层时代划分.铀矿地质,15(5):257～266.
[66] 俞凯,侯洪斌.松辽盆地南部断陷层系石油天然气地质.北京:石油工业出版社,2002
[67] 曾允孚,夏文杰. 沉积岩石学.北京:地质出版社,1986,32-34.
[68] 翟光明,宋建国,靳久强,高维亮.板块构造演化与含油气盆地形成和评价.北京:石油工业出版社,2002.
[69] 翟光明,宋建国,靳久强,高维亮.板块构造演化与含油气盆地形成和评价.北京:石油工业出版社,2002.
[70] 张国栋. 现代滨岸风暴沉积—以舟山普陀岛、朱家尖岛为例.沉积学报,1987,5(2):17-27.
[71] 张善文,王英民,李群.应用坡折带理论寻找隐蔽油气藏.石油勘探与开发,2003,30(3):5-7
[72] 张万选,张厚福,曾洪流,刘震,高先志,刘镇江.陆相地震地层学.山东东营:石油大学出版社:1993.
[73] 张玉明,夏响华.松辽盆地南部低渗透油气田勘探技术.北京:石油工业出版社,2001
[74] 赵文智,何登发,范土芝.含油气系统术语、研究流程与核心内容之我见. 中国含油气系统的应用与进展.北京:石油工业出版社,2001.
[75] 赵文智,何登发等.复合含油气盆地中油气运移流向研究的意义.石油学报,2001,22(4):7～14
[76] 赵文智,何登发等.含油气系统术语、研究流程与核心内容之我见. 中国含油气系统的应用与进展.北京:石油工业出版社,2001.9～22
[77] 周济元等.地质力学导论.四川:成都科技大学出版社,1989
[78] 朱英.中国及邻区大地构造和深部构造纲要.北京:地质出版社,2004.
[79] Aitken J. F.,Howell J. A. High-resolution sequence stratigraphy: innovation,application and future prospects. In: Howell J. A.,Aitken J F. High resolution sequence stratigraphy, innovations and application. Geology Society Special publication,1996:1-9.
[80] Brett C E,Goodman W M,LoDuca S T. 1990.Sequence,cycles,and basin dynamics in the Silurian of the Appalachian Foreland Basin. Sedimentary Geology, 69:191～224.
[81] Brett C. E.,Goodman W. M.,LoDuca S. T. Sequence,cycles,and basin dynamics in the Silurian of the Appalachian Foreland Basin. Sedimentary Geology,1990,69:191-224.
[82] Cross Timothy A., Lessenger Margaret A. Sediment Volume Partitioning: Rationale for Stratigraphic Model Evaluation and High Resolution Stratigraphic Correlation. 1998, Predictive high resolution sequence stratigraphy: Norwegian Petroleum Society Special Publication 8: 1-23.
[83] FL W Posamentier, G P Allen, D P Jamses, et al. High Resolution Sequence Stratigraphy – the East Coulee Delta,Alberta. Journal of Sedimentary Petrology, 1992,62(2):310-317.
[84] Gladstone C., Ritchie L. J., Sparks R. S. J.,Woods A. W. An experimental investigation of density – stratified inertial gravity currents. Sedimentology,2004,51:767-789.
[85] Lister G S, Etheridge M A, Symonds P A. Detachment faulting and the evolution of passive continental margion. geology, 1986,14:246～250
[86] Lister G S, Etheridge M A, Symonds P A. Detachment faulting and the evolution of passive continental margion. geology, 1986,14:246-250
[87] Magoon L B(著),杨瑞召等(译).含油气系统及其研究方法.北京:地质出版社,1992
[88] Magoon L B. petroleum system of the United States. U.S. Geological Survey Bulletin 1870,1988
[89] Magoon L B. and Dow W G. The petroleum system: from source to trap. AAPG Memoir 60,1994
[90] Marsaglia K. M,Klein G. D. The Paleogeograpgy of Paleozoic and Mesozoic storm depositional systems. Journal of Geology,1983,91(2):117-142.
[91] Mckenzic D P.Some remarks on the development of sedimentary basins. Earth Planet Sci Letters,1987,40:25~32
[92] Mckenzic D P.Some remarks on the development of sedimentary basins. Earth Planet Sci Letters,1987,40:25-32
[93] Mitchum R. M. Jr.,Van Wagoner J. C. High frequency sequence and their stacking patter-Sequence stratigraphic evidence of high frequency eustatic cycles. Sedimentary Geology,1991,70:131-160.
[94] Perrodon A and Masse P. Subsidence, sedimentation and petroleum system, Journal of Petroleum Geology,1984,7(1):5～26
[95] Perrodon A. Geodynamics of oil and gas accumulations. Pau, Elf Aquitaine,1983,187～210
[96] Perrodon A. Geodynamique petroliere. Genese et repartition des qisements d' hydrocarbures. Paris, Masson-Elf Aquitaine,1980
[97] Seber D, Barazang M, Ibebrahim A et al. Geophysical evidence for lithosperic delam ination beneath the Alboran Sea and Rif-betic mountain. Nature. 1996,379:785～790
[98] Seber D, Barazang M, Ibebrahim A et al. Geophysical evidence for lithosperic delam ination beneath the Alboran Sea and Rif-betic mountain. Nature. 1996,379:785-790
[99] Timothy A. Cross and Margaret A. Lessenger, et al. Sedimentary Volume Partitioning: Rationale for Stratigraphic Model Evaluation and High-Resolution Stratigraphic Correlation. Preprint from K.O. Sandvik, F.Gradstein, and N. Miltion, eds., 1998,Predictive high resolution sequence stratigraphy: Norwegian petroleum Society Special publication 8.
[100] Wemick B. Uniform – sense normal simple shear of the continental lithosphere. Can J Earth Sci, 1985,22:108～125
[101] Wemick B. Uniform – sense normal simple shear of the continental lithosphere. Can J Earth Sci, 1985,22:108-125
[2] 陈广军,宋国奇,王永诗,等.斜坡扇低位域砂岩体岩性油气藏勘探方法-以埕岛潜山披覆构造东部斜坡带为例. 石油学报,2002,23(3):34-38.
[3] 程学儒.松辽盆地北部油气聚集地基本特征和勘探方向.见:徐数宝,胡见义.中国油气聚集与分布 .北京:石油工业出版社,1991.24～38
[4] 程学儒.松辽盆地北部油气聚集地基本特征和勘探方向.徐数宝,胡见义.中国油气聚集与分布.北京:石油工业出版社,1991.
[5] 迟元林,云金表等.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
[6] 邓宏文,王红亮,王居峰,等. 层序地层构成与层序控砂、控藏的自相似性特征-以三角洲-浊积扇为例.石油与天然气地质,2004,25(5):491-495.
[7] 丁正言,韩广玲,张 惠,等.松辽盆地南部油气聚集的成因类型和分部模式. 见:徐数宝,胡见义.中国油气聚集与分布 .北京:石油工业出版社,1991.38～48
[8] 高 山,金振民等.拆沉作用及其壳—幔演化动力学意义.地质科技情报,1997,16(1):1～9
[9] 高瑞琪,赵传本,乔秀云,郑玉龙,闫凤云,万传彪.松辽盆地白垩纪石油地层孢粉学.北京:地质出版社,1999
[10] 高瑞琪,赵传本,乔秀云,郑玉龙,闫凤云,万传彪.松辽盆地白垩纪石油地层孢粉学.北京:地质出版社,1999
[11] 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.
[12] 高瑞祺,赵政璋.中国油气新区勘探(第二卷)—中国陆上天然气勘探新领域.290～315.北京:石油工业出版社,2001
[13] 高山林,陈海泓,窦伟坦,等. 鄂尔多斯盆地延长组的湖泊风暴沉积.沉积学报,1999,17(增刊):758-763.
[14] 韩晓东,楼章华,姚炎明,杨卫东,蔡希源.松辽盆地湖泊浅水三角洲沉积动力学研究. 矿物学报,2000,20(3):305-314
[15] 候贵廷,冯大晨,等.松辽盆地的反转构造作用及其对油气成藏的影响.石油与天然气地质.2004,25(1):49～57
[16] 胡见义,王明明等.含油气地质单元序列中含油气系统的研究与应用.中国含油气系统的应用与进展.北京:石油工业出版社,2001.3～8
[17] 胡明毅,贺 萍. 潮坪风暴沉积特征及其研究意义.地球科学进展,2002,17(3):391-396.
[18] 胡望水.正反转构造与油气聚集.北京:石油工业出版社,2000.
[19] 胡望水.正反转构造与油气聚集.北京:石油工业出版社,2000.
[20] 黄福堂.松辽盆地油气水地球化学.北京:石油工业出版社,1999
[21] 贾承造.前陆冲断带油气勘探.北京:石油工业出版社,2000.
[22] 李德生.中国含油气盆地构造学.北京:石油工业出版社,2002.
[23] 李冬旭.旋钮构造动力学—理论、方法及应用. 北京:地质出版社,2003.
[24] 李丕龙,张善文,宋国奇,肖焕钦,等.济阳成熟区非构造油气藏深化勘探.石油学报,2003,24(5):10-15
[25] 李思田,路凤香,林畅松,等.中国东部及邻区中、新生代盆地演化及地球动力学背景.北京:中国地质大学出版社,1997
[26] 李思田,潘元林,陆永潮,等. 断陷湖盆隐蔽性油气藏预测及勘探的关键技术—高精度地震探测基础上的层序地层学研究. 地球科学—中国地质大学学报,2002,27(5):592-598.
[27] 林畅松,潘元林,肖建新,等.构造坡折带断陷湖盆层序和油气预测的重要概念.地球科学-中国地质大学学报,2000,25(3):260-267.
[28] 刘和甫;梁慧社,等.中国东部新生代裂陷盆地与伸展山岭耦合机制.地学前缘.2000,7(4):477～487
[29] 刘招君;董清水等.陆相层序地层学导轮与应用.北京:石油工业出版社,2002.
[30] 马宗晋,杜品仁,洪汉净.地球构造与动力学.广州:广东科技出版社,2003.
[31] 马宗晋,杜品仁,洪汉净.地球构造与动力学.广州:广东科技出版社,2003.
[32] 牛数银,孙爱群等.造山带与盆地间物质的横向迁移.地学前缘.1995,2(1～2):85～93
[33] 潘元林,宋国洪,郭玉新,等.济阳断陷湖盆层序地层学及砂砾岩油气藏群.石油学报,2003,24(3):16-23.
[34] 潘元林等. 1998. 中国隐蔽油气藏. 地质出版社
[35] 宋国洪,冯有良,刘承华,李传华,等.同沉积断裂带砂砾岩隐蔽性油藏研究-以东营凹陷胜北断裂带为例.石油试验地质,2003,25(3):274～281
[36] 隋淑玲,赵开连等.断裂构造在油气成藏中的作用-以齐阳坳陷曲堤油田为例.石油地球物理勘探.2003,38(6):666～670
[37] 万天丰;朱 鸿等.中国大陆及邻区中生代—新生代大地构造与环境变迁.现代地质.2002,16(2):107～121
[38] 王春鹏,马玉龙,时庚戊.辽河油区油田开发实践.北京:石油工业出版社,2002.
[39] 王东坡等. 沉积盆地地球动力学系统的研究—以辽西、辽北、松辽盆地为例.石油与天然气地质.1999,20(4):273～279
[40] 王建功,王天琦,粱苏娟,等. 松辽盆地北部葡萄花油层事件沉积.石油学报,2005,26(6):20～24
[41] 王建功,王天琦,粱苏娟,等. 松辽盆地北部葡萄花油层事件沉积.石油学报,2005,26(6):20～24
[42] 王建功,卫平生,贺顺义,王斌婷.松辽盆地南部大麻苏—大情字井区低阻油层识别.西北油气勘探,2004,16(4):27～33.
[43] 王建功,卫平生,史永苏,王斌婷,潘树新.松辽盆地南部西部斜坡区大规模岩性油气藏和地层超覆油气藏成藏条件.中国石油勘探,2003,8(3):27～30.
[44] 王建功,卫平生,杨建礼.松辽盆地南部青山口组三段底界不整合面与油气分布.地质论评,2005,26(2):26～29
[45] 王建功,卫平生,赵占银,潘树新,赵志魁,等.松南西部勘探领域及前景.中国石油勘探,2005,10(3):8～15
[46] 王建功,卫平生,郑浚茂,等.挠曲坡折带特征与油气勘探-以松辽盆地南部为例.石油学报,2005,26(2):1～5
[47] 王建功,吴克平,卫平生,赵占银,潘树新,赵志魁.松辽盆地南部西区断裂体系与油气分布.新疆石油地质,2005,26(1):29～32.
[48] 王涛.中国东部裂谷盆地油气藏地质.北京:石油工业出版社,1997.
[49] 王燮培;费 琪等.石油勘探构造分析.北京:中国地质大学出版社,1992
[50] 王训练. 露头层序地层学研究中定义和识别不同级别沉积层序的标准.中国科学(D 辑),2003,33(11):1057-1068.
[51] 王英民,金武弟等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义.石油与天然气地质,2003,24(3):199-203.
[52] 王英民,刘豪等.准噶尔大型坳陷湖盆坡折带的类型和分布特征.地球科学,2002,27(5):683-688.
[53] 王永春.松辽盆地南部岩性油藏的形成和分布. 北京:地质出版社,2001.
[54] 卫平生,李天顺,李安春,王建功.巴彦浩特盆地石炭系沉积相及沉积演化. 沉积学报,2005,23(2).
[55] 卫平生,王建功,潘树新,王斌婷.河口坝、沿岸坝的形成及成藏机制-以松辽盆地西、南沉积体系为例,新 疆石油地质,2004,25(6)592-595
[56] 魏魁生. 非海相层序地层学.北京:地质出版社,1996.
[57] 吴孔友,查 明,柳广弟.2002.准噶尔盆地二叠系不整合面及其油气运聚特征.石油勘探与开发,29(2):53～58.
[58] 吴永平,杨池银,王喜双.2000.渤海湾盆地北部奥陶系潜山油气藏成藏组合及勘探技术.石油勘探与开发,27(5):1-6.
[59] 许怀大,王世凤,陈开远.地震地层学解释基础.武汉:中国地质大学出版社,1990.
[60] 许世远,邵虚生. 杭州湾北部滨岸的风暴沉积.中国科学(B),1984(12):1136-1143.
[61] 许世远. 长江三角洲地区风暴沉积研究.北京:科学出版社,1997.
[62] 严钦尚. 论滨岸浅海的风暴沉积.海洋与沼泽,1984,15(1):14-19.
[63] 杨万里,高瑞琪,郭庆福,刘耀光. 松辽盆地陆相油气生成运移和聚集.哈尔滨:黑龙江科学技术出版社,1985.
[64] 叶德泉,黄清华,张 莹,陈春瑞. 松辽盆地白垩纪介形类生物地层学学. 北京:石油工业出版社,2002,56-74.
[65] 于文卿,松 希,于恩君,屈旭钧.1999.松辽盆地白垩系地层时代划分.铀矿地质,15(5):257～266.
[66] 俞凯,侯洪斌.松辽盆地南部断陷层系石油天然气地质.北京:石油工业出版社,2002
[67] 曾允孚,夏文杰. 沉积岩石学.北京:地质出版社,1986,32-34.
[68] 翟光明,宋建国,靳久强,高维亮.板块构造演化与含油气盆地形成和评价.北京:石油工业出版社,2002.
[69] 翟光明,宋建国,靳久强,高维亮.板块构造演化与含油气盆地形成和评价.北京:石油工业出版社,2002.
[70] 张国栋. 现代滨岸风暴沉积—以舟山普陀岛、朱家尖岛为例.沉积学报,1987,5(2):17-27.
[71] 张善文,王英民,李群.应用坡折带理论寻找隐蔽油气藏.石油勘探与开发,2003,30(3):5-7
[72] 张万选,张厚福,曾洪流,刘震,高先志,刘镇江.陆相地震地层学.山东东营:石油大学出版社:1993.
[73] 张玉明,夏响华.松辽盆地南部低渗透油气田勘探技术.北京:石油工业出版社,2001
[74] 赵文智,何登发,范土芝.含油气系统术语、研究流程与核心内容之我见. 中国含油气系统的应用与进展.北京:石油工业出版社,2001.
[75] 赵文智,何登发等.复合含油气盆地中油气运移流向研究的意义.石油学报,2001,22(4):7～14
[76] 赵文智,何登发等.含油气系统术语、研究流程与核心内容之我见. 中国含油气系统的应用与进展.北京:石油工业出版社,2001.9～22
[77] 周济元等.地质力学导论.四川:成都科技大学出版社,1989
[78] 朱英.中国及邻区大地构造和深部构造纲要.北京:地质出版社,2004.
[79] Aitken J. F.,Howell J. A. High-resolution sequence stratigraphy: innovation,application and future prospects. In: Howell J. A.,Aitken J F. High resolution sequence stratigraphy, innovations and application. Geology Society Special publication,1996:1-9.
[80] Brett C E,Goodman W M,LoDuca S T. 1990.Sequence,cycles,and basin dynamics in the Silurian of the Appalachian Foreland Basin. Sedimentary Geology, 69:191～224.
[81] Brett C. E.,Goodman W. M.,LoDuca S. T. Sequence,cycles,and basin dynamics in the Silurian of the Appalachian Foreland Basin. Sedimentary Geology,1990,69:191-224.
[82] Cross Timothy A., Lessenger Margaret A. Sediment Volume Partitioning: Rationale for Stratigraphic Model Evaluation and High Resolution Stratigraphic Correlation. 1998, Predictive high resolution sequence stratigraphy: Norwegian Petroleum Society Special Publication 8: 1-23.
[83] FL W Posamentier, G P Allen, D P Jamses, et al. High Resolution Sequence Stratigraphy – the East Coulee Delta,Alberta. Journal of Sedimentary Petrology, 1992,62(2):310-317.
[84] Gladstone C., Ritchie L. J., Sparks R. S. J.,Woods A. W. An experimental investigation of density – stratified inertial gravity currents. Sedimentology,2004,51:767-789.
[85] Lister G S, Etheridge M A, Symonds P A. Detachment faulting and the evolution of passive continental margion. geology, 1986,14:246～250
[86] Lister G S, Etheridge M A, Symonds P A. Detachment faulting and the evolution of passive continental margion. geology, 1986,14:246-250
[87] Magoon L B(著),杨瑞召等(译).含油气系统及其研究方法.北京:地质出版社,1992
[88] Magoon L B. petroleum system of the United States. U.S. Geological Survey Bulletin 1870,1988
[89] Magoon L B. and Dow W G. The petroleum system: from source to trap. AAPG Memoir 60,1994
[90] Marsaglia K. M,Klein G. D. The Paleogeograpgy of Paleozoic and Mesozoic storm depositional systems. Journal of Geology,1983,91(2):117-142.
[91] Mckenzic D P.Some remarks on the development of sedimentary basins. Earth Planet Sci Letters,1987,40:25~32
[92] Mckenzic D P.Some remarks on the development of sedimentary basins. Earth Planet Sci Letters,1987,40:25-32
[93] Mitchum R. M. Jr.,Van Wagoner J. C. High frequency sequence and their stacking patter-Sequence stratigraphic evidence of high frequency eustatic cycles. Sedimentary Geology,1991,70:131-160.
[94] Perrodon A and Masse P. Subsidence, sedimentation and petroleum system, Journal of Petroleum Geology,1984,7(1):5～26
[95] Perrodon A. Geodynamics of oil and gas accumulations. Pau, Elf Aquitaine,1983,187～210
[96] Perrodon A. Geodynamique petroliere. Genese et repartition des qisements d' hydrocarbures. Paris, Masson-Elf Aquitaine,1980
[97] Seber D, Barazang M, Ibebrahim A et al. Geophysical evidence for lithosperic delam ination beneath the Alboran Sea and Rif-betic mountain. Nature. 1996,379:785～790
[98] Seber D, Barazang M, Ibebrahim A et al. Geophysical evidence for lithosperic delam ination beneath the Alboran Sea and Rif-betic mountain. Nature. 1996,379:785-790
[99] Timothy A. Cross and Margaret A. Lessenger, et al. Sedimentary Volume Partitioning: Rationale for Stratigraphic Model Evaluation and High-Resolution Stratigraphic Correlation. Preprint from K.O. Sandvik, F.Gradstein, and N. Miltion, eds., 1998,Predictive high resolution sequence stratigraphy: Norwegian petroleum Society Special publication 8.
[100] Wemick B. Uniform – sense normal simple shear of the continental lithosphere. Can J Earth Sci, 1985,22:108～125
[101] Wemick B. Uniform – sense normal simple shear of the continental lithosphere. Can J Earth Sci, 1985,22:108-125