垦东凸起及邻区构造特征与油气聚集
|
摘要
垦东凸起是渤海湾盆地南部的一个次级凸起,周围凹陷众多、油气资源丰富,是渤海湾盆地重要的油气勘探区之一。垦东凸起及邻区构造样式复杂,包含伸展构造体系、扭动构造体系和反转构造体系控制下的断层和断块体组合。
为了深入研究垦东凸起及邻区的构造特征与油气聚集规律,寻找有利的油气圈闭,利用伸展构造研究的理论和方法,以勘探实践和地质研究为基础,研究了垦东凸起及邻区的构造演化史,分析了构造几何学、运动学特征,探讨了各种类型的构造样式,初步总结了油气圈闭类型,提出了勘探目标,主要取得成果如下:
1、垦东凸起及邻区经历了裂谷期前(前古近纪)、裂谷期(古近纪)、裂谷期后(新近纪)三大发育阶段,纵向上呈三层结构分布。
2、垦东凸起周围众多凹陷和凸起平面上被一系列北北东向调节带所分开,呈现“南北分带、东西分块”的断块构造格局。渤海湾中南部地区五条大型的横向调节带中,控制垦东凸起构造格局的为第三条调节带和第四条调节带。
3、通过计算伸展系数、断层生长指数、沉降速率、断层落差等参数,分析了垦东凸起及邻区断块体运动类型:伸展运动、掀斜或旋转运动和垂直差异升降运动,总结出区域构造演化活动具有断陷早期活动剧烈、断陷晚期逐步减弱并趋于中止的特点。
4、垦东凸起及邻区构造样式可划分为伸展构造、扭动构造、局部反转构造等三大类共9种构造样式。
5、垦东凸起及邻区的油气圈闭包括构造圈闭、地层圈闭、岩性圈闭和复合圈闭四大类15种类型。
6、垦东凸起油气主要来自古近纪黄河口伸展断陷生油中心,自北向南沿砂体、不整合面和正断层呈阶梯状侧向和垂向运移至北部斜坡带和凸起,在新近纪和古近纪地层组成的二楼结构和其中有利圈闭处聚集。
7、断层是垦东凸起、青东凹陷及邻区油气藏形成与分布的主控因素,储层及盖层发育影响油气富集与分布,不整合面控制了青东凹陷岩性、地层油气藏的分布。
Kendong Uplift is a subsidiary uplift of the southern Bohai Bay basin. There are four sags adjoining the uplift and hydrocarbon is rich, so the uplift and adjacent region is an important target area of Bohai Bay basin. The tectonic style of Kendong Uplift and adjacent region is complex, including all kinds of faults and fault-block associations which are controlled by extensional tectonic system, shear tectonic system, and reversal tectonic system.
In order to study the tectonic characteristics and hydrocarbon accumulation rules of Kendong uplift, Qingdong sag and adjacent region, and look for advantaged traps, based on the exploring practice and research of geology, the study utilizes the theories and methods about extensional structure, recovers the tectonic evolution history of Kendong Uplift and adjacent region, analyzes structural geometry and kinematics characteristics, discusses all kinds of structure styles, summarizes the trap types, and brings forward exploring targets. Seven results are gained from the study on the geology, geophysics, and geochemistry of Kendong Uplift and adjacent region:
1. The tectonic evolution history shows that Kendong Uplift and adjacent region experienced three stages: Pre-rift Period, Rifting Period, and Post-rift Period. So the stratum shows three-layer structure in architecture.
2. For the existence of the extensional rift, uplift and transverse accommodation zone joined the rift and uplift, the regional structure of the Kendong Uplift and adjacent region can be divided into several belts and sections on the SN and EW direction. Among the five transverse accommodation zones, the third and forth the transverse accommodation zone control the tectonic pattern of the Kendong Uplift and adjacent region.
3. Based on the calculating of the extensional coefficient, fault growing index, subsidence rate, and fault throw, the study analyzes the fault block movement types of Kendong Uplift and adjacent region: extensional movement, rotational movement and differential uplift and depression. The characteristic of the region structural evolution movement was strengthen in the early stage of rift Period and gradually weakened in the late rift Period and Post-rift Period are concluded.
4. The tectonic style of Kendong uplift, Qingdong sag and adjacent region can be divided three systems: extensional system, shear system, and reversal system, which including nine style.
5. The hydrocarbon trap of Kendong Uplift, Qingdong sag and adjacent region can be divided five types: structure trap, lithologic trap, stratigraphic trap, and combination trap, which including fifteen subtypes.
6. The hydrocarbon of Kendong Uplift and adjacent region mainly come from the source center of Palogene Huanghekou extensional rift. By stair-stepping broadside and lengthways pathway formed by unconformity surface, sand bodies, and normal faults, hydrocarbon migrates to Kendong Uplift from north to south, and accumulates in advantaged traps of the Palogene and Neogene stratum.
7. Fault is one of the main controlling factors of hydrocarbon formation, migration, accumulation, and distribution in Kendong uplift, Qingdong sag and other adjacent region; reservoir and cap rock influence the hydrocarbon concentration and distribution; unconformity surface controls the distribution of lithologic reservoir and stratigraphic reservoir in Qingdong sag.
为了深入研究垦东凸起及邻区的构造特征与油气聚集规律,寻找有利的油气圈闭,利用伸展构造研究的理论和方法,以勘探实践和地质研究为基础,研究了垦东凸起及邻区的构造演化史,分析了构造几何学、运动学特征,探讨了各种类型的构造样式,初步总结了油气圈闭类型,提出了勘探目标,主要取得成果如下:
1、垦东凸起及邻区经历了裂谷期前(前古近纪)、裂谷期(古近纪)、裂谷期后(新近纪)三大发育阶段,纵向上呈三层结构分布。
2、垦东凸起周围众多凹陷和凸起平面上被一系列北北东向调节带所分开,呈现“南北分带、东西分块”的断块构造格局。渤海湾中南部地区五条大型的横向调节带中,控制垦东凸起构造格局的为第三条调节带和第四条调节带。
3、通过计算伸展系数、断层生长指数、沉降速率、断层落差等参数,分析了垦东凸起及邻区断块体运动类型:伸展运动、掀斜或旋转运动和垂直差异升降运动,总结出区域构造演化活动具有断陷早期活动剧烈、断陷晚期逐步减弱并趋于中止的特点。
4、垦东凸起及邻区构造样式可划分为伸展构造、扭动构造、局部反转构造等三大类共9种构造样式。
5、垦东凸起及邻区的油气圈闭包括构造圈闭、地层圈闭、岩性圈闭和复合圈闭四大类15种类型。
6、垦东凸起油气主要来自古近纪黄河口伸展断陷生油中心,自北向南沿砂体、不整合面和正断层呈阶梯状侧向和垂向运移至北部斜坡带和凸起,在新近纪和古近纪地层组成的二楼结构和其中有利圈闭处聚集。
7、断层是垦东凸起、青东凹陷及邻区油气藏形成与分布的主控因素,储层及盖层发育影响油气富集与分布,不整合面控制了青东凹陷岩性、地层油气藏的分布。
Kendong Uplift is a subsidiary uplift of the southern Bohai Bay basin. There are four sags adjoining the uplift and hydrocarbon is rich, so the uplift and adjacent region is an important target area of Bohai Bay basin. The tectonic style of Kendong Uplift and adjacent region is complex, including all kinds of faults and fault-block associations which are controlled by extensional tectonic system, shear tectonic system, and reversal tectonic system.
In order to study the tectonic characteristics and hydrocarbon accumulation rules of Kendong uplift, Qingdong sag and adjacent region, and look for advantaged traps, based on the exploring practice and research of geology, the study utilizes the theories and methods about extensional structure, recovers the tectonic evolution history of Kendong Uplift and adjacent region, analyzes structural geometry and kinematics characteristics, discusses all kinds of structure styles, summarizes the trap types, and brings forward exploring targets. Seven results are gained from the study on the geology, geophysics, and geochemistry of Kendong Uplift and adjacent region:
1. The tectonic evolution history shows that Kendong Uplift and adjacent region experienced three stages: Pre-rift Period, Rifting Period, and Post-rift Period. So the stratum shows three-layer structure in architecture.
2. For the existence of the extensional rift, uplift and transverse accommodation zone joined the rift and uplift, the regional structure of the Kendong Uplift and adjacent region can be divided into several belts and sections on the SN and EW direction. Among the five transverse accommodation zones, the third and forth the transverse accommodation zone control the tectonic pattern of the Kendong Uplift and adjacent region.
3. Based on the calculating of the extensional coefficient, fault growing index, subsidence rate, and fault throw, the study analyzes the fault block movement types of Kendong Uplift and adjacent region: extensional movement, rotational movement and differential uplift and depression. The characteristic of the region structural evolution movement was strengthen in the early stage of rift Period and gradually weakened in the late rift Period and Post-rift Period are concluded.
4. The tectonic style of Kendong uplift, Qingdong sag and adjacent region can be divided three systems: extensional system, shear system, and reversal system, which including nine style.
5. The hydrocarbon trap of Kendong Uplift, Qingdong sag and adjacent region can be divided five types: structure trap, lithologic trap, stratigraphic trap, and combination trap, which including fifteen subtypes.
6. The hydrocarbon of Kendong Uplift and adjacent region mainly come from the source center of Palogene Huanghekou extensional rift. By stair-stepping broadside and lengthways pathway formed by unconformity surface, sand bodies, and normal faults, hydrocarbon migrates to Kendong Uplift from north to south, and accumulates in advantaged traps of the Palogene and Neogene stratum.
7. Fault is one of the main controlling factors of hydrocarbon formation, migration, accumulation, and distribution in Kendong uplift, Qingdong sag and other adjacent region; reservoir and cap rock influence the hydrocarbon concentration and distribution; unconformity surface controls the distribution of lithologic reservoir and stratigraphic reservoir in Qingdong sag.
引文
[1]李丕龙,张善文,曲寿利,等.2003,陆相断陷盆地油气地质与勘探(一)[M].北京:石油工业出版社,地质出版社,105-108.
[2]陈发景,汪新文. 1997,中国中.新生代含油气盆地成因类型.构造体系及地球动力学模式[J].现代地质, 11(4): 411-424.
[3] Andrew D Miall, Principles of Sedimentary Basin Analysis[M]. 1984, New York: Springer- Verlag, 668.
[4] Allen P A, Allen J R.1990. Basin analysis: principle and application. Blackwell scientific publications, Oxford, London, 464.
[5] Lerche I. 1990, Basin Analysis:Quantitative Methods. Academic Press Inc,164.
[6] Einsele G. 1992. Sedimentary Basins-evolution, Facies, and Sediment Budget. Springer- Verlag, 628.
[7] Busby C J, Ingersoll R V. 1995.Tectonics of Sedimentary Basin. Blackwell Scientific Publications. Oxford. 234-236.
[8]陆克政,朱筱敏,漆家福. 2004,含油气盆地分析[M].东营,石油大学出版社. 67-73.
[9]陈发景,汪新文,陈昭年等. 2004,2伸展断陷盆地分析[M].北京:地质出版社, 48-251.
[10]陆克政,漆家福,戴俊生.1997.渤海湾盆地新生代含油气盆地构造模式[M].北京:地质出版社, 102-104.
[11]陈发景. 1993,盆地分析-伸展盆地[M].北京:地质出版社, 100-120.
[12]朱夏.1982,试论中国中新生代含油气盆地的地球动力学背景[M].见朱夏主编,中国中新生代盆地构造和演化.北京:科学出版社,1-10.
[13]马杏垣,刘和甫,王维襄. 1983,中国东部中新生代裂陷作用及伸展构造[J].地质学报,57(1)22-32.
[14]李德生. 1980.渤海湾地质构造特征[J].石油学报,1(1):7-20.
[15]李德生. 1980,渤海湾含油气盆地的地质构造特征与油气田分布规律[J].海洋地质与第四纪地质, 1(1):1-12.
[16]刘和甫,梁惠社,李晓清等.2000.中国东部中新生代裂陷盆地与伸展山岭耦合机制[J].地学前缘.7(4)477-486.
[17]陆克政,戴俊生.1994.胶莱走滑拉分盆地的形成和演化[M].东营:石油大学出版社.167.
[18]陆克政,戴俊生,陈书平.1995.胶莱盆地的形成和演化[M].东营:石油大学出版社.153.
[19]李思田,解习农,王华,焦养泉,任建业,庄新国,陆永潮. 2004,沉积盆地分析基础与应用[M],高等教育出版社,403.
[20]陈发景,赵海玲,陈昭年.1996.中国东部中.新生代伸展盆地构造特征及地球动力学背景[J].地球科学,21(4):355-365.
[21] Robert L. 1987Bates and Julia A. Jackson, Glossary of geology,American Geological Institute, 23-30.
[22] Sylvester AG, 1994,走向滑动断层[M],师开业译,见:构造地质学进展,地质出版社, 68-115.
[23]徐嘉炜. 1995,论走滑断层作用的几个主要问题[J],《地学前缘》,2(2):125-136.
[24] Wilson J T. 1965A new class of fault and their bearing on continental drift,NATURE.
[25] Wilcox R E, Harding T P. 1973,Seely D R. Basic wrench tectonics. AAPG, 57:74-96.
[26] Woodcock N H., Fischer M. 1986, Strike-slip duplexes. Journal of Structural Geology, 8(7):725-735.
[27] Sylvester A G. 1988.Strike-slip faults. Centennial Articles. Geological Society of America bulletin. 100:206-214.
[28] Tapponnier P.Peltzer G.Armijo R. 1986,On the Mechanics of the collision between India and Asia. Collision Tectonics. Geol. Soc. London Special Publication,19:115-157.
[29]徐嘉炜,马国锋. 1992,郯庐断裂带研究的十年回顾[J],地质论评,38(4):316-324.
[30]张用夏,李卢玲.1984,郯庐断裂的平移及其对邻区的影响[M].构造地质论丛.北京:地质出版社, 1-8.
[31]邓乃恭. 1984,中生代华夏类型构造和郯庐断裂体系的特征与形成机制[M].构造地质论丛.北京:地质出版社, 33-38.
[32]冯先岳. 1982,阿尔金断裂带.中国活断裂[M].北京:地震出版, 219-225.
[33]周勇,潘裕生. 1998,茫崖-肃北段阿尔金断裂右旋走滑运动的确定[J].地质科学, 33(1):9- 16.
[34]张连生,钟大赉. 1996,从红河剪切带走滑运动看东亚大陆新生代构造[J],地质科学, 31(4):25-31.
[35]钟大赉,Tapponier P,吴海威等. 1989,大型走滑断裂-碰撞后陆内变形的重要形式[J].科学通报, 34(7):526-529.
[36]吴海威,张连生,秸少承. 1989,红河-哀牢山断裂带-喜山期陆内大型左行走滑剪切带[J].地质科学, (1):1-7.
[37]刘和甫,夏义平.1999,走滑造山带与盆地耦合机制[J],地学前缘,3:12-17.
[38]池英柳,赵文智. 2000,渤海湾盆地新生代走滑构造与油气聚集[J],石油学报, 21(2):14-20.
[39]杨云岭,郭栋. 2004,鲁西地区的走滑断层[J],油气地质与采收率, 11(2):1-5.
[40]姚继峰,廖兴明,于天欣. 1995,辽河盆地构造分析[J].断块油气田, 2(5):21-26.
[41]乔秀夫,张安棣.2002,华北块体-胶辽朝块体与郯庐断裂[J],中国地质,29(4):1-9.
[42]李春昱.1975,用板块构造学说对中国部分地区构造发展的初步分析[J],地球物理学报, 18(1):52-76.
[43]陈宣华,王小凤,张青,陈柏林,陈正乐.Harrison TMark, YinAn,2000,郯庐断裂带形成演化的年代学研究[J],长春科技大学学报, 30(3):215-220.
[44]朱光,宋传中,王道轩,刘国生,徐嘉炜. 2001,郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义[J],中国科学(D辑),31(3):250-256.
[45]牛漫兰,朱光,刘国生,王道轩,宋传中,2002,郯庐断裂带中-南段中生代岩浆活动的构造背景与深部过程[J],地质科学,37(4):393-404.
[46]程捷,万天丰. 1996,郯庐断裂带在新生代的演化[J],地质科技情报,15(3):35-42.
[47] Dahlstrom C.D.A., 1970,Structural geology in the eastern margin of the Canadian Rocky mountains. Bull Of Canadian Petroleum Geology, V.187:332-406.
[48] Morley C.K, 1989,Extension, detachment and sedimentation in continental rifts(with particular reference to East Africa).Tectonics, V.8,No.6:1175-1192.
[49] Faulds J.E., Varga R.J., 1998:The role of accommodation zones and transfer zones in the regional segmentation of extended terranes.In:Faulds J.E.,Stewart J.H. (editors), Accommodation zones and Transfer zones:the regional segmentation of the basinand range provinces. Geol.Soc.,Am.,Special paper 323, 1-45.
[50] Morley CK,Nelson RA,patton TL, etl. 1990,Transfer zone in the east African rift System and their relevance to hydrocarbon exploration in rifts AAPG Bull,[J]. 74(8):1234-1253.
[51] Gibbs A.D., 1983,Balanced cross-section constructions from seismic section in areas of extensional tectonics.[J].Structure Geology, V.5:152-160.
[52]陈发景. 2003,调节带(或传递带)的基本概念和分类[J].现代地质, 17(2): 186-186.
[53]刘德来,王伟. 1994,伸展盆地转换带分析──以松辽盆地北部为例[J],地质科技情报,(2):45-52.
[54]赵红格,刘池阳,杨明慧,王定一, 2000,调节带和转换带及其在伸展区的分段作用[J],世界地质,(2):105-111.
[55]陈昭年,陈发景,王琦.2005,正断层软联接及其传递带类型[J],现代地质,(4):19-23.
[56]陈发景,贾庆素,张洪年.2004,传递带及其在砂体发育中的作用[J].石油与天然气地质, (2):27-31.
[57]张亚敏,陈发景. 2006,穆格莱德盆地构造调节带与勘探前景[J],中国石油勘探,(3):87-91.
[58]石砥石,王永诗,王大华. 2001,垦东凸起上第三系油气成藏特征及勘探技术[J],中国海上油气(地质),15(1):51-55.
[59]林玉祥,唐洪三. 2001,垦东凸起石油地球化学特征与成藏系统划分[J].油气地质与采收率, 8(5): 27-31.
[60]彭存仓,顾菊萍. 2002,垦东地区上第三系馆陶组上段成藏规律研究[J],江汉石油学院学报, 24(4):10-12.
[61]王大华,苏宪锋,魏艳萍. 2003,垦东凸起上第三系油气分布与断层关系研究[J],中国海上油气(地质), 17(4):232-235.
[62]方旭庆, 2006试论走滑运动对垦东地区油气聚集的影响[J],河南石油,20(4):1-3.
[63]付兆辉,李敏.2005,郯庐断裂对垦东地区构造和成藏的影响[J].海洋石油, 25(2): 15-20.
[64]方旭庆,林会喜,王智帮. 2007垦东凸起“陀螺式”演化与油气成藏[J],西安石油大学学报(自然科学版), 22(4):13-16.
[65]胜利油田中国石油地质志编写组.中国石油地质志[M],卷六,胜利油田.北京:石油工业出版社,1987.
[66]杨超,陈清华.2005,济阳坳陷构造演化及其构造层的划分[J].油气地质与采收率, 12(2):9-12.
[67]朱筱敏. 1993,层序地层学原理及应用[M].北京:石油工业出版社, 85-90.
[68]付兆辉,高喜龙,陆友明,李敏,侯仔明.2008.渤海湾盆地垦东凸起构造特征与油气聚集[J],现代地质, 22(4):619-627.
[69] Berg R R, DeMis W D, 1994,Mitsdarffer A R. Hydrodynamic effects on Mission Canyon (Mississippian) oil accumulations, Billings Nose area, North Dakota [J].AAPG Bulletin, 78: 501-518.
[70] Hilde T W C, Uyeda S, Kroenke L. 1977, Evolution of the western Pacific and its margins[J]. Tectonophysics, 38:145-165.
[71]徐嘉炜. 1984,郯城庐江平移断裂系统[M].构造地质论丛.北京:地质出版社, 18-32.
[72]万天丰,朱鸿. 1996,郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报, 2(1):14-27.
[73]邬光辉,漆家福,黄骅盆地一级构造变换带的特征与成因[J].石油与天然气地质, 1999,520(2): 125-128.
[74]茹克. 1990,裂陷盆地的半地堑分析[J],中国海上油气(地质),4(6):1-10.
[75]陈昭年,陈发景,周建生,等.1997,黄骅坳陷中北区和歧口凹陷断裂构造特征及古应力分析[J].现代地质, 11(4): 471-477.
[76]周建生,杨池银,陈发景,等.1997.黄骅坳陷横向变换带的构造特征及成因[J].现代地质, 11(4): 425-432.
[77]王纪祥,陈发景,李趁义. 2003,山东惠民凹陷伸展构造及调节带特征[J].现代地质, 17(2): 203-209.
[78]万天丰,王明明,殷秀兰,等. 2004,渤海湾地区不同方向断裂带的封闭性[J].现代地质, 18(2): 157-163.
[79]陈发景.1983.中国东部第三纪含油气盆地的性质.演化和形成机制[M],北京:科学出版社, 78-83.
[80] Stewart J H.1980. Regional tilt patterns of late Cenozoic basin-range fault blocks, western United States. Bull. Geol. Soc. Am., V. 91,460-464.
[81]陈发景.1983.中国东部第三纪含油气盆地的性质演化和形成机制[M].见朱夏主编,中国中新生代盆地构造和演化.北京:科学出版社,1-10.
[82]漆家福,陈发景. 1992,辽东湾—下辽河裂陷盆地的构造样式[J].石油与天然气地质, 13(3): 272-283.
[83] Riedel W. 1929, Zur mechanic geologischer brucherscheinungen[J].Centralbl F Mineral Geol U pal, B, 354-368.
[84] Camand J F. 1987,Bridge structure as sense of displacement criteria in brittle fault zones[J].Struct Geol, 9:609-620.
[85]严俊君,王燮培. 1996,关于扭动构造的鉴别问题[J].石油与天然气地质, 17(1):8-14.
[86] Larsen P H. 1988,Relay structures in a Lower Permian basement-involved tension system East Greenland[J]. Journal of Structure Geology, 10(1):3-8.
[87]唐辉明. 1992,雁行式断裂构造的形成及其断裂力学意义[J].地球科学, 17(1):25-30.
[88]朱战军,周建勋. 2004,雁列构造是走滑断层存在的充分判据[J],大地构造与成矿学, 28(2):142-148.
[89]葛双成,陈焕疆,丁晓, 1993,花状构造及其对油气勘探的意义[J],石油地球物理勘探, 28(4):453-461.
[90] Harding T P, Lowell J D. 1979,Structural styles,their plate tectonic habitats and hydrocarbon traps in petroleum provinces[J].Bull AAPG, 63:1016-1058.
[91]夏义平,刘万辉,徐礼贵等. 2007,走滑断层的识别标志及其石油地质意义[J].中国石油勘探, (1):17-23.
[92]张交东,刘德良,林会喜,邱连贵,徐佑德,任凤楼,裴磊, 2003,郯庐断裂带南段巨型正花状构造的发现及地质意义[J],中国科学技术大学学报,33(4):486-490.
[93]张岳桥,董树文. 2008,郯庐断裂带中生代构造演化史:进展与新认识[J],地质通报,27(9):23-42.
[94]漆家福,陆克政,张一伟,杨桥,陈发景, 1995,渤海湾盆地区新生代构造与油气的关系[J],石油大学学报(自然科学版), 19(S1):7-13.
[95]漆家福,于福生,陆克政,周建勋,王子煜,杨桥, 2003,渤海湾地区的中生代盆地构造概论[J],地学前缘, 10(S1):199-206.
[96]邓运华, 2001,郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J],中国海上油气(地质), 15(5):301-305.
[97]吴时国,余朝华,邹东波,张海英, 2006,莱州湾地区郯庐断裂带的构造特征及其新生代演化[J],海洋地质与第四纪地质, 26(6):101-110.
[98] Wernicke B. and BurchfielB. 1982, Modes of extensional tectonics. Journal of Structural Geology, 04.
[99] Thorsen C E. 1963,Age of growth faulting in southeast Louisiana 1963(2) Trans Gulf-Coast Ass Geol Socs Age of growth faulting in southeast Louisianna, Gulf Coast Association of Geological Societies Transactions, THORSENCE ,23: 103-110
[100] R.E.Chapman, 1983, Petroleum Geology, Elsevier Science Publishers, Amsterdam, Oxford, New York.
[101]朱世新, 1985,向斜中油气藏圈闭条件的探讨[J],石油实验地质,3: 50-55.
[102]朱世新.宋志祥,王定一,1987,油气田调查勘探与资源评价[M],北京:地质出版社,60-67.
[103] Chamberlin R T. 1919,The building of the Colorado Rockies[J], Journal of Geology, 27: 225–251.
[104] Bucher W H. 1933.The Deformation of the Earth's Crust, Princeton: Princeton University Press.
[105] Dahlstrom C D A.1969,Balanced Cross Sections.Canadian Journal of Earth Science, 6,743~ 757.
[106] Ramsay J G and Huber M I. 1987.The techniques of modern structural Geology V.2. Folds and Fractures,London:Academic Press.
[107]刘光炎,蒋录全. 1994,平衡剖面技术与地震资料解释[J].石油地球物理勘探, 1995, 30: 833-844.
[108]肖安成.1999,平衡剖面的正演模拟方法[J].江汉石油学院学报, 6:1-7.
[109] Eaton G P.1980. Geophysical characteristics of the crust of the Basin and Range Province. In:Continental tectonics, National Academy of Sciences, Washington, D. C.,96-114.
[110] Midland Valley.2007,2Dmove Technical Specification.Download from www.mve.com.
[111] Gibbs A D.1983. Balance cross-section constructions from seismic section in areas of extensional tectonics. Structure Geology, V.5:152-160.
[112]李丕龙,张善文,曲寿利,等,2003,陆相断陷盆地油气地质与勘探(四) [M].北京:石油工业出版社,地质出版社,105-108.
[113]王燮培,费琪,张家骅.1990,石油勘探构造分析[M].武汉:中国地质大学出版社, 174-183.
[114] Otofuji Y,Hayashida A and Torii M. 1985, When was the Japan Sea opened Paleomagnetic evidence from southern Japan. In: Nasu,N., Uyeda,S., Kushiro,I., Kobayashi,K. and Kagami,H. eds. Formation of Active Ocean Margins. Tokyo:Terra, 551-566.
[115] Maruyama S,Isozaki Y,Kimura G,et al. 1997,Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from 750 Ma to the present.Island Arc, 6:121-142.
[116] Northrup C J,Royden L H,Burchfiel B C. 1995,Motion of the Pacific plate relative of Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia.Geology, 23(8):719-722.
[117]国家地震局地质研究所,1998,郯庐断裂[M],北京:地震出版社,12-20.
[118]余朝华,韩清华,董冬冬,陈珊珊,兖鹏. 2008,莱州湾地区郯庐断裂中段新生代右行走滑位移量的估算[J],天然气地球科学,19 (1):62-69.
[119]朱光,王道轩,刘国生,牛漫兰,宋传中.2004.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学, 39(1) : 36-49.
[120]许世红, 2007.深大断裂的研究思路与方法探讨,内部资料.
[121]李春荣,辛仁臣,李建平,刘豪, 2008,郯庐断裂对青东凹陷古近纪沉积体系的控制[J] ,新疆石油地质,29(2):209-213.
[122]徐杰,宋长青,高占武. 1999.营口—潍坊断裂带新生代活动的特征[J].地震地质, 21 (4) :289-300.
[123]陈丕基.1988.郯庐断裂巨大平移的时代与格局[J] .科学通报, 33 (4) : 289-293.
[124]龚再升.2004.中国近海盆地晚期断裂活动和油气成藏[J].中国石油勘探,9 (2) : 12-19.
[125]葛建党.2001.郯庐断裂在渤中凹陷的构造特征与油气成藏的关系[J],海洋石油,(1):14-20.
[126]高祥林.2006.渤海中部郯庐断裂带的近期活动与渤海新近纪新生断裂[J],地质科学, 41 (2) : 355-364.
[127] Glennie K W,Boegner P L. 1981Sole pit inversion tectonics. In:Petroleum Geology of the Continental Shelf of Northwest Europe(Edited by Illing, L V & Hobson, G D). Institute of Petroleum, London,110-120.
[128]胡望水,吕炳全,毛治国,官大勇, 2004,中国东部中新生代含油气盆地的反转构造[J],同济大学学报(自然科学版),24(2)164-170.
[129]褚庆忠, 2004,含油气盆地反转构造研究综述[J],西安石油大学学报(自然科学版),1:34-38.
[130]赵国连.2001.构造反转与油气聚集[J],新疆石油地质,15(6):23-28.
[131]何文渊,钱祥麟,张臣, 1999,区域性构造反转地区含油气性研究[J],地学前缘, S1:52-56.
[132]陈洁,董冬,邱明文,1999,济阳坳陷内的负反转构造及其石油地质意义[J],石油实验地质,3:234-238.
[133]汤良杰,金之钧,张一伟,陆克政,1999,塔里木盆地北部隆起负反转构造及其地质意义[J],现代地质.
[134]林玉祥,俞家声,2001,垦东地区石油成藏系统及其演化[J],地质与勘探,37(5):29-33.
[135]林玉祥, 2000,桩东凹陷西洼油气资源潜力分析[J],地质地球化学,4:42-48.
[136]陈永红,陈庆春,林玉祥,王秀朋,2003,渤海湾盆地垦东凸起油源对比与成藏条件研究[J],地质地球化学, 31(1):16-22.
[137]张善文,王永诗,石砥石,等.2003,网毯式油气成藏体系——以济阳坳陷新近系为例[J].石油勘探与开发, 30(1): 1-9.
[138]胡贤根,姜素华,高平,2005,东营凹陷网毯式成藏体系结构研究[J],石油地球物理勘探.40(4):478-481.
[139]姜素华,查明,张善文,2004,网毯式油气成藏体系的动态平衡研究[J],石油大学学报(自然科学版),28(4):16-20.
[140]石砥石,2005,济阳坳陷太平油田网毯式油气成藏体系研究[J],成都理工大学学报(自然科学版),32(6),592-596.
[141] Norman H Foster and Edward A Beaumont .traps and seals I. Structual/Fault-seal and Hydrodynamic traps. published by aapg.
[142] Rich, J L. 1934, Mechanics of low-angle overthrust faulting as illustrated by Cumberland thrust block, Virginia, Kentucky and Tennessee. Am. Assoc. Petroleum Geologists Bull., 18: 1584-1596.
[143] John Suppe and Donald A. Medwedeff. 1990, Geometry and kinematics of fault- propapation folding. Eclogae geol.Helv. 83(3): 409-454.
[144] Shaw J H, Suppe J. 1994,Active faulting and growth folding in the eastern Santa Barbara Channel, California.Geological Society of America Bulletin, 607-626.
[145] John Suppe. 1985.Principles of structural geology[M]. Prentice-Hall Inc., Englewood Cliffs, New Jersey,203-210.
[146] Clapp F G. 1929,The role of geologic structure in the accumulation of petroleum, in structure of typical American oil fields [J].AAPG, 29(3): 667-716.
[147] Wilson W B. 1934Proposed classification of oil and gas reservoirs [C] // Wrather W E, Lahee F M. Problems of petroleum geology, AAPG Sidney Powers Volume. Tulas: AAPG,433-445.
[148] Levorson A I. 1936,Stratigraphic versus structural accumulation [J].AAPG Bulletin, 20(1): 521-530.
[149] Sanders C W. 1943,Stratigraphic type oil fields and proposed new classification of reservoir traps [J].AAPG Bulletin, 26(2): 538-550.
[150] Wilhelm O. 1945,Classification of petroleum reservoirs [J].AAPG Bulletin, 29(8): 1537-1579.
[151] Levorson A I. 1936,Stratigraphic versus structural accumulation [J].AAPG Bulletin, 20(5): 521-530.
[152] Levorson A I. 2001,Geology of petroleum [J].AAPG Foundation, 85(4): 724-726.
[153] Rittenhouse G. 1972,Stratigraphic-trap classification [C] //King R E. Stratigraphic oil and gas fields-lassification,exploration methods, and case histories, AAPG Memoir. Tulas: AAPG, 10: 14-28.
[154] Biddle K T, Wielchowsky C C. 1994. Hydrocarbon traps[C] // Magoon L B, Dow W G. The petroleum system-from source to trap, AAPG Memoir, Tulas:AAPG,60: 219-235.
[155] Vincelette R R, Beaumont E A, Foster N H. 1999,Classification of exploration traps [C] // Beaumont E A, Foster N H. Exploring for oil and gas traps, AAPG Treatise of Petroleum Geology, Handbook. Tulas: AAPG, 2: 1-42.
[156]张运东,薛红兵,朱如凯,等. 2005,国内外隐蔽油气藏勘探现状[J].中国石油勘探, (3): 64-68.
[157] Norman H Foster and Edward A Beaumont .traps and seals II, Stratigraphic/ Capillary traps. Published by AAPG..
[158]赵追.赵全民.孙冲.王继英.古哲.2001,陆相断陷湖盆的成岩圈闭──以泌阳凹陷下第三系核桃园组三段为例[J],石油与天然气地质,22(2):154-157.
[159] Kusznir N J,Park R G.1987,The extensional strength of the continental lithosphere: its dependence on geothermal gradient,crustal composition and thickness. In: Coward M P,Dewey J F,Hamcock P L(editors). Continental extensional tectonics. Geol. Soc. Spe. Publ, No.28:35-52.
[160] Allen R W Jr. 1955,Stratigraphic gas development in the Blanco-Mesa Verde pool of the San Juan Basin [J].AAPG, 5(1): 195-205.
[161] Andresen M J. 1962,Paleodrainage patterns: their mapping from subsurface data and their paleogeographic value [J].AAPG Bulletin, 46(7): 398-405.
[162] Berg O R. 1982,Seismic detection and evaluation of delta and turbidite sequences: their application to exploration for the subtle trap [J].AAPG Bulletin, 66(9):1271-1288.
[163] Dolson J C, 1999,Bahorich M S, Tobin R C,et al.Exploring for stratigraphic traps [C] // Beaumont E A, Foster N H. exploring for oil. AAPG Treatise of Petroleum Geology. Tulas: AAPG,21: 1-68.
[164]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[J].石油勘探与开发, 27(5):1-4.
[2]陈发景,汪新文. 1997,中国中.新生代含油气盆地成因类型.构造体系及地球动力学模式[J].现代地质, 11(4): 411-424.
[3] Andrew D Miall, Principles of Sedimentary Basin Analysis[M]. 1984, New York: Springer- Verlag, 668.
[4] Allen P A, Allen J R.1990. Basin analysis: principle and application. Blackwell scientific publications, Oxford, London, 464.
[5] Lerche I. 1990, Basin Analysis:Quantitative Methods. Academic Press Inc,164.
[6] Einsele G. 1992. Sedimentary Basins-evolution, Facies, and Sediment Budget. Springer- Verlag, 628.
[7] Busby C J, Ingersoll R V. 1995.Tectonics of Sedimentary Basin. Blackwell Scientific Publications. Oxford. 234-236.
[8]陆克政,朱筱敏,漆家福. 2004,含油气盆地分析[M].东营,石油大学出版社. 67-73.
[9]陈发景,汪新文,陈昭年等. 2004,2伸展断陷盆地分析[M].北京:地质出版社, 48-251.
[10]陆克政,漆家福,戴俊生.1997.渤海湾盆地新生代含油气盆地构造模式[M].北京:地质出版社, 102-104.
[11]陈发景. 1993,盆地分析-伸展盆地[M].北京:地质出版社, 100-120.
[12]朱夏.1982,试论中国中新生代含油气盆地的地球动力学背景[M].见朱夏主编,中国中新生代盆地构造和演化.北京:科学出版社,1-10.
[13]马杏垣,刘和甫,王维襄. 1983,中国东部中新生代裂陷作用及伸展构造[J].地质学报,57(1)22-32.
[14]李德生. 1980.渤海湾地质构造特征[J].石油学报,1(1):7-20.
[15]李德生. 1980,渤海湾含油气盆地的地质构造特征与油气田分布规律[J].海洋地质与第四纪地质, 1(1):1-12.
[16]刘和甫,梁惠社,李晓清等.2000.中国东部中新生代裂陷盆地与伸展山岭耦合机制[J].地学前缘.7(4)477-486.
[17]陆克政,戴俊生.1994.胶莱走滑拉分盆地的形成和演化[M].东营:石油大学出版社.167.
[18]陆克政,戴俊生,陈书平.1995.胶莱盆地的形成和演化[M].东营:石油大学出版社.153.
[19]李思田,解习农,王华,焦养泉,任建业,庄新国,陆永潮. 2004,沉积盆地分析基础与应用[M],高等教育出版社,403.
[20]陈发景,赵海玲,陈昭年.1996.中国东部中.新生代伸展盆地构造特征及地球动力学背景[J].地球科学,21(4):355-365.
[21] Robert L. 1987Bates and Julia A. Jackson, Glossary of geology,American Geological Institute, 23-30.
[22] Sylvester AG, 1994,走向滑动断层[M],师开业译,见:构造地质学进展,地质出版社, 68-115.
[23]徐嘉炜. 1995,论走滑断层作用的几个主要问题[J],《地学前缘》,2(2):125-136.
[24] Wilson J T. 1965A new class of fault and their bearing on continental drift,NATURE.
[25] Wilcox R E, Harding T P. 1973,Seely D R. Basic wrench tectonics. AAPG, 57:74-96.
[26] Woodcock N H., Fischer M. 1986, Strike-slip duplexes. Journal of Structural Geology, 8(7):725-735.
[27] Sylvester A G. 1988.Strike-slip faults. Centennial Articles. Geological Society of America bulletin. 100:206-214.
[28] Tapponnier P.Peltzer G.Armijo R. 1986,On the Mechanics of the collision between India and Asia. Collision Tectonics. Geol. Soc. London Special Publication,19:115-157.
[29]徐嘉炜,马国锋. 1992,郯庐断裂带研究的十年回顾[J],地质论评,38(4):316-324.
[30]张用夏,李卢玲.1984,郯庐断裂的平移及其对邻区的影响[M].构造地质论丛.北京:地质出版社, 1-8.
[31]邓乃恭. 1984,中生代华夏类型构造和郯庐断裂体系的特征与形成机制[M].构造地质论丛.北京:地质出版社, 33-38.
[32]冯先岳. 1982,阿尔金断裂带.中国活断裂[M].北京:地震出版, 219-225.
[33]周勇,潘裕生. 1998,茫崖-肃北段阿尔金断裂右旋走滑运动的确定[J].地质科学, 33(1):9- 16.
[34]张连生,钟大赉. 1996,从红河剪切带走滑运动看东亚大陆新生代构造[J],地质科学, 31(4):25-31.
[35]钟大赉,Tapponier P,吴海威等. 1989,大型走滑断裂-碰撞后陆内变形的重要形式[J].科学通报, 34(7):526-529.
[36]吴海威,张连生,秸少承. 1989,红河-哀牢山断裂带-喜山期陆内大型左行走滑剪切带[J].地质科学, (1):1-7.
[37]刘和甫,夏义平.1999,走滑造山带与盆地耦合机制[J],地学前缘,3:12-17.
[38]池英柳,赵文智. 2000,渤海湾盆地新生代走滑构造与油气聚集[J],石油学报, 21(2):14-20.
[39]杨云岭,郭栋. 2004,鲁西地区的走滑断层[J],油气地质与采收率, 11(2):1-5.
[40]姚继峰,廖兴明,于天欣. 1995,辽河盆地构造分析[J].断块油气田, 2(5):21-26.
[41]乔秀夫,张安棣.2002,华北块体-胶辽朝块体与郯庐断裂[J],中国地质,29(4):1-9.
[42]李春昱.1975,用板块构造学说对中国部分地区构造发展的初步分析[J],地球物理学报, 18(1):52-76.
[43]陈宣华,王小凤,张青,陈柏林,陈正乐.Harrison TMark, YinAn,2000,郯庐断裂带形成演化的年代学研究[J],长春科技大学学报, 30(3):215-220.
[44]朱光,宋传中,王道轩,刘国生,徐嘉炜. 2001,郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义[J],中国科学(D辑),31(3):250-256.
[45]牛漫兰,朱光,刘国生,王道轩,宋传中,2002,郯庐断裂带中-南段中生代岩浆活动的构造背景与深部过程[J],地质科学,37(4):393-404.
[46]程捷,万天丰. 1996,郯庐断裂带在新生代的演化[J],地质科技情报,15(3):35-42.
[47] Dahlstrom C.D.A., 1970,Structural geology in the eastern margin of the Canadian Rocky mountains. Bull Of Canadian Petroleum Geology, V.187:332-406.
[48] Morley C.K, 1989,Extension, detachment and sedimentation in continental rifts(with particular reference to East Africa).Tectonics, V.8,No.6:1175-1192.
[49] Faulds J.E., Varga R.J., 1998:The role of accommodation zones and transfer zones in the regional segmentation of extended terranes.In:Faulds J.E.,Stewart J.H. (editors), Accommodation zones and Transfer zones:the regional segmentation of the basinand range provinces. Geol.Soc.,Am.,Special paper 323, 1-45.
[50] Morley CK,Nelson RA,patton TL, etl. 1990,Transfer zone in the east African rift System and their relevance to hydrocarbon exploration in rifts AAPG Bull,[J]. 74(8):1234-1253.
[51] Gibbs A.D., 1983,Balanced cross-section constructions from seismic section in areas of extensional tectonics.[J].Structure Geology, V.5:152-160.
[52]陈发景. 2003,调节带(或传递带)的基本概念和分类[J].现代地质, 17(2): 186-186.
[53]刘德来,王伟. 1994,伸展盆地转换带分析──以松辽盆地北部为例[J],地质科技情报,(2):45-52.
[54]赵红格,刘池阳,杨明慧,王定一, 2000,调节带和转换带及其在伸展区的分段作用[J],世界地质,(2):105-111.
[55]陈昭年,陈发景,王琦.2005,正断层软联接及其传递带类型[J],现代地质,(4):19-23.
[56]陈发景,贾庆素,张洪年.2004,传递带及其在砂体发育中的作用[J].石油与天然气地质, (2):27-31.
[57]张亚敏,陈发景. 2006,穆格莱德盆地构造调节带与勘探前景[J],中国石油勘探,(3):87-91.
[58]石砥石,王永诗,王大华. 2001,垦东凸起上第三系油气成藏特征及勘探技术[J],中国海上油气(地质),15(1):51-55.
[59]林玉祥,唐洪三. 2001,垦东凸起石油地球化学特征与成藏系统划分[J].油气地质与采收率, 8(5): 27-31.
[60]彭存仓,顾菊萍. 2002,垦东地区上第三系馆陶组上段成藏规律研究[J],江汉石油学院学报, 24(4):10-12.
[61]王大华,苏宪锋,魏艳萍. 2003,垦东凸起上第三系油气分布与断层关系研究[J],中国海上油气(地质), 17(4):232-235.
[62]方旭庆, 2006试论走滑运动对垦东地区油气聚集的影响[J],河南石油,20(4):1-3.
[63]付兆辉,李敏.2005,郯庐断裂对垦东地区构造和成藏的影响[J].海洋石油, 25(2): 15-20.
[64]方旭庆,林会喜,王智帮. 2007垦东凸起“陀螺式”演化与油气成藏[J],西安石油大学学报(自然科学版), 22(4):13-16.
[65]胜利油田中国石油地质志编写组.中国石油地质志[M],卷六,胜利油田.北京:石油工业出版社,1987.
[66]杨超,陈清华.2005,济阳坳陷构造演化及其构造层的划分[J].油气地质与采收率, 12(2):9-12.
[67]朱筱敏. 1993,层序地层学原理及应用[M].北京:石油工业出版社, 85-90.
[68]付兆辉,高喜龙,陆友明,李敏,侯仔明.2008.渤海湾盆地垦东凸起构造特征与油气聚集[J],现代地质, 22(4):619-627.
[69] Berg R R, DeMis W D, 1994,Mitsdarffer A R. Hydrodynamic effects on Mission Canyon (Mississippian) oil accumulations, Billings Nose area, North Dakota [J].AAPG Bulletin, 78: 501-518.
[70] Hilde T W C, Uyeda S, Kroenke L. 1977, Evolution of the western Pacific and its margins[J]. Tectonophysics, 38:145-165.
[71]徐嘉炜. 1984,郯城庐江平移断裂系统[M].构造地质论丛.北京:地质出版社, 18-32.
[72]万天丰,朱鸿. 1996,郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报, 2(1):14-27.
[73]邬光辉,漆家福,黄骅盆地一级构造变换带的特征与成因[J].石油与天然气地质, 1999,520(2): 125-128.
[74]茹克. 1990,裂陷盆地的半地堑分析[J],中国海上油气(地质),4(6):1-10.
[75]陈昭年,陈发景,周建生,等.1997,黄骅坳陷中北区和歧口凹陷断裂构造特征及古应力分析[J].现代地质, 11(4): 471-477.
[76]周建生,杨池银,陈发景,等.1997.黄骅坳陷横向变换带的构造特征及成因[J].现代地质, 11(4): 425-432.
[77]王纪祥,陈发景,李趁义. 2003,山东惠民凹陷伸展构造及调节带特征[J].现代地质, 17(2): 203-209.
[78]万天丰,王明明,殷秀兰,等. 2004,渤海湾地区不同方向断裂带的封闭性[J].现代地质, 18(2): 157-163.
[79]陈发景.1983.中国东部第三纪含油气盆地的性质.演化和形成机制[M],北京:科学出版社, 78-83.
[80] Stewart J H.1980. Regional tilt patterns of late Cenozoic basin-range fault blocks, western United States. Bull. Geol. Soc. Am., V. 91,460-464.
[81]陈发景.1983.中国东部第三纪含油气盆地的性质演化和形成机制[M].见朱夏主编,中国中新生代盆地构造和演化.北京:科学出版社,1-10.
[82]漆家福,陈发景. 1992,辽东湾—下辽河裂陷盆地的构造样式[J].石油与天然气地质, 13(3): 272-283.
[83] Riedel W. 1929, Zur mechanic geologischer brucherscheinungen[J].Centralbl F Mineral Geol U pal, B, 354-368.
[84] Camand J F. 1987,Bridge structure as sense of displacement criteria in brittle fault zones[J].Struct Geol, 9:609-620.
[85]严俊君,王燮培. 1996,关于扭动构造的鉴别问题[J].石油与天然气地质, 17(1):8-14.
[86] Larsen P H. 1988,Relay structures in a Lower Permian basement-involved tension system East Greenland[J]. Journal of Structure Geology, 10(1):3-8.
[87]唐辉明. 1992,雁行式断裂构造的形成及其断裂力学意义[J].地球科学, 17(1):25-30.
[88]朱战军,周建勋. 2004,雁列构造是走滑断层存在的充分判据[J],大地构造与成矿学, 28(2):142-148.
[89]葛双成,陈焕疆,丁晓, 1993,花状构造及其对油气勘探的意义[J],石油地球物理勘探, 28(4):453-461.
[90] Harding T P, Lowell J D. 1979,Structural styles,their plate tectonic habitats and hydrocarbon traps in petroleum provinces[J].Bull AAPG, 63:1016-1058.
[91]夏义平,刘万辉,徐礼贵等. 2007,走滑断层的识别标志及其石油地质意义[J].中国石油勘探, (1):17-23.
[92]张交东,刘德良,林会喜,邱连贵,徐佑德,任凤楼,裴磊, 2003,郯庐断裂带南段巨型正花状构造的发现及地质意义[J],中国科学技术大学学报,33(4):486-490.
[93]张岳桥,董树文. 2008,郯庐断裂带中生代构造演化史:进展与新认识[J],地质通报,27(9):23-42.
[94]漆家福,陆克政,张一伟,杨桥,陈发景, 1995,渤海湾盆地区新生代构造与油气的关系[J],石油大学学报(自然科学版), 19(S1):7-13.
[95]漆家福,于福生,陆克政,周建勋,王子煜,杨桥, 2003,渤海湾地区的中生代盆地构造概论[J],地学前缘, 10(S1):199-206.
[96]邓运华, 2001,郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J],中国海上油气(地质), 15(5):301-305.
[97]吴时国,余朝华,邹东波,张海英, 2006,莱州湾地区郯庐断裂带的构造特征及其新生代演化[J],海洋地质与第四纪地质, 26(6):101-110.
[98] Wernicke B. and BurchfielB. 1982, Modes of extensional tectonics. Journal of Structural Geology, 04.
[99] Thorsen C E. 1963,Age of growth faulting in southeast Louisiana 1963(2) Trans Gulf-Coast Ass Geol Socs Age of growth faulting in southeast Louisianna, Gulf Coast Association of Geological Societies Transactions, THORSENCE ,23: 103-110
[100] R.E.Chapman, 1983, Petroleum Geology, Elsevier Science Publishers, Amsterdam, Oxford, New York.
[101]朱世新, 1985,向斜中油气藏圈闭条件的探讨[J],石油实验地质,3: 50-55.
[102]朱世新.宋志祥,王定一,1987,油气田调查勘探与资源评价[M],北京:地质出版社,60-67.
[103] Chamberlin R T. 1919,The building of the Colorado Rockies[J], Journal of Geology, 27: 225–251.
[104] Bucher W H. 1933.The Deformation of the Earth's Crust, Princeton: Princeton University Press.
[105] Dahlstrom C D A.1969,Balanced Cross Sections.Canadian Journal of Earth Science, 6,743~ 757.
[106] Ramsay J G and Huber M I. 1987.The techniques of modern structural Geology V.2. Folds and Fractures,London:Academic Press.
[107]刘光炎,蒋录全. 1994,平衡剖面技术与地震资料解释[J].石油地球物理勘探, 1995, 30: 833-844.
[108]肖安成.1999,平衡剖面的正演模拟方法[J].江汉石油学院学报, 6:1-7.
[109] Eaton G P.1980. Geophysical characteristics of the crust of the Basin and Range Province. In:Continental tectonics, National Academy of Sciences, Washington, D. C.,96-114.
[110] Midland Valley.2007,2Dmove Technical Specification.Download from www.mve.com.
[111] Gibbs A D.1983. Balance cross-section constructions from seismic section in areas of extensional tectonics. Structure Geology, V.5:152-160.
[112]李丕龙,张善文,曲寿利,等,2003,陆相断陷盆地油气地质与勘探(四) [M].北京:石油工业出版社,地质出版社,105-108.
[113]王燮培,费琪,张家骅.1990,石油勘探构造分析[M].武汉:中国地质大学出版社, 174-183.
[114] Otofuji Y,Hayashida A and Torii M. 1985, When was the Japan Sea opened Paleomagnetic evidence from southern Japan. In: Nasu,N., Uyeda,S., Kushiro,I., Kobayashi,K. and Kagami,H. eds. Formation of Active Ocean Margins. Tokyo:Terra, 551-566.
[115] Maruyama S,Isozaki Y,Kimura G,et al. 1997,Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from 750 Ma to the present.Island Arc, 6:121-142.
[116] Northrup C J,Royden L H,Burchfiel B C. 1995,Motion of the Pacific plate relative of Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia.Geology, 23(8):719-722.
[117]国家地震局地质研究所,1998,郯庐断裂[M],北京:地震出版社,12-20.
[118]余朝华,韩清华,董冬冬,陈珊珊,兖鹏. 2008,莱州湾地区郯庐断裂中段新生代右行走滑位移量的估算[J],天然气地球科学,19 (1):62-69.
[119]朱光,王道轩,刘国生,牛漫兰,宋传中.2004.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学, 39(1) : 36-49.
[120]许世红, 2007.深大断裂的研究思路与方法探讨,内部资料.
[121]李春荣,辛仁臣,李建平,刘豪, 2008,郯庐断裂对青东凹陷古近纪沉积体系的控制[J] ,新疆石油地质,29(2):209-213.
[122]徐杰,宋长青,高占武. 1999.营口—潍坊断裂带新生代活动的特征[J].地震地质, 21 (4) :289-300.
[123]陈丕基.1988.郯庐断裂巨大平移的时代与格局[J] .科学通报, 33 (4) : 289-293.
[124]龚再升.2004.中国近海盆地晚期断裂活动和油气成藏[J].中国石油勘探,9 (2) : 12-19.
[125]葛建党.2001.郯庐断裂在渤中凹陷的构造特征与油气成藏的关系[J],海洋石油,(1):14-20.
[126]高祥林.2006.渤海中部郯庐断裂带的近期活动与渤海新近纪新生断裂[J],地质科学, 41 (2) : 355-364.
[127] Glennie K W,Boegner P L. 1981Sole pit inversion tectonics. In:Petroleum Geology of the Continental Shelf of Northwest Europe(Edited by Illing, L V & Hobson, G D). Institute of Petroleum, London,110-120.
[128]胡望水,吕炳全,毛治国,官大勇, 2004,中国东部中新生代含油气盆地的反转构造[J],同济大学学报(自然科学版),24(2)164-170.
[129]褚庆忠, 2004,含油气盆地反转构造研究综述[J],西安石油大学学报(自然科学版),1:34-38.
[130]赵国连.2001.构造反转与油气聚集[J],新疆石油地质,15(6):23-28.
[131]何文渊,钱祥麟,张臣, 1999,区域性构造反转地区含油气性研究[J],地学前缘, S1:52-56.
[132]陈洁,董冬,邱明文,1999,济阳坳陷内的负反转构造及其石油地质意义[J],石油实验地质,3:234-238.
[133]汤良杰,金之钧,张一伟,陆克政,1999,塔里木盆地北部隆起负反转构造及其地质意义[J],现代地质.
[134]林玉祥,俞家声,2001,垦东地区石油成藏系统及其演化[J],地质与勘探,37(5):29-33.
[135]林玉祥, 2000,桩东凹陷西洼油气资源潜力分析[J],地质地球化学,4:42-48.
[136]陈永红,陈庆春,林玉祥,王秀朋,2003,渤海湾盆地垦东凸起油源对比与成藏条件研究[J],地质地球化学, 31(1):16-22.
[137]张善文,王永诗,石砥石,等.2003,网毯式油气成藏体系——以济阳坳陷新近系为例[J].石油勘探与开发, 30(1): 1-9.
[138]胡贤根,姜素华,高平,2005,东营凹陷网毯式成藏体系结构研究[J],石油地球物理勘探.40(4):478-481.
[139]姜素华,查明,张善文,2004,网毯式油气成藏体系的动态平衡研究[J],石油大学学报(自然科学版),28(4):16-20.
[140]石砥石,2005,济阳坳陷太平油田网毯式油气成藏体系研究[J],成都理工大学学报(自然科学版),32(6),592-596.
[141] Norman H Foster and Edward A Beaumont .traps and seals I. Structual/Fault-seal and Hydrodynamic traps. published by aapg.
[142] Rich, J L. 1934, Mechanics of low-angle overthrust faulting as illustrated by Cumberland thrust block, Virginia, Kentucky and Tennessee. Am. Assoc. Petroleum Geologists Bull., 18: 1584-1596.
[143] John Suppe and Donald A. Medwedeff. 1990, Geometry and kinematics of fault- propapation folding. Eclogae geol.Helv. 83(3): 409-454.
[144] Shaw J H, Suppe J. 1994,Active faulting and growth folding in the eastern Santa Barbara Channel, California.Geological Society of America Bulletin, 607-626.
[145] John Suppe. 1985.Principles of structural geology[M]. Prentice-Hall Inc., Englewood Cliffs, New Jersey,203-210.
[146] Clapp F G. 1929,The role of geologic structure in the accumulation of petroleum, in structure of typical American oil fields [J].AAPG, 29(3): 667-716.
[147] Wilson W B. 1934Proposed classification of oil and gas reservoirs [C] // Wrather W E, Lahee F M. Problems of petroleum geology, AAPG Sidney Powers Volume. Tulas: AAPG,433-445.
[148] Levorson A I. 1936,Stratigraphic versus structural accumulation [J].AAPG Bulletin, 20(1): 521-530.
[149] Sanders C W. 1943,Stratigraphic type oil fields and proposed new classification of reservoir traps [J].AAPG Bulletin, 26(2): 538-550.
[150] Wilhelm O. 1945,Classification of petroleum reservoirs [J].AAPG Bulletin, 29(8): 1537-1579.
[151] Levorson A I. 1936,Stratigraphic versus structural accumulation [J].AAPG Bulletin, 20(5): 521-530.
[152] Levorson A I. 2001,Geology of petroleum [J].AAPG Foundation, 85(4): 724-726.
[153] Rittenhouse G. 1972,Stratigraphic-trap classification [C] //King R E. Stratigraphic oil and gas fields-lassification,exploration methods, and case histories, AAPG Memoir. Tulas: AAPG, 10: 14-28.
[154] Biddle K T, Wielchowsky C C. 1994. Hydrocarbon traps[C] // Magoon L B, Dow W G. The petroleum system-from source to trap, AAPG Memoir, Tulas:AAPG,60: 219-235.
[155] Vincelette R R, Beaumont E A, Foster N H. 1999,Classification of exploration traps [C] // Beaumont E A, Foster N H. Exploring for oil and gas traps, AAPG Treatise of Petroleum Geology, Handbook. Tulas: AAPG, 2: 1-42.
[156]张运东,薛红兵,朱如凯,等. 2005,国内外隐蔽油气藏勘探现状[J].中国石油勘探, (3): 64-68.
[157] Norman H Foster and Edward A Beaumont .traps and seals II, Stratigraphic/ Capillary traps. Published by AAPG..
[158]赵追.赵全民.孙冲.王继英.古哲.2001,陆相断陷湖盆的成岩圈闭──以泌阳凹陷下第三系核桃园组三段为例[J],石油与天然气地质,22(2):154-157.
[159] Kusznir N J,Park R G.1987,The extensional strength of the continental lithosphere: its dependence on geothermal gradient,crustal composition and thickness. In: Coward M P,Dewey J F,Hamcock P L(editors). Continental extensional tectonics. Geol. Soc. Spe. Publ, No.28:35-52.
[160] Allen R W Jr. 1955,Stratigraphic gas development in the Blanco-Mesa Verde pool of the San Juan Basin [J].AAPG, 5(1): 195-205.
[161] Andresen M J. 1962,Paleodrainage patterns: their mapping from subsurface data and their paleogeographic value [J].AAPG Bulletin, 46(7): 398-405.
[162] Berg O R. 1982,Seismic detection and evaluation of delta and turbidite sequences: their application to exploration for the subtle trap [J].AAPG Bulletin, 66(9):1271-1288.
[163] Dolson J C, 1999,Bahorich M S, Tobin R C,et al.Exploring for stratigraphic traps [C] // Beaumont E A, Foster N H. exploring for oil. AAPG Treatise of Petroleum Geology. Tulas: AAPG,21: 1-68.
[164]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[J].石油勘探与开发, 27(5):1-4.