塔里木盆地东部地区盆山耦合与油气聚集
|
摘要
塔里木盆地东部(塔东)为天山及阿尔金山夹持的中新生代盆地,自南华纪至第四纪,经历不同构造环境,发育古隆起,伸展构造、冲断构造和走滑构造,构成盆山耦合。早古生代处于克拉通边缘盆地环境,不同类型原型盆地充填各种沉积序列,形成各类油气系统和评价单元。本文以地球动力学环境为主线,进一步分析塔东地区原型盆地层序格架及油气系统。将油气盆地—油气系统—油气区带—油气圈闭作为完整系统进行研究,并对勘探战略及评价划分为4个层次。取得了以下四个方面十二点主要进展和认识:
1、塔东地区地层层序格架的建立。塔里木盆地自震旦纪以来经历不同类型盆地的演化阶段,因此,建立不同构造背景层序充填,可以作为各类油气系统的基础。1)早期伸展阶段形成裂谷盆地层序(南华纪—震旦纪);2)中期稳定发展阶段,形成克拉通盆地层序(古生代);3)晚期聚合与伸展交替阶段,形成前陆盆地层序与造山后裂陷层序交替出现,并有走滑盆地层序出现(中、新生代)。但塔东地区下古生界寒武—奥陶系沉积与塔里木盆地中西部不同,中西部广大地区主要为克拉通内部盆地台地相碳酸盐沉积,而塔东主要为克拉通边缘盆陆架—斜坡相浊流沉积。
2、盆地演化与盆山耦合。塔里木盆地演化受控于大洋旋回与大陆旋回的发展。4)离散期塔里木板块从超大陆分离,形成南华纪—震旦纪裂谷;5)漂移期塔里木板块漂移—热沉降,形成古生代克拉通盆地,但局部碰撞时,在克拉通边缘叠加志留纪前陆盆地;6)聚合期塔里木盆地于石炭纪—二叠纪时与欧亚大陆拼合,形成三叠纪前陆盆地,塔东地区与塔西—塔北地区库车坳陷类似;7)大陆旋回:塔里木盆地在侏罗纪时呈现为造山后—弧后伸展,形成裂陷盆地,白垩纪—古近纪为克拉通陆内稳定发展期,新近纪开始为陆内造山及陆内前陆盆地发育,新天山及阿尔金山与塔东盆地形成盆山耦合。
3、油气成藏系统分析。塔里木盆地为一大型叠合盆地,塔东地区主要由下古生界克拉通盆地与中新生界前陆盆地叠合而成,因此可以划分为古生代台地型油气系统与中新生代造山型油气系统。8)古生代台地型油气成藏系统主要与寒武—奥陶系古隆起形成良好有效圈闭有关,岩溶带及裂缝带构成良好储层;9)中新生代造山型油气成藏系统与冲断层及走滑断层相关的褶皱构成有效圈闭有关,砂岩及泥岩构成良好储盖组合。
4、油气区带评价及勘探目标优选。塔东地区通过地震及钻井资料分析,可以划分出英吉苏凹陷、塔东—古城低隆带及满东低凸起为有利勘探区带。10)英吉苏凹陷中英东1 号构造、阿拉干构造及英南2 号构造将成为优选勘探目标;11)塔东—古城低隆带中塔东1 号构造、塔东2 构及古城2 号构造将成古隆起中优选勘探目标;12)满东低凸起中满东1 号构造则为该区优选勘探目标。
Tarim Basin is a huge and superimposed basin, which was formed by the polymerization of cratonic basin, rift basin and foreland basin. From the Sinian Period to the Quaternary Period, many different tectonic settings had been undergone, and paleohigh, as well as extensional, thrust and strike-slip structures had developed. Various types of prototype basins filled in different sedimentary sequences, forming various types of hydrocarbon systems and evaluation units. In the eastern Tarim Basin, there is a Mesozoic ~ Cenozoic basin held between Tianshan Mountain and Altun Mountain, constituting the mountain-basin coupling; and the pericratonic basin environment existed during the early Paleozoic Era, which should be the strategic superseding area for hydrocarbon exploration in Tarim Basin for the near future. Aiming at the geodynamic environment, this paper further analyzes the sequence framework and hydrocarbon systems of prototype basins in the east Tarim region. In addition to regarding the hydrocarbon basin –hydrocarbon system –hydrocarbon block –hydrocarbon trap as one complete system for study, it classifies the exploration strategy and evaluation into four levels. Based on lots of actual data and in combination with the exploration practices within the region, this paper presents the following 12 main progress and understanding points concerning 4 aspects:
1. Establishment of a formation sequence framework for the eastern Tarim region
1) the rift basin sequence was formed during the early stretching period (South China Period ~ Sinian Period);
2) the cratonic basin sequence was formed during the mid-stable development period (Paleozoic Era);
3) in the late alternative period of tectonic superimposed and stretching, the alternative foreland sequence and the post-orogenic sequence was formed, accompanied with strike-slip basin sequence (Mesozoic Era, and Cenozoic Era). Since the Sinian Period, Tarim Basin has experienced different types of basin evolution stages. Hence, the sequence infill established on different tectonic background can be used as the basis for various types of hydrocarbon systems. However, the Cambrian ~ Ordovician sedimentation in the east Tarim region is different from the central and west Tarim regions. The latter is featured by intra-cratonic basin platform-facies carbonate deposit, while the former is characterized by peri-cratonic basin shelf-slope facies turbidite deposit.
2. Basin evolution and basin-mountain coupling The evolution of Tarim Basin is controlled by the development of oceanic cycle and continental cycle:
4) Divergent stage: Tarim plate was separated from the supercontinent, forming the South China Period ~ Sinian rift;
5) Drifting stage: the Paleozoic cratonic basin was formed through drifting –
1、塔东地区地层层序格架的建立。塔里木盆地自震旦纪以来经历不同类型盆地的演化阶段,因此,建立不同构造背景层序充填,可以作为各类油气系统的基础。1)早期伸展阶段形成裂谷盆地层序(南华纪—震旦纪);2)中期稳定发展阶段,形成克拉通盆地层序(古生代);3)晚期聚合与伸展交替阶段,形成前陆盆地层序与造山后裂陷层序交替出现,并有走滑盆地层序出现(中、新生代)。但塔东地区下古生界寒武—奥陶系沉积与塔里木盆地中西部不同,中西部广大地区主要为克拉通内部盆地台地相碳酸盐沉积,而塔东主要为克拉通边缘盆陆架—斜坡相浊流沉积。
2、盆地演化与盆山耦合。塔里木盆地演化受控于大洋旋回与大陆旋回的发展。4)离散期塔里木板块从超大陆分离,形成南华纪—震旦纪裂谷;5)漂移期塔里木板块漂移—热沉降,形成古生代克拉通盆地,但局部碰撞时,在克拉通边缘叠加志留纪前陆盆地;6)聚合期塔里木盆地于石炭纪—二叠纪时与欧亚大陆拼合,形成三叠纪前陆盆地,塔东地区与塔西—塔北地区库车坳陷类似;7)大陆旋回:塔里木盆地在侏罗纪时呈现为造山后—弧后伸展,形成裂陷盆地,白垩纪—古近纪为克拉通陆内稳定发展期,新近纪开始为陆内造山及陆内前陆盆地发育,新天山及阿尔金山与塔东盆地形成盆山耦合。
3、油气成藏系统分析。塔里木盆地为一大型叠合盆地,塔东地区主要由下古生界克拉通盆地与中新生界前陆盆地叠合而成,因此可以划分为古生代台地型油气系统与中新生代造山型油气系统。8)古生代台地型油气成藏系统主要与寒武—奥陶系古隆起形成良好有效圈闭有关,岩溶带及裂缝带构成良好储层;9)中新生代造山型油气成藏系统与冲断层及走滑断层相关的褶皱构成有效圈闭有关,砂岩及泥岩构成良好储盖组合。
4、油气区带评价及勘探目标优选。塔东地区通过地震及钻井资料分析,可以划分出英吉苏凹陷、塔东—古城低隆带及满东低凸起为有利勘探区带。10)英吉苏凹陷中英东1 号构造、阿拉干构造及英南2 号构造将成为优选勘探目标;11)塔东—古城低隆带中塔东1 号构造、塔东2 构及古城2 号构造将成古隆起中优选勘探目标;12)满东低凸起中满东1 号构造则为该区优选勘探目标。
Tarim Basin is a huge and superimposed basin, which was formed by the polymerization of cratonic basin, rift basin and foreland basin. From the Sinian Period to the Quaternary Period, many different tectonic settings had been undergone, and paleohigh, as well as extensional, thrust and strike-slip structures had developed. Various types of prototype basins filled in different sedimentary sequences, forming various types of hydrocarbon systems and evaluation units. In the eastern Tarim Basin, there is a Mesozoic ~ Cenozoic basin held between Tianshan Mountain and Altun Mountain, constituting the mountain-basin coupling; and the pericratonic basin environment existed during the early Paleozoic Era, which should be the strategic superseding area for hydrocarbon exploration in Tarim Basin for the near future. Aiming at the geodynamic environment, this paper further analyzes the sequence framework and hydrocarbon systems of prototype basins in the east Tarim region. In addition to regarding the hydrocarbon basin –hydrocarbon system –hydrocarbon block –hydrocarbon trap as one complete system for study, it classifies the exploration strategy and evaluation into four levels. Based on lots of actual data and in combination with the exploration practices within the region, this paper presents the following 12 main progress and understanding points concerning 4 aspects:
1. Establishment of a formation sequence framework for the eastern Tarim region
1) the rift basin sequence was formed during the early stretching period (South China Period ~ Sinian Period);
2) the cratonic basin sequence was formed during the mid-stable development period (Paleozoic Era);
3) in the late alternative period of tectonic superimposed and stretching, the alternative foreland sequence and the post-orogenic sequence was formed, accompanied with strike-slip basin sequence (Mesozoic Era, and Cenozoic Era). Since the Sinian Period, Tarim Basin has experienced different types of basin evolution stages. Hence, the sequence infill established on different tectonic background can be used as the basis for various types of hydrocarbon systems. However, the Cambrian ~ Ordovician sedimentation in the east Tarim region is different from the central and west Tarim regions. The latter is featured by intra-cratonic basin platform-facies carbonate deposit, while the former is characterized by peri-cratonic basin shelf-slope facies turbidite deposit.
2. Basin evolution and basin-mountain coupling The evolution of Tarim Basin is controlled by the development of oceanic cycle and continental cycle:
4) Divergent stage: Tarim plate was separated from the supercontinent, forming the South China Period ~ Sinian rift;
5) Drifting stage: the Paleozoic cratonic basin was formed through drifting –
引文
1. 王鸿祯、杨森楠、刘本培,中国及邻区构造古地理和生物古地理,武汉:中国地质大学出版社,1990
2. 王鸿祯,全球构造研究的简要回顾,地学前缘,1995,2(1):37-42
3. 李思田,沉积盆地的动力学分析,地学前缘,1995,第2 卷,第3～4 期
4. 刘和甫,中国沉积盆地演化与旋回动力学环境,地球科学,1996,21(4)
5. 刘和甫,盆地演化与地球动力学旋回,地学前缘,1997,Vol.4,No.3-4
6. 李景明,魏国齐,曾宪斌,中国大中型气田富集区带,北京:地质出版社,2002
7. 贾承造,中国塔里木盆地构造特征与油气,北京:石油工业出版社,1997
8. 童晓光,梁狄刚,贾承造,塔里木盆地石油地质研究新进展,北京:科技出版社,1996
9. 刘和甫,扭动构造分析与油气聚集,见:第二届全国构造地质学术会议论文选集,第三卷中新生代构造,.北京:科学出版社,1982,131～141。
10. 刘和甫,夏义平,殷进垠等,走滑造山带与盆地耦合机制,地学前缘,1999,6/3,121~132
11. 梁慧社,刘和甫,新疆塔里木盆地构造样式研究,河北地质学院学报,1996,19/3-4,268-277
12. 王鸿祯,史晓颖,王训练等,中国层序地层研究,广州,广东科技出版社,2002,P1-457
13. 刘和甫,前陆盆地类型及褶皱-冲断层样式,地学前缘,1995,2/3:59～68
14. 周兴熙,胡素云,张国良,塔里木盆地油气藏,北京:石油工业出版社,1995
15. 周兴熙,塔里木盆地天然气形成条件及分布规律,北京:石油工业出版社,1998
16. 李小地,张光亚,田作基,塔里木盆地油气系统与油气分布规律,北京:地 质出版社,2002
17. 刘和甫,亚洲大陆平移断裂系的构造分析,见:第二十六届国际地质大会国际交流地质学术论文集,北京:地质出版社,1980,1:201～210
18. 刘和甫,盆地—山岭耦合体系与地球动力学机制[J],地球科学,2001,26(6);581-596
19. 赵文智,何登发,中国含油气系统的基本特征与勘探对策[J],石油学报,2002,23(6):1-11
20. 汤良杰,塔里木盆地演化和构造样式[M],北京:地质出版社,1996,41-73
21. 刘和甫,伸展构造及其反转,地学前缘,1995,2/1,113~124
22. 刘和甫,梁慧社,蔡立国等,天山两侧前陆冲断第构造样式与前陆盆地演化,地球科学,1994,19/6,727~741
23. 何登发,李德生,塔里木盆地构造演化与油气聚集,北京:石油工业出版社,1996,98-99
24. 田兴澄、毕研鹏等,论成藏动力学系统,北京,地震出版社,2000,1-172
25. 单汝俭,塔里木盆地东部边缘区深部构造研究,长春科技大学学报,1999,28/4,377-381
26. 张德润,塔里木地台东部边界问题,地质论评,1991,38/1,28-32
27. 陈发景、赵海玲、陈昭年等,中国东部中、新生代伸展盆地构造特征及地球动力学背景,地球科学,1996,21(4):357~365
28. 朱英,塔里木盆地东部的地质构造和油气远景,航空物探技术,1988,35(1):44~50
29.邓振球,塔里木盆地东部(罗布泊)区域重磁特征及区域地质构造的意义,新疆地质,1987,5/1,85~91
30.P. A. 艾伦,J. R. 艾伦著,陈全茂等译,盆地分析:原理及应用,北京,石油工业出版社,1995,pp47~48
31.N. B. Woodward,S. E. Boyer,J. Suppe 著;贾维民,杜秀霞译,1989: 平衡地质剖面,武汉,中国地质大学出版社,pp1—7
32.杨克明,徐国友,塔里木盆地东部地区古生代地质构造特征及找油前景, 新疆石油地质,1987,8/2,16~23
33.贾润胥,中国塔里木盆地北部油气地质研究,北京:中国地质大学出版社,1991
34.新疆石油局南疆勘探指挥部地质所,古特提斯海北支塔里木古海湾岩相古地理,北京:科学出版社,1989
35.李小军,李景明,刘立群,刘和甫,塔里木盆地东部盆山耦合与区带分析,现代地质,2004,第18 卷第2 期,164~170
36.李思田,沉积盆地的动力学分析——盆地研究领域的主要趋向,地学前缘,1995,2(3),pp1~9
37.李小军,刘和甫,刘立群,新区油气勘探及评价层次,现代地质,2003,第17 卷第1 期,86-86
38. 刘和甫,李小军,刘立群,地球动力学与盆地层序及油气系统分析,现代地质,2003 年第17 卷第1 期,80-86
39. 解习农等,1996,陆相盆地幕式构造旋回与层序构成,地球科学—中国地质大学学报,21(17):27-33
40. 钱奕中、陈洪德、刘文均主编,1994,层序地层学理论和研究方法,成都:四川科学技术出版社
41. P.A.艾伦,J.R.艾伦,盆地分析—原理与应用(中译本),陈金茂等译,石油工业出版社,1995
42. C.K.威尔格斯等编,层序地层学原理(中译本),徐怀大等译,石油工业出版社,1993
43.罗志立,李景明,李小军,中国前陆盆地特征及含油气远景分析,中国石油勘探,2004 年第9 卷第2 期,1-11。
44.李亚红,魏国齐,钱凯,李小军,“九五”我国陆上天然气勘探的突破性进展与启示,天然气工业,2001 年第21 卷第2 期,114-115
45.王启军,陈建渝等,油气地球化学,湖北:中国地质大学出版社,1988
46.黄汝昌等,中国低熟油及凝析气藏形成与分布规律,1997,北京:石油工业出版社
47.黄汝昌等,天然气气源岩地化特征及成气机理,1995
48.钟宁宁等,石油地球化学进展,1998,北京:石油工业出版社
49. Maruyma S, Plume tectonics .J Geol Soc. Japan, 1994,100(1):24~49
50. Verrall P. Tectonic history of Western North America, California AAPG Short course,1990,615~630
51. Davis G A , Qian X, Zheng Y et al, Mesozoic deformation and Platonism in the Yunmeng Shan: a metamorphic core complex north of Beijing, China , in Yin A and M. Harrison ed.: The tectonic evolution of Asia , Cambridge University Press,1996:253~280
52.Yin, A., An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, Eastern Asia, Tectonics, 1993, 12(4), 801~803
53. Sherman S I.Faults of the Baikal rift zone. Tectonoph ysics, 1978, 3(6): 479～522
54. Molnar P, Tapponnier P. Cenozioc tectonics of Asia: effec ts of a continental collision. Science, 1975, 189(4201):419～426
55.A. D. Gibbs: Balanced Cross-section Construction from Seismic Sections in Areas of Extensional Tectonics . J. Struct. Geol.,1983,Vol. 5, No. 2, pp153~160.
56.Ziegler P.A.,Geodynamic Processes Governing Development of Rifted Basins. In:Roure F.,Ellouz N.Shein V.S.Skvortsov I.(eds), Geodynamic Evolution of Sedimentary Basins, Edition Technip, Paris, 1996:19—673. Sylvester A G. Strike slip fault. Bull Geol Soc Am,198 9,100:1666～1703
57. Harland W H.Tectonic transpression in Caledonian Spitsber gen.Geol Mag, 1971, 108:27～42
58. Sylvester A G, Wrench fault tectonics. AAPG, Reprint S eries, 1984(28):1～374
59. Sylvester A. G., Strike slip fault, Bull Geol. Soc. Am. 1989, 100, 1666~1703
60. Harding T P. Petroleum traps associated with wrench faults .AAPG Bull,1974,57:97～166
61. Wu Genyao. Tethyan evolution in South China and its environments. In: Xiao Xuchang, Liu Hefu, eds. Proc 30th Int'l Geol Congr, 1997,6: 55～76
62. Zhong Dalai, Tapponnier, Wu Haiwei, et al. Large scale strike slip fault: the major structure of intercontinental deformation after collision. Chinese Science Bulletin,1990, 35: 304～309
63. Wan Tianfeng, et al. Formation and evolution of the Tan cheng-Lujiang fault zone,China. Wuhan: China University of Geosiences Press. 1996.1～11
64.Marjorie Wilson,Magmatism and the Geodynamics of Basin Formation,In:Sedimentary Geology,1993,86,pp5~30
65. J.F.Aitken & J.A.Howell,1996,High resolution sequence stratigraphy: innovations, applications and future prespects,High Resolution Sequence stratigraphy,The Alden Press,London
66. Bluck,B.J.,1980,Structure,generation and preservation of upward fining,braided stream cycles in the Old Red Sandstone of Scotland:Transactions Royal Society of Edinburgh,v.71,p.29-46
67. Brown,L.F.,1991,Variations in lowstand systems tracts:constraints on exploration(abs.):AAPG Bulletin,v.75,p.547
68. Brush,L.M.,and M.G.Wolman,1960,Knickpoint behavior in noncohesive material:a laboratory study:GSA Bulletin,v.71,p.59-74
69. Cross,T.A.,ed.,1990,Quantitative dynamic stratigraphy;Prentice Hall,Englewood Cliffs,625p.
70. Galloway,W.E.,1989,Genetic stratigraphic sequences in basin analysis I:architecture and genesis of flooding-surface bounded depositional units:AAPG Bulletin,v.73,p.125-142.
71. Gardner,T.W.,1983,Experimental study of knickpoint and longitudinal profile evolution in cohesive,homogeneous material:GSA Bulletin,v.94,p.664-672.
72. Gawthorpe,R.L.,and J.M.Hurst,1933,Transfer zones in extensional basins:their structural style and influ-ence on drainage development and stratigraphy:Journal of the Geological Society of London,v.150,p.1137-1152.
73. Goldhammer,R.K.,P.A.Dunn,and L.A.Hardie,1990,Depositional cycles,composite sea level changes,cycle stacking patterns,and the hierarchy of strati-graphic forcing:examples from the Alpine plat-form carbonates:GSA Bulletin,v.102,p.535-562.
74. Haq,B.U.,J.Hardenbol,and P.R.Vail,1987,Chronology of fluctuating sea levels since the Triassic:Science,v.235,p.1156-1167.
75. HOWELL,J.A.& FLINT,S.S.,1996,A model for high resolution sequence stratigraphy within extensisonal basins,in J.A.Howell and J.F.Aitken,eds.,High
resolution sequence stratigraphy:innovations,applications and future
prospects,GSSP,No.104.
76. Huaida,H.,1991,Sequence stratigraphic features of nonmarine Cretaceous sediments in Songliao basin,northeast China (abs.):AAPG Bulletin,v.75,p.598.
77. Jervey,M.T.,1988,Quantitative geological modeling of siliciclastic rock sequences and their seismic expression,in C.K.Wilgus,B.S.Hastings,C.G.St.C.Kendall, H.W.Posamentier, C.A. Ross, and J.C.Van Wagoner,eds.,Sea level change:an integrated approach:SEPM Special Publication 42,p.47-69.
78. Miall,A.D.,1986,Eustatic sea-level changes interpreted from seismic stratigraphy:a critique of the methodology with parth particular reference to the North Sea Jurassic record:AAPG Bulletin,v.70,p.131-137.
79. Miall,A.D.,1992,Exxon global cycle chart:an event for every occasion? :Geology,v.20,p.787-790.
80. Mitchum,R.M.,Jr.,J.B.Sangree,P.R.Vail,and W.W.Wornardt, 1990, Sequence stratigraphy in Gulf Coast expanded sections,Gulf of Mexico: GCSSEPM Eleventh Annual Research Conference, p.237-256.
81. Mitchum,R.M.,Jr., and J.C.Van Wagoner,1991, High-fre-quency sequences and their stacking patterns: sequence-stratigraphic evidence of high-frequency eustatic cycles:Sedimentary Geology,v.70,p.131-160.
82. Payton,C.E.,ed.,1977, Seismic stratigraphy-applica-tions to hydrocarbon exploration: AAPG Memoir 26, 516p.
83. Posamentier,H.W., and G.P.Allen,1993, Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins: Geology, v.21, p. 455-458.
84. Posamentier,H.W.,and C.J.Chamberlain,1933,Sequence stratigraphic analysis of lowstand beach deposits at Joarcam field,Alberta,Canada,in H.W.Posamentier,C.P.Summerhayes,B.U.Haq,and G.P.Allen,eds.,Sequence stratigraphy and facies associa-tions:International Association of Sedimentologists Special Publication 18,p.469-485.
85. Posamentier,H.W.,and D.H.James,1993,An wverview of sequence stratigraphic concepts: uses and abuses, in H.W.Posamentier, C.P.Summerhayes, B.U.Haq, and G.P.Allen,eds., Sequence stratigraphy and facies associations:International
2. 王鸿祯,全球构造研究的简要回顾,地学前缘,1995,2(1):37-42
3. 李思田,沉积盆地的动力学分析,地学前缘,1995,第2 卷,第3～4 期
4. 刘和甫,中国沉积盆地演化与旋回动力学环境,地球科学,1996,21(4)
5. 刘和甫,盆地演化与地球动力学旋回,地学前缘,1997,Vol.4,No.3-4
6. 李景明,魏国齐,曾宪斌,中国大中型气田富集区带,北京:地质出版社,2002
7. 贾承造,中国塔里木盆地构造特征与油气,北京:石油工业出版社,1997
8. 童晓光,梁狄刚,贾承造,塔里木盆地石油地质研究新进展,北京:科技出版社,1996
9. 刘和甫,扭动构造分析与油气聚集,见:第二届全国构造地质学术会议论文选集,第三卷中新生代构造,.北京:科学出版社,1982,131～141。
10. 刘和甫,夏义平,殷进垠等,走滑造山带与盆地耦合机制,地学前缘,1999,6/3,121~132
11. 梁慧社,刘和甫,新疆塔里木盆地构造样式研究,河北地质学院学报,1996,19/3-4,268-277
12. 王鸿祯,史晓颖,王训练等,中国层序地层研究,广州,广东科技出版社,2002,P1-457
13. 刘和甫,前陆盆地类型及褶皱-冲断层样式,地学前缘,1995,2/3:59～68
14. 周兴熙,胡素云,张国良,塔里木盆地油气藏,北京:石油工业出版社,1995
15. 周兴熙,塔里木盆地天然气形成条件及分布规律,北京:石油工业出版社,1998
16. 李小地,张光亚,田作基,塔里木盆地油气系统与油气分布规律,北京:地 质出版社,2002
17. 刘和甫,亚洲大陆平移断裂系的构造分析,见:第二十六届国际地质大会国际交流地质学术论文集,北京:地质出版社,1980,1:201～210
18. 刘和甫,盆地—山岭耦合体系与地球动力学机制[J],地球科学,2001,26(6);581-596
19. 赵文智,何登发,中国含油气系统的基本特征与勘探对策[J],石油学报,2002,23(6):1-11
20. 汤良杰,塔里木盆地演化和构造样式[M],北京:地质出版社,1996,41-73
21. 刘和甫,伸展构造及其反转,地学前缘,1995,2/1,113~124
22. 刘和甫,梁慧社,蔡立国等,天山两侧前陆冲断第构造样式与前陆盆地演化,地球科学,1994,19/6,727~741
23. 何登发,李德生,塔里木盆地构造演化与油气聚集,北京:石油工业出版社,1996,98-99
24. 田兴澄、毕研鹏等,论成藏动力学系统,北京,地震出版社,2000,1-172
25. 单汝俭,塔里木盆地东部边缘区深部构造研究,长春科技大学学报,1999,28/4,377-381
26. 张德润,塔里木地台东部边界问题,地质论评,1991,38/1,28-32
27. 陈发景、赵海玲、陈昭年等,中国东部中、新生代伸展盆地构造特征及地球动力学背景,地球科学,1996,21(4):357~365
28. 朱英,塔里木盆地东部的地质构造和油气远景,航空物探技术,1988,35(1):44~50
29.邓振球,塔里木盆地东部(罗布泊)区域重磁特征及区域地质构造的意义,新疆地质,1987,5/1,85~91
30.P. A. 艾伦,J. R. 艾伦著,陈全茂等译,盆地分析:原理及应用,北京,石油工业出版社,1995,pp47~48
31.N. B. Woodward,S. E. Boyer,J. Suppe 著;贾维民,杜秀霞译,1989: 平衡地质剖面,武汉,中国地质大学出版社,pp1—7
32.杨克明,徐国友,塔里木盆地东部地区古生代地质构造特征及找油前景, 新疆石油地质,1987,8/2,16~23
33.贾润胥,中国塔里木盆地北部油气地质研究,北京:中国地质大学出版社,1991
34.新疆石油局南疆勘探指挥部地质所,古特提斯海北支塔里木古海湾岩相古地理,北京:科学出版社,1989
35.李小军,李景明,刘立群,刘和甫,塔里木盆地东部盆山耦合与区带分析,现代地质,2004,第18 卷第2 期,164~170
36.李思田,沉积盆地的动力学分析——盆地研究领域的主要趋向,地学前缘,1995,2(3),pp1~9
37.李小军,刘和甫,刘立群,新区油气勘探及评价层次,现代地质,2003,第17 卷第1 期,86-86
38. 刘和甫,李小军,刘立群,地球动力学与盆地层序及油气系统分析,现代地质,2003 年第17 卷第1 期,80-86
39. 解习农等,1996,陆相盆地幕式构造旋回与层序构成,地球科学—中国地质大学学报,21(17):27-33
40. 钱奕中、陈洪德、刘文均主编,1994,层序地层学理论和研究方法,成都:四川科学技术出版社
41. P.A.艾伦,J.R.艾伦,盆地分析—原理与应用(中译本),陈金茂等译,石油工业出版社,1995
42. C.K.威尔格斯等编,层序地层学原理(中译本),徐怀大等译,石油工业出版社,1993
43.罗志立,李景明,李小军,中国前陆盆地特征及含油气远景分析,中国石油勘探,2004 年第9 卷第2 期,1-11。
44.李亚红,魏国齐,钱凯,李小军,“九五”我国陆上天然气勘探的突破性进展与启示,天然气工业,2001 年第21 卷第2 期,114-115
45.王启军,陈建渝等,油气地球化学,湖北:中国地质大学出版社,1988
46.黄汝昌等,中国低熟油及凝析气藏形成与分布规律,1997,北京:石油工业出版社
47.黄汝昌等,天然气气源岩地化特征及成气机理,1995
48.钟宁宁等,石油地球化学进展,1998,北京:石油工业出版社
49. Maruyma S, Plume tectonics .J Geol Soc. Japan, 1994,100(1):24~49
50. Verrall P. Tectonic history of Western North America, California AAPG Short course,1990,615~630
51. Davis G A , Qian X, Zheng Y et al, Mesozoic deformation and Platonism in the Yunmeng Shan: a metamorphic core complex north of Beijing, China , in Yin A and M. Harrison ed.: The tectonic evolution of Asia , Cambridge University Press,1996:253~280
52.Yin, A., An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, Eastern Asia, Tectonics, 1993, 12(4), 801~803
53. Sherman S I.Faults of the Baikal rift zone. Tectonoph ysics, 1978, 3(6): 479～522
54. Molnar P, Tapponnier P. Cenozioc tectonics of Asia: effec ts of a continental collision. Science, 1975, 189(4201):419～426
55.A. D. Gibbs: Balanced Cross-section Construction from Seismic Sections in Areas of Extensional Tectonics . J. Struct. Geol.,1983,Vol. 5, No. 2, pp153~160.
56.Ziegler P.A.,Geodynamic Processes Governing Development of Rifted Basins. In:Roure F.,Ellouz N.Shein V.S.Skvortsov I.(eds), Geodynamic Evolution of Sedimentary Basins, Edition Technip, Paris, 1996:19—673. Sylvester A G. Strike slip fault. Bull Geol Soc Am,198 9,100:1666～1703
57. Harland W H.Tectonic transpression in Caledonian Spitsber gen.Geol Mag, 1971, 108:27～42
58. Sylvester A G, Wrench fault tectonics. AAPG, Reprint S eries, 1984(28):1～374
59. Sylvester A. G., Strike slip fault, Bull Geol. Soc. Am. 1989, 100, 1666~1703
60. Harding T P. Petroleum traps associated with wrench faults .AAPG Bull,1974,57:97～166
61. Wu Genyao. Tethyan evolution in South China and its environments. In: Xiao Xuchang, Liu Hefu, eds. Proc 30th Int'l Geol Congr, 1997,6: 55～76
62. Zhong Dalai, Tapponnier, Wu Haiwei, et al. Large scale strike slip fault: the major structure of intercontinental deformation after collision. Chinese Science Bulletin,1990, 35: 304～309
63. Wan Tianfeng, et al. Formation and evolution of the Tan cheng-Lujiang fault zone,China. Wuhan: China University of Geosiences Press. 1996.1～11
64.Marjorie Wilson,Magmatism and the Geodynamics of Basin Formation,In:Sedimentary Geology,1993,86,pp5~30
65. J.F.Aitken & J.A.Howell,1996,High resolution sequence stratigraphy: innovations, applications and future prespects,High Resolution Sequence stratigraphy,The Alden Press,London
66. Bluck,B.J.,1980,Structure,generation and preservation of upward fining,braided stream cycles in the Old Red Sandstone of Scotland:Transactions Royal Society of Edinburgh,v.71,p.29-46
67. Brown,L.F.,1991,Variations in lowstand systems tracts:constraints on exploration(abs.):AAPG Bulletin,v.75,p.547
68. Brush,L.M.,and M.G.Wolman,1960,Knickpoint behavior in noncohesive material:a laboratory study:GSA Bulletin,v.71,p.59-74
69. Cross,T.A.,ed.,1990,Quantitative dynamic stratigraphy;Prentice Hall,Englewood Cliffs,625p.
70. Galloway,W.E.,1989,Genetic stratigraphic sequences in basin analysis I:architecture and genesis of flooding-surface bounded depositional units:AAPG Bulletin,v.73,p.125-142.
71. Gardner,T.W.,1983,Experimental study of knickpoint and longitudinal profile evolution in cohesive,homogeneous material:GSA Bulletin,v.94,p.664-672.
72. Gawthorpe,R.L.,and J.M.Hurst,1933,Transfer zones in extensional basins:their structural style and influ-ence on drainage development and stratigraphy:Journal of the Geological Society of London,v.150,p.1137-1152.
73. Goldhammer,R.K.,P.A.Dunn,and L.A.Hardie,1990,Depositional cycles,composite sea level changes,cycle stacking patterns,and the hierarchy of strati-graphic forcing:examples from the Alpine plat-form carbonates:GSA Bulletin,v.102,p.535-562.
74. Haq,B.U.,J.Hardenbol,and P.R.Vail,1987,Chronology of fluctuating sea levels since the Triassic:Science,v.235,p.1156-1167.
75. HOWELL,J.A.& FLINT,S.S.,1996,A model for high resolution sequence stratigraphy within extensisonal basins,in J.A.Howell and J.F.Aitken,eds.,High
resolution sequence stratigraphy:innovations,applications and future
prospects,GSSP,No.104.
76. Huaida,H.,1991,Sequence stratigraphic features of nonmarine Cretaceous sediments in Songliao basin,northeast China (abs.):AAPG Bulletin,v.75,p.598.
77. Jervey,M.T.,1988,Quantitative geological modeling of siliciclastic rock sequences and their seismic expression,in C.K.Wilgus,B.S.Hastings,C.G.St.C.Kendall, H.W.Posamentier, C.A. Ross, and J.C.Van Wagoner,eds.,Sea level change:an integrated approach:SEPM Special Publication 42,p.47-69.
78. Miall,A.D.,1986,Eustatic sea-level changes interpreted from seismic stratigraphy:a critique of the methodology with parth particular reference to the North Sea Jurassic record:AAPG Bulletin,v.70,p.131-137.
79. Miall,A.D.,1992,Exxon global cycle chart:an event for every occasion? :Geology,v.20,p.787-790.
80. Mitchum,R.M.,Jr.,J.B.Sangree,P.R.Vail,and W.W.Wornardt, 1990, Sequence stratigraphy in Gulf Coast expanded sections,Gulf of Mexico: GCSSEPM Eleventh Annual Research Conference, p.237-256.
81. Mitchum,R.M.,Jr., and J.C.Van Wagoner,1991, High-fre-quency sequences and their stacking patterns: sequence-stratigraphic evidence of high-frequency eustatic cycles:Sedimentary Geology,v.70,p.131-160.
82. Payton,C.E.,ed.,1977, Seismic stratigraphy-applica-tions to hydrocarbon exploration: AAPG Memoir 26, 516p.
83. Posamentier,H.W., and G.P.Allen,1993, Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins: Geology, v.21, p. 455-458.
84. Posamentier,H.W.,and C.J.Chamberlain,1933,Sequence stratigraphic analysis of lowstand beach deposits at Joarcam field,Alberta,Canada,in H.W.Posamentier,C.P.Summerhayes,B.U.Haq,and G.P.Allen,eds.,Sequence stratigraphy and facies associa-tions:International Association of Sedimentologists Special Publication 18,p.469-485.
85. Posamentier,H.W.,and D.H.James,1993,An wverview of sequence stratigraphic concepts: uses and abuses, in H.W.Posamentier, C.P.Summerhayes, B.U.Haq, and G.P.Allen,eds., Sequence stratigraphy and facies associations:International
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |