黄骅坳陷孔南地区层序地层学研究
摘要
黄骅坳陷处于天津东南,研究区位于黄骅坳陷南部,是早第三纪以来新生代陆内伸展盆地。本文以层序地层学、沉积学和石油地质学为理论依据,并结合测井、地震以层序地层分析研究为主线,找出区域对比标准;采用旋回对比、分级控制的原则,对全区进行层序及体系域划分和对比、建立该区等时层序地层格架;并主要分析了构造在沙河街时期对层序发育的影响;总结出四种油气藏类型;在此基础上提出了孔南地区有利的勘探区带。
研究认为,孔南地区沙河街组构造演化经历了3个阶段,可划分为3个三级层序,8个四级层序,9个体系域,9个基准面中期旋回,16个半旋回。沧东、徐西断层为边界控盆断层,分别在沧东断层东侧级徐西断层西侧发育多个三角洲及扇三角洲。盆地中部孔店凸起在沙河街时期同步发育,为滚动背斜,并形成了孔东孔西断层。盆地总体格局呈北东向展布,古地貌上从南西向北东方向地势逐渐增高。在北部靠沧东断层一侧形成沧东凹陷,在南部靠徐西断层一侧形成南皮凹陷。河街时期的孔南地区为右旋张扭性构造应力场中形成的拉分盆地。边界断层活动速率控制盆地的沉降速率,进而控制了层序的形成及演化。低水位体系域砂体,上倾斜坡区砂体及孔店凸起生物灰岩层为有利的勘探区域。本文的研究结论对孔南地区的勘探具有重要的意义。
The south of KongNian Area is located the south of HuangHua Depression , is north from NanDi south to DengMingSi, CangDong fault to the west as the boundaries XuXi fault to the east as the boundaries,its area is 4700km2.It includes seven the second structural unit which are two big depressions which are CangDong and NanPi-XuXi depression,JieDi-QiLiDian secondary bump,SheNvSi slope,DengMingSi-WuMaYing slope,KongDian bump,and XiaoGuanTun secondary bump.
The south of KongDian Area ShaHeJie Group layer after structure,its original lake basin construction changed a lot.So the structure affected the deposition.The lake basin deposition is so indistinct that it is possiable to make some huge blindness during exploring.This article’s substance is to resume ShaHeJie’s the lake basin sequence development mode.
To analysis ShaHeJie’s the lake basin sequence development mode, the first,we have to establish isochronal layer framework. According the foundation of sequence stratigraphy, interpreting the earthquake well tie section, comparing the basal level cycle, the ShaHeJie can be divided three tertiary sequences,eight tchetvertyi sequences,nine systems,nine basal level middle period cycles and sixteen half cycles.And the Sequence One is the Sha Three, the Sequence Two is the Sha Two, the Sequence Three is the Sha One.
Under the inhibition of isochronal layer framework, analysis the palaeoenvironment of ShaHeJie’s three sequances.The first,with analysising the lithofacies, lithofacies group type and electrofacies,we can know the ShaHeJie grows three sedimentary facies which are braid river delta, fan delta and lake,including seven subfacies and fifteen microfacies.The second ,with analysising the material source with light mineral and heavy mineral,we can know:the south WuMaYing area grows the braid river delta along the basin axial direction,SeNuSi,CangZou and NanDi near the CangDong faultage grow fan delta,WangGuanTun near the XuXi faultage grows fan delta.The last one,make the layer changing,the sandstone thickness changing and the sediment charge changing together,we can clearly recognize flat feature of ShaHeJie sedimentary facies.
With the foundation of isochronal layer framework, confirming the sedimentary facies distribution,and interpreting the earthquake well tie section,we can analysis the ShaHeJie basic structure morphotype and filling pattern. It is concluded that two basic structure morphotypes and filling patterns which are duplex fault duplex filling and duplex fault single filling. Sedimentary deposit particles are thiner from sedimentation center of amphi boundary fault to upwarping of basin inner.
The next ,to confirm the key point of the lake basin structure focuses the two factors:the moving period of CangDong ,XuXi faults and the formation period of KongDian structural belt.With anaylsising layer filling model and boundary sedimentary facies ,we can know that the CangDong fault,XuXi fault are border fault which deposites and controles the basin in the same time,KongDian structural belt forms in the same time when the ShaHeJie deposites.It is concluded that the ShaHeJie basin is continental facies syndeposit fault basin in the context of HuangHua depression.
Based on the structure movement of the east of china tertiary,we know that this kind of the basin is formed under the action of the right hand rotation drawing tectonic stress. Based on the above views,we can clearly recognize ShaHeJie period’s structure and deposition.We can anaylsis the possiable hydrocarbon accumulation type.There are three hydrocarbon accumulation types in the ShaHeJie period:structure-stratigraphic hydrocarbon reservoir,lithologic updip pinchout hydrocarbon reservoir and layer upfold hydrocarbon reservoir.This conclusion is important significance to exploration activity of KongNan area ShaHeJie.
研究认为,孔南地区沙河街组构造演化经历了3个阶段,可划分为3个三级层序,8个四级层序,9个体系域,9个基准面中期旋回,16个半旋回。沧东、徐西断层为边界控盆断层,分别在沧东断层东侧级徐西断层西侧发育多个三角洲及扇三角洲。盆地中部孔店凸起在沙河街时期同步发育,为滚动背斜,并形成了孔东孔西断层。盆地总体格局呈北东向展布,古地貌上从南西向北东方向地势逐渐增高。在北部靠沧东断层一侧形成沧东凹陷,在南部靠徐西断层一侧形成南皮凹陷。河街时期的孔南地区为右旋张扭性构造应力场中形成的拉分盆地。边界断层活动速率控制盆地的沉降速率,进而控制了层序的形成及演化。低水位体系域砂体,上倾斜坡区砂体及孔店凸起生物灰岩层为有利的勘探区域。本文的研究结论对孔南地区的勘探具有重要的意义。
The south of KongNian Area is located the south of HuangHua Depression , is north from NanDi south to DengMingSi, CangDong fault to the west as the boundaries XuXi fault to the east as the boundaries,its area is 4700km2.It includes seven the second structural unit which are two big depressions which are CangDong and NanPi-XuXi depression,JieDi-QiLiDian secondary bump,SheNvSi slope,DengMingSi-WuMaYing slope,KongDian bump,and XiaoGuanTun secondary bump.
The south of KongDian Area ShaHeJie Group layer after structure,its original lake basin construction changed a lot.So the structure affected the deposition.The lake basin deposition is so indistinct that it is possiable to make some huge blindness during exploring.This article’s substance is to resume ShaHeJie’s the lake basin sequence development mode.
To analysis ShaHeJie’s the lake basin sequence development mode, the first,we have to establish isochronal layer framework. According the foundation of sequence stratigraphy, interpreting the earthquake well tie section, comparing the basal level cycle, the ShaHeJie can be divided three tertiary sequences,eight tchetvertyi sequences,nine systems,nine basal level middle period cycles and sixteen half cycles.And the Sequence One is the Sha Three, the Sequence Two is the Sha Two, the Sequence Three is the Sha One.
Under the inhibition of isochronal layer framework, analysis the palaeoenvironment of ShaHeJie’s three sequances.The first,with analysising the lithofacies, lithofacies group type and electrofacies,we can know the ShaHeJie grows three sedimentary facies which are braid river delta, fan delta and lake,including seven subfacies and fifteen microfacies.The second ,with analysising the material source with light mineral and heavy mineral,we can know:the south WuMaYing area grows the braid river delta along the basin axial direction,SeNuSi,CangZou and NanDi near the CangDong faultage grow fan delta,WangGuanTun near the XuXi faultage grows fan delta.The last one,make the layer changing,the sandstone thickness changing and the sediment charge changing together,we can clearly recognize flat feature of ShaHeJie sedimentary facies.
With the foundation of isochronal layer framework, confirming the sedimentary facies distribution,and interpreting the earthquake well tie section,we can analysis the ShaHeJie basic structure morphotype and filling pattern. It is concluded that two basic structure morphotypes and filling patterns which are duplex fault duplex filling and duplex fault single filling. Sedimentary deposit particles are thiner from sedimentation center of amphi boundary fault to upwarping of basin inner.
The next ,to confirm the key point of the lake basin structure focuses the two factors:the moving period of CangDong ,XuXi faults and the formation period of KongDian structural belt.With anaylsising layer filling model and boundary sedimentary facies ,we can know that the CangDong fault,XuXi fault are border fault which deposites and controles the basin in the same time,KongDian structural belt forms in the same time when the ShaHeJie deposites.It is concluded that the ShaHeJie basin is continental facies syndeposit fault basin in the context of HuangHua depression.
Based on the structure movement of the east of china tertiary,we know that this kind of the basin is formed under the action of the right hand rotation drawing tectonic stress. Based on the above views,we can clearly recognize ShaHeJie period’s structure and deposition.We can anaylsis the possiable hydrocarbon accumulation type.There are three hydrocarbon accumulation types in the ShaHeJie period:structure-stratigraphic hydrocarbon reservoir,lithologic updip pinchout hydrocarbon reservoir and layer upfold hydrocarbon reservoir.This conclusion is important significance to exploration activity of KongNan area ShaHeJie.
引文
[1]高锡兴.黄骅坳陷石油天然气地质(第二版)[M].北京:石油工业出版社.2004.
[2]徐怀大等.从地震地层学到层序地层学.北京:石油工业出版社.1997.
[3]刘镇、吴因业.层序地层框架与油气藏勘探.北京:石油工业出版社.1999.
[4]操应长.断陷湖盆层序地层学.北京:地质出版社.2005.
[5]陆基孟.地震勘探原理.北京:石油大学出版社.2005.
[6]冯有良、李思田.陆相断陷盆地层序地层学研究—以渤海湾盆地东营凹陷为例.北京:科学教育出版社.2006.
[7]李明、候连华、邹才能、殷积峰、刘晓等.岩性地层油气藏地球物理勘探技术与应用.北京:石油工业出版社.2005.
[8]邹才能、池应柳、李明、薛叔浩等.陆相层序地层学分析技术.北京:石油工业出版社.2004.
[9]杨宝俊、张梅生、王璞珺.中国油气区地质—地球物理解析.北京:科学教育出版社.2003.
[10]谭廷栋等.测井学.北京:石油工业出版社.2004.
[11]田在艺、张庆春.中国含油气沉积盆地论.北京:石油工业出版社.1996.
[12]姜在兴.沉积学.北京:石油工业出版社.2005.
[13]宋万超、刘波、宋新民.层序地层学概念、原理、方法及应用.北京:石油工业出版社.2003.
[14]何幼斌、王文广.沉积岩与沉积相.北京:石油工业出版社.2007.
[15]吴元燕、吴胜和、蔡正旗.油矿地质学(第三版).北京:石油工业出版社.2005.
[16]陈恭洋.油气田地下地质学.北京:石油工业出版社.2007.
[17] Fred J.Hilterman著,孙夕平、赵良武等译.地震振幅解释.北京:石油工业出版社.2004.
[18]张厚福等.石油地质学.北京:石油工业出版社.1999.
[19]杨毅恒、韩燕等.多维地学数据处理技术与方法.北京:科学教育出版社.2002.
[20]徐怀大.陆相层序地层学研究中的某些问题.石油与天然气地质,1997,18(2):83～89[Xu Huaida. Some issuses on the study of continental sequence stratigraphy. Oil & Gas Geology, 1997, 18(2):83～89] [21魏魁生.二连盆地白垩系非海相沉积层序地层特征.地球科学,1994, 19[Wei Kuisheng. Characteristics of the Cretaceous non-marine sequence stratigraphy in Erlian Basin. Earth Science, 1994, 19]
[22]魏魁生,徐怀大,雷怀玉,等.非海相层序地层学—以松辽盆地为例.北京:地质出版社,1996[Wei Kuisheng. Xu Huaida, Lei Huaiyu, et al. Non-marine sequence stratigraphy: a case study in Songliao Basin. Beijing: Geological Publishing House, 1996]
[23]樊太亮,李庆谋.沉积基准面变化分析技术及应用.石油与天然气地质,1997, 18(2): 108～113[Fan Tailiang, Li Qingmou. Analytical technique and application of deposited base-level change. Oil & Gas Geology, 1997, 18(2): 108～113]
[24]松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究杜江峰、刘招君、董清水、何玉平,吉林大学学报(地球科学版), 2005 Vol.35 No.2 171-176。
[25]冯有良,周海民,李思田等.陆相断陷盆地层序类型与构造特征.地质论评.
[26] Van Wagoner JC.Sequence stratigraphy and marine to non-marine facies architecture of foreland basin strata [J].AAPG Memoir,1995,64:137-223.
[27]刘招君,董清水,王嗣敏,等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002. Liu Zhao-jun, Dong Qing-shui, Wang Si-min, et al. Introduction to continental sequence stratigraphy and application[M]. Beijing: Petroleum Industry Press, 2002.
[28]徐怀大.陆相层序地层学研究中的某此问题[J].石油与天然气地质,1997,18(2):83-89. XU Huan-da. Some problems in study of continental sequence stratigraphy[J]. Oil and Gas Geology, 1997, 18(2): 83-89.
[29]薛良清.湖相盆地中的层序、体系域与隐蔽油气藏[J].石油与天然气地质,2002,23(2):115-120. XUE Liang-qing. Sequence, system tracts and subtle hyuduocarbon pools in lacustrine basins[J]. Oil and Gas Geology, 2002, 23(2): 115-120.
[30]邓宏文.美国层序地层研究中的新学派一高分辨率层序地层学[[J].石油与天然气地质. 1995.16(2):89-97.
[31]廖远涛.层序地层学的研究现状及反展方向.重庆石油高等专科学校学报. 2002.4(2):9-13.
[32]徐强,姜烨等.中国层序地层学研究现状和发展方向.沉积学报. 2003.21(1):157-167.
[33]汪彦,彭军等.中国高分辨率层序地层学的研究现状.天然气地球科学. 2005.16(3):352-358.
[34]于红枫,王英民,李雪.Stratimagic波形地震相分析在层序地层岩性分析中的应用.煤田地质与勘探. 2006.34(1):64-67.
[35]余杰,陈钢花.测井资料高分辨率层序地层分析.测井技术. 2007.31(1):21-24.
[36]房文静,范宜仁等.高斯小波用于测井层序地层自动划分的研究.中国石油大学学报(自然科学版). 2007.31(2):55-58.
[37]严德天,王华等.黄骅坳陷沙河街组层序地层样式及隐蔽圈闭预测.中国矿业大学学报. 2008.37(1):30-37.
[38]陈钢花,余杰,张孝珍.基于小波时频分析德测井层序地层划分方法.新疆石油地质. 2007.28(3):355-358.
[39]郭少滨.陆相断陷盆地层序地层模式.石油勘探与开发. 2006.33(5):548-552.
[40]纪友亮,张善文,冯建辉.陆相湖盆古地形、可容纳空间德体积变化率与层序结构德关系.沉积学报. 2005.23(4):631-638.
[41] Craver S, Memon N, Boon-Lock Yeo. Resolving Rightful Ownerships with Invisible Watermarking Techniques: limitations, Attack, and Implication. IEEE Journal on Selected Areas in Communication.1998. 16(4):573-586.
[42] Craver. Technical Trials and Legal Tribulations. Communications of the ACM.1998. 41(7):45-54.
[43] Ghose B. K. STRECH—a subroutine for stretching time series and its use in stratigraphic correlation. Computers & Geosciences.1984.10 (1):137- 147.
[44] Gordon A. D. 1973. A sequence comparison statistic and algorithm. Biometrika. 1973. 60 :197-200.
[45] Gordon A. D. SLOTSEQ—a FORTRAN IV program for comparing two sequences of observations. Computers & Geosciences.1980. 6(1): 7-20.
[46] Gordon A. D, Reyment R. A. Slotting of a borehole sequence. Mathematical Geology. 1079.11 (3):309-327.
[47] Krumbein W C, Sloss L L. Stratigraphy and Sedimentation.W. H. Freeman & Co. 1963:332 .
[48] B. A. Reymond and G. M. Stampfli.Three-dimensional sequence stratigraphy and subtle stratigraphic traps associated with systems tracts: West Cameron region, offshore Lousiana, Gulf of Mexico. Marine and Petroleum Geology. 1996.13(1):41-60.
[49] David C. Jennette, Khaled Fouad,etl.Slope and basin-floor reservoirs from the Miocene and Pliocene of the Veracruz Basin, southeastern Mexico. Marine and Petroleum Geology. 2003.20(8):587-600.
[50] Christian Ravenne. Sequence stratigraphy evolution since 1970[J]. C. R. Palevol. 2002.415-438
[51] Gareth T.George.Characterization and high resolution sequence stratigraphy of storm-dominated braid delta and shoreface sequences from the Basal Grit Group(Namurian) of the South Wales Variscan peripheral foreland basin[J]. Marine Petroleum Geology. 2000.17:445-475.
[52] David Jennette, Tim Wawrzyniec, Khaled Fouad etc. Traps and turbidite reservoir characteristics from a complex and evolving tectonic setting, Veracruz Basin, southeasternMexico[J]. AAPG Bulletin.2003.87(10): 1599-1622.
[53] Van Wagoner J C.An overview of the fundamentals of sequence stratigraphy andkey difinations[A]. Wilgus C K. Sea-level Changes: An Integrated Approach[C]. Society of Economic Paleonto logiste and Mineralogists Special Publication. 1988.125一154.
[54] Van Waggoner J C. et al. Sliliciclastic sequence stratigraphy in well logs cores and outcrops: concepts for high-resolutions correlation oftime and facies[J]. AAPG, Methods in exploration series 1990.55:1-240.
[55] Van Wagoner, M itchum J C, Camp ion R M, et al.Siliciclastic sequence stratigraphy in well logs, cores and outcrops[J]. AAPG. Methods in Exploration.1990.7:55-78.
[56] Posamentier H W, Weimer P. Siliciclastic sequence stratigraphy and petroleum geology where to from here[J]. AAPG. Bulletin. 1993.77(5):731-742.
[57] Vail P R. Mitchum R M. Todd R G et al. Seismic stratigraphy and global changes of sea level In: Paton C E ed Seismic stratigraphy-application to hydrocarbon exploration American Association of Petroleum Geologist[J]. Memories1997.26:A9-212.
[58] Gawthorpe R.L,Leeder M. R. Tectonic Sedimentary Evolution of Active Extensional Basins[J]. Basin Research. 2000.12:95-218.
[59] Gawthorpe R L, Fraser A J and Collier R E L. Sequence Stratigraphy in Active Extensional Basins: Implications for the Inter Pretation of Ancient Basin fills[J]. Marine and Petroleum Geology 1994.11:642 -658.
[60] Bruhn, C. H. L.,and R. G. Walker.High-resolution stratigraphy and sedimentary evolutionof coarse-grained canyon-filling turbidities form the Upper Cretaceous transgressive megasequence, Campos Basin,offshore Brazil[J]. Journal of Sedimentary Research. 1995. B65:426-442.
[61] Henry W Posamentier.Paul Weimer. Siliciclastic sequence stratigraphy and petroleum geology-where to from there?[J].AAPG Bulletin. 1993.77(5):731-742.
[62] Dalrymple R M, Zaitlin B A. High-resolution sequence stratigraphy of a complex, incised valley succession, Clbequid Bay-Salmon River Estuary, Bay of Fundy,Canada[3].Sedimentology.1995.41(6):1069-1091.
[63] Galloway W E. Genetic stratigraphic sequence in basin analysis I:architecture and genetics of flooding surface bounded depositional Units[J].AAPG Bulletin. 1989.73:125-142.
[64] Van Wgoner John C.Sequence stratigraphy and marine to nonmarine facies architecture of Forland Basin Strata,Book Cliiffs, Utah, U S A: reply[J].AAPG Bulletin. 1998. 82(8):1607-1618.
[65] Strecker Uwe, Stridtmann J R, Smithson.A conceptual tectonostratigraphic model for seismic facies migration in a fluvio-lacustrine extensional basion[J].AAPG Bulletin. 1999.83(1):43-61.
[66] Karen J Houck.Effects of sedimentation, tectonics, and glacio-eustasy on depositional sequences,Pennsylvanian mintum formation, North-central Colorado[J].AAPG Bulletin. 1997.(9):1510-1533.
[67] Gert Jan Weltje, Xander D Meijer, Poppel Deboer.Stratigraphic inversion of siliciclastic basin fills : a note on the distinction between supply signals resulting from tectonic and climatic forcing[J].Basin Research. 1998.10:129-153.
[68] Eschard R,Lemouzy P, Bacchiuna,et al.Combining sequence stratigraphy, geostatistical simulations and production data for modeling a fluvial reservoir in the chauchoy field(Triassic ,France)[J].AAPG Bulletin. 1998.82(4):545-568.
[69] Ryand W H, ChoughS K. Sequentialdevelopment of alluvial/lacustrine system :southeastern Eumsuny basin (Cretaceous), Korea[J].Journal of Sedimentary Research. 1997.67(2):274-285.
[70] Ziegler P.A. Geodynamic Processes Governing Development of Rifted Basins. In: Roure F,Ellouz N .Shein V .S .Skvortsov I.(eds),Geodynamic Evolartion of Sedimentary Basins, Edition Technip, Paris. 2001.19-673.
[71] Sylvester A G.Strike slip fault. Bull Geol Soc Am. 1989.100:1666-1703.
[72] Harland W H. Tectonic transpression in Caledonian Spitsber gen.Geol Mag.1971.108:27-42.
[73] Sylvester A G.Wrench fault tectonics. AAPG, Reprint S eries. 1984. (28):1-374.
[74] Harding T P.Petroleum traps associated with wrench faults .AAPG. Bu11. 1974.57:97-166.
[75] 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.
[76] Zhong Dalai, Tapponnier, Wu 1-laiwei, et al. Large scale strike slip fault: the major structure of intercontinental deformation after collision. Chinese Science Bulletin. 1990.35:304-309.
[77] Wan Tianfeng, et al.Formation and evolution of the Tan cheng-Lujiang fault zone,China. Wuhan: China University of Geosiences Press. 1996.1-11.
[78] Block,B.J.Structure,generation and preservation of upward fining,braided stream cycles in the Old Red Sandstone of Scotland:Transactions Royal Society of Edinburgh.1980.71:29-46.
[79] Gawthorpe,R.L.,and J,M.Hurst.Transfer zones in extensional basinsaheir structural style and influ-once on drainage development and stratigraphy:Journal of the Geological Society of London. 1933.150:1137-1152.
[80] Goldhammer,R.K.,P.A.Dunn,and L.A.Hardie.Depositional cycles, composite sea level changes,cycle stacking patterns,and the hierarchy of stratigraphic forcing:examples from the Alpine plat-form carbonates:GSA Bulletin.1990.102:535-562.
[81] Carlo Tansi, Francesco Muto, Salvatore Critelli and Giulio Iovine. Neogene-Quaternary strike-slip tectonics in the central Calabrian Arc (southern Italy). Journal of Geodynamics. 2007.43(3):393-414.
[82] Dimitrios K. Karamitros, George D. Bouckovalas and George P. Kouretzis. Stress analysis of buried steel pipelines at strike-slip fault crossings. Soil Dynamics and Earthquake Engineering. 2007.27(3):200-211.
[83] V. Mouslopoulou, A. Nicol, T.A. Little and J.J. Walsh. Displacement transfer between intersecting regional strike-slip and extensional fault systems. Journal of Structural Geology. 2007.29(1):59-72.
[84] R.T. Walker, A. Bayasgalan, R. Carson, R. Hazlett, L. McCarthy, J. Mischler, E. Molor, P. Sarantsetseg, L. Smith, B. Tsogtbadrakh, et al. Geomorphology and structure of the Jid right-lateral strike-slip fault in the Mongolian Altay mountains. Journal of Structural Geology. 2006.28(9):1607-1622.
[85] Michael Lazar, Zvi Ben-Avraham and Uri Schattner. Formation of sequential basins along a strike–slip fault–Geophysical observations from the Dead Sea basin. Tectonophysics. 2006.421(1-2):53-69. [59] Smith T R, Zhan Ci -xiang, Gao Peng. A knowledge-based,two-step procedure for extracting channel networks from noisy DEM data .Computers & Geosciences, 1990,166, 16(6) :777~786 .
[2]徐怀大等.从地震地层学到层序地层学.北京:石油工业出版社.1997.
[3]刘镇、吴因业.层序地层框架与油气藏勘探.北京:石油工业出版社.1999.
[4]操应长.断陷湖盆层序地层学.北京:地质出版社.2005.
[5]陆基孟.地震勘探原理.北京:石油大学出版社.2005.
[6]冯有良、李思田.陆相断陷盆地层序地层学研究—以渤海湾盆地东营凹陷为例.北京:科学教育出版社.2006.
[7]李明、候连华、邹才能、殷积峰、刘晓等.岩性地层油气藏地球物理勘探技术与应用.北京:石油工业出版社.2005.
[8]邹才能、池应柳、李明、薛叔浩等.陆相层序地层学分析技术.北京:石油工业出版社.2004.
[9]杨宝俊、张梅生、王璞珺.中国油气区地质—地球物理解析.北京:科学教育出版社.2003.
[10]谭廷栋等.测井学.北京:石油工业出版社.2004.
[11]田在艺、张庆春.中国含油气沉积盆地论.北京:石油工业出版社.1996.
[12]姜在兴.沉积学.北京:石油工业出版社.2005.
[13]宋万超、刘波、宋新民.层序地层学概念、原理、方法及应用.北京:石油工业出版社.2003.
[14]何幼斌、王文广.沉积岩与沉积相.北京:石油工业出版社.2007.
[15]吴元燕、吴胜和、蔡正旗.油矿地质学(第三版).北京:石油工业出版社.2005.
[16]陈恭洋.油气田地下地质学.北京:石油工业出版社.2007.
[17] Fred J.Hilterman著,孙夕平、赵良武等译.地震振幅解释.北京:石油工业出版社.2004.
[18]张厚福等.石油地质学.北京:石油工业出版社.1999.
[19]杨毅恒、韩燕等.多维地学数据处理技术与方法.北京:科学教育出版社.2002.
[20]徐怀大.陆相层序地层学研究中的某些问题.石油与天然气地质,1997,18(2):83～89[Xu Huaida. Some issuses on the study of continental sequence stratigraphy. Oil & Gas Geology, 1997, 18(2):83～89] [21魏魁生.二连盆地白垩系非海相沉积层序地层特征.地球科学,1994, 19[Wei Kuisheng. Characteristics of the Cretaceous non-marine sequence stratigraphy in Erlian Basin. Earth Science, 1994, 19]
[22]魏魁生,徐怀大,雷怀玉,等.非海相层序地层学—以松辽盆地为例.北京:地质出版社,1996[Wei Kuisheng. Xu Huaida, Lei Huaiyu, et al. Non-marine sequence stratigraphy: a case study in Songliao Basin. Beijing: Geological Publishing House, 1996]
[23]樊太亮,李庆谋.沉积基准面变化分析技术及应用.石油与天然气地质,1997, 18(2): 108～113[Fan Tailiang, Li Qingmou. Analytical technique and application of deposited base-level change. Oil & Gas Geology, 1997, 18(2): 108～113]
[24]松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究杜江峰、刘招君、董清水、何玉平,吉林大学学报(地球科学版), 2005 Vol.35 No.2 171-176。
[25]冯有良,周海民,李思田等.陆相断陷盆地层序类型与构造特征.地质论评.
[26] Van Wagoner JC.Sequence stratigraphy and marine to non-marine facies architecture of foreland basin strata [J].AAPG Memoir,1995,64:137-223.
[27]刘招君,董清水,王嗣敏,等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002. Liu Zhao-jun, Dong Qing-shui, Wang Si-min, et al. Introduction to continental sequence stratigraphy and application[M]. Beijing: Petroleum Industry Press, 2002.
[28]徐怀大.陆相层序地层学研究中的某此问题[J].石油与天然气地质,1997,18(2):83-89. XU Huan-da. Some problems in study of continental sequence stratigraphy[J]. Oil and Gas Geology, 1997, 18(2): 83-89.
[29]薛良清.湖相盆地中的层序、体系域与隐蔽油气藏[J].石油与天然气地质,2002,23(2):115-120. XUE Liang-qing. Sequence, system tracts and subtle hyuduocarbon pools in lacustrine basins[J]. Oil and Gas Geology, 2002, 23(2): 115-120.
[30]邓宏文.美国层序地层研究中的新学派一高分辨率层序地层学[[J].石油与天然气地质. 1995.16(2):89-97.
[31]廖远涛.层序地层学的研究现状及反展方向.重庆石油高等专科学校学报. 2002.4(2):9-13.
[32]徐强,姜烨等.中国层序地层学研究现状和发展方向.沉积学报. 2003.21(1):157-167.
[33]汪彦,彭军等.中国高分辨率层序地层学的研究现状.天然气地球科学. 2005.16(3):352-358.
[34]于红枫,王英民,李雪.Stratimagic波形地震相分析在层序地层岩性分析中的应用.煤田地质与勘探. 2006.34(1):64-67.
[35]余杰,陈钢花.测井资料高分辨率层序地层分析.测井技术. 2007.31(1):21-24.
[36]房文静,范宜仁等.高斯小波用于测井层序地层自动划分的研究.中国石油大学学报(自然科学版). 2007.31(2):55-58.
[37]严德天,王华等.黄骅坳陷沙河街组层序地层样式及隐蔽圈闭预测.中国矿业大学学报. 2008.37(1):30-37.
[38]陈钢花,余杰,张孝珍.基于小波时频分析德测井层序地层划分方法.新疆石油地质. 2007.28(3):355-358.
[39]郭少滨.陆相断陷盆地层序地层模式.石油勘探与开发. 2006.33(5):548-552.
[40]纪友亮,张善文,冯建辉.陆相湖盆古地形、可容纳空间德体积变化率与层序结构德关系.沉积学报. 2005.23(4):631-638.
[41] Craver S, Memon N, Boon-Lock Yeo. Resolving Rightful Ownerships with Invisible Watermarking Techniques: limitations, Attack, and Implication. IEEE Journal on Selected Areas in Communication.1998. 16(4):573-586.
[42] Craver. Technical Trials and Legal Tribulations. Communications of the ACM.1998. 41(7):45-54.
[43] Ghose B. K. STRECH—a subroutine for stretching time series and its use in stratigraphic correlation. Computers & Geosciences.1984.10 (1):137- 147.
[44] Gordon A. D. 1973. A sequence comparison statistic and algorithm. Biometrika. 1973. 60 :197-200.
[45] Gordon A. D. SLOTSEQ—a FORTRAN IV program for comparing two sequences of observations. Computers & Geosciences.1980. 6(1): 7-20.
[46] Gordon A. D, Reyment R. A. Slotting of a borehole sequence. Mathematical Geology. 1079.11 (3):309-327.
[47] Krumbein W C, Sloss L L. Stratigraphy and Sedimentation.W. H. Freeman & Co. 1963:332 .
[48] B. A. Reymond and G. M. Stampfli.Three-dimensional sequence stratigraphy and subtle stratigraphic traps associated with systems tracts: West Cameron region, offshore Lousiana, Gulf of Mexico. Marine and Petroleum Geology. 1996.13(1):41-60.
[49] David C. Jennette, Khaled Fouad,etl.Slope and basin-floor reservoirs from the Miocene and Pliocene of the Veracruz Basin, southeastern Mexico. Marine and Petroleum Geology. 2003.20(8):587-600.
[50] Christian Ravenne. Sequence stratigraphy evolution since 1970[J]. C. R. Palevol. 2002.415-438
[51] Gareth T.George.Characterization and high resolution sequence stratigraphy of storm-dominated braid delta and shoreface sequences from the Basal Grit Group(Namurian) of the South Wales Variscan peripheral foreland basin[J]. Marine Petroleum Geology. 2000.17:445-475.
[52] David Jennette, Tim Wawrzyniec, Khaled Fouad etc. Traps and turbidite reservoir characteristics from a complex and evolving tectonic setting, Veracruz Basin, southeasternMexico[J]. AAPG Bulletin.2003.87(10): 1599-1622.
[53] Van Wagoner J C.An overview of the fundamentals of sequence stratigraphy andkey difinations[A]. Wilgus C K. Sea-level Changes: An Integrated Approach[C]. Society of Economic Paleonto logiste and Mineralogists Special Publication. 1988.125一154.
[54] Van Waggoner J C. et al. Sliliciclastic sequence stratigraphy in well logs cores and outcrops: concepts for high-resolutions correlation oftime and facies[J]. AAPG, Methods in exploration series 1990.55:1-240.
[55] Van Wagoner, M itchum J C, Camp ion R M, et al.Siliciclastic sequence stratigraphy in well logs, cores and outcrops[J]. AAPG. Methods in Exploration.1990.7:55-78.
[56] Posamentier H W, Weimer P. Siliciclastic sequence stratigraphy and petroleum geology where to from here[J]. AAPG. Bulletin. 1993.77(5):731-742.
[57] Vail P R. Mitchum R M. Todd R G et al. Seismic stratigraphy and global changes of sea level In: Paton C E ed Seismic stratigraphy-application to hydrocarbon exploration American Association of Petroleum Geologist[J]. Memories1997.26:A9-212.
[58] Gawthorpe R.L,Leeder M. R. Tectonic Sedimentary Evolution of Active Extensional Basins[J]. Basin Research. 2000.12:95-218.
[59] Gawthorpe R L, Fraser A J and Collier R E L. Sequence Stratigraphy in Active Extensional Basins: Implications for the Inter Pretation of Ancient Basin fills[J]. Marine and Petroleum Geology 1994.11:642 -658.
[60] Bruhn, C. H. L.,and R. G. Walker.High-resolution stratigraphy and sedimentary evolutionof coarse-grained canyon-filling turbidities form the Upper Cretaceous transgressive megasequence, Campos Basin,offshore Brazil[J]. Journal of Sedimentary Research. 1995. B65:426-442.
[61] Henry W Posamentier.Paul Weimer. Siliciclastic sequence stratigraphy and petroleum geology-where to from there?[J].AAPG Bulletin. 1993.77(5):731-742.
[62] Dalrymple R M, Zaitlin B A. High-resolution sequence stratigraphy of a complex, incised valley succession, Clbequid Bay-Salmon River Estuary, Bay of Fundy,Canada[3].Sedimentology.1995.41(6):1069-1091.
[63] Galloway W E. Genetic stratigraphic sequence in basin analysis I:architecture and genetics of flooding surface bounded depositional Units[J].AAPG Bulletin. 1989.73:125-142.
[64] Van Wgoner John C.Sequence stratigraphy and marine to nonmarine facies architecture of Forland Basin Strata,Book Cliiffs, Utah, U S A: reply[J].AAPG Bulletin. 1998. 82(8):1607-1618.
[65] Strecker Uwe, Stridtmann J R, Smithson.A conceptual tectonostratigraphic model for seismic facies migration in a fluvio-lacustrine extensional basion[J].AAPG Bulletin. 1999.83(1):43-61.
[66] Karen J Houck.Effects of sedimentation, tectonics, and glacio-eustasy on depositional sequences,Pennsylvanian mintum formation, North-central Colorado[J].AAPG Bulletin. 1997.(9):1510-1533.
[67] Gert Jan Weltje, Xander D Meijer, Poppel Deboer.Stratigraphic inversion of siliciclastic basin fills : a note on the distinction between supply signals resulting from tectonic and climatic forcing[J].Basin Research. 1998.10:129-153.
[68] Eschard R,Lemouzy P, Bacchiuna,et al.Combining sequence stratigraphy, geostatistical simulations and production data for modeling a fluvial reservoir in the chauchoy field(Triassic ,France)[J].AAPG Bulletin. 1998.82(4):545-568.
[69] Ryand W H, ChoughS K. Sequentialdevelopment of alluvial/lacustrine system :southeastern Eumsuny basin (Cretaceous), Korea[J].Journal of Sedimentary Research. 1997.67(2):274-285.
[70] Ziegler P.A. Geodynamic Processes Governing Development of Rifted Basins. In: Roure F,Ellouz N .Shein V .S .Skvortsov I.(eds),Geodynamic Evolartion of Sedimentary Basins, Edition Technip, Paris. 2001.19-673.
[71] Sylvester A G.Strike slip fault. Bull Geol Soc Am. 1989.100:1666-1703.
[72] Harland W H. Tectonic transpression in Caledonian Spitsber gen.Geol Mag.1971.108:27-42.
[73] Sylvester A G.Wrench fault tectonics. AAPG, Reprint S eries. 1984. (28):1-374.
[74] Harding T P.Petroleum traps associated with wrench faults .AAPG. Bu11. 1974.57:97-166.
[75] 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.
[76] Zhong Dalai, Tapponnier, Wu 1-laiwei, et al. Large scale strike slip fault: the major structure of intercontinental deformation after collision. Chinese Science Bulletin. 1990.35:304-309.
[77] Wan Tianfeng, et al.Formation and evolution of the Tan cheng-Lujiang fault zone,China. Wuhan: China University of Geosiences Press. 1996.1-11.
[78] Block,B.J.Structure,generation and preservation of upward fining,braided stream cycles in the Old Red Sandstone of Scotland:Transactions Royal Society of Edinburgh.1980.71:29-46.
[79] Gawthorpe,R.L.,and J,M.Hurst.Transfer zones in extensional basinsaheir structural style and influ-once on drainage development and stratigraphy:Journal of the Geological Society of London. 1933.150:1137-1152.
[80] Goldhammer,R.K.,P.A.Dunn,and L.A.Hardie.Depositional cycles, composite sea level changes,cycle stacking patterns,and the hierarchy of stratigraphic forcing:examples from the Alpine plat-form carbonates:GSA Bulletin.1990.102:535-562.
[81] Carlo Tansi, Francesco Muto, Salvatore Critelli and Giulio Iovine. Neogene-Quaternary strike-slip tectonics in the central Calabrian Arc (southern Italy). Journal of Geodynamics. 2007.43(3):393-414.
[82] Dimitrios K. Karamitros, George D. Bouckovalas and George P. Kouretzis. Stress analysis of buried steel pipelines at strike-slip fault crossings. Soil Dynamics and Earthquake Engineering. 2007.27(3):200-211.
[83] V. Mouslopoulou, A. Nicol, T.A. Little and J.J. Walsh. Displacement transfer between intersecting regional strike-slip and extensional fault systems. Journal of Structural Geology. 2007.29(1):59-72.
[84] R.T. Walker, A. Bayasgalan, R. Carson, R. Hazlett, L. McCarthy, J. Mischler, E. Molor, P. Sarantsetseg, L. Smith, B. Tsogtbadrakh, et al. Geomorphology and structure of the Jid right-lateral strike-slip fault in the Mongolian Altay mountains. Journal of Structural Geology. 2006.28(9):1607-1622.
[85] Michael Lazar, Zvi Ben-Avraham and Uri Schattner. Formation of sequential basins along a strike–slip fault–Geophysical observations from the Dead Sea basin. Tectonophysics. 2006.421(1-2):53-69. [59] Smith T R, Zhan Ci -xiang, Gao Peng. A knowledge-based,two-step procedure for extracting channel networks from noisy DEM data .Computers & Geosciences, 1990,166, 16(6) :777~786 .