川西前陆盆地中侏罗统上沙溪庙组砂体展布特征其主控因素
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摘要
论文以沉积学，层序地层学，构造地质学，地球物理学等学科理论为指导，通过对川西前陆盆地中侏罗统沙溪庙组野外露头，钻井岩心，测井资料以及前人成果的综合分析，研究了川西前陆盆地中侏罗统上沙溪庙组的沉积体系特征，层序地层学特征，在此基础上进一步分析了川西前陆盆地上沙溪庙组沉积相带分布规律及砂体展布特征。根据岩石组合、沉积组构、沉积序列以及沉积机理等因素，并综合运用前人已有工作成果，本文认为川西前陆盆地上沙溪庙组主要发育大陆沉积体系组，包括冲积扇沉积体系、河流沉积体系，湖泊三角洲沉积体系和湖泊沉积体系。
通过野外露头与钻井岩心观测，结合测井分析，川西前陆盆地上沙溪庙组层序的底界面主要表现为岩性岩相转换面；顶界面为上侏罗统遂宁组与中侏罗统上沙溪庙组的分界面，识别出上沙溪庙组发育一个三级层序。
通过沉积物平面变化，碎屑成分分析，石英颗粒成因类型，古流向分析及重矿物分析对川西前陆盆地上沙溪庙组进行了物源分析，发现研究区存在盆地西缘龙门山逆冲推覆带及北缘米仓山－大巴山逆冲推覆带两个物源。
通过分析盆地内沉积相带分布规律研究了其砂体展布特征，发现龙门山及米仓山－大巴山逆冲推覆带的构造运动沉积相带分布的主控因素，而砂体展布特征则完全受控于沉积相带的分布。并在研究层序发育短期基准面旋回的基础上，分析了砂体结构特征，发现盆缘造山带构造运动引起的可容纳空间变化机制通过控制短期基准面升降过程，控制了川西前陆盆地侏罗纪上沙溪庙地层中砂体结构、成因类型及发育规模。
Guided by sedimentology, sequence stratigraphy, structural geology, geophysics and soon, Integrated researched the outcrops, cores ,logging data from the Middle Jurassic upperShaximiao formation in the western Sichuan foreland Basin, realized the charaters ofdepositional system, sequence stratigraphy, discussion the dis-tribution of sedimentaryfacies and the characteristics of sand body distribution.
According to the petrofabric, depositional fabric , sedimentary sequence, life assemblageand so on, combined with predecessor’s research,Continental sedimentary system groupcontain alluvial fan sedimentary system, fluvial sedimentary system and lake sedimentarysystem were recognized in the western Sichuan foreland Basin.
According to the outcrops and cores ,combined with logging data , the bottom surfaces ofsequence in upper Shaximiao formation in western sichuan foreland Basin mainly astransition surface of rock character and facies，the top surfaces of sequence were the interfaceof Suining formation and upper Shaximiao formation.one sedimentary sequence wererecognized in upper Shaximiao formation.
According to the sediment level change，clastic component analysis，genetic types ofquartz grains，paleocurrent analysis and heavy mineral analysis，conducted the sourcs analysisof Middle Jurassic upper Shaximiao formation in western sichuan foreland Basin.Found outthere were tow sources of western sichuan fore-land Basin：Longmenshan thrust belt inwestern margin of basin and Micangshan-Dabashan thrust belt in northern margin of basin.
According to discussion the distribution of sedimentary facies in the basin，re-searchedthe characteristics of sand body distribution. Found out that the tectonic movement ofLongmenshan thrust belt and Micangshan-Dabashan thrust belt were the top management of the distribution of sedimentary facies，and the characteristics of sand body distribution fullycontrolled by he distribution of sedimentary facies.And according to discussion sequencedevelopment short-term base level cycle，analyzied the structural characteristics of sandbody，found out the tectonic movement of orogenisc belt in the basin margin caused thechange in accommodation space control mechanism of the process of short-term base-levelmovements controlling the structural characteristics of sand body，genetic type and thedevelopment scale of Middle Jurassic upper Shaximiao formation in western sichuan forelandBasin.
通过野外露头与钻井岩心观测，结合测井分析，川西前陆盆地上沙溪庙组层序的底界面主要表现为岩性岩相转换面；顶界面为上侏罗统遂宁组与中侏罗统上沙溪庙组的分界面，识别出上沙溪庙组发育一个三级层序。
通过沉积物平面变化，碎屑成分分析，石英颗粒成因类型，古流向分析及重矿物分析对川西前陆盆地上沙溪庙组进行了物源分析，发现研究区存在盆地西缘龙门山逆冲推覆带及北缘米仓山－大巴山逆冲推覆带两个物源。
通过分析盆地内沉积相带分布规律研究了其砂体展布特征，发现龙门山及米仓山－大巴山逆冲推覆带的构造运动沉积相带分布的主控因素，而砂体展布特征则完全受控于沉积相带的分布。并在研究层序发育短期基准面旋回的基础上，分析了砂体结构特征，发现盆缘造山带构造运动引起的可容纳空间变化机制通过控制短期基准面升降过程，控制了川西前陆盆地侏罗纪上沙溪庙地层中砂体结构、成因类型及发育规模。
Guided by sedimentology, sequence stratigraphy, structural geology, geophysics and soon, Integrated researched the outcrops, cores ,logging data from the Middle Jurassic upperShaximiao formation in the western Sichuan foreland Basin, realized the charaters ofdepositional system, sequence stratigraphy, discussion the dis-tribution of sedimentaryfacies and the characteristics of sand body distribution.
According to the petrofabric, depositional fabric , sedimentary sequence, life assemblageand so on, combined with predecessor’s research,Continental sedimentary system groupcontain alluvial fan sedimentary system, fluvial sedimentary system and lake sedimentarysystem were recognized in the western Sichuan foreland Basin.
According to the outcrops and cores ,combined with logging data , the bottom surfaces ofsequence in upper Shaximiao formation in western sichuan foreland Basin mainly astransition surface of rock character and facies，the top surfaces of sequence were the interfaceof Suining formation and upper Shaximiao formation.one sedimentary sequence wererecognized in upper Shaximiao formation.
According to the sediment level change，clastic component analysis，genetic types ofquartz grains，paleocurrent analysis and heavy mineral analysis，conducted the sourcs analysisof Middle Jurassic upper Shaximiao formation in western sichuan foreland Basin.Found outthere were tow sources of western sichuan fore-land Basin：Longmenshan thrust belt inwestern margin of basin and Micangshan-Dabashan thrust belt in northern margin of basin.
According to discussion the distribution of sedimentary facies in the basin，re-searchedthe characteristics of sand body distribution. Found out that the tectonic movement ofLongmenshan thrust belt and Micangshan-Dabashan thrust belt were the top management of the distribution of sedimentary facies，and the characteristics of sand body distribution fullycontrolled by he distribution of sedimentary facies.And according to discussion sequencedevelopment short-term base level cycle，analyzied the structural characteristics of sandbody，found out the tectonic movement of orogenisc belt in the basin margin caused thechange in accommodation space control mechanism of the process of short-term base-levelmovements controlling the structural characteristics of sand body，genetic type and thedevelopment scale of Middle Jurassic upper Shaximiao formation in western sichuan forelandBasin.
引文
1] Allen PA,Homewood P. Foreland Basin[M]. Oxford: Blackwell scientific publication,1986
[2] Beaumont C., Quinlan G., Hamilton J. Orogeny and stratigraphy: numerical models ofthePalaeozoic in the eastern interior of North America[J].Tectonics, 1988,7(3):389~416
[3] Beaumont C., Tankand A J. Sedimentary basin-forming mechanism[J].Canadian Society ofPetroleum Geologists, Memoir,1987
[4] Bohacs K M ,et a1.Lake~basin type,source potential,and hydrocarbon characterl anintegrated sequence—stratigraphiegeochemical framework[A]Gierlowski EH,Kordesch,Kelts K R.Lake Basins Through Space and Time[C].AAPG Studies in Geology46,2000:3~34.
[5] Cross T A. And Lessenger M A, Sediment Volume Partitioning: Rationale for StratigraphicModel Evaluation and High~Resolution Stratigraphic Correlation[R]. Accepted forpublication in Norwegian Petroleums~Forening Conference Volume, 1996. 1~24.
[6] Cross T A. Controls on coal distribution in transgressive~regressive cycles, UpperCretaceous, Western Interior, D.S.A. In:Wilgans c k, et al. Sea~level changes:Anintergratedapproach[J]. SEPM Sepecial Publication, 42,1988, 371~380.
[7] Cross T A. Straigraphic controls on reservoir attributes in continental strata（地层因素对陆相沉积储层特征的控制)[J].地学前缘,2000,7(4):322~350.
[8] Cross T.A.,Applications of high~resolution sequence stratigraphy in petroleum explorationand pnouetion short course Notes[J]. Canadian Society of Petroleum geologists,1993:290.
[9] Decelles G., Giles K A. Foreland basin systems[J]. Basin Reasearh, 1996,8:105~123
[10] Dickinson W R. Plate tectonic evolution of sedimentary basin[J].AAPG ContinuingEducation Course Notes Series 1,1976, pp. 62
[11] Galloway W E.Genetic stratigraphic sequence in basin analysis(I):architecture and geneticsof flooding surface bounded by depositional unites[J].AAPG Bulletin,1989,73(1):125~142.
[12] Ingersol R V and Busby C J. Tectonics of sedimentary basins.In: Busby C J,Ingersol RV.eds.Tectonics of Sedimentary Basins[J].Cambridge:Blackwell,1995.1-51.
[13] Johnson J G., Klapper G,Sandberg C A. Devonian eustatic fluctuation inEurameria[J].Geological Socitery of America Bulletin, 1985, 96:567~87.
[14] Krapez B. Sequence stratigraphic concepts applied to the identification of basin－fillingrhythems in Precambrian successions. Australian Journal of Earth Sciences,1996,43(3):355~380.
[15] Krapez B. Sequence stratigraphic concepts applies to the identification of depositionalbasins and global tectonic cycles .Australian Journal of Earth Science,1997,44(1):1~36.
[16] Miall A D. Sequence stratigraphy and their chronostratigraphical correlation. Jour sedimentpetrol,1991,61(4):497~505.
[17] Peters K E,et a1.A new geochmical~sequence stratigraphic model for the Mahakam Deltaand M akassar Slope,Kalimantan,Indonesia[J].AAPG Bulletin,2000,84(1):12~44.
[18] Posamentier H W, et al. Variability of the sequence stratigraphic model effects of local basinfactors[J]. Sedimentary Geology,1993,86:91~109
[19] Shanley, K. W.. Perspectives on the Sequence Stratigraphy of Continental Strata[J].AAPG,1994,78:544~568.
[20] Vail P R and Hardenbol J R. Effect of sea level change on shelf~slope boundary. AAPGBulletin 1981,65(5):1003.
[21] Vail P R,Mitchum R M. Global cycles of relative changes of sea level from seismicstratigraphy (in Geological and geophysical investigations of continental margins). Memoir－American Association of Petroleum Geologists,1979,（29):469~472.
[22] Vail P R. Seismic stratigraphy and the evaluation of depositional sequences and facies.Geophysical Journal of the Royal Astronomical Society.1983,73（1):278.
[23] Vail P R. Seismic stratigraphy interpretation using sequence stratigraphy. Part1: Seismicstratigraphy interpretation procedure. In: Bally A W ed. Atlas of seismic stratigraphy. AAPGStudies in Geology,1987,27:1~10.
[24] Vail P R.Sequence stratigraphy workbook,fundamentals of sequence stratigraphy.AAPGAnnual Conventio n Short Course:Sequence Stratigraphy Interpretation of Seismic Well andOutcrop Data[J].AAPG, 1998:217~223.
[25] Watts A B. Lithospheric flexure due to prograding sediment loads一imphcations for theorigin of offalp/onlap patterns in sedimenfary basins[J].Basin Research, 1989, 2:133~144
[26] Wheeler H E. Time Stratigraphy[J].AAPG,1999,42:1047~1063.
[27]陈洪德等.层序地层学理论和研究方法[J].四川科学技术出版社,1994.
[28]陈洪德,覃建雄,田景春,等.中国南方二叠纪层序岩相古地理特征及演化[J].沉积学报,1999,17(4):510~521.
[29]陈洪德,覃建雄,田景春,等.右江盆地层序充填动力学初探[J].沉积学报,2000,18(2):165~171.
[30]陈洪德,侯中健,田景春,等.鄂尔多斯地区晚占生代沉积层序地层学与盆地构造演化研究[J].矿物岩石,2001,21(003):16~22.
[31]陈洪德等.中国南方海相震旦系-中三叠统构造-层序岩相古地理研究及编图[内部报告],2002.
[32]陈洪德等.中国南方陆相中—新生代构造—层序岩相古地理研究及编图[内部报告],2006.
[33]陈洪德,倪新锋.陇东地区三叠系延长组沉积层序及充填响应特征[J].石油与天然气地质,2006,27(2):143~151
[34]陈洪德,赵俊兴,付锁堂,等.鄂尔多斯盆地中南部早中侏罗世沉积层序充填动力学作用过程[J].天然气工业,2007,27(5):21~25.
[35]邓宏文,王洪亮,宁宁,等.沉积物体积分配原理－高分辨率层序地层学的理论基础[J].地学前缘, 2000.7(4): 305~313.
[36]邓宏文,王红亮,王敦则.古地貌对陆相裂谷盆地层序充填特征的控制－以渤中凹陷西斜坡区下第三系为例[J].石油与天然气地质,2001,22(4):293~296.
[37]邓宏文,王红亮,祝永军,等.高分辨率层序地层学－原理及应用[M].北京:地质出版社,2002a.3~24.
[38]邓宏文, T. A. Cross等.高分辨率层序地层学－原理及应用[M].北京:地质出版社,2002b.
[39]邓宏文,王红亮,阎伟鹏,等.河流相层序地层构成模式探讨[J].沉积学报,2004a,22(3):373~379.
[40]邓宏文,王红亮,王居峰,等.层序地层构成与层序控砂、控藏的自相似特征—以三角洲~浊积扇体系为例[J].石油与天然气地质,2004b,25(5):491~495.
[41]邓康龄.四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(5):7~12.
[42]方世虎,宋岩,贾承造,等.新疆博格达地区中—新生代碎屑成分特征与盆山分异过程[J].地质学报,2007,81（9):1229~1237.
[43]甘克文,等世界含油气盆地图说明书[M].北京:石油I.业出版社,1992.
[44]高红灿,郑荣才,柯光明,等.川东北前陆盆地须家河组层序-岩相古地理特征[J].沉积与特提斯地质,2005, 25(3):38~45.
[45]高红灿.川东北前陆盆地须家河组沉积相及高分辨率层序地层学特征[硕士毕业论文].成都理工大学,2003.
[46]古俊林,郑荣才,罗平,等.川西坳陷中-南段须家河组层序地层格架与生储盖组合[J].成都理工大学学报(自然科学版),2004, 31(3):282~290.
[47]关士聪,渲怀玉,丘东洲等.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.
[48]郭令智,朱文斌,马瑞士,等.论构造耦合作用[J].大地构造与成矿学,2003,27(3) :197~205.
[49]何登发,李德生.沉积盆地动力学研究的新进展[J].地学前缘,1995,2(3):53~58.
[50]何鲤,段勇,罗潇,等.川西坳陷上三叠统层序地层划分新方案[J].天然气工业,2007,27(2):6~11.
[51]解习农,李思田.伊通地堑层序地层分析及充填史研究[J].中国地质大学学报,1993,18(l):20~24.
[52]柯光明,郑荣才,高红灿,等.四川盆地须家河组高分辨率层序-岩相古地理特征[J].成都理工大学学报(自然科学版),2008, 35(6):630~638.
[53]李继亮,肖文交,等.盆山耦合与沉积作用[J].沉积学报, 2003 21(1): 52~60.
[54]李绍虎,吴冲龙,王华,等.四川须家河组层序地层格架与天然气成藏的关系[J].石油与天然气地质, 1998,19(2):146~151.
[55]李双建,王清晨,李忠,等.砂岩碎屑组份变化对库车坳陷和南天山盆山演化的指示[J].地质科学,2006,41(3): 465~478.
[56]李思田,杨十恭.论沉积盆地的等时地层格架和基本建造单元[J].沉积学报,1992,10(4):11~22.
[57]李思田.层序地层学分析与海平面变化研究~进展与争论[J].地质科技情报,1992,11(4):23~29.
[58]李思田.鄂尔多斯盆地东北部层序地层及沉积体系分析[M].北京:地质出版社,1992.
[59]李思田.论沉积盆地分析领域的追踪与创新[J].沉积学报,1992,10(3):10~15.
[60]李文汉.层序地层学基础和关键定义[J].岩相占地理,1989,9(6):32~41
[61]李耀西,宋礼生,周志强等.大巴山西段早古生代地层志[M].北京:地质出版社,1975,1~372.
[62]林良彪,陈洪德,侯明才.须家河组砂岩组分特征与龙门山推覆体的形成演化[J].天然气工业,2007,27(4):4-6,28-30.
[63]林良彪,陈洪德,翟常博,等.四川盆地西部须家河组砂岩组分及其古地理探讨[J].石油实验地质,2006,28(6):511~517.
[64]林良彪.川西前陆盆地上三叠统须家河组沉积相及岩相古地理演化[硕士毕业论文].成都理工大学,2005.
[65]林茂炳,苟宗海,吴山,等.龙门山地质考察指南[M].成都:成都科技大学出版社,1997,1~204.
[66]刘宝珺,李文汉.层序地层学研究与应用[M].成都:四川科学技术出版社.1994.
[67]刘和甫.前陆盆地类型及褶皱一冲断层样式[J].地学前缘,1995,2(3-4):59~68.
[68]刘树根,罗志立,曹树恒.一种新的陆内俯冲类型－龙门山型俯冲成因机制研究[J].石油实验地质,1991,13(4):314~324.
[69]刘树根.龙门山冲断带与川西前陆盆地的形成与演化[M].成都:成都科技大学出版社,1993.
[70]刘树根,童崇光,罗志立,等.川西晚三叠世前陆盆地的形成与演化[J].天然气工业,1995,15(2):11~15.
[71]刘树根等,龙门山造山带-川西前陆盆地系统构造事件研究[J].成都理工大学学报(自然科学版),2001,28(3):221~230.
[72]马永生,陈洪德,王国力等.中国南方层序地层与古地理[M].2009a,1~603.
[73]马永生,陈洪德,王国力等.中国南方陆相中-新生代构造-层序岩相古地理研究及编图[M].2009b,1~299.
[74]牛树银,孙爱群,白文吉.造山带与相邻盆地间物质的横向迁移[J].地学前缘,1995,2(1):85~92.
[75]彭军.黔桂地区石炭纪层序地层特征及发育机制[M].成都理工大学,1999.
[76]彭军,陈景山,郑荣才.百色盆地百岗组高分辨率层序分析及研究意义[J].地球学报,2002,23(2):153~158.
[77]田景春,张翔,聂永生,等.层序的测井、地震响应特征研究[J].物探化探计算技术,2005,27(4):321~326.
[78]田景春,陈高武,张翔,等.沉积地球化学在层序地层分析中的应用[J].成都理工大学学报：自然科学版,2006,33(1):30~35.
[79]田树刚,章雨旭.华北地台北部奥陶纪露头层序地层[J].地球学报－中国地质科学院院报,1997,l:87~96.
[80]童崇光.四川盆地断褶构造形成机制[J].天然气工业, 1992.12(5):1~6.
[81]童金南,崔玮霞.碳酸盐缓坡区的露头层序地层研究[J].地球科学－中国地质人学学报,2002,27(5):565~569.
[82]王俊.四川盆地上三叠统_侏罗系沉积体系及层序地层学研究[硕士毕业论文].成都理工大学,2007.
[83]吴根耀.构造层序地层学[J].地球科学进展,1996,11(3):310~310.
[84]许效松.层序地层序研究进展[J].岩相古地理,1994,14(1):34~39.
[85]许效松,徐强.盆山转换和当代盆地分析中的新问题[J].岩相古地理,1996a,16(2):24~33.
[86]许效松.被动大陆边缘碳酸盐生长序列与盆山转换耦合[J].地球学报－中国地质科学院院报,1996b,17(1):41~53.
[87]许效松.层序地层在沉积学和油储勘探中研究的关键点[J].岩相古地理,1996c,16(6):55~62.
[88]许效松,刘宝珺,徐强,等.中国西部大型盆地分析及地球动力学[M].地质出版社,1997a,1~168.
[89]许效松,刘宝珺,赵玉光,等.上扬子西缘二叠纪－三叠纪层序地层与盆山转换耦合[M].北京:地质出版社:1997b,9~16.
[90]许效松.盆山转移与造盆,造山过程分析[J].岩相古地理,1998,18(6):1~10.
[91]姚根顺,李大成,卢文忠,等.四川叠合盆地盆山耦合特征分析[J].大地构造与成矿学,2006,30(4):435~444.
[92]叶黎明,陈洪德,胡晓强,等.川西前陆盆地须家河期高分辨率层序格架与古地理演化[J].地层学杂志,2006,30(1):89~94.
[93]叶茂才,易智强,李剑波.川西坳陷蓬莱镇组沉积体系时空配置规律.成都理工大学学报,2000,20(1):54~58.
[94]叶泰然.川西坳陷合兴场—罗江地区上三叠统须家河组二段致密裂缝性砂岩储层预测[硕士毕业论文].成都理工大学,2003
[95]尹世明.川西坳陷蓬莱镇组构造—充填层序特征[J].矿物岩石,1999,19(4):40~46.
[96]曾允孚,李勇.龙门山前陆盆地形成与演化[J].矿物岩石,1995,40~49.
[97]赵俊兴,陈洪德,傅锁堂,等.鄂尔多斯盆地侏罗系层序地层与盆地充填演化耦合关系[J].成都理工大学学报:自然科学版,2007,.34(5):511~518
[98]赵永刚,陈景山,雷卞军,等.川西邛崃县白马庙气田上侏罗统蓬莱镇组高分辨率层序地层分析[J].中国地质,2005,23(4):674~681.
[99]郑德文张培震万景林,等.碎屑颗粒热年代学-一种揭示盆山耦合过程的年代学方法[J].地震地质,2000,22(b12):25~36.
[100]郑荣才,彭军,彭光明,等.高分辨率层序分析在油藏开发工程中的应用－以百色盆地仑35块那二段油藏为例[J].沉积学报, 2003,21(4):654~662.
[101]郑荣才,周祺,王华,等.鄂尔多斯盆地长北气田山西组2段高分辨率层序构型与砂体预测[J].高校地质学报,2009a,15(1):69~79.
[102]郑荣才,朱如凯,戴朝成,等.川东北类前陆盆地须家河组盆－山耦合过程的沉积－层序特征[J].地质学报, 2008b,82(8):1077~1087.
[103]朱志军,陈洪德,林良彪,等.川西前陆盆地蓬莱镇期层序、岩相古地理特征及演化[J].地层学杂志,2009, 33(3):318~325.
[104]邹光富,陈永明,夏彤.层序地层学在区域地质调杳中的应用[J].四川地质学报,2003,23(l):l~4.
[2] Beaumont C., Quinlan G., Hamilton J. Orogeny and stratigraphy: numerical models ofthePalaeozoic in the eastern interior of North America[J].Tectonics, 1988,7(3):389~416
[3] Beaumont C., Tankand A J. Sedimentary basin-forming mechanism[J].Canadian Society ofPetroleum Geologists, Memoir,1987
[4] Bohacs K M ,et a1.Lake~basin type,source potential,and hydrocarbon characterl anintegrated sequence—stratigraphiegeochemical framework[A]Gierlowski EH,Kordesch,Kelts K R.Lake Basins Through Space and Time[C].AAPG Studies in Geology46,2000:3~34.
[5] Cross T A. And Lessenger M A, Sediment Volume Partitioning: Rationale for StratigraphicModel Evaluation and High~Resolution Stratigraphic Correlation[R]. Accepted forpublication in Norwegian Petroleums~Forening Conference Volume, 1996. 1~24.
[6] Cross T A. Controls on coal distribution in transgressive~regressive cycles, UpperCretaceous, Western Interior, D.S.A. In:Wilgans c k, et al. Sea~level changes:Anintergratedapproach[J]. SEPM Sepecial Publication, 42,1988, 371~380.
[7] Cross T A. Straigraphic controls on reservoir attributes in continental strata（地层因素对陆相沉积储层特征的控制)[J].地学前缘,2000,7(4):322~350.
[8] Cross T.A.,Applications of high~resolution sequence stratigraphy in petroleum explorationand pnouetion short course Notes[J]. Canadian Society of Petroleum geologists,1993:290.
[9] Decelles G., Giles K A. Foreland basin systems[J]. Basin Reasearh, 1996,8:105~123
[10] Dickinson W R. Plate tectonic evolution of sedimentary basin[J].AAPG ContinuingEducation Course Notes Series 1,1976, pp. 62
[11] Galloway W E.Genetic stratigraphic sequence in basin analysis(I):architecture and geneticsof flooding surface bounded by depositional unites[J].AAPG Bulletin,1989,73(1):125~142.
[12] Ingersol R V and Busby C J. Tectonics of sedimentary basins.In: Busby C J,Ingersol RV.eds.Tectonics of Sedimentary Basins[J].Cambridge:Blackwell,1995.1-51.
[13] Johnson J G., Klapper G,Sandberg C A. Devonian eustatic fluctuation inEurameria[J].Geological Socitery of America Bulletin, 1985, 96:567~87.
[14] Krapez B. Sequence stratigraphic concepts applied to the identification of basin－fillingrhythems in Precambrian successions. Australian Journal of Earth Sciences,1996,43(3):355~380.
[15] Krapez B. Sequence stratigraphic concepts applies to the identification of depositionalbasins and global tectonic cycles .Australian Journal of Earth Science,1997,44(1):1~36.
[16] Miall A D. Sequence stratigraphy and their chronostratigraphical correlation. Jour sedimentpetrol,1991,61(4):497~505.
[17] Peters K E,et a1.A new geochmical~sequence stratigraphic model for the Mahakam Deltaand M akassar Slope,Kalimantan,Indonesia[J].AAPG Bulletin,2000,84(1):12~44.
[18] Posamentier H W, et al. Variability of the sequence stratigraphic model effects of local basinfactors[J]. Sedimentary Geology,1993,86:91~109
[19] Shanley, K. W.. Perspectives on the Sequence Stratigraphy of Continental Strata[J].AAPG,1994,78:544~568.
[20] Vail P R and Hardenbol J R. Effect of sea level change on shelf~slope boundary. AAPGBulletin 1981,65(5):1003.
[21] Vail P R,Mitchum R M. Global cycles of relative changes of sea level from seismicstratigraphy (in Geological and geophysical investigations of continental margins). Memoir－American Association of Petroleum Geologists,1979,（29):469~472.
[22] Vail P R. Seismic stratigraphy and the evaluation of depositional sequences and facies.Geophysical Journal of the Royal Astronomical Society.1983,73（1):278.
[23] Vail P R. Seismic stratigraphy interpretation using sequence stratigraphy. Part1: Seismicstratigraphy interpretation procedure. In: Bally A W ed. Atlas of seismic stratigraphy. AAPGStudies in Geology,1987,27:1~10.
[24] Vail P R.Sequence stratigraphy workbook,fundamentals of sequence stratigraphy.AAPGAnnual Conventio n Short Course:Sequence Stratigraphy Interpretation of Seismic Well andOutcrop Data[J].AAPG, 1998:217~223.
[25] Watts A B. Lithospheric flexure due to prograding sediment loads一imphcations for theorigin of offalp/onlap patterns in sedimenfary basins[J].Basin Research, 1989, 2:133~144
[26] Wheeler H E. Time Stratigraphy[J].AAPG,1999,42:1047~1063.
[27]陈洪德等.层序地层学理论和研究方法[J].四川科学技术出版社,1994.
[28]陈洪德,覃建雄,田景春,等.中国南方二叠纪层序岩相古地理特征及演化[J].沉积学报,1999,17(4):510~521.
[29]陈洪德,覃建雄,田景春,等.右江盆地层序充填动力学初探[J].沉积学报,2000,18(2):165~171.
[30]陈洪德,侯中健,田景春,等.鄂尔多斯地区晚占生代沉积层序地层学与盆地构造演化研究[J].矿物岩石,2001,21(003):16~22.
[31]陈洪德等.中国南方海相震旦系-中三叠统构造-层序岩相古地理研究及编图[内部报告],2002.
[32]陈洪德等.中国南方陆相中—新生代构造—层序岩相古地理研究及编图[内部报告],2006.
[33]陈洪德,倪新锋.陇东地区三叠系延长组沉积层序及充填响应特征[J].石油与天然气地质,2006,27(2):143~151
[34]陈洪德,赵俊兴,付锁堂,等.鄂尔多斯盆地中南部早中侏罗世沉积层序充填动力学作用过程[J].天然气工业,2007,27(5):21~25.
[35]邓宏文,王洪亮,宁宁,等.沉积物体积分配原理－高分辨率层序地层学的理论基础[J].地学前缘, 2000.7(4): 305~313.
[36]邓宏文,王红亮,王敦则.古地貌对陆相裂谷盆地层序充填特征的控制－以渤中凹陷西斜坡区下第三系为例[J].石油与天然气地质,2001,22(4):293~296.
[37]邓宏文,王红亮,祝永军,等.高分辨率层序地层学－原理及应用[M].北京:地质出版社,2002a.3~24.
[38]邓宏文, T. A. Cross等.高分辨率层序地层学－原理及应用[M].北京:地质出版社,2002b.
[39]邓宏文,王红亮,阎伟鹏,等.河流相层序地层构成模式探讨[J].沉积学报,2004a,22(3):373~379.
[40]邓宏文,王红亮,王居峰,等.层序地层构成与层序控砂、控藏的自相似特征—以三角洲~浊积扇体系为例[J].石油与天然气地质,2004b,25(5):491~495.
[41]邓康龄.四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(5):7~12.
[42]方世虎,宋岩,贾承造,等.新疆博格达地区中—新生代碎屑成分特征与盆山分异过程[J].地质学报,2007,81（9):1229~1237.
[43]甘克文,等世界含油气盆地图说明书[M].北京:石油I.业出版社,1992.
[44]高红灿,郑荣才,柯光明,等.川东北前陆盆地须家河组层序-岩相古地理特征[J].沉积与特提斯地质,2005, 25(3):38~45.
[45]高红灿.川东北前陆盆地须家河组沉积相及高分辨率层序地层学特征[硕士毕业论文].成都理工大学,2003.
[46]古俊林,郑荣才,罗平,等.川西坳陷中-南段须家河组层序地层格架与生储盖组合[J].成都理工大学学报(自然科学版),2004, 31(3):282~290.
[47]关士聪,渲怀玉,丘东洲等.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.
[48]郭令智,朱文斌,马瑞士,等.论构造耦合作用[J].大地构造与成矿学,2003,27(3) :197~205.
[49]何登发,李德生.沉积盆地动力学研究的新进展[J].地学前缘,1995,2(3):53~58.
[50]何鲤,段勇,罗潇,等.川西坳陷上三叠统层序地层划分新方案[J].天然气工业,2007,27(2):6~11.
[51]解习农,李思田.伊通地堑层序地层分析及充填史研究[J].中国地质大学学报,1993,18(l):20~24.
[52]柯光明,郑荣才,高红灿,等.四川盆地须家河组高分辨率层序-岩相古地理特征[J].成都理工大学学报(自然科学版),2008, 35(6):630~638.
[53]李继亮,肖文交,等.盆山耦合与沉积作用[J].沉积学报, 2003 21(1): 52~60.
[54]李绍虎,吴冲龙,王华,等.四川须家河组层序地层格架与天然气成藏的关系[J].石油与天然气地质, 1998,19(2):146~151.
[55]李双建,王清晨,李忠,等.砂岩碎屑组份变化对库车坳陷和南天山盆山演化的指示[J].地质科学,2006,41(3): 465~478.
[56]李思田,杨十恭.论沉积盆地的等时地层格架和基本建造单元[J].沉积学报,1992,10(4):11~22.
[57]李思田.层序地层学分析与海平面变化研究~进展与争论[J].地质科技情报,1992,11(4):23~29.
[58]李思田.鄂尔多斯盆地东北部层序地层及沉积体系分析[M].北京:地质出版社,1992.
[59]李思田.论沉积盆地分析领域的追踪与创新[J].沉积学报,1992,10(3):10~15.
[60]李文汉.层序地层学基础和关键定义[J].岩相占地理,1989,9(6):32~41
[61]李耀西,宋礼生,周志强等.大巴山西段早古生代地层志[M].北京:地质出版社,1975,1~372.
[62]林良彪,陈洪德,侯明才.须家河组砂岩组分特征与龙门山推覆体的形成演化[J].天然气工业,2007,27(4):4-6,28-30.
[63]林良彪,陈洪德,翟常博,等.四川盆地西部须家河组砂岩组分及其古地理探讨[J].石油实验地质,2006,28(6):511~517.
[64]林良彪.川西前陆盆地上三叠统须家河组沉积相及岩相古地理演化[硕士毕业论文].成都理工大学,2005.
[65]林茂炳,苟宗海,吴山,等.龙门山地质考察指南[M].成都:成都科技大学出版社,1997,1~204.
[66]刘宝珺,李文汉.层序地层学研究与应用[M].成都:四川科学技术出版社.1994.
[67]刘和甫.前陆盆地类型及褶皱一冲断层样式[J].地学前缘,1995,2(3-4):59~68.
[68]刘树根,罗志立,曹树恒.一种新的陆内俯冲类型－龙门山型俯冲成因机制研究[J].石油实验地质,1991,13(4):314~324.
[69]刘树根.龙门山冲断带与川西前陆盆地的形成与演化[M].成都:成都科技大学出版社,1993.
[70]刘树根,童崇光,罗志立,等.川西晚三叠世前陆盆地的形成与演化[J].天然气工业,1995,15(2):11~15.
[71]刘树根等,龙门山造山带-川西前陆盆地系统构造事件研究[J].成都理工大学学报(自然科学版),2001,28(3):221~230.
[72]马永生,陈洪德,王国力等.中国南方层序地层与古地理[M].2009a,1~603.
[73]马永生,陈洪德,王国力等.中国南方陆相中-新生代构造-层序岩相古地理研究及编图[M].2009b,1~299.
[74]牛树银,孙爱群,白文吉.造山带与相邻盆地间物质的横向迁移[J].地学前缘,1995,2(1):85~92.
[75]彭军.黔桂地区石炭纪层序地层特征及发育机制[M].成都理工大学,1999.
[76]彭军,陈景山,郑荣才.百色盆地百岗组高分辨率层序分析及研究意义[J].地球学报,2002,23(2):153~158.
[77]田景春,张翔,聂永生,等.层序的测井、地震响应特征研究[J].物探化探计算技术,2005,27(4):321~326.
[78]田景春,陈高武,张翔,等.沉积地球化学在层序地层分析中的应用[J].成都理工大学学报：自然科学版,2006,33(1):30~35.
[79]田树刚,章雨旭.华北地台北部奥陶纪露头层序地层[J].地球学报－中国地质科学院院报,1997,l:87~96.
[80]童崇光.四川盆地断褶构造形成机制[J].天然气工业, 1992.12(5):1~6.
[81]童金南,崔玮霞.碳酸盐缓坡区的露头层序地层研究[J].地球科学－中国地质人学学报,2002,27(5):565~569.
[82]王俊.四川盆地上三叠统_侏罗系沉积体系及层序地层学研究[硕士毕业论文].成都理工大学,2007.
[83]吴根耀.构造层序地层学[J].地球科学进展,1996,11(3):310~310.
[84]许效松.层序地层序研究进展[J].岩相古地理,1994,14(1):34~39.
[85]许效松,徐强.盆山转换和当代盆地分析中的新问题[J].岩相古地理,1996a,16(2):24~33.
[86]许效松.被动大陆边缘碳酸盐生长序列与盆山转换耦合[J].地球学报－中国地质科学院院报,1996b,17(1):41~53.
[87]许效松.层序地层在沉积学和油储勘探中研究的关键点[J].岩相古地理,1996c,16(6):55~62.
[88]许效松,刘宝珺,徐强,等.中国西部大型盆地分析及地球动力学[M].地质出版社,1997a,1~168.
[89]许效松,刘宝珺,赵玉光,等.上扬子西缘二叠纪－三叠纪层序地层与盆山转换耦合[M].北京:地质出版社:1997b,9~16.
[90]许效松.盆山转移与造盆,造山过程分析[J].岩相古地理,1998,18(6):1~10.
[91]姚根顺,李大成,卢文忠,等.四川叠合盆地盆山耦合特征分析[J].大地构造与成矿学,2006,30(4):435~444.
[92]叶黎明,陈洪德,胡晓强,等.川西前陆盆地须家河期高分辨率层序格架与古地理演化[J].地层学杂志,2006,30(1):89~94.
[93]叶茂才,易智强,李剑波.川西坳陷蓬莱镇组沉积体系时空配置规律.成都理工大学学报,2000,20(1):54~58.
[94]叶泰然.川西坳陷合兴场—罗江地区上三叠统须家河组二段致密裂缝性砂岩储层预测[硕士毕业论文].成都理工大学,2003
[95]尹世明.川西坳陷蓬莱镇组构造—充填层序特征[J].矿物岩石,1999,19(4):40~46.
[96]曾允孚,李勇.龙门山前陆盆地形成与演化[J].矿物岩石,1995,40~49.
[97]赵俊兴,陈洪德,傅锁堂,等.鄂尔多斯盆地侏罗系层序地层与盆地充填演化耦合关系[J].成都理工大学学报:自然科学版,2007,.34(5):511~518
[98]赵永刚,陈景山,雷卞军,等.川西邛崃县白马庙气田上侏罗统蓬莱镇组高分辨率层序地层分析[J].中国地质,2005,23(4):674~681.
[99]郑德文张培震万景林,等.碎屑颗粒热年代学-一种揭示盆山耦合过程的年代学方法[J].地震地质,2000,22(b12):25~36.
[100]郑荣才,彭军,彭光明,等.高分辨率层序分析在油藏开发工程中的应用－以百色盆地仑35块那二段油藏为例[J].沉积学报, 2003,21(4):654~662.
[101]郑荣才,周祺,王华,等.鄂尔多斯盆地长北气田山西组2段高分辨率层序构型与砂体预测[J].高校地质学报,2009a,15(1):69~79.
[102]郑荣才,朱如凯,戴朝成,等.川东北类前陆盆地须家河组盆－山耦合过程的沉积－层序特征[J].地质学报, 2008b,82(8):1077~1087.
[103]朱志军,陈洪德,林良彪,等.川西前陆盆地蓬莱镇期层序、岩相古地理特征及演化[J].地层学杂志,2009, 33(3):318~325.
[104]邹光富,陈永明,夏彤.层序地层学在区域地质调杳中的应用[J].四川地质学报,2003,23(l):l~4.