层序地层学研究现状及进展:模式多样化Review of Sequence Stratigraphy: Diversification of Models
吴和源;
摘要(Abstract):
1977年至1988年,层序地层学从诞生逐渐走向成熟,并且形成了一套完整的概念体系和工作方法,这段特殊时期被称为层序地层学的Exxon时代。之后,将最大海泛面作为层序界面的R-T层序模式则代表了后Exxon时代模式多样化的开始。随后,对Exxon层序地层学概念体系不协调的认识则代表了由模式多样化所表征的后Exxon时代,与此几乎同时出现的T-R层序及淹没不整合型层序等模式意味着层序地层学"百家争鸣"的新景象。阐释各种层序地层学模式出现的原因,追索这些模式对解决问题的针对性以及存在的问题,将有助于深入理解"在地层框架内划分和对比沉积岩"的层序地层学,并且为分析复杂的地层记录提供更多的思考途径。
关键词(KeyWords): 层序地层学;后Exxon时代;进展;争论
基金项目(Foundation): 国家自然科学基金项目(40472065)
作者(Author): 吴和源;
Email:
DOI:
参考文献(References):
- [1]Payton C E.Seismic stratigraphy:Applications to hydrocar-bon exploration[J].AAPG Memoir,1977,26:1-516.
- [2]Brown L F,Fisher W L.Seismic stratigraphic interpretationof depositional systems:Examples from Brazilian rift and pullapart basins[C]∥Payton C E.Seismic stratigraphy:Applica-tions to hydrocarbon exploration.[S.l.]:AAPG Memoir 26,1977:213-248.
- [3]Vail P R.Seismic stratigraphy interpretation using sequencestratigraphy:Part 1.Seismic stratigraphy interpretation pro-cedure[C]∥Bally A W.Atlas of seismic stratigraphy.AAPGStudies in Geology.Vol.27.[S.l.]:[s.n.],1987:1-10.
- [4]van Wagoner J C,Mitchum R M,Posamentier H W,et al.Se-simic stratigraphy interpretation using sequence stratigraphy:Part 2.Key definitions of sequence stratigraphy[C]∥Bally AW.Atlas of seismic stratigraphy.AAPG Studies in Geology.Vol.27.[S.l.]:[s.n.],1987:11-14.
- [5]Mitchum R M,Vail P,Thompson S.Seismic stratigraphy andglobal changes in sea level:Part 2.The depositional sequenceas the basic unit for stratigraphic analysis[C]∥Paton C E.Seismic stratigraphy:Application to hydrocarbon exploration.[S.l.]:AAPG Memoir 26,1977:53-62.
- [6]梅冥相.从正常海退与强迫海退的辨别进行层序界面对比:层序地层学进展之一[J].古地理学报,2010,12(5):549-564.
- [7]Wilgus C K,Hastings B S,Kendall C G St C,et al.Sea levelchanges:An integrated approach.Vol.42.[M].[S.l.]:SEPM Special Publication,1988:407.
- [8]Vail P R,Mitchum R M,Thompson S.Seismic stratigraphyand global changes of sea level:Part 4.Global cycles of rela-tive changes of sea level[C]∥Paton C E.Seismic stratigra-phy:Application to hydrocarbon exploration.[S.l.]:AAPGMemoir 26,1977:83-98.
- [9]Posamentier H W,Jervey M T,Vail P R.Eustatic controls onclastic deposition I-conceptual framework[C]∥Wilgus C K,Hastings B S,Kendall C G St C,et al.Sea level changes:Anintegrated approach.Vol.42.[S.l.]:SEPM Special Publica-tion,1988:109-124.
- [10]Posamentier H W,Vali P.Eustatic controls on clastic deposi-tionⅡ-sequence and systems tract models[C]∥Wilgus C K,Hastings B S,Kendall C G St C,et al.Sea level changes:AnIntegrated Approach.Vol.42.[S.l.]:SEPM Special Publica-tion,1988:125-154.
- [11]Haq B U,Hardenbol J,Vail P R.Chronology of fluctuatingsea levels since the Triassic(250million years ago to present)[J].Science,1987,235:1156-1166.
- [12]Catuneanu O,Abreu V,Bhattacharya J P,et al.Towards thestandardization of sequence stratigraphy[J].Earth-Science Re-view,2009,92:1-33.
- [13]Vail P R,Hardenbol J,Todd R G.Jurassic unconformities,chronostratigraphy,and sea-level changes from seismic stratig-raphy and biostratigraphy[C]∥Schlee J S.Interregional un-conformities and hydrocarbon accumulation.[S.l.]:AAPGMemoir 36,1984:129-144.
- [14]Frazier D E.Depositional episodes:Their relationship to the Qua-ternary stratigraphic framework in the northwestern portion of theGulf basin[J].University of Texas at Austin,Bureau of EconomicGeology Geological Circular,1974,74(1):1-26.
- [15]Hunt D,Tucker M E.Stranded parasequences and the forcedregressive wedge systems tract:Deposition during base-levelfall[J].Sedimentary Geology,1992,81:1-9.
- [16]Galloway W E.Genetic stratigraphic sequences in basin analy-sis:Ⅰ.Architecture and genesis of flooding-surface boundeddepositional units[J].AAPG Bulletin,1989,73:125-142.
- [17]Posamentier H W,Allen G P.Siliciclastic sequence stratigra-phy:Concepts and applications[J].SEPM Concepts in Sedim-entology and Paleontology,1999,7:1-210.
- [18]Posamentier H W,Allen G P,James D P,et al.Forced re-gressions in a sequence stratigraphic framework:Concepts,examples and exploration significance[J].AAPG Bulletin,1992,76:1687-1709.
- [19]Jervey M.Siliciclastic sequence development in foreland ba-sins,with examples from the western Canada foreland basin[C]∥Macqueen R,Leckie D.Foreland basins and fold belts.[S.l.]:AAPG Memoir 55,1992:47-80.
- [20]Emery D,Myers K.Sequence Stratigraphy[M].London:Black-Well,1997:1-297.
- [21]Hallam A.Interpreting sea level[C]∥Doyle P,Bennett M R.Unlocking the stratigraphical record:Advance in modern stra-tigraphy.Chichester:John Wiley&Sons,1998:421-439.
- [22]Plint A G,Nummedal D.The falling stage systems tract:Recognition and importance in sequence stratigraphic analysis[C]∥Hunt D,Gawthorpe R L.Sedimentary response toforced regression.Vol.172.[S.l.]:Geological Society of Lon-don Special Publication,2000:1-17.
- [23]van Wagoner J C,Mitchum R M,Campion K M,et al.Silici-clastic sequence stratigraphy in well logs,cores,and outcrops:Concepts for high-resolution correlation of time and facies[J].AAPG Methods in Exploration Series,1990,7:55.
- [24]Mellere D,Steel R.Variability of lowstand wedges and theirdistinction from forced-regressive wedges in the MesaverdeGroup,southeast Wyoming[J].Geology,1995,23:803-806.
- [25]梅冥相,杨欣德.强迫型海退及强迫型海退楔体系域:对传统Exxon层序地层学模式的修正[J].地质科技情报,2000,19(2):17-21.
- [26]Hunt D,Tucker M E.Reply to discussion[J].SedimentaryGeology,1995,95:147-160.
- [27]Hunt D,Tucker M E.Stranded parasequences and the forcedregressive wedge systems tract:Deposition during base-levelfall-reply[J].Sedimentary Geology,1995,95:147-160.
- [28]Catuneanu O.Principles of sequence stratigraphy[M].Am-sterdam:Elsevier,2006:1-375.
- [29]Johnson J G,Klapper G,Sandberg C A.Devonian eustaticfluctuations in Euramerica[J].Geological Society of AmericaBulletin,1985,96:567-587.
- [30]Ross C A,Ross J R P.Late Paleozoic transgressive-regressivedeposition[C]∥Wilgus C K,Hastings B S,Kendall C G St C,et al.Sea level changes:An integrated approach.Vol.42.[S.l.]:SEPM Special Publication,1988:227-247.
- [31]Embry A F.Triassic sea-level changes:Evidence from the Ca-nadian Arctic Archipelago[C]∥Wilgus C K,Hastings B S,Kendall C G St C,et al.Sea level changes:An integrated ap-proach.Vol.42.[S.l.]:SEPM Special Publication,1988:249-259.
- [32]Embry A F,Johannessen E P.T-R sequence stratigraphy,fa-cies analysis and reservoir distribution in the uppermost Trias-sic lower Jurassic succession,western Sverdrup Basin,ArcticCanada[C]∥Vorren T,Bergsager E,Dahl-Stamnes O A,etal.Arctic geology and petroleum potential.Vol.2.[S.l.]:NPF Special Publication,1992:121-146.
- [33]Embry A F.Transgressive-regressive(T-R)sequence analysisof the Jurassic succession of the Sverdrup Basin[J].CanadianArctic Archipelago,Canadian Journal of Earth Sciences,1993,30:301-320.
- [34]Vail P R,Audemard F,Bowman S A,et al.The stratigraphicsignature of tectonics,eustasy and sedimentology:An over-view[C]∥Einsele G,Ricken W,Seilacher A.Cycles and e-vents in stratigraphy.Berlin:Springer-Verlag,1991:617-659.
- [35]Embry A F.Sequence boundaries and sequence hierarchies:Problems and proposals[C]∥Steel R J,Felt V L,Johannes-sen E P,et al.Sequence stratigraphy on the Northwest Euro-pean Margin.Vol.5.[S.l.]:Norwegian Petroleum SocietySpecial Publication,1995:1-11.
- [36]Helland-Hansen W,Gjelberg J.Coceptual basis and variabilityin sequence stratigraphy:A different perspective[J].Sedimen-tary Geology,1994,92:1-52.
- [37]Embry A F.Transgresive-regressive(T-R)sequence stratig-raphy[C]∥Armentrout J M,Rosen N C.Sequence strati-graphic models for exploration and production:Evolving meth-odology,emerging models and application histories.[S.l.]:[s.n.],2002:151-172.
- [38]Haq B U,Schutter S R.A chronology of paleozoic sea-levelchanges[J].Science,2008,322:64.
- [39]Helland-Hansen W,Martinsen O J.Shoreline trajectories andsequences:Description of variable depositional-dip scenarios[J].Journal of Sedimentary Research,1996,66:670-688.
- [40]Catuneanu O,Willis A,Miall A D.Temporal significance ofsequence boundaries[J].Sedimentary Geology,1998,121:157-178.
- [41]Catuneanu O.Sequence stratigraphy of clastic systems:Con-cepts,merits,and pitfalls[J].Journal of African Earth Sci-ence,2002,35:1-43.
- [42]Embry A F,Catuneanu O.Practical sequence stratigraphy:Concepts and application[J].Canadian Society of PetroleumGeologists,2002:147.
- [43]Jervey M.Quantitative geological modeling of siliciclastic rocksequences and their seismic expression[C]∥Wilgus C,Has-tings B S,Kendall C G,et al.Foreland basins and fold belts.[S.l.]:AAPG Memoir 55,1988:47-80.
- [44]Schumm S A.River response to base-level change:Implica-tions for sequence stratigraphy[J].Journal of Geology,1993,101:279-294.
- [45]梅冥相,马永生.从旋回层序的特征论地层记录的两种相变面及两种穿时性[J].地层学杂志,2001,25(2):150-153.
- [46]Schlager W.The Paradox of drowned reefs and carbonate plat-form[J].Geol.Soc.Am.Bull.,1981,92:197-211.
- [47]Schlager W.Drowning unconformities on carbonate platforms[J].SEPM Special Publication,1989,44:15-25.
- [48]Tucker M E,Wright V P.Carbonate sedimentology[M].Ox-ford,London:Bluckwell Scientific Publications,1990:482.
- [49]Goldhammer R K,Dunn P A,Hardle L A.Depositional cy-cles,composite sea-level changes,cycle stacking patterns,andthe hierarchy of stratigraphic forcing[J].Geol.Soc.Am.Bull.,1990,102:535-562.
- [50]梅冥相.淹没不整合型碳酸盐三级旋回层序:兼论碳酸盐台地的凝缩作用[J].岩相古地理,1996,16(6):24-33.
- [51]梅冥相,张海,孟晓庆,等.上扬子区下寒武统的层序地层划分和层序地层格架的建立[J].中国地质,2006,33(6):1292-1304.
- [52]雷振宇,周洪瑞.露头层序地层研究中的几个基本问题[J].地质科技情报,1995,14(2):37-44.
- [53]孙枢.中国沉积学的今后发展:若干思考与建议[J].地学前缘,2005,12(2):3-10.
- [54]刘宝珺,韩作振,杨仁超.当代沉积学研究进展、前瞻与思考[J].特种油气藏,2006,13(5):1-3,9.
- [55]刘占红,李思田.沉积记录中的古气候周期及其在高频层序形成中的意义[J].地质科技情报,2007,26(2):30-34.
- [56]吴因业,张天舒,张志杰,等.沉积体系域类型、特征及石油地质意义[J].古地理学报,2010,12(1):69-81.
- [57]梅冥相.长周期层序形成机制的探索:层序地层学进展之二[J].古地理学报,2010,12(6):711-728.
- [58]李绍虎.对国外层序地层学研究进展的几点思考及L-H-T层序地层学[J].沉积学报,2010,28:735-744.