引文
[1]Allen J R L.The plan shape of current ripples in relation to flowcondition[J].Sedimentology,1977,24(1):53-62.
[2]Miall AD.Architectural-element analysis:Anewmethod of faciesanalysis applied to fluvial deposits[J].Earth Science Reviews,1985,22:261-308.
[3]Neton MJ,Joachim D,Christopher D O,et al.Young Architec-ture and directional scales of heterogeneity in alluvial-fan aquifers[J].Journal ofSedimentary Research,1994,64(5):245-257.
[4]Willis B J,Behrensmeyer A K.Architecture of Miocene overbankdeposits in northern Pakistan[J].Journal ofSedimentary Re-search,1994,64(2):60-67.
[5]Yin Taiju,Zhang Changmin,Zhao Hongjing.Remaining oil pre-diction based on comprehensive geological analysis methods[J].Advances in Earth Science,2006,21(5):539-544.[尹太举,张昌民,赵红静.地质综合法预测剩余油[J].地球科学进展,2006,21(5):539-544.]
[6]Fu Qingping,Li Sitian.Outcrop analysis of architecture of lacus-trine deltaic plain sand bodies[J].SedimentaryFacies and Palaeo-geography,1994,14(5):21-33.[付清平,李思田.湖泊三角洲平原砂体的露头构形分析[J].岩相古地理,1994,14(5):21-33.]
[7]Clark J D,Kevin TP.Architectural elements and growth patternsof submarine channels,application to hydrocarbon exploration[J].AAPG Bulletin,1996,80(2):194-221.
[8]Xie Xinong,Li Sitian,Gao Dongsheng,et al.Architectural ele-ments and sedimentary model for barrier sandbodies in theFengcheng Mining district,Jiangxi[J].Sedimentary Facies andPalaeogeography,1994,14(4):1-9.[解习农,李思田,高东升,等.江西丰城矿区障壁坝砂体内部构成及沉积模式[J].岩相古地理,1994,14(4):1-9.]
[9]Yu Xinghe,Ma Xingxiang,Mu Longxin,et al.Geology Modeland Hierarchy Interface Analysis of Braid River[M].Beijing:Pe-troleum Industry Press,2004:60-106.[于兴河,马兴祥,穆龙新,等.辫状河储层地质模式及层次界面分析[M].北京:石油工业出版社,2004:60-106.]
[10]Jiao Yangquan,Yan Jiaxin,Li Sitian,et al.Architectural unitsand heterogeneity of channel reservoirs in the Karamay Forma-tion,outcrop area of Karamay oil field,Junggar Basin,northwestChina[J].AAPG Bulletin,2005,89(4):529-545.
[11]Li Yang,Guo Changchun.The architecture and reservoir evalua-tion of underground lateral accretion bar:A case study on theNg52+3sand-body in 7thblock west of the Gudong oil field[J].Acta Sedimentologica Sinica,2007,25(6):942-948.[李阳,郭长春.地下侧积砂坝建筑结构研究及储层评价———以孤东油田七区西Ng52+3砂体为例[J].沉积学报,2007,25(6):942-948.]
[12]Allen J R L.Studies in fluviatile sedimentation:Bars,bar com-plexes and sandstone sheets(lower-sinuosity braided streams)inthe Brownstones(L.Devonian),Welsh Borders[J].Sedimenta-ry Geology,1983,33:237-293.
[13]Miall AD.Architectural elements and bounding surfaces in fluvi-al deposits:Anatomy of the Kayenta Formation(Lower Juras-sic),Southwest Colorado[J].Sedimentary Geology,1988,55:233-262.
[14]Miall AD.Hierarchies of architectural units in terrigenous clasticrocks,and their relationship to sedimentation rate[C]∥Miall AD,Tyler N,eds.The Three-dimensional Facies Architecture ofTerrigenous Clastic Sediments and Its Implications for Hydrocar-bon Discovery and Recovery.SEPM Concepts in Sedimentologyand Paleontology,1991,3:6-12.
[15]Halfar J,Riegel W,Walther H.Facies architecture and sedim-entology of a meandering fluvial system:A Palaeogene examplefrom the Weisselster Basin,Germany[J].Sedimentology,1998,45:1-17.
[16]Allen J R L.A review of the origin and characteristics of recentalluvial sediments[J].Sedimentology,1965,5(2):89-191.
[17]Bridge J S,Tye R S.Interpreting the dimensions of ancient fluvi-al channel bars,channels,and channel belts from wireline-logsand cores[J].AAPG Bulletin,2000,84(8):1 205-1 228.
[18]Matthew J P,Marielis F V,Thomas L D.Characterization and3D reservoir modelling of fluvial sandstones of the Williams ForkFormation,Rulison Field,Piceance Basin,Colorado,USA[J].AAPG Bulletin,2008,5(2):158-172.
[19]Marinus E D,Irina O.Connectivity of fluvial point-bar deposits:An example from the Miocene Huesca fluvial fan,Ebro Basin,Spain[J].AAPG Bulletin,2008,92(9):1 109-1 129.
[20]Qian Ning,Zhang Ren,Zhou Zhide.Fluvial Process[M].Bei-jing:Science Press,1987:111-112.[钱宁,张仁,周志德.河床演变学[M].北京:科学出版社,1987:111-112.]
[21]Xue Peihua.Reservoir Model Introduction of Fluvial Point Bar[M].Beijing:Petroleum Industry Press,1991:23-35.[薛培华.河流点坝相储层模式概论[M].北京:石油工业出版社,1991:23-35.]
[22]Ma Shizhong,Yang Qingyan.The depositional model,3-D Archi-tecture and heterogeneous model of point bar in meandering chan-nels[J].Acta Sedimentologica Sinica,2006,18(2):241-247.[马世忠,杨清彦.曲流点坝沉积模式、三维构形及其非均质模型[J].沉积学报,2000,18(2):241-247.]
[23]Yue Dali.The Study on Architecture Analysis and Remaining OilDistribution Patterns of Meandering River Reservoir—A casestudy of Guantao Formation,Gudao OilfieldChina[D].Beijing:China University of Petroleum,2006.[岳大力.曲流河储层构型分析与剩余油分布模式研究———以孤岛油田馆陶组为例[D].北京:中国石油大学,2006.]
[24]Alexander J,Bridge J S,Gawthorpe R L,et al,Holocene mean-der belt evolution in an extensional basin,SWMontana USA[J].Journal ofSedimentary Research,1994,64:542-559.
[25]Corbeanu R M,Soegaard K,Szerbiak R B,et al.Detailed inter-nal architecture of fluvial channel sandstone determined from out-crop and 3-D ground penetrating radar:Example from mid-Creta-ceous Ferron Sandstone,east-central Utah[J].American Associa-tion ofPetroleum Geologists Bulletin,2001,85:1 583-1 608.
[26]Rijks E J H,Jauffred J E E M.Attribute extraction:An impor-tant application in any 3-D interpretation study[J].The LeadingEdge,1991,3(9):11-19.
[27]Vitor A,Morgan S,Calos P,et al.Lateral Accretion Packages(LAPs):An important reservoir element in deep water sinuouschannels[J].Marine and Petroleum Geology,2003,20(7):631-648.
[28]Richard Labourdette,Richard R J.Characterization of fluvial ar-chitectural elements using a three-dimensional outcrop data set:Escanilla braided system,South-Central Pyrenees,Spain[J].Geosphere,2007,3(6):422-434.
[29]Bruce S H.Channel detection in 3-D seismic data using sweet-ness[J].AAPG Bulletin,2008,92(6):733-742.
[30]Schumm S A.Fluvial paleochannels[C]∥Rigby J K,HamblinW K,eds.Recognition of Ancient Sedimentary Environments.SEPM,1972,16(special published):98-107.
[31]Leeder MR.Fluviatile fining upwards cycles and the magnitudeof paleochannels[J].Geological Magazine,1973,110:265-276.
[32]Leopold LB,Wolman MG,Miller J P.Fluvial Processesin Geo-morphology[M].New York:Dover Publications,1964:522.
[33]Bridge J S,Tye R S.Interpreting the dimensions of ancient fluvi-al channel bars,channels,and channel belts from wireline-logsand cores[J].AAPG Bulletin,2000,84(8):1 205-1 228.
[34]Lorenz J C,Heinze D M,Clark J A,et al.Determination ofwidth of meander-belt sandstone reservoirs from vertical downholedata,Mesaverde Group,Piceance Greek Basin,Colorado[J].AAPG Bulletin,1985,69(2):710-721.
[35]Zhao Hanqing,Fu Zhiguo,Liu Bo.Identification of the pa-leochannel sandbodies based on detailed geological study[J].Petroleum Exploration and Development,1995,79(2):68-70.[赵翰卿,付志国,刘波.应用精细地质研究准确鉴别古代河流砂体[J].石油勘探与开发,1995,79(2):68-70.]
[36]Chen Qinghua,Zeng Ming,Zhang Fengqi,et al.Identificationof single channel in fluvial reservoir and its significance to the oil-field development[J].Oil&Gas Recovery Technology,2004,11(3):11-15.[陈清华,曾明,章凤奇,等.河流相储层单一河道的识别及其对油田开发的意义[J].油气地质与采收率,2004,11(3):11-15.]
[37]Ma Shizhong.The method for studying thin interbed architectureof burial meandering channel sandbody[J].Acta SedimentologicaSinica,2008,26(4):632-639.[马世忠.地下曲流河道单砂体内部薄夹层建筑结构研究方法[J].沉积学报,2008,26(4):632-639.]
[38]Liu Zhanli,Jiao Yangquan.Composition of facies of meanderingriver origin and relationship of its spatial configuration an on-the-spot geology investigation on sedimentology of mesozoic outcrop inEerduosi Basin[J].Petroleun Geology and Oil Field Developmentin Daqing,1996,15(3):6-9.[刘站立,焦养泉.曲流河成因相构成及其空间配置关系———鄂尔多斯盆地中生代露头沉积学地质考察[J].大庆石油地质与开发,1996,15(3):6-9.]
[39]Zhou Yinbang,Wu Shenghe,Yue Dali,et al.Controlling factoranalysis and identification method of lateral accretion shale bed-dings angle in point bar[J].Journal ofChina UniversityofPetro-leum(Edition ofNatural Science),2009,33(2):7-11.[周银邦,吴胜和,岳大力,等.点坝内部侧积层倾角控制因素分析及地下识别[J].石油大学学报:自然科学版,2009,33(2):7-11.]
[40]Wu Shenghe,Yue Dali,Liu Jianmin,et al.Hirearchical model-ing of paleochannel reservoir architecture[J].Science in China(Series D),2008,38(Suppl.Ⅰ):111-121.[吴胜和,岳大力,刘建民,等.地下古河道储层构型的层次建模研究[J].中国科学:D辑,2008,38(增刊Ⅰ):111-121.]