安塞油田三叠系延长组长4+5层沉积相与储层特征研究
|
摘要
本文在充分掌握、收集研究区区域地质资料和前人研究成果的基础上,以沉积学的基本原理和方法为指导,进行野外露头观测,结合钻井、岩心、测井、地震等资料,综合构造、地层、储层地质学、地球化学、盆地分析等理论和方法,对安塞油田长4+5油层组的沉积体系发育、展布特征和砂体分布特征进行了深入研究。较为详尽地查明了研究区含油气情况,分析了不同层段的含油气性特征,评价了研究区长4+5油层组的有利勘探区域,了解了含油气规模及其勘探前景。同时全面地整理了地质、分析化验、测井、测试等资料和数据,系统分析了长4+5油层组有利储集体的展布和沉积相与油气分布的关系。
研究区主要为湖泊、三角洲沉积模式,大部分地区为三角洲前缘沉积,砂体均呈北东-南西向条带状展布。研究区东北部地区为三角洲平原沉积,长4+5_2的浅湖面积大,仅在东北部存在少量的三角洲平原,而长4+5_1东北部的三角洲平原相面积稍大些。三角洲前缘水下分流河道及平原分流河道是重要的油气储集体。
研究区内长4+5储层的岩石类型主要为长石砂岩或岩屑质长石砂岩。胶结物类型复杂多样,其中以绿泥石、方解石最为重要。安塞油田长4+5储集层砂岩具有矿物成熟度低、结构成熟度高的特征。长石等溶蚀孔占总面孔率较大,成为长4+5的相对优质储层。成岩矿物主要为薄膜状绿泥石及加大状石英质矿物,还有自生磷灰石、充填状硅质及碳酸盐矿物。
安塞油田长4+5油层组主要为岩性和构造-岩性复合式油气藏,其中以岩性油气藏为主。长4+5_2以砂岩上倾致密遮挡和上倾尖灭为主的岩性油气藏为主。油藏的分布受沉积作用、生油中心、有利储集相、生储盖有利配置、鼻隆及上倾方向遮挡的控制。
研究区长4+5_2为长4+5油层组的主要含油层段,有利区主要分布在杏河、坪桥及安塞沿河湾地区,这些区域电测物性较好,具备一定的成藏条件,为长4+5_2油层组下一步的勘探目标,西河口-高桥为次要有利区;研究区长4+5_1油层组整体的含油性较差,油气显示好的区域面积少,塞80井区为长4+5_1较有利区,谭家营、坪桥、杏河、西河口-高桥地区为次有利区。总体上看,长4+5_2的油气显示情况好于长4+5_1。
This paper lucubrates about the sedimentary system development and distributing feature and sandbody distributing features of Chang 4+5 oil formation in Ansai Oilfield, finds hydrocarbon condition at large, analyses and estimates hydrocarbon-bearing characteristics in different stratum and favorable exploration area, finds out petroleum scale and exploration prospects on the basis of gripping investigation areal geological data and digestion and absorption of previous research results. This conclusion is directed by sedimentary theory and methods integrating with theories of technical , stratum, reservoir geology , geochemistry , basin analysis and data of outcrop , drilling , well logging. Meanwhile, the study gets the general geology, analysis assay, well logging and test data, predicts the relation of sedimentary facies and petroleum distribution and the distribution of favorable reservoir of Chang 4+5 oil formation.
The study area mainly includes lake and delta sedimentary model, most areas are delta front deposits, and sandbody all show NE-SW banding distribution. The northeast part of study region is deltaplain deposits , shallow lake of Chang 4+5_2 has large scale , only in northeast part there are a spot of deltaplain, while the deltaplain acreage in same part of Chang 4+5_2 is slightly larger. In this part, channel sandbars, deltaic front subaqueous distributary channel and deltaic plain distributary channel are main reservoir bodies.
The rock types of Chang 4+5 in this region are mostly arkose or lithic arkose sandstone. Cement types are complicated and various, which are mainly chlorite and calcite. Reservoir sandstone of Chang 4+5 in Ansai oilfield has features as low maturity of mineral and high textural maturity. Dissolve pores of feldspar and so on have high ratio of total pore amount and become relative high quality reservoir of Chang 4+5. Diagenetic minerals are mainly thin film shaped chlorite and increasing shaped quartz minerals. There are autogenous apatites, filled silicious and carbonate minerals as well.
Chang 4+5 oil formation in Ansai oilfield is mainly lithology and structure-lithology combination reservoir, in which lithology reservoir is the main part. Chang 4+5_2 formation is mostly composed of lithology reservoir which mainly composed by sandstone undig finely barrier and updig pinch. The distribution of reservoir is controlled by sedimentary processes, source-reservoir-cap favorable assemblage, oil-generating center, favorable reservoif phase, and nose structure and updig direction favorable occlusion.
Chang 4+5_2 in the region is main oil-bearing horizon of Chang 4+5 formation, favorable area mainly distributes around Xinghe, Pingqiao, Ansai Yanhewan , where electrical measurement and physical properties are better and have certain reservoir forming conditions, thus , become next exploration target of Chang 4+5_2 . Xihekou-Gaoqiao region is the minor favorable area; Oiliness of Chang 4+5_1 formation in the region is poor as a whole , the area that oil-gas has better show is limited , Sai 80 well field is the more favorable area of Chang 4+5_1 formation, Tanjiaying, Pingqiao, Xinghe, Xihekou-Gaoqiao region are minor favorable area. In general, Chang 4+5_2 oil-gas show is better than Chang 4+5_1.
研究区主要为湖泊、三角洲沉积模式,大部分地区为三角洲前缘沉积,砂体均呈北东-南西向条带状展布。研究区东北部地区为三角洲平原沉积,长4+5_2的浅湖面积大,仅在东北部存在少量的三角洲平原,而长4+5_1东北部的三角洲平原相面积稍大些。三角洲前缘水下分流河道及平原分流河道是重要的油气储集体。
研究区内长4+5储层的岩石类型主要为长石砂岩或岩屑质长石砂岩。胶结物类型复杂多样,其中以绿泥石、方解石最为重要。安塞油田长4+5储集层砂岩具有矿物成熟度低、结构成熟度高的特征。长石等溶蚀孔占总面孔率较大,成为长4+5的相对优质储层。成岩矿物主要为薄膜状绿泥石及加大状石英质矿物,还有自生磷灰石、充填状硅质及碳酸盐矿物。
安塞油田长4+5油层组主要为岩性和构造-岩性复合式油气藏,其中以岩性油气藏为主。长4+5_2以砂岩上倾致密遮挡和上倾尖灭为主的岩性油气藏为主。油藏的分布受沉积作用、生油中心、有利储集相、生储盖有利配置、鼻隆及上倾方向遮挡的控制。
研究区长4+5_2为长4+5油层组的主要含油层段,有利区主要分布在杏河、坪桥及安塞沿河湾地区,这些区域电测物性较好,具备一定的成藏条件,为长4+5_2油层组下一步的勘探目标,西河口-高桥为次要有利区;研究区长4+5_1油层组整体的含油性较差,油气显示好的区域面积少,塞80井区为长4+5_1较有利区,谭家营、坪桥、杏河、西河口-高桥地区为次有利区。总体上看,长4+5_2的油气显示情况好于长4+5_1。
This paper lucubrates about the sedimentary system development and distributing feature and sandbody distributing features of Chang 4+5 oil formation in Ansai Oilfield, finds hydrocarbon condition at large, analyses and estimates hydrocarbon-bearing characteristics in different stratum and favorable exploration area, finds out petroleum scale and exploration prospects on the basis of gripping investigation areal geological data and digestion and absorption of previous research results. This conclusion is directed by sedimentary theory and methods integrating with theories of technical , stratum, reservoir geology , geochemistry , basin analysis and data of outcrop , drilling , well logging. Meanwhile, the study gets the general geology, analysis assay, well logging and test data, predicts the relation of sedimentary facies and petroleum distribution and the distribution of favorable reservoir of Chang 4+5 oil formation.
The study area mainly includes lake and delta sedimentary model, most areas are delta front deposits, and sandbody all show NE-SW banding distribution. The northeast part of study region is deltaplain deposits , shallow lake of Chang 4+5_2 has large scale , only in northeast part there are a spot of deltaplain, while the deltaplain acreage in same part of Chang 4+5_2 is slightly larger. In this part, channel sandbars, deltaic front subaqueous distributary channel and deltaic plain distributary channel are main reservoir bodies.
The rock types of Chang 4+5 in this region are mostly arkose or lithic arkose sandstone. Cement types are complicated and various, which are mainly chlorite and calcite. Reservoir sandstone of Chang 4+5 in Ansai oilfield has features as low maturity of mineral and high textural maturity. Dissolve pores of feldspar and so on have high ratio of total pore amount and become relative high quality reservoir of Chang 4+5. Diagenetic minerals are mainly thin film shaped chlorite and increasing shaped quartz minerals. There are autogenous apatites, filled silicious and carbonate minerals as well.
Chang 4+5 oil formation in Ansai oilfield is mainly lithology and structure-lithology combination reservoir, in which lithology reservoir is the main part. Chang 4+5_2 formation is mostly composed of lithology reservoir which mainly composed by sandstone undig finely barrier and updig pinch. The distribution of reservoir is controlled by sedimentary processes, source-reservoir-cap favorable assemblage, oil-generating center, favorable reservoif phase, and nose structure and updig direction favorable occlusion.
Chang 4+5_2 in the region is main oil-bearing horizon of Chang 4+5 formation, favorable area mainly distributes around Xinghe, Pingqiao, Ansai Yanhewan , where electrical measurement and physical properties are better and have certain reservoir forming conditions, thus , become next exploration target of Chang 4+5_2 . Xihekou-Gaoqiao region is the minor favorable area; Oiliness of Chang 4+5_1 formation in the region is poor as a whole , the area that oil-gas has better show is limited , Sai 80 well field is the more favorable area of Chang 4+5_1 formation, Tanjiaying, Pingqiao, Xinghe, Xihekou-Gaoqiao region are minor favorable area. In general, Chang 4+5_2 oil-gas show is better than Chang 4+5_1.
引文
[1] Andrew H and Bryan T C.The Origin of Consolidation Laminate and Dish Structures in some Deep-Water Sandstones, Sedimentary Research, 2001, 71 (1): 136-143.
[2] Bhatia M R, Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 1986, 92:181-193.
[3] Bhatia M R. Plate tectonics and geochemical composition of sandstone[J]. Earth Science-Journal of China University of Geosciences, 1983, 91(6): 611-627.
[4] Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J]. Sedimentary Geology, 1985, 45: 97-113.
[5] Clark J D and Pickering K T.Architectural elements and growth patterns of submarine channels:application to hydrocarbon explorationAAPG Bulletin, 1996, 80 (2): 194-211.
[6] Cross T A.High-resolution stratigraphic correlation from the perception of base-level cycles and sediment accommodation.In: Proceeding of Northwestern Europian Sequence Stratigraphy Congress, 1994: 105-123.
[7] Cullers R L, Basu A, Suttner L J. Geochemical signature of provenance in sand-mixed material in soils and stream sediments near the Tobucco Root Botholith, Montana, USA. Chem Geol, 1988,70: 335-348.
[8] Davis R A. Depositional systems: an introduction to sedimentology and stratigraghy. Prentice-hall,Inc.1992.
[9] Demaison G and Hutiinga B J.Genetic classification of petroleum systems. AAPG Bulletin.1991, 75(10): 1626-1643.
[10]Dutton S P and Willis B J.Comparison of outcrop and subsurface sandstone permeability distribution, Lower Cretaceous Fall River Formation, South Dakota and Wyoming.Journal of Sedimentary Research, 1998, 68 (5) : 890-900.
[11]Einsele G, S.K.Chough and T.Shiki. Depositional events and their records-an introduction.Sedimentary Geology [J]. 1996, Vol.104:1-9.
[12]Embry A F. Transgressive-regressive (T-R) sequence analysis of the Jurassic succesion of Sverdrup Basin, Canadian Arctic Archipelago. Can. J. Earth Sci.,1993,30:301-320.
[13]Friedman G M and Sanders J E.Principles of Sedimentology.New York: Wiley, 1978.
[14] Galloway W E.Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units.AAPG Bulletin. 1989: 73 (2): 125-142.
[15]Galloway W E.Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units.AAPG Bulletin. 1989: 73 (2):125-142.
[16]Gao S and Collins M. Net sedimenttransportpatternsinferred from grain size trends, based upon definition of transport vectors"[J]. Sedimentary Geology, 1992, 81: 47-60.
[17]Halforsen H H and Macdonald C G.Stochastic modeling of Underground Reservoir Fades, SPE(16751), 1987, 575-589.
[18] Jerry Lucla F and Graham E Fogg. Geologic/Stochasticmapping of heterogeneity in a carbonate reservoir[J]. Journal of Petroleum Technology, 1990, 42 (10):1298-1303.
[19]Jiao Yangquan, Yan Jiaxin, Li Sitian, et al. Architectural units and heterogeneity of channel reservoirs in the Karamay Formation, outcrop area of Karamay oil field, Junggar basin, northwest China[J]. AAPG Bulletin, 2005, 89 (4):529-545.
[20]Lewis D W.. Practical Sedimentology[M]. Hutchinson Ross Publish ing Co., 1984, 31-39.
[21]Martinius A W and Nieuwenhuijs R A.Geological description of flow units in channel sandstones in a fluvial reservoir analogue (Loranca Basin, Spain) .Petroleum Geoscience, 1995, 1(3): 237-252.
[22]Mclennan S M. Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes[M]. in: Lipin B.R.et al.(ed.): Geochemistry and Mineralogy of Rare earth elements. The Mineralogical Society of America, Washington, D.C., 1989, 169-200.
[23]Nelson R A. Natural Fracture Systems, Description and Classification[J]. AAPG Bulletin. 1979,63(12): 2214-2221.
[24]Nelson Ronald A. GeologicAnalysis of Naturally Fractured Reservoirs[M]. Beijing: Petroleum IndustryPress, 1991. 6-26.
[25]Pettijohn F J..Sedimentary Rocks (3rd edition)[M]. Harper & Row Publishers Inc., 1975, 106-108.
[26]Pramod S and Rajamani V. Geochemistry of the Floodplain Sediments of the Kaveri River, Southern India, Sedimentary Research, 2001, 71 (1): 50-60.
[27]Ramon J C and Cross T A.Characterization and prediction of reservoir architecture and petrophysical properties in fluvial channel sandstones, Middle Magdalena Basin, Colombia.Ciencia,Tecnology Future, 1997, 1 (3): 19-46.
[28]Rea D K, Snoeckx H and Joseph L H. Late Cenozoic eolian deposition the North Pacific: Asian drying, Tibetan uplift and cooling of the northern hemisphere[J]. Paleoceanography, 1998, 13 (3):215-224.
[29]Reading H G. Sedimentary Environments: Processes,Facies and Stratigraphy.Oxford,UK:Blackwell. 1996.
[30]Rollinson H R. Using geochemical date: evaluation, presentation, interpretation[M]. London:Longman Scientific Technical Press, 1993, 1-352.
[3 l]Roser B P, Korsch R J. Determination of tectonic setting of sandstone-mudstone suites using SiO_2 content and K_2O/Na_2O ratio[J]. The Journal of Geology, 1986, 94(5): 635-650.
[32]Roser B P, Korsch R J. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of majorelement data[J]. Chemical Geology, 1988, 67: 119-139.
[33]Selly R C. An introduction to sedimentology[M]. London: Academic Press Inc., 1976.208-209.
[34]Shanly K W, et al.Perspective on the sequence stratigraphy of continental strata.AAPG Bulletin.1994, 74 (4): 544-568.
[35]Shanmugam G and Moiola R J.Types of submarine fan lobes: models and implication.AAPG Bulletin. 1991, (75): 156-179.
[36] Steams D W and Friedman M. Reservoirs in Fractured Rock[J]. AAPG Memoir 16. 1972. 82-100.
[37]Stow D A V and Johansson M.Deep water massive sands: nature, origin and hydrocarbon implications.Marine and Petroleum Geology, 2000, 17 (1): 145-174.
[38] Thomas F Moslow, Graham R Davies. Turbidite reservoir facies in the Lower TriassicMontney Formation,west-central Alberta [J].Bulletin of Canadian Petroleum Geology, 1997, 45 (4): 507-536.
[39]Thomas Pichler and John D H.Formation of Dolomite in Recent Island-arc Sediments due to Gas-Seawater-Sediment interaction, Sedimentary Research, 2001, 71 (3), 394-399.
[40] Vail P R, Mitchum R M, Todd R G, et al. Seismic stratigraphy and global changes of sea level.In:Payton C E ed.Seismic stratigraphy-application to hydrocarbon exploration.AAPG Memoir, 1977,26: 83-97.
[41] Weber K J and Maatschappij B V. How Heterogeneity Affects Oil Recovery; Reservoir Characterization, 1986, 487-544.
[42] Weber K J , Kantorowicz J D and Williams H.Geological modelling of hydrocarbon reservoirs.Marine and Petroleum Geology, 1991, 8 (2) : 245-246.
[43]Weimer P R, Bouma A H and Perkins B F.Submarine fans and turbidite systems, sequence stratigraphic, reservoir architecture and production characteristics.In: Aon.Gulf of Mexico and International: Gulf Coast Section of the SEPM Foundation 15th Annual Research Conference Proceedings.TULSA: SEPM, 1994: 440.
[44]Weimer P R. Envelopments in sequence statigraphy: foreland and cratonic basins. AAPG Bulletin.1992, 76 (7): 965-982.
[45]Wong P M, Tamhane D and Wang L.A neural-network approach to knowledge-based well interpolation: a case study of a fluvial sandstone reservoir.Journal of Petroleum Geology, 1997,20 (3) : 363-372.
[46]Zheng R C, Yin S M and Peng J. Sedimentary dynamic analysis of sequence structure and stacking patten of base-level cycle. Acta Sediment to logica Sinica, 2000, 18 (3):369-375.
[47]曹红霞,李文厚,何卫军,等.鄂尔多斯盆地宜川地区延长组物源分析[J].煤田地质与勘探,2007(12).35(6):14-17.
[48]曹红霞,张云翔,岳乐平,等.毛乌素沙地全新世地层粒度组成特征及古气候意义[J].沉积学报,2003(9),21(3):482-486.
[49]代金友,张一伟,熊琦华,等.成岩作用对储集层物性贡献比率研究[J].石油勘探与开发,2003,30(4):54-55.
[50]邓军,王庆飞,高帮飞,等.鄂尔多斯盆地演化与多种能源矿产分布[J].现代地质,2005,19(4):538-545.
[51]邓希光,李献华,陈志刚,等.广西钦州板城晚泥盆世硅质岩地球化学特征及沉积环境探讨[J].地质科学,2003,38(4):460-469.
[52]邸志欣,谭绍泉,姜维才,等.川东北地区山地三维高分辨率地震采集技术[J].石油物探,2005,44(5):517-524.
[53]丁仲礼,孙继敏,刘东生.联系沙漠-黄土演变过程中耦合关系的沉积学指标[J].中国科学,1999,29(1):82-87.
[54]方少仙,候方浩.石油天然气储层地质学[M].北京:石油大学出版社,1998.
[55]冯增昭.沉积岩石学(第二版)[M].北京:石油工业出版社,1993,108-131.
[56]付金华,段晓文,席胜利.鄂尔多斯盆地上古生界气藏特征[J].天然气工业,2000,20(6):16-19.
[57]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003.21(1),137-141.
[58]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003(3),21(1):137-141.
[59]郭沫贞,朱国华,寿建峰,等.碎屑岩压裂缝的特征、成因与油气勘探意义[J].沉积学报,2006,24(4):483-487.
[60]郭艳琴,李文厚,胡友州,等.陇东地区上三叠统延长组早中期物源分析与沉积体系[J].煤田地质与勘探,2006(2),34(1):1-4.
[61]韩宗元,苗建宇,许威,等.鄂尔多斯盆地子洲-清涧地区上古生界山2_3段储层砂岩成岩作用[J].地质科技情报,2008,27(2):49-55.
[62]何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.
[63]胡斌,张利伟,齐永安,等.济源下侏罗统鞍腰组沉积构造特征及环境解释[J].焦作工学院学报,2004(1),23(1):18-22.
[64]胡光义,于会娟,刘静,等.番30-1砂岩强水驱气藏储层非均质性研究[J].油气地质与采收率,2006,13(4):34-35,51.
[65]胡见义,黄第藩等.中国陆相石油地质理论基础[M].北京:石油工业出版社,1991.
[66]胡向阳,熊琦华,吴胜和.储层建模方法研究进展[J].石油大学学报(自然科学版),2001,25(1):107-113.
[67]黄思静,武文慧,刘洁等,大气水在碎屑岩次生孔隙形成中的作用-以鄂尔多斯盆地三叠系延长组为例[J].地球科学-中国地质大学学报,2003,28(4):419-424.
[68]黄思静.用excel计算沉积物粒度分布参数[J].成都理工学院学报,1999(4),26(4):195-199.
[69]纪友亮,张宏,张立强.祁连盆地木里坳陷上三叠统辫状三角洲沉积模式[J].石油勘探与开发,1998,25(5):30-33.
[70]纪友亮,张世奇.陆相断陷湖盆层序地层学[M].北京:石油工业出版社,1996.
[71]姜在兴.沉积学[M].北京:石油工业出版社,2003.
[72]况军,唐勇,朱国华,等.准噶尔盆地侏罗系储集层的基本特征及其主控因素分析[J].石油勘探与开发,2002,29(1):52-55.
[73]李德生.重新认识鄂尔多斯盆地油气地质学[J].石油勘探与开发,2004(12),31(6):1-7.
[74]李凤杰,王多云.坳陷湖盆三角洲前缘沉积微相构成及其分带性[J].天然气地球科学,2006(12),17(6):775-779.
[75]李红,柳益群,刘林玉.鄂尔多斯盆地西峰油田延长组长8_1低渗透储层成岩作用[J].石油与天然气地质,2006,27(2):209-217.
[76]李会军,程文艳,张文才,等.深层异常温压条件下碎屑岩成岩作用特征初探-以板桥凹陷下第三系碎屑岩地层为例[J].石油勘探与开发,2001,28(6):28-31.
[77]李克勤,等.长庆油田石油地质志[M].北京:石油工业出版社,1992.
[78]李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998,25(6):5-7.
[79]林承焰,侯加根,侯连华,等.油气储层三维定量地质建模方法和配套技术.石油大学学报(自然科学版),1996,20(4):20-25.
[80]刘宝瑶,王剑,谢渊,等.当代沉积学研究的新进展与发展趋势-来自第三十一届国际地质大会的信息[J].沉积与特提斯地质,22(1),2002.
[81]刘俊海,杨香华,于水,等.东海盆地丽水凹陷古新统沉积岩的稀土元素地球化学特征[J].现代地质,2003,17(4):421-427.
[82]刘少峰,杨少恭.鄂尔多斯盆地西缘南北差异及其形成机制.地质科学[J].1997,32(3):397-408.
[83]刘岫峰.沉积岩实验室研究方法[M].北京:地质出版社,1991.
[84]柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3):87-95.
[85]鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D辑),1998,6,28(3):278-283.
[86]吕晓光,李长山,蔡希源,等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型.沉积学报,1999,17(4):572-577.
[87]吕晓光,王家华,潘懋,等.指示主成分模拟建立分流河道砂体相模型.石油学报,2003,24(1):51-57.
[88]吕晓光,张永庆,陈兵,等.深度开发油田确定性与随机建模结合的相控建模.石油学报,2004,25(5):60-64.
[89]罗静兰,J.Marcelo Ketzer,李文厚,阎世可,武富礼,李玉宏.延长油区侏罗系-上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341.
[90]罗静兰,S.Morad,阎世可,武富礼,李玉宏,薛军民,张晓莉.河流-湖泊三角洲相砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例.中国科学(D辑)[J].2001,31(12):1006-1016.
[91]罗静兰,Sorad S,阎世可,等.河流湖泊三角洲砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例[J].中国科学:D辑,2001,31(12):1006-1016.
[92]罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报,2006(5),80(5):664-673.
[93]罗静兰,史成恩,李博,等.鄂尔多斯盆地周缘及西峰地区延长组长8、长6沉积物源-来自岩石地球化学的证据[J].中国科学(D辑),2007,37(增刊1):62-72.
[94]罗静兰,张晓莉,张云翔,李玉宏,武富礼.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4):541-547.
[95]罗明高.定量储层地质学[M].北京:地质出版社,1998.
[96]梅志超,林晋炎.湖泊三角洲的地层模式和骨架砂体的特征[J].沉积学报,1991(9)9(4):1-11.
[97]牟泽辉,朱宏权,张克银,等.鄂尔多斯盆地南部中生界成油体系[M].北京:石油工业出版社,2001.1-10:120.
[98]穆立华,彭仕宓,尹志军,等.冀东柳赞油田古近系沙河街组层序地层及岩相古地理[J].古地理学报,2003,5(3):304-315.
[99]聂永生,田景春,夏青松,等.鄂尔多斯盆地白豹-姬源地区上三叠统延长组物源分析[J].油气地质与采收率,2004(10),11(5):4-7.
[100]钱青,张旗,孙晓猛,等.北祁连老虎山玄武岩和硅岩的地球化学特征及形成环境[J].地质科学,2001(10),36(4):444-453.
[101]邱荣华,李纯菊,郭双亭.泌阳凹陷三类三角洲沉积特征及储集性能[J].石油勘探与开发,1994,21(1):99-105.
[102]裘亦楠,薛叔浩.油气储层评价技术[M].修订版.北京:石油工业出版社,2001.
[103]裘亦楠.储层沉积学研究工程流程.石油勘探与开发,1990,17(1):85-90.
[104]裘亦楠.储层地质模型.石油学报,1991,12(4):55-62.
[105]裘亦楠.中国陆相储层沉积学的进展[J].沉积学报.1992,10(3):16-24.
[106]裘怿楠,贾爱林.储层地质模型10年.石油学报,2000,21(4):101-104.
[107]任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造——中国及邻区大地构造图简要说明[M].北京:地质出版社,2000,1-60.
[108]芮拥军,石林光.准格尔盆地中部地震资料提高分辨率处理研究[J].石油物探,2007(3), 46(2):181-188.
[109]邵磊,Stattegger K,李文厚.从砂岩地球化学探讨盆地构造背景[J].科学通报,1998,43(9):985-988.
[110]邵磊,刘志伟,朱伟林.陆源碎屑岩地球化学在盆地分析中的应用[J].地学前缘,2000,7(9):297-304.
[111]宋国初,杨俊杰.陕北上三叠统湖泊三角洲沉积与油气藏形成,见杨俊杰主编,低渗透油气藏勘探开发技术[M].北京:石油工业出版社,1993.
[112]宋凯,吕剑文,杜金良,等,鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系[J].古地理学报,2002(8),4(3):59-60
[113]孙国凡,刘景平,柳克琪,等.华北中生代大型沉积盆地的发育及其地球动力学背景[J].石油与天然气地质,1985,6(3):278-287.
[114]孙国凡,谢秋元,刘景平等.鄂尔多斯盆地的演化叠加与含油气性[J].石油与天然气地质,1986,7(4):356-366.
[115]孙国凡.鄂尔多斯盆地印支运动及其在形成三叠系、侏罗系油藏中的作用[A].石油地质文集(3).地质出版社,1981.
[116]孙肇才,谢秋元.叠合盆地的发展特征及其含油性-以鄂尔多斯盆地为例[J].石油实验地质,1980,2(1):13-21.
[117]谭胜章,杜惠平,宋国良,等.高精度三维地震资料采集技术-以官渡地区山地地震勘探为例[J].石油物探,2007(1),46(1):74-82.
[118]田在艺.中国含油气盆地构造特征及其远景评价.见:田在艺著.田在艺石油地质论文选集.北京:石油工业出版社,1996.56-68.
[119]汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000(12),20(4):104-110.
[120]王良忱,张金亮.沉积环境与沉积相[M].北京:石油工业出版社,1996.
[121]王世虎,焦养泉,吴立群,等.鄂尔多斯盆地西北部延长组中下部古物源与沉积体空间配置[J].地球科学-中国地质大学学报,2007(3),32(2):201-208.
[122]王卓卓,陈代钊,汪建国.广西南宁地区泥盆系硅质岩地球化学特征及沉积环境[J].沉积学报,207(4),25(2):239-245.
[123]魏斌,魏红红,陈全红,等.鄂尔多斯盆地上三叠统延长组物源分析[J].西北大学学报(自然科学版),2003(8),33(4):447-450.
[124]吴元燕,刘震,王伟华,等.歧北凹陷沙河街组层序地层学研究[J].沉积学报,1996,14(1):167-175.
[125]武富礼,李文厚等鄂尔多斯盆地上三叠统延长组三角洲沉积及演化[J].古地理学报,2004,6(3):307-315
[126]鲜本忠,姜在兴,胡书毅,等.黄河三角洲冰冻沉积构造及其环境意义[J].沉积学报,2003(12),21(4):586-592.
[127]谢庆宾,韩德馨,朱筱敏,等.三塘湖盆地火成岩储集空间类型及特征[J].石油勘探与开发,2002,29(1):84-86.
[128]徐亚军,杜远生,杨江海.沉积物物源分析研究进展[J].地质科技情报,2007(5),26(3):26-32.
[129]闫小雄.鄂尔多斯中生代盆地古物源分析与沉积环境格局恢复[D].西北大学硕士论文,2001.
[130]闫义,林舸,王岳军,等.盆地陆源碎屑沉积物对源区构造背景的指示意义[J].地球科学进展,2002(2),17(1):85-90.
[131]闫臻,肖文交,刘传周,等.祁连山老君山砾岩的碎屑组成和源区大地构造背景[J].地质通报,2006(2),25(1-2):83-98.
[132]杨宝忠,夏文臣,杨坤光.吉林中部地区二叠纪岩相古地理及沉积构造背景[J].现代地质,2006(3),20(1):61-68.
[133]杨虎,郭华东,李新武,等.极化雷达目标信息分解技术及其在古湖岸线探测中的应用[J].地球信息科学,2003(6),4:109-114.
[134]杨辉廷,颜其彬,李敏.油藏描述中的储层建模技术[J].天然气勘探与开发,2004,27(3):45-51.
[135]杨江海,杜远生,朱杰.甘肃景泰崔家墩下奥陶统阴沟组砂岩化学组分特征及物源区构造背景判别[J].古地理学报,2007(4),9(2):197-206.
[136]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.130-181.
[137]杨俊杰.鄂尔多斯盆地构造与演化[M].北京:石油工业出版社,2000.
[138]杨少春,周建林.胜坨油田二区高含水期三角洲储层非均质特征[J].石油大学学报:自然科学版,2001,25(1):37-41.
[139]杨守业,李从先.REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):164-167.
[140]杨小萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发,2001,28(4):38-40.
[141]杨友运.印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响[J].煤田地质与勘探,2004,32(5):7-9.
[142]叶连俊.论华北地台沉积建造.见:中国科学院地质研究所主编,岩石学研究,第1辑.北京:地质出版社,1982,1-10.
[143]叶连俊.华北地台沉积建造[M].北京:科学出版社,1983.
[144]印兴耀,刘永社.储层建模中地质统计学整合地震数据的方法及研究进展[J].石油地球物理勘探,2002,37(4):423-431.
[145]于翠玲,林承焰.储层非均质性研究进展[J].油气地质与采收率,2007,14(4):15-22.
[146]于兴河编著.碎屑岩系油气储层沉积学[M].北京:石油工业出版社,2002.
[147]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油试验地质,2004(4),26(2):138-142.
[148]张抗.鄂尔多斯断块构造和资源[M].西安:陕西省科学技术出版社,1989,193-250.
[149]张旗,孙晓猛,周德进,等.北祁连蛇绿岩的特征、形成环境及其构造意义[J].地球科学进展,1997,12(4):366-393.
[150]张永贵,李允,陈明强.储层地质统计随机建模.石油大学学报(自然科学版),1998,22(3):113-119.
[151]赵俊峰,刘池洋,喻林,等.鄂尔多斯盆地中侏罗世直罗-安定期沉积构造特征[J].石油与天然气地质,2006(4),27(2):159-166.
[152]赵重远,等.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990.
[153]赵重远,刘池洋.华北克拉通中新生代区域地质构造及含油气盆地的形成和演化[A].见:赵重远,刘池洋等著.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990,10-21.
[154]赵重远.鄂尔多斯地块西缘演化及其板块应力机制初探[A].见赵重远,刘池洋等著.华北克拉通沉积盆地形成与演化及其油气赋存[C].西安:西北大学出版社,1990,107-114.
[155]钟广法,邬宁芬.成岩岩相分析:一种全新的成岩非均质性研究方法[J].石油勘探与开发,1997,24(5):62-66.
[156]周鼎武,李文厚,张云翔,等.区域地质综合研究的方法与实践[M].北京:科学出版社,2002.123-129.
[157]周竹生,黎家盆.叠后高分辨率资料处理方法及应用效果[J].石油地球物理勘探,1994,25(5):601-609.
[158]朱杰,杜远生.北祁连造山带老虎山奥陶系硅质岩地球化学特征及古地理意义[J].古地理学报,2007(2),9(1):69-76.
[159]朱如凯,郭宏莉,何东博,等.中国西北地区石炭系泥岩稀土元素地球化学特征及其地质意义[J].现代地质,2002,16(2):130-136.
[2] Bhatia M R, Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 1986, 92:181-193.
[3] Bhatia M R. Plate tectonics and geochemical composition of sandstone[J]. Earth Science-Journal of China University of Geosciences, 1983, 91(6): 611-627.
[4] Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J]. Sedimentary Geology, 1985, 45: 97-113.
[5] Clark J D and Pickering K T.Architectural elements and growth patterns of submarine channels:application to hydrocarbon explorationAAPG Bulletin, 1996, 80 (2): 194-211.
[6] Cross T A.High-resolution stratigraphic correlation from the perception of base-level cycles and sediment accommodation.In: Proceeding of Northwestern Europian Sequence Stratigraphy Congress, 1994: 105-123.
[7] Cullers R L, Basu A, Suttner L J. Geochemical signature of provenance in sand-mixed material in soils and stream sediments near the Tobucco Root Botholith, Montana, USA. Chem Geol, 1988,70: 335-348.
[8] Davis R A. Depositional systems: an introduction to sedimentology and stratigraghy. Prentice-hall,Inc.1992.
[9] Demaison G and Hutiinga B J.Genetic classification of petroleum systems. AAPG Bulletin.1991, 75(10): 1626-1643.
[10]Dutton S P and Willis B J.Comparison of outcrop and subsurface sandstone permeability distribution, Lower Cretaceous Fall River Formation, South Dakota and Wyoming.Journal of Sedimentary Research, 1998, 68 (5) : 890-900.
[11]Einsele G, S.K.Chough and T.Shiki. Depositional events and their records-an introduction.Sedimentary Geology [J]. 1996, Vol.104:1-9.
[12]Embry A F. Transgressive-regressive (T-R) sequence analysis of the Jurassic succesion of Sverdrup Basin, Canadian Arctic Archipelago. Can. J. Earth Sci.,1993,30:301-320.
[13]Friedman G M and Sanders J E.Principles of Sedimentology.New York: Wiley, 1978.
[14] Galloway W E.Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units.AAPG Bulletin. 1989: 73 (2): 125-142.
[15]Galloway W E.Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units.AAPG Bulletin. 1989: 73 (2):125-142.
[16]Gao S and Collins M. Net sedimenttransportpatternsinferred from grain size trends, based upon definition of transport vectors"[J]. Sedimentary Geology, 1992, 81: 47-60.
[17]Halforsen H H and Macdonald C G.Stochastic modeling of Underground Reservoir Fades, SPE(16751), 1987, 575-589.
[18] Jerry Lucla F and Graham E Fogg. Geologic/Stochasticmapping of heterogeneity in a carbonate reservoir[J]. Journal of Petroleum Technology, 1990, 42 (10):1298-1303.
[19]Jiao Yangquan, Yan Jiaxin, Li Sitian, et al. Architectural units and heterogeneity of channel reservoirs in the Karamay Formation, outcrop area of Karamay oil field, Junggar basin, northwest China[J]. AAPG Bulletin, 2005, 89 (4):529-545.
[20]Lewis D W.. Practical Sedimentology[M]. Hutchinson Ross Publish ing Co., 1984, 31-39.
[21]Martinius A W and Nieuwenhuijs R A.Geological description of flow units in channel sandstones in a fluvial reservoir analogue (Loranca Basin, Spain) .Petroleum Geoscience, 1995, 1(3): 237-252.
[22]Mclennan S M. Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes[M]. in: Lipin B.R.et al.(ed.): Geochemistry and Mineralogy of Rare earth elements. The Mineralogical Society of America, Washington, D.C., 1989, 169-200.
[23]Nelson R A. Natural Fracture Systems, Description and Classification[J]. AAPG Bulletin. 1979,63(12): 2214-2221.
[24]Nelson Ronald A. GeologicAnalysis of Naturally Fractured Reservoirs[M]. Beijing: Petroleum IndustryPress, 1991. 6-26.
[25]Pettijohn F J..Sedimentary Rocks (3rd edition)[M]. Harper & Row Publishers Inc., 1975, 106-108.
[26]Pramod S and Rajamani V. Geochemistry of the Floodplain Sediments of the Kaveri River, Southern India, Sedimentary Research, 2001, 71 (1): 50-60.
[27]Ramon J C and Cross T A.Characterization and prediction of reservoir architecture and petrophysical properties in fluvial channel sandstones, Middle Magdalena Basin, Colombia.Ciencia,Tecnology Future, 1997, 1 (3): 19-46.
[28]Rea D K, Snoeckx H and Joseph L H. Late Cenozoic eolian deposition the North Pacific: Asian drying, Tibetan uplift and cooling of the northern hemisphere[J]. Paleoceanography, 1998, 13 (3):215-224.
[29]Reading H G. Sedimentary Environments: Processes,Facies and Stratigraphy.Oxford,UK:Blackwell. 1996.
[30]Rollinson H R. Using geochemical date: evaluation, presentation, interpretation[M]. London:Longman Scientific Technical Press, 1993, 1-352.
[3 l]Roser B P, Korsch R J. Determination of tectonic setting of sandstone-mudstone suites using SiO_2 content and K_2O/Na_2O ratio[J]. The Journal of Geology, 1986, 94(5): 635-650.
[32]Roser B P, Korsch R J. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of majorelement data[J]. Chemical Geology, 1988, 67: 119-139.
[33]Selly R C. An introduction to sedimentology[M]. London: Academic Press Inc., 1976.208-209.
[34]Shanly K W, et al.Perspective on the sequence stratigraphy of continental strata.AAPG Bulletin.1994, 74 (4): 544-568.
[35]Shanmugam G and Moiola R J.Types of submarine fan lobes: models and implication.AAPG Bulletin. 1991, (75): 156-179.
[36] Steams D W and Friedman M. Reservoirs in Fractured Rock[J]. AAPG Memoir 16. 1972. 82-100.
[37]Stow D A V and Johansson M.Deep water massive sands: nature, origin and hydrocarbon implications.Marine and Petroleum Geology, 2000, 17 (1): 145-174.
[38] Thomas F Moslow, Graham R Davies. Turbidite reservoir facies in the Lower TriassicMontney Formation,west-central Alberta [J].Bulletin of Canadian Petroleum Geology, 1997, 45 (4): 507-536.
[39]Thomas Pichler and John D H.Formation of Dolomite in Recent Island-arc Sediments due to Gas-Seawater-Sediment interaction, Sedimentary Research, 2001, 71 (3), 394-399.
[40] Vail P R, Mitchum R M, Todd R G, et al. Seismic stratigraphy and global changes of sea level.In:Payton C E ed.Seismic stratigraphy-application to hydrocarbon exploration.AAPG Memoir, 1977,26: 83-97.
[41] Weber K J and Maatschappij B V. How Heterogeneity Affects Oil Recovery; Reservoir Characterization, 1986, 487-544.
[42] Weber K J , Kantorowicz J D and Williams H.Geological modelling of hydrocarbon reservoirs.Marine and Petroleum Geology, 1991, 8 (2) : 245-246.
[43]Weimer P R, Bouma A H and Perkins B F.Submarine fans and turbidite systems, sequence stratigraphic, reservoir architecture and production characteristics.In: Aon.Gulf of Mexico and International: Gulf Coast Section of the SEPM Foundation 15th Annual Research Conference Proceedings.TULSA: SEPM, 1994: 440.
[44]Weimer P R. Envelopments in sequence statigraphy: foreland and cratonic basins. AAPG Bulletin.1992, 76 (7): 965-982.
[45]Wong P M, Tamhane D and Wang L.A neural-network approach to knowledge-based well interpolation: a case study of a fluvial sandstone reservoir.Journal of Petroleum Geology, 1997,20 (3) : 363-372.
[46]Zheng R C, Yin S M and Peng J. Sedimentary dynamic analysis of sequence structure and stacking patten of base-level cycle. Acta Sediment to logica Sinica, 2000, 18 (3):369-375.
[47]曹红霞,李文厚,何卫军,等.鄂尔多斯盆地宜川地区延长组物源分析[J].煤田地质与勘探,2007(12).35(6):14-17.
[48]曹红霞,张云翔,岳乐平,等.毛乌素沙地全新世地层粒度组成特征及古气候意义[J].沉积学报,2003(9),21(3):482-486.
[49]代金友,张一伟,熊琦华,等.成岩作用对储集层物性贡献比率研究[J].石油勘探与开发,2003,30(4):54-55.
[50]邓军,王庆飞,高帮飞,等.鄂尔多斯盆地演化与多种能源矿产分布[J].现代地质,2005,19(4):538-545.
[51]邓希光,李献华,陈志刚,等.广西钦州板城晚泥盆世硅质岩地球化学特征及沉积环境探讨[J].地质科学,2003,38(4):460-469.
[52]邸志欣,谭绍泉,姜维才,等.川东北地区山地三维高分辨率地震采集技术[J].石油物探,2005,44(5):517-524.
[53]丁仲礼,孙继敏,刘东生.联系沙漠-黄土演变过程中耦合关系的沉积学指标[J].中国科学,1999,29(1):82-87.
[54]方少仙,候方浩.石油天然气储层地质学[M].北京:石油大学出版社,1998.
[55]冯增昭.沉积岩石学(第二版)[M].北京:石油工业出版社,1993,108-131.
[56]付金华,段晓文,席胜利.鄂尔多斯盆地上古生界气藏特征[J].天然气工业,2000,20(6):16-19.
[57]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003.21(1),137-141.
[58]顾家裕,张兴阳.油气沉积学发展回顾和应用现状[J].沉积学报,2003(3),21(1):137-141.
[59]郭沫贞,朱国华,寿建峰,等.碎屑岩压裂缝的特征、成因与油气勘探意义[J].沉积学报,2006,24(4):483-487.
[60]郭艳琴,李文厚,胡友州,等.陇东地区上三叠统延长组早中期物源分析与沉积体系[J].煤田地质与勘探,2006(2),34(1):1-4.
[61]韩宗元,苗建宇,许威,等.鄂尔多斯盆地子洲-清涧地区上古生界山2_3段储层砂岩成岩作用[J].地质科技情报,2008,27(2):49-55.
[62]何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.
[63]胡斌,张利伟,齐永安,等.济源下侏罗统鞍腰组沉积构造特征及环境解释[J].焦作工学院学报,2004(1),23(1):18-22.
[64]胡光义,于会娟,刘静,等.番30-1砂岩强水驱气藏储层非均质性研究[J].油气地质与采收率,2006,13(4):34-35,51.
[65]胡见义,黄第藩等.中国陆相石油地质理论基础[M].北京:石油工业出版社,1991.
[66]胡向阳,熊琦华,吴胜和.储层建模方法研究进展[J].石油大学学报(自然科学版),2001,25(1):107-113.
[67]黄思静,武文慧,刘洁等,大气水在碎屑岩次生孔隙形成中的作用-以鄂尔多斯盆地三叠系延长组为例[J].地球科学-中国地质大学学报,2003,28(4):419-424.
[68]黄思静.用excel计算沉积物粒度分布参数[J].成都理工学院学报,1999(4),26(4):195-199.
[69]纪友亮,张宏,张立强.祁连盆地木里坳陷上三叠统辫状三角洲沉积模式[J].石油勘探与开发,1998,25(5):30-33.
[70]纪友亮,张世奇.陆相断陷湖盆层序地层学[M].北京:石油工业出版社,1996.
[71]姜在兴.沉积学[M].北京:石油工业出版社,2003.
[72]况军,唐勇,朱国华,等.准噶尔盆地侏罗系储集层的基本特征及其主控因素分析[J].石油勘探与开发,2002,29(1):52-55.
[73]李德生.重新认识鄂尔多斯盆地油气地质学[J].石油勘探与开发,2004(12),31(6):1-7.
[74]李凤杰,王多云.坳陷湖盆三角洲前缘沉积微相构成及其分带性[J].天然气地球科学,2006(12),17(6):775-779.
[75]李红,柳益群,刘林玉.鄂尔多斯盆地西峰油田延长组长8_1低渗透储层成岩作用[J].石油与天然气地质,2006,27(2):209-217.
[76]李会军,程文艳,张文才,等.深层异常温压条件下碎屑岩成岩作用特征初探-以板桥凹陷下第三系碎屑岩地层为例[J].石油勘探与开发,2001,28(6):28-31.
[77]李克勤,等.长庆油田石油地质志[M].北京:石油工业出版社,1992.
[78]李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998,25(6):5-7.
[79]林承焰,侯加根,侯连华,等.油气储层三维定量地质建模方法和配套技术.石油大学学报(自然科学版),1996,20(4):20-25.
[80]刘宝瑶,王剑,谢渊,等.当代沉积学研究的新进展与发展趋势-来自第三十一届国际地质大会的信息[J].沉积与特提斯地质,22(1),2002.
[81]刘俊海,杨香华,于水,等.东海盆地丽水凹陷古新统沉积岩的稀土元素地球化学特征[J].现代地质,2003,17(4):421-427.
[82]刘少峰,杨少恭.鄂尔多斯盆地西缘南北差异及其形成机制.地质科学[J].1997,32(3):397-408.
[83]刘岫峰.沉积岩实验室研究方法[M].北京:地质出版社,1991.
[84]柳益群,李文厚.陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3):87-95.
[85]鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D辑),1998,6,28(3):278-283.
[86]吕晓光,李长山,蔡希源,等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型.沉积学报,1999,17(4):572-577.
[87]吕晓光,王家华,潘懋,等.指示主成分模拟建立分流河道砂体相模型.石油学报,2003,24(1):51-57.
[88]吕晓光,张永庆,陈兵,等.深度开发油田确定性与随机建模结合的相控建模.石油学报,2004,25(5):60-64.
[89]罗静兰,J.Marcelo Ketzer,李文厚,阎世可,武富礼,李玉宏.延长油区侏罗系-上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341.
[90]罗静兰,S.Morad,阎世可,武富礼,李玉宏,薛军民,张晓莉.河流-湖泊三角洲相砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例.中国科学(D辑)[J].2001,31(12):1006-1016.
[91]罗静兰,Sorad S,阎世可,等.河流湖泊三角洲砂岩成岩作用的重建及其对储层物性演化的影响-以延长油区侏罗系-上三叠统砂岩为例[J].中国科学:D辑,2001,31(12):1006-1016.
[92]罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报,2006(5),80(5):664-673.
[93]罗静兰,史成恩,李博,等.鄂尔多斯盆地周缘及西峰地区延长组长8、长6沉积物源-来自岩石地球化学的证据[J].中国科学(D辑),2007,37(增刊1):62-72.
[94]罗静兰,张晓莉,张云翔,李玉宏,武富礼.成岩作用对河流-三角洲相砂岩储层物性演化的影响-以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4):541-547.
[95]罗明高.定量储层地质学[M].北京:地质出版社,1998.
[96]梅志超,林晋炎.湖泊三角洲的地层模式和骨架砂体的特征[J].沉积学报,1991(9)9(4):1-11.
[97]牟泽辉,朱宏权,张克银,等.鄂尔多斯盆地南部中生界成油体系[M].北京:石油工业出版社,2001.1-10:120.
[98]穆立华,彭仕宓,尹志军,等.冀东柳赞油田古近系沙河街组层序地层及岩相古地理[J].古地理学报,2003,5(3):304-315.
[99]聂永生,田景春,夏青松,等.鄂尔多斯盆地白豹-姬源地区上三叠统延长组物源分析[J].油气地质与采收率,2004(10),11(5):4-7.
[100]钱青,张旗,孙晓猛,等.北祁连老虎山玄武岩和硅岩的地球化学特征及形成环境[J].地质科学,2001(10),36(4):444-453.
[101]邱荣华,李纯菊,郭双亭.泌阳凹陷三类三角洲沉积特征及储集性能[J].石油勘探与开发,1994,21(1):99-105.
[102]裘亦楠,薛叔浩.油气储层评价技术[M].修订版.北京:石油工业出版社,2001.
[103]裘亦楠.储层沉积学研究工程流程.石油勘探与开发,1990,17(1):85-90.
[104]裘亦楠.储层地质模型.石油学报,1991,12(4):55-62.
[105]裘亦楠.中国陆相储层沉积学的进展[J].沉积学报.1992,10(3):16-24.
[106]裘怿楠,贾爱林.储层地质模型10年.石油学报,2000,21(4):101-104.
[107]任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造——中国及邻区大地构造图简要说明[M].北京:地质出版社,2000,1-60.
[108]芮拥军,石林光.准格尔盆地中部地震资料提高分辨率处理研究[J].石油物探,2007(3), 46(2):181-188.
[109]邵磊,Stattegger K,李文厚.从砂岩地球化学探讨盆地构造背景[J].科学通报,1998,43(9):985-988.
[110]邵磊,刘志伟,朱伟林.陆源碎屑岩地球化学在盆地分析中的应用[J].地学前缘,2000,7(9):297-304.
[111]宋国初,杨俊杰.陕北上三叠统湖泊三角洲沉积与油气藏形成,见杨俊杰主编,低渗透油气藏勘探开发技术[M].北京:石油工业出版社,1993.
[112]宋凯,吕剑文,杜金良,等,鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系[J].古地理学报,2002(8),4(3):59-60
[113]孙国凡,刘景平,柳克琪,等.华北中生代大型沉积盆地的发育及其地球动力学背景[J].石油与天然气地质,1985,6(3):278-287.
[114]孙国凡,谢秋元,刘景平等.鄂尔多斯盆地的演化叠加与含油气性[J].石油与天然气地质,1986,7(4):356-366.
[115]孙国凡.鄂尔多斯盆地印支运动及其在形成三叠系、侏罗系油藏中的作用[A].石油地质文集(3).地质出版社,1981.
[116]孙肇才,谢秋元.叠合盆地的发展特征及其含油性-以鄂尔多斯盆地为例[J].石油实验地质,1980,2(1):13-21.
[117]谭胜章,杜惠平,宋国良,等.高精度三维地震资料采集技术-以官渡地区山地地震勘探为例[J].石油物探,2007(1),46(1):74-82.
[118]田在艺.中国含油气盆地构造特征及其远景评价.见:田在艺著.田在艺石油地质论文选集.北京:石油工业出版社,1996.56-68.
[119]汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000(12),20(4):104-110.
[120]王良忱,张金亮.沉积环境与沉积相[M].北京:石油工业出版社,1996.
[121]王世虎,焦养泉,吴立群,等.鄂尔多斯盆地西北部延长组中下部古物源与沉积体空间配置[J].地球科学-中国地质大学学报,2007(3),32(2):201-208.
[122]王卓卓,陈代钊,汪建国.广西南宁地区泥盆系硅质岩地球化学特征及沉积环境[J].沉积学报,207(4),25(2):239-245.
[123]魏斌,魏红红,陈全红,等.鄂尔多斯盆地上三叠统延长组物源分析[J].西北大学学报(自然科学版),2003(8),33(4):447-450.
[124]吴元燕,刘震,王伟华,等.歧北凹陷沙河街组层序地层学研究[J].沉积学报,1996,14(1):167-175.
[125]武富礼,李文厚等鄂尔多斯盆地上三叠统延长组三角洲沉积及演化[J].古地理学报,2004,6(3):307-315
[126]鲜本忠,姜在兴,胡书毅,等.黄河三角洲冰冻沉积构造及其环境意义[J].沉积学报,2003(12),21(4):586-592.
[127]谢庆宾,韩德馨,朱筱敏,等.三塘湖盆地火成岩储集空间类型及特征[J].石油勘探与开发,2002,29(1):84-86.
[128]徐亚军,杜远生,杨江海.沉积物物源分析研究进展[J].地质科技情报,2007(5),26(3):26-32.
[129]闫小雄.鄂尔多斯中生代盆地古物源分析与沉积环境格局恢复[D].西北大学硕士论文,2001.
[130]闫义,林舸,王岳军,等.盆地陆源碎屑沉积物对源区构造背景的指示意义[J].地球科学进展,2002(2),17(1):85-90.
[131]闫臻,肖文交,刘传周,等.祁连山老君山砾岩的碎屑组成和源区大地构造背景[J].地质通报,2006(2),25(1-2):83-98.
[132]杨宝忠,夏文臣,杨坤光.吉林中部地区二叠纪岩相古地理及沉积构造背景[J].现代地质,2006(3),20(1):61-68.
[133]杨虎,郭华东,李新武,等.极化雷达目标信息分解技术及其在古湖岸线探测中的应用[J].地球信息科学,2003(6),4:109-114.
[134]杨辉廷,颜其彬,李敏.油藏描述中的储层建模技术[J].天然气勘探与开发,2004,27(3):45-51.
[135]杨江海,杜远生,朱杰.甘肃景泰崔家墩下奥陶统阴沟组砂岩化学组分特征及物源区构造背景判别[J].古地理学报,2007(4),9(2):197-206.
[136]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.130-181.
[137]杨俊杰.鄂尔多斯盆地构造与演化[M].北京:石油工业出版社,2000.
[138]杨少春,周建林.胜坨油田二区高含水期三角洲储层非均质特征[J].石油大学学报:自然科学版,2001,25(1):37-41.
[139]杨守业,李从先.REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):164-167.
[140]杨小萍,陈丽华.陕北斜坡延长统低渗储集层成岩相研究[J].石油勘探与开发,2001,28(4):38-40.
[141]杨友运.印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响[J].煤田地质与勘探,2004,32(5):7-9.
[142]叶连俊.论华北地台沉积建造.见:中国科学院地质研究所主编,岩石学研究,第1辑.北京:地质出版社,1982,1-10.
[143]叶连俊.华北地台沉积建造[M].北京:科学出版社,1983.
[144]印兴耀,刘永社.储层建模中地质统计学整合地震数据的方法及研究进展[J].石油地球物理勘探,2002,37(4):423-431.
[145]于翠玲,林承焰.储层非均质性研究进展[J].油气地质与采收率,2007,14(4):15-22.
[146]于兴河编著.碎屑岩系油气储层沉积学[M].北京:石油工业出版社,2002.
[147]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油试验地质,2004(4),26(2):138-142.
[148]张抗.鄂尔多斯断块构造和资源[M].西安:陕西省科学技术出版社,1989,193-250.
[149]张旗,孙晓猛,周德进,等.北祁连蛇绿岩的特征、形成环境及其构造意义[J].地球科学进展,1997,12(4):366-393.
[150]张永贵,李允,陈明强.储层地质统计随机建模.石油大学学报(自然科学版),1998,22(3):113-119.
[151]赵俊峰,刘池洋,喻林,等.鄂尔多斯盆地中侏罗世直罗-安定期沉积构造特征[J].石油与天然气地质,2006(4),27(2):159-166.
[152]赵重远,等.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990.
[153]赵重远,刘池洋.华北克拉通中新生代区域地质构造及含油气盆地的形成和演化[A].见:赵重远,刘池洋等著.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990,10-21.
[154]赵重远.鄂尔多斯地块西缘演化及其板块应力机制初探[A].见赵重远,刘池洋等著.华北克拉通沉积盆地形成与演化及其油气赋存[C].西安:西北大学出版社,1990,107-114.
[155]钟广法,邬宁芬.成岩岩相分析:一种全新的成岩非均质性研究方法[J].石油勘探与开发,1997,24(5):62-66.
[156]周鼎武,李文厚,张云翔,等.区域地质综合研究的方法与实践[M].北京:科学出版社,2002.123-129.
[157]周竹生,黎家盆.叠后高分辨率资料处理方法及应用效果[J].石油地球物理勘探,1994,25(5):601-609.
[158]朱杰,杜远生.北祁连造山带老虎山奥陶系硅质岩地球化学特征及古地理意义[J].古地理学报,2007(2),9(1):69-76.
[159]朱如凯,郭宏莉,何东博,等.中国西北地区石炭系泥岩稀土元素地球化学特征及其地质意义[J].现代地质,2002,16(2):130-136.