松辽盆地南部中浅层沉积演化与油气分布
|
摘要
松辽盆地南部蕴藏着丰富的油气资源,目前探明储量主要集中在泉三段至嫩江组中浅层储层。本论文是以储层沉积学、石油地质学和油气成藏动力学为理论指导,综合利用地质、地球化学、地球物理和分析化验等资料,开展沉积体系研究及有利储集体相带划分,确定松辽盆地南部中浅层沉积相类型与分布规律,建立沉积演化模式,对不同沉积类型的各相带进行综合评价。结合该区油气成藏主控因素和成藏模式,对有利区域进行预测,从而达到开拓油气勘探新领域的目的。
根据详细的岩心观察和描述,结合测井资料、区域地质资料及各项分析化验资料等进行综合分析,确定了松辽盆地南部中浅层的沉积体系分布规律,识别出了辫状河、曲流河、末端扇、辫状河扇、三角洲、浅水三角洲、辫状三角洲与滩坝等沉积相类型,同时提出了新的沉积模式与沉积演化规律。泉三段沉积时期,气候环境炎热干燥,主要发育河流-末端扇沉积体系,河流相包括曲流河与辫状河。泉四段沉积时期,研究区内没有统一的汇水中心,同样以河流-末端扇沉积为主,研究区西北部发育辫状河扇-曲流河沉积。青山口组主要发育三角洲沉积和浅水三角洲沉积,砂体主要分布在西部地区,物源主要来自西部、西南部和南部,研究区东部为泥质沉积。姚家组沉积时期,西北部英台-白城水系发育辫状三角洲,西南部通榆-保康水系、南部长春水系发育浅水三角洲沉积。嫩一段和嫩二段主要发育滨—浅湖和半深—深湖沉积,零星分布薄层砂滩砂体。从嫩三段开始到嫩五段,水体逐渐变浅,湖盆范围缩小,北部物源主要发育三角洲沉积,南部缺乏恒定物源注入。
基于实验室分析资料,研究了松辽盆地南部中浅层储集空间类型,分析了不同沉积相类型各相带和储集岩储集性质的关系,对不同沉积相带的储集体进行了综合评价,确定了有利相带分布范围。研究认为,三角洲前缘水下分流河道与河口砂坝、末端扇分流河道、辫状河扇中部亚相辫状河道、河流相河道亚相储层物性较好。河流相堤岸亚相、浅水三角洲分流河道、三角洲前缘远河道与远砂坝、前缘席状砂、末端扇河道漫溢相储层物性次之。河流相河漫滩、末端扇泥滩沉积与远端盆地、前三角洲及分流间地区储层物性较差。
采用油气成藏组合观点,在平面、剖面上研究油藏的分布特点,分析了油气的分布与烃源岩分布、有利储集相带分布、油气输导体系等之间的关系,确定了油气分布的主要控制因素,总结了油气分布的规律性认识。松辽盆地南部中浅层油气分布主要受烃源岩分布、储集体分布、有利的生储盖组合配置、有效的圈闭与断层等因素的影响。在区带成藏条件和油气分布控制因素研究的基础上,分析了松辽盆地南部中浅层不同区带的成藏机理,对有利目标区域进行了预测。
There are abundant hydrocarbon resources in the south of Songliao Basin. The proven reserves mainly concentrate in the middle-shallow layer of the third member of Quantou formation to Nenjiang formation at present. This thesis is on the instruction of reservoir sedimentology, petroleum geology and hydrocarbon accumulation dynamics. Setting up the rearch of sedimentary system and classify of profitable facies belt in middle-shallow layer in the south of Songliao Basin using geology, geochemistry, geophysics and analyzed assay datum. To establish the sedimentary facies type and it’s distribution pattern, and sedimentary evolution mode. Evaluate each facies belts of different sedimentary facies comprehensively. Predict the range of profitability combine with the master factors of hydrocarbon accumulation and accumulation mode of Middle-shallow layer in the south of Songliao Basin. So obtain the object to uncover the new region of exploration activity.
According to the detailed observation and description of core, progress the synthesized analysis by combinbing the well logging, data of areal geology and all kinds of analyzed assay datum, assured the distribution regular pattern of sedimentary system in this area. Braided river, meandering river, terminal fan, braided river fan, delta, shallow delta, braided delta and beach bar sedimentation types are identified, and bring forward the new sedimentary mode and Sedimentary evolution regular. The climate is heat and arid in the third member of Quantou formation, and river-terminal fan sedimentary system develops in this period. There is no unitary water catchment center in the fourth member of Quantou formation, river-terminal fan sediment is the major sedimentation type, braided river fan-meandering river develops in the northwest of research area. Delta and shallow delta develops in the Qingshankou formation. The sand body distributes in the western area, the provenance come from the west, southwest and south of the research area, the east is muddy sediment. The braided delta develops in the northwestern Yingtai-Baicheng water system in Yaojia formation,and shallow delta develops in the southwestern Tongyu-Baokang water system and southern Changchun water system. The shore-shallow lake and hemi-deep-deep lake develop in the first and second member of Nenjiang formation, and thin bed beach sands distribute fragmentarily. The water body becomes shallow and the lake basin reduces from the third member of Nenjiang formation to the fifth member of Nenjiang formation, delta develops from the north provenance, and the constant provenance absent from the south provenance.
The reservoir types in the middle-shallow layer in the south of Songliao Basin are studied based on the analytical data from the laboratory, and the relation between facies belts and reservoir characters of different sedimentary facies are analyzed. The reservoir of different facies belt are evaluated, and profitable facies belts are defined. The result shows that the reservoir quality of underwater distributary channel and channel mouth bar of delta front, distributary channel of terminal fan, braided channel of middle braided river fan and the channel of river facies are well. The reservoir quality of bank of river facies, distributary channel of shallow delta, distal bar and distal channel of delta front, sand sheet, overbank of terminal fan take second place. The reservoir quality of flood plain of river facies, mud flat and distal basin of terminal fan, predelta and interchannel area are bad.
Take the point of hydrocarbon accumulation association to study the planar and sectional distribution pattern of petroleum reservoir. The relation between petroleum distribution and sources rocks distribution, profitable facies belt, petroleum dredge system and so on. Summary the regularity recognition of petroleum distribution. The petroleum distribution in the middle-shallow layer in the south of Songliao Basin is under the control of sources rocks distribution, accumulate facies belt, profitable association of source rock, reservoir and cap, effective trapping and fault and so on. The hydrocarbon accumulation mechanism is analyzed in different belt of the middle-shallow layer in the south of Songliao Basin on the base of research of hydrocarbon accumulation and petroleum distribution, and predict the range of profitability.
根据详细的岩心观察和描述,结合测井资料、区域地质资料及各项分析化验资料等进行综合分析,确定了松辽盆地南部中浅层的沉积体系分布规律,识别出了辫状河、曲流河、末端扇、辫状河扇、三角洲、浅水三角洲、辫状三角洲与滩坝等沉积相类型,同时提出了新的沉积模式与沉积演化规律。泉三段沉积时期,气候环境炎热干燥,主要发育河流-末端扇沉积体系,河流相包括曲流河与辫状河。泉四段沉积时期,研究区内没有统一的汇水中心,同样以河流-末端扇沉积为主,研究区西北部发育辫状河扇-曲流河沉积。青山口组主要发育三角洲沉积和浅水三角洲沉积,砂体主要分布在西部地区,物源主要来自西部、西南部和南部,研究区东部为泥质沉积。姚家组沉积时期,西北部英台-白城水系发育辫状三角洲,西南部通榆-保康水系、南部长春水系发育浅水三角洲沉积。嫩一段和嫩二段主要发育滨—浅湖和半深—深湖沉积,零星分布薄层砂滩砂体。从嫩三段开始到嫩五段,水体逐渐变浅,湖盆范围缩小,北部物源主要发育三角洲沉积,南部缺乏恒定物源注入。
基于实验室分析资料,研究了松辽盆地南部中浅层储集空间类型,分析了不同沉积相类型各相带和储集岩储集性质的关系,对不同沉积相带的储集体进行了综合评价,确定了有利相带分布范围。研究认为,三角洲前缘水下分流河道与河口砂坝、末端扇分流河道、辫状河扇中部亚相辫状河道、河流相河道亚相储层物性较好。河流相堤岸亚相、浅水三角洲分流河道、三角洲前缘远河道与远砂坝、前缘席状砂、末端扇河道漫溢相储层物性次之。河流相河漫滩、末端扇泥滩沉积与远端盆地、前三角洲及分流间地区储层物性较差。
采用油气成藏组合观点,在平面、剖面上研究油藏的分布特点,分析了油气的分布与烃源岩分布、有利储集相带分布、油气输导体系等之间的关系,确定了油气分布的主要控制因素,总结了油气分布的规律性认识。松辽盆地南部中浅层油气分布主要受烃源岩分布、储集体分布、有利的生储盖组合配置、有效的圈闭与断层等因素的影响。在区带成藏条件和油气分布控制因素研究的基础上,分析了松辽盆地南部中浅层不同区带的成藏机理,对有利目标区域进行了预测。
There are abundant hydrocarbon resources in the south of Songliao Basin. The proven reserves mainly concentrate in the middle-shallow layer of the third member of Quantou formation to Nenjiang formation at present. This thesis is on the instruction of reservoir sedimentology, petroleum geology and hydrocarbon accumulation dynamics. Setting up the rearch of sedimentary system and classify of profitable facies belt in middle-shallow layer in the south of Songliao Basin using geology, geochemistry, geophysics and analyzed assay datum. To establish the sedimentary facies type and it’s distribution pattern, and sedimentary evolution mode. Evaluate each facies belts of different sedimentary facies comprehensively. Predict the range of profitability combine with the master factors of hydrocarbon accumulation and accumulation mode of Middle-shallow layer in the south of Songliao Basin. So obtain the object to uncover the new region of exploration activity.
According to the detailed observation and description of core, progress the synthesized analysis by combinbing the well logging, data of areal geology and all kinds of analyzed assay datum, assured the distribution regular pattern of sedimentary system in this area. Braided river, meandering river, terminal fan, braided river fan, delta, shallow delta, braided delta and beach bar sedimentation types are identified, and bring forward the new sedimentary mode and Sedimentary evolution regular. The climate is heat and arid in the third member of Quantou formation, and river-terminal fan sedimentary system develops in this period. There is no unitary water catchment center in the fourth member of Quantou formation, river-terminal fan sediment is the major sedimentation type, braided river fan-meandering river develops in the northwest of research area. Delta and shallow delta develops in the Qingshankou formation. The sand body distributes in the western area, the provenance come from the west, southwest and south of the research area, the east is muddy sediment. The braided delta develops in the northwestern Yingtai-Baicheng water system in Yaojia formation,and shallow delta develops in the southwestern Tongyu-Baokang water system and southern Changchun water system. The shore-shallow lake and hemi-deep-deep lake develop in the first and second member of Nenjiang formation, and thin bed beach sands distribute fragmentarily. The water body becomes shallow and the lake basin reduces from the third member of Nenjiang formation to the fifth member of Nenjiang formation, delta develops from the north provenance, and the constant provenance absent from the south provenance.
The reservoir types in the middle-shallow layer in the south of Songliao Basin are studied based on the analytical data from the laboratory, and the relation between facies belts and reservoir characters of different sedimentary facies are analyzed. The reservoir of different facies belt are evaluated, and profitable facies belts are defined. The result shows that the reservoir quality of underwater distributary channel and channel mouth bar of delta front, distributary channel of terminal fan, braided channel of middle braided river fan and the channel of river facies are well. The reservoir quality of bank of river facies, distributary channel of shallow delta, distal bar and distal channel of delta front, sand sheet, overbank of terminal fan take second place. The reservoir quality of flood plain of river facies, mud flat and distal basin of terminal fan, predelta and interchannel area are bad.
Take the point of hydrocarbon accumulation association to study the planar and sectional distribution pattern of petroleum reservoir. The relation between petroleum distribution and sources rocks distribution, profitable facies belt, petroleum dredge system and so on. Summary the regularity recognition of petroleum distribution. The petroleum distribution in the middle-shallow layer in the south of Songliao Basin is under the control of sources rocks distribution, accumulate facies belt, profitable association of source rock, reservoir and cap, effective trapping and fault and so on. The hydrocarbon accumulation mechanism is analyzed in different belt of the middle-shallow layer in the south of Songliao Basin on the base of research of hydrocarbon accumulation and petroleum distribution, and predict the range of profitability.
引文
[1] Rust B R. A classification of alluvial channel systems, In:Miall A.D. ed. Fluvial sedimentology. Can. Soc. Petrol. Geol. Mem. 1978,5: 187-198
[2] Schumm S A. The fluvial system, John Wiley & Sons, NewYork,1977, 338p
[3]钱宁,张仁,周志德.河床演变学.北京:科学出版社,1987.2-51
[4]钱宁.关于河流分类及成因问题的讨论.地理学报,1995,40(1):1-10
[5]王随继,任明达.根据河道形态和沉积物特征的河流新分类.沉积学报,1999,17(2):240-246
[6] Allen J R L. Late Quaternary Niger Delta and adjacent areas: sedimentary environments and lithofacies. AAPG. Bull., 1965,49: 547-600
[7] Coleman J M, Wright L D. Modem river deltas: variability of process and sand bodies. In: BROUSSARD, M.L. (ed.) Deltas: Models for Exploration. Houston Geological Society, Houston, TX, 1975,99-150
[8] Coleman J M. Dynamic changes and processes in the Mississippi River delta. Geol. Soc. Am. Bull. 1988,100: 999-1015
[9] Edwards M B. Upper Wilcox Rosita delta system of South Texas. Growth-faulted shelf-edge deltas. AAPG Bull., 1981,65: 54-73
[10]王建功,王天琦,卫平生,等.大型坳陷湖盆浅水三角洲沉积模式—以松辽盆地北部葡萄花油层为例.岩性油气藏. 2007,19(2): 28-34
[11]楼章华,兰翔,卢庆梅,等.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用.地质学报,1999,73(1):83-91
[12] Mcpherson J G, Shanmugam G., Moiola R J. Fan deltas and braid deltas:conceptural problems. In: Fan Deltas: Sedimentology and Tectonic Setting (Eds by W.Nemec and R.J.Steel). Blackie and Son. London. 1988,14-22p
[13] Gareth T G. Characterisation 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, Marine and Petroleum Geology,2000, 17:445-475
[14]杨东明,姜在兴,李葵英,等.济阳坳陷馆陶组辫状三角洲—浅水湖泊沉积体系.西安石油大学学报(自然科学版),2004,19(6):15-19
[15]朱筱敏,张义娜,杨俊生,等.准噶尔盆地侏罗系辫状河三角洲沉积特征.石油与天然气地质,2008,29(2):244-251
[16]高志勇,郭宏莉,张水昌.满加尔凹陷南缘志留系柯坪塔格组上段不同体系域内辫状三角洲砂体与储集性研究.中国地质,2008,35(5):951-962
[17] Stanistreet I G, McCarthy T S. The Okavango Fan and the classification of subaerial fan systems. Sedimentary Geology, 1993, 85(1):115-133
[18]李国斌,姜在兴,陈诗望,等.利津洼陷沙四上亚段滩坝沉积特征及控制因素分析.中国地质,2008,35(5):911-921
[19]邓宏文,马立祥,姜正龙,等.车镇凹陷大王北地区沙二段滩坝成因类型、分布规律与控制因素研究.沉积学报,2008,26(5):715-724
[20]杨西燕,沈昭国,方少仙,等.鄂尔多斯盆地乌审旗气田中二叠统下石盒子组盒8段下亚段滩坝砂体沉积特征.古地理学报,2007,9(2):175-183
[21] Mukerji A B. Terminal fans of inland streams in Sutlej-Yamuna Plain, India. Zeitschrift fur Geomorphologie, 1976,20: 190-204
[22] Mukerji A B. Geomorphic patterns and processes in the terminal tract of inland streams in Sutlej-Yamuna plain.Journal of the Geological Society of India, 1975,16: 450-459
[23] Friend P F. Distinctive features of some ancient river systems. In: Miall, A.D. (Ed.), Fluvial,1978
[24] Parkash B, Awasthi A K, Gohain K. Lithofacies of the Markanda terminal fan, Kurukshetra district, Haryana, India. In: Collinson J.D., Lewin J. (eds) Modern and ancient fluvial systems.International Association of Sedimentologists special publication, 1983,6: 337-374
[25] Kelly S B, Olsen H. Terminal fans-a review with reference to Devonian examples. Sedimentary Geology, 1993,85: 339-374
[26]张金亮,戴朝强,张晓华.末端扇-一种新的沉积作用类型.地质论评,2007,53(2):170-179
[27]王永春.松辽盆地南部岩性油藏的形成和分布.北京:石油工业出版社,2001.2-80
[28]张庆国,鲍志东,那未红,等.松辽盆地中央坳陷南部下白垩统泉头组四段沉积相.古地理学报,2007,9(3):267-276
[29]邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布.地质学报,2008,82(6):813-825
[30]陈少军,董清水,宋立忠,等.松辽盆地南部泉四段沉积体系再认识.大庆石油地质与开发,2006,25(6):4-8
[31]李树青,李和,徐伟,等.松辽盆地南部下白垩统层序构型及沉积特征.天然气工业,2007,27(4):36-39
[32]张大伟,贾庆素.大情字井地区青一段沉积微相分布特征.断块油气田,2006,13(6):1-3
[33]单玄龙,胡金祥,任利军,等.松辽盆地乾安地区青山口组三段沉积微相特征.地质学报,2008,82(1):65-71
[34]王衡鉴,曹文富.松辽湖盆白垩纪沉积相模式.石油与天然气地质,1981,2(3):227-241
[35]王衡鉴,曹文富.松辽盆地白垩纪湖泊三角洲沉积.大庆石油地质与开发,1983,2(2):92-100
[36]王永春,康伟力,毛超林.吉林探区油气勘探理论与实践.北京:石油工业出版社,2007.3-89
[37]任以发,赵晓华,田培进,等.松南盆地长岭凹陷腰英台区块断裂构造及储层特征.天然气地球科学,2005,16(2):206-209
[38]綦敦科.临江地区扶杨油层有利储层研究及油气富集区预测:[博士学位论文].武汉:中国地质大学,2005
[39]毛超林.松辽盆地南部长岭凹陷高台子油层三角洲前缘砂体储层特征评价:[博士学位论文].武汉:中国地质大学,2006
[40]徐晓东.腰英台地区青山口组储层孔隙结构与成岩作用研究:[硕士学位论文].西安:西北大学,2007
[41]赵占银,李洪革,王兴光,等.松辽盆地南部中浅层成藏机制研究.石油勘探与开发,2004,31(6):17-19
[42]刘宝柱,孙万军,陈少军,等.松辽盆地南部中浅层油气藏的成藏史.现代地质,2003,17(1):87-91
[43]唐振兴,苗洪波,王立武,等.松辽盆地中浅层油气运移机理.石油天然气学报,2005,27(5):690-693
[44]唐振兴,苗洪波,李爱民,等.松辽盆地南部嫩江组—泉四段油气运移特征.大庆石油地质与开发,2007,26(6):40-46
[45]李国玉,吕鸣岗,等.中国含油气盆地图集.北京:石油工业出版社,2002.25-27
[46]刘鸿友,苗洪波,陈文龙,等.松辽盆地南部中浅层资源潜力.中国石油勘探,2003,8(3):13-17,49
[47]沈安江,康伟力.松辽盆地南部白垩纪层序地层与岩性地层油气藏勘探.北京:石油工业出版社,2006.4-131
[48]孙振城,杨藩.中国新生代咸化湖泊沉积环境与油气生成.北京:石油工业出版社,1997.193-203
[49]黎彤.化学元素的地球丰度.地球化学,1976,(3):167-174
[50]王中刚,于学元,赵振华,等.稀土元素地球化学.北京:科学出版社,1989.20-535
[51] Murry R W. Chemical criteria to identify the depositional environment of chert:general principles and applications. Sedimentary Geology,1994,90(3-4):213-232
[52]张金亮,张鑫.塔中地区志留系砂岩元素地球化学特征与物源判别意义.岩石学报,2007,23(11):2990-3002
[53]张鑫,张金亮.东营凹陷南坡沙河街组四段砂岩地球化学特征.地质科学,2007,42(2):303-318
[54] Zhang Jinliang, Zhang Xin. Composition and Provenance of Sandstones and Siltstones in Paleogene, Huimin Depression, Bohai Bay Basin, Eastern China. Journal of China University of Geosciences, 2008,19(3):252-270
[55] Henderson P. Rare Earth Element Geochemistry. Amsterdam: Elsevier,1984.343-374
[56]赵澄林,朱筱敏.沉积岩石学.北京:石油工业出版社,2001.91-92
[57]张学才.东营凹陷南坡沙四段沉积相与油气分布.北京:石油工业出版社,2008.49-60
[58]刘宝珺.沉积岩石学.北京:地质出版社,1980.
[59]张金亮,常象春.石油地质学.北京:石油工业出版社,2004.68-75
[60]张金亮,谢俊. 2008.储层沉积相.北京:石油工业出版社,55-173
[61] Galloway W E, Hobday D K. Terrigenous clastic depositional systems-Application to petroleum. Coal, and Uranium Exploration. Springer. New York,1983
[62]王良忱,张金亮.沉积环境和沉积相.北京:石油工业出版社,1996.26-27
[63] Newell A J, Tverdokhlebov V P, Benton M J. Interplay of tectonics and climate on a transverse fluvial system, Upper Permian, Southern Uralian Foreland Basin, Russia. Sedimentary Geology, 1999,127:11-29
[64] Talbot M R, Holm K, Williams M A J. Sedimentation in low-gradient desert margin systems: a comparison of the Late Triassic of northwest Somerset, England, and the late Quaternary of east-central Australia. Geol. Soc. Am. Spec. Pap. 1994,289: 97-117
[65] Tunbridge I P. Facies model for a sandy ephemeral stream and clay playa complex; the Middle Devonian Trentishoe Formation of North Devon, UK. Sedimentology, 1984,31: 697-715
[66]张金亮,李恕军,靳文奇.安塞油田侯市地区长6油层沉积微相研究.西安石油学院学报,2000,15(4):1-7
[67] Friend P F. Distinctive features of some ancient river systems. In: Miall, A.D. (Ed.), Fluvial,1978
[68] Schumm S A. The fluvial system, John Wiley & Sons, NewYork, 1977,338p
[69] Schumm S A. Variability of the fluvial system in space and time. In: Rosswall T., Woodmansee R.G., Risser P.G. (Eds.), Scales and Global change. Wiley, New York, 1988, 225-250
[70] McGowen J H, Groat G G. Van Horn Sandstone, West Taxas: an alluvial fan model for mineral exploration. Report of Investigations, Bureau of Economic Geology, Univ. of Texas, Austin,1971
[71]贺君玲,邓守伟,陈文龙,等.利用测井技术评价松辽盆地南部油页岩.吉林大学学报(地球科学版),2006,36(6): 909-914
[72] Peters K E,Moldowan J M. The Biomarker Guide: Interpreting Molecular Fossils in Petroleum and Ancient Sediments. Englewood Cliffs (NJ) : Prentice Hall, 1993
[73] Irwin H,Meyer T. Lacustrine Organic Facies: A Biomarker Study Using Multivariate Statistical Analysis. Org. Geochem, 1990, 16 (1 - 3) : 197-210
[74]张厚福,方朝亮,张枝焕,等.石油地质学.北京:石油工业出版社,1999
[75]毛凤鸣,张金亮,许正龙.高邮凹陷油气成藏地球化学.北京:石油工业出版社,2002,132-142
[76]黄志龙,高岗.松辽盆地南部海坨子地区油气成藏研究.石油大学学报,2003,27(1):4-7
[77]陈荷立.油气运移研究的有效途径.石油与天然气地质, 1995, 16 (2) : 126 -131
[78]徐田武,曾溅辉,魏刚,等.辽东湾地区油气运移输导体系特征及意义.西南石油大学学报(自然科学版),2008, 30 (5) : 69-72
[79]李明诚.对油气运聚研究中一些概念的再思考.石油勘探与开发, 2000, 29 (2) : 13 - 16
[80]柳广弟,郑玉凌.油气成藏动力场模型及其应用.石油勘探与开发, 2000, 27 (2) : 11 - 14
[81]雷茂盛,蔡利学,等.松辽盆地敖古拉断裂对油气运移的控制作用.勘探家,1999,13(3):24-26
[82]胡望水.松辽盆地“青一段底界面”断层系及青山口早期伸展裂陷.石油勘探与开发,1995,22(2):8-12
[83]张建林.地层不整合对油气运移和封堵的作用.油气地质与采收率,2005,12 (2) :26-29
[84]吕修祥,周新源,李建交,等.塔里木盆地塔北隆起碳酸盐岩油气成藏特点.地质学报,2007,81 (8) :1057-1063
[85]刘宝柱,孙万军,陈少军等.松辽盆地南部中浅层油气藏的成藏史.现代地质,2003,17(1):87-91
[86]吴亚东,赵文智,邹才能,等.松辽盆地南部岩性—地层油气藏成藏规律.新疆石油地质,2006,27(1):19-22
[87]关德师,李建忠.松辽盆地南部岩性油藏成藏要素及勘探方向.石油学报,2003,24(3):24-27
[88]张金亮,常象春.深盆地地质理论及应用.北京:地质出版社,2002. 3-45
[89] Cant D J. Spirit River Formation a stratigraphic diagenetic gas trap in t he deep basin of Alberta. AAPG Bull. , 1983,67 (4) :577-587
[90] Gies R M. Gas history for a major Alberta deep basin trap the Cadomin Formation. AAPG Memoir, 1984,38 :15-140
[91] Law B E, Dickinson W W. Conceptual model or origin of Abnormally pressured gas accumulation in low permeability reservoirs. AAPG Bull . , 1985,69 (8) : 1295-1304
[92] Rice D D. Nonassociated gas potential of San Juan basin considerable. Oil & Gas Journal ,1991,88 (2) :60-61
[93]侯启军,魏兆胜,赵占银,等.松辽盆地的深盆油藏.石油勘探与开发,2006,33(4):406-411
[2] Schumm S A. The fluvial system, John Wiley & Sons, NewYork,1977, 338p
[3]钱宁,张仁,周志德.河床演变学.北京:科学出版社,1987.2-51
[4]钱宁.关于河流分类及成因问题的讨论.地理学报,1995,40(1):1-10
[5]王随继,任明达.根据河道形态和沉积物特征的河流新分类.沉积学报,1999,17(2):240-246
[6] Allen J R L. Late Quaternary Niger Delta and adjacent areas: sedimentary environments and lithofacies. AAPG. Bull., 1965,49: 547-600
[7] Coleman J M, Wright L D. Modem river deltas: variability of process and sand bodies. In: BROUSSARD, M.L. (ed.) Deltas: Models for Exploration. Houston Geological Society, Houston, TX, 1975,99-150
[8] Coleman J M. Dynamic changes and processes in the Mississippi River delta. Geol. Soc. Am. Bull. 1988,100: 999-1015
[9] Edwards M B. Upper Wilcox Rosita delta system of South Texas. Growth-faulted shelf-edge deltas. AAPG Bull., 1981,65: 54-73
[10]王建功,王天琦,卫平生,等.大型坳陷湖盆浅水三角洲沉积模式—以松辽盆地北部葡萄花油层为例.岩性油气藏. 2007,19(2): 28-34
[11]楼章华,兰翔,卢庆梅,等.地形、气候与湖面波动对浅水三角洲沉积环境的控制作用.地质学报,1999,73(1):83-91
[12] Mcpherson J G, Shanmugam G., Moiola R J. Fan deltas and braid deltas:conceptural problems. In: Fan Deltas: Sedimentology and Tectonic Setting (Eds by W.Nemec and R.J.Steel). Blackie and Son. London. 1988,14-22p
[13] Gareth T G. Characterisation 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, Marine and Petroleum Geology,2000, 17:445-475
[14]杨东明,姜在兴,李葵英,等.济阳坳陷馆陶组辫状三角洲—浅水湖泊沉积体系.西安石油大学学报(自然科学版),2004,19(6):15-19
[15]朱筱敏,张义娜,杨俊生,等.准噶尔盆地侏罗系辫状河三角洲沉积特征.石油与天然气地质,2008,29(2):244-251
[16]高志勇,郭宏莉,张水昌.满加尔凹陷南缘志留系柯坪塔格组上段不同体系域内辫状三角洲砂体与储集性研究.中国地质,2008,35(5):951-962
[17] Stanistreet I G, McCarthy T S. The Okavango Fan and the classification of subaerial fan systems. Sedimentary Geology, 1993, 85(1):115-133
[18]李国斌,姜在兴,陈诗望,等.利津洼陷沙四上亚段滩坝沉积特征及控制因素分析.中国地质,2008,35(5):911-921
[19]邓宏文,马立祥,姜正龙,等.车镇凹陷大王北地区沙二段滩坝成因类型、分布规律与控制因素研究.沉积学报,2008,26(5):715-724
[20]杨西燕,沈昭国,方少仙,等.鄂尔多斯盆地乌审旗气田中二叠统下石盒子组盒8段下亚段滩坝砂体沉积特征.古地理学报,2007,9(2):175-183
[21] Mukerji A B. Terminal fans of inland streams in Sutlej-Yamuna Plain, India. Zeitschrift fur Geomorphologie, 1976,20: 190-204
[22] Mukerji A B. Geomorphic patterns and processes in the terminal tract of inland streams in Sutlej-Yamuna plain.Journal of the Geological Society of India, 1975,16: 450-459
[23] Friend P F. Distinctive features of some ancient river systems. In: Miall, A.D. (Ed.), Fluvial,1978
[24] Parkash B, Awasthi A K, Gohain K. Lithofacies of the Markanda terminal fan, Kurukshetra district, Haryana, India. In: Collinson J.D., Lewin J. (eds) Modern and ancient fluvial systems.International Association of Sedimentologists special publication, 1983,6: 337-374
[25] Kelly S B, Olsen H. Terminal fans-a review with reference to Devonian examples. Sedimentary Geology, 1993,85: 339-374
[26]张金亮,戴朝强,张晓华.末端扇-一种新的沉积作用类型.地质论评,2007,53(2):170-179
[27]王永春.松辽盆地南部岩性油藏的形成和分布.北京:石油工业出版社,2001.2-80
[28]张庆国,鲍志东,那未红,等.松辽盆地中央坳陷南部下白垩统泉头组四段沉积相.古地理学报,2007,9(3):267-276
[29]邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布.地质学报,2008,82(6):813-825
[30]陈少军,董清水,宋立忠,等.松辽盆地南部泉四段沉积体系再认识.大庆石油地质与开发,2006,25(6):4-8
[31]李树青,李和,徐伟,等.松辽盆地南部下白垩统层序构型及沉积特征.天然气工业,2007,27(4):36-39
[32]张大伟,贾庆素.大情字井地区青一段沉积微相分布特征.断块油气田,2006,13(6):1-3
[33]单玄龙,胡金祥,任利军,等.松辽盆地乾安地区青山口组三段沉积微相特征.地质学报,2008,82(1):65-71
[34]王衡鉴,曹文富.松辽湖盆白垩纪沉积相模式.石油与天然气地质,1981,2(3):227-241
[35]王衡鉴,曹文富.松辽盆地白垩纪湖泊三角洲沉积.大庆石油地质与开发,1983,2(2):92-100
[36]王永春,康伟力,毛超林.吉林探区油气勘探理论与实践.北京:石油工业出版社,2007.3-89
[37]任以发,赵晓华,田培进,等.松南盆地长岭凹陷腰英台区块断裂构造及储层特征.天然气地球科学,2005,16(2):206-209
[38]綦敦科.临江地区扶杨油层有利储层研究及油气富集区预测:[博士学位论文].武汉:中国地质大学,2005
[39]毛超林.松辽盆地南部长岭凹陷高台子油层三角洲前缘砂体储层特征评价:[博士学位论文].武汉:中国地质大学,2006
[40]徐晓东.腰英台地区青山口组储层孔隙结构与成岩作用研究:[硕士学位论文].西安:西北大学,2007
[41]赵占银,李洪革,王兴光,等.松辽盆地南部中浅层成藏机制研究.石油勘探与开发,2004,31(6):17-19
[42]刘宝柱,孙万军,陈少军,等.松辽盆地南部中浅层油气藏的成藏史.现代地质,2003,17(1):87-91
[43]唐振兴,苗洪波,王立武,等.松辽盆地中浅层油气运移机理.石油天然气学报,2005,27(5):690-693
[44]唐振兴,苗洪波,李爱民,等.松辽盆地南部嫩江组—泉四段油气运移特征.大庆石油地质与开发,2007,26(6):40-46
[45]李国玉,吕鸣岗,等.中国含油气盆地图集.北京:石油工业出版社,2002.25-27
[46]刘鸿友,苗洪波,陈文龙,等.松辽盆地南部中浅层资源潜力.中国石油勘探,2003,8(3):13-17,49
[47]沈安江,康伟力.松辽盆地南部白垩纪层序地层与岩性地层油气藏勘探.北京:石油工业出版社,2006.4-131
[48]孙振城,杨藩.中国新生代咸化湖泊沉积环境与油气生成.北京:石油工业出版社,1997.193-203
[49]黎彤.化学元素的地球丰度.地球化学,1976,(3):167-174
[50]王中刚,于学元,赵振华,等.稀土元素地球化学.北京:科学出版社,1989.20-535
[51] Murry R W. Chemical criteria to identify the depositional environment of chert:general principles and applications. Sedimentary Geology,1994,90(3-4):213-232
[52]张金亮,张鑫.塔中地区志留系砂岩元素地球化学特征与物源判别意义.岩石学报,2007,23(11):2990-3002
[53]张鑫,张金亮.东营凹陷南坡沙河街组四段砂岩地球化学特征.地质科学,2007,42(2):303-318
[54] Zhang Jinliang, Zhang Xin. Composition and Provenance of Sandstones and Siltstones in Paleogene, Huimin Depression, Bohai Bay Basin, Eastern China. Journal of China University of Geosciences, 2008,19(3):252-270
[55] Henderson P. Rare Earth Element Geochemistry. Amsterdam: Elsevier,1984.343-374
[56]赵澄林,朱筱敏.沉积岩石学.北京:石油工业出版社,2001.91-92
[57]张学才.东营凹陷南坡沙四段沉积相与油气分布.北京:石油工业出版社,2008.49-60
[58]刘宝珺.沉积岩石学.北京:地质出版社,1980.
[59]张金亮,常象春.石油地质学.北京:石油工业出版社,2004.68-75
[60]张金亮,谢俊. 2008.储层沉积相.北京:石油工业出版社,55-173
[61] Galloway W E, Hobday D K. Terrigenous clastic depositional systems-Application to petroleum. Coal, and Uranium Exploration. Springer. New York,1983
[62]王良忱,张金亮.沉积环境和沉积相.北京:石油工业出版社,1996.26-27
[63] Newell A J, Tverdokhlebov V P, Benton M J. Interplay of tectonics and climate on a transverse fluvial system, Upper Permian, Southern Uralian Foreland Basin, Russia. Sedimentary Geology, 1999,127:11-29
[64] Talbot M R, Holm K, Williams M A J. Sedimentation in low-gradient desert margin systems: a comparison of the Late Triassic of northwest Somerset, England, and the late Quaternary of east-central Australia. Geol. Soc. Am. Spec. Pap. 1994,289: 97-117
[65] Tunbridge I P. Facies model for a sandy ephemeral stream and clay playa complex; the Middle Devonian Trentishoe Formation of North Devon, UK. Sedimentology, 1984,31: 697-715
[66]张金亮,李恕军,靳文奇.安塞油田侯市地区长6油层沉积微相研究.西安石油学院学报,2000,15(4):1-7
[67] Friend P F. Distinctive features of some ancient river systems. In: Miall, A.D. (Ed.), Fluvial,1978
[68] Schumm S A. The fluvial system, John Wiley & Sons, NewYork, 1977,338p
[69] Schumm S A. Variability of the fluvial system in space and time. In: Rosswall T., Woodmansee R.G., Risser P.G. (Eds.), Scales and Global change. Wiley, New York, 1988, 225-250
[70] McGowen J H, Groat G G. Van Horn Sandstone, West Taxas: an alluvial fan model for mineral exploration. Report of Investigations, Bureau of Economic Geology, Univ. of Texas, Austin,1971
[71]贺君玲,邓守伟,陈文龙,等.利用测井技术评价松辽盆地南部油页岩.吉林大学学报(地球科学版),2006,36(6): 909-914
[72] Peters K E,Moldowan J M. The Biomarker Guide: Interpreting Molecular Fossils in Petroleum and Ancient Sediments. Englewood Cliffs (NJ) : Prentice Hall, 1993
[73] Irwin H,Meyer T. Lacustrine Organic Facies: A Biomarker Study Using Multivariate Statistical Analysis. Org. Geochem, 1990, 16 (1 - 3) : 197-210
[74]张厚福,方朝亮,张枝焕,等.石油地质学.北京:石油工业出版社,1999
[75]毛凤鸣,张金亮,许正龙.高邮凹陷油气成藏地球化学.北京:石油工业出版社,2002,132-142
[76]黄志龙,高岗.松辽盆地南部海坨子地区油气成藏研究.石油大学学报,2003,27(1):4-7
[77]陈荷立.油气运移研究的有效途径.石油与天然气地质, 1995, 16 (2) : 126 -131
[78]徐田武,曾溅辉,魏刚,等.辽东湾地区油气运移输导体系特征及意义.西南石油大学学报(自然科学版),2008, 30 (5) : 69-72
[79]李明诚.对油气运聚研究中一些概念的再思考.石油勘探与开发, 2000, 29 (2) : 13 - 16
[80]柳广弟,郑玉凌.油气成藏动力场模型及其应用.石油勘探与开发, 2000, 27 (2) : 11 - 14
[81]雷茂盛,蔡利学,等.松辽盆地敖古拉断裂对油气运移的控制作用.勘探家,1999,13(3):24-26
[82]胡望水.松辽盆地“青一段底界面”断层系及青山口早期伸展裂陷.石油勘探与开发,1995,22(2):8-12
[83]张建林.地层不整合对油气运移和封堵的作用.油气地质与采收率,2005,12 (2) :26-29
[84]吕修祥,周新源,李建交,等.塔里木盆地塔北隆起碳酸盐岩油气成藏特点.地质学报,2007,81 (8) :1057-1063
[85]刘宝柱,孙万军,陈少军等.松辽盆地南部中浅层油气藏的成藏史.现代地质,2003,17(1):87-91
[86]吴亚东,赵文智,邹才能,等.松辽盆地南部岩性—地层油气藏成藏规律.新疆石油地质,2006,27(1):19-22
[87]关德师,李建忠.松辽盆地南部岩性油藏成藏要素及勘探方向.石油学报,2003,24(3):24-27
[88]张金亮,常象春.深盆地地质理论及应用.北京:地质出版社,2002. 3-45
[89] Cant D J. Spirit River Formation a stratigraphic diagenetic gas trap in t he deep basin of Alberta. AAPG Bull. , 1983,67 (4) :577-587
[90] Gies R M. Gas history for a major Alberta deep basin trap the Cadomin Formation. AAPG Memoir, 1984,38 :15-140
[91] Law B E, Dickinson W W. Conceptual model or origin of Abnormally pressured gas accumulation in low permeability reservoirs. AAPG Bull . , 1985,69 (8) : 1295-1304
[92] Rice D D. Nonassociated gas potential of San Juan basin considerable. Oil & Gas Journal ,1991,88 (2) :60-61
[93]侯启军,魏兆胜,赵占银,等.松辽盆地的深盆油藏.石油勘探与开发,2006,33(4):406-411
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |