辽河坳陷东部凹陷沙三段沉积储层特征与油气关系
|
摘要
东部凹陷沙三期(始新世中晚期)为裂谷发育的断陷期,断裂发育,构造条带狭窄,沉积作用与火山作用交互发生,砂岩与火成岩纵横交错,具有复杂而特殊的石油地质条件,并且沉积、储层缺乏系统地研究,制约了油气勘探。本文以沉积学、岩石学、储层地质学、石油地质学的新理论和新方法作指导,在沙三段沉积、储层整体研究的基础上,针对地区特点,开展沉积、储层特征及油气关系研究,构建沉积模式和火成岩发育模式,指出有利储层的分布区,提出勘探目标。构造演化控制了沉积演化及岩浆喷发,进而控制了储层的发育。本区主要物源为两侧的凸起,具近物源、多物源、物源交叉重叠等特征;火成岩体的存在可改变物源走向。
通过大量沉积相标志的研究,建立了冲积扇、扇三角洲、三角洲、河流及浊流的相模式,确定优势沉积相带和优势储层发育区。研究认为沙三下亚段发育冲积扇-辫状河-冲积平原沉积体系,沙三中亚段发育冲积扇-扇三角洲-湖泊沉积体系,沙三上亚段北段发育冲积扇-辫状河三角洲-湖泊沉积体系,南段发育冲积扇-河流-三角洲-湖泊沉积体系,明确了各沉积相带的平面展布特征,沙三下、中、上亚段的砂砾岩体、浊积体、河道及滩坝砂体,是油气藏勘探的有利地区。
砂岩储层分布和物性受沉积相、成岩作用和成岩相等综合控制;碎屑岩与火成岩储层交互发育,可减弱火成岩下伏砂岩的成岩作用,提高储集性能;砂岩储层综合评价为低孔-低渗储层。沙三上亚段储层主要处于中成岩A_1期,以溶蚀成岩相、溶蚀及部分再胶结成岩相为主,次生孔隙较发育,储集性能较好,多为Ⅱ类储层。火成岩储层主要为粗面岩(热河台-黄沙坨地区)、辉绿岩(驾掌寺、青龙台地区)、安山岩(大平房地区)、玄武岩、火山角砾岩(红星地区)和凝灰岩等。火成岩储层受埋深影响较小,将是中深层勘探的重要目标。除火山沉积相和边缘相带外,爆发相、溢流相、次火山岩相均为有利储集相带。综合考虑岩相、物性、产能、裂缝发育程度等因素,综合岩性、岩相、裂缝、测井储层预测、地震储层预测的结果,将火成岩储层分为Ⅰ、Ⅱ、Ⅲ、Ⅳ类。控制火成岩成藏因素主要有:油气输导条件、裂缝发育程度、有利岩相带等。
论文在沉积模式建立、沉积作用与火山作用的关系、两类储层发育与油气的关系研究等方面取得了新认识。研究成果对今后的油气勘探具有一定的应用价值。
The Es3(The middle-late Eocene) in the Eastern Depression is at a stage of rift and fracture development. The structure belt is narrow and the sedimentation occurred alternatively with volcanic action, with sandstone and igneous rock reticulated, showing complex and conspicuous petroleum geology conditions. The lack of systematic research on sedimentation and reservoir has restricted oil and gas exploration in this area. This paper applies the new theory and method of sedimentology, sequence stratigraphy, petrology, reservoir geology and petroleum geology to guide the study on the Es3 sedimentation and overall reservoir research. Sedimentation and reservoir characteristics and oil/gas relationship are studied as per regional feature; depositional pattern and igneous rock development mode are constructed; the distribution of favorable reservoir is presented; and exploration deployment suggestion is proposed.
Structural evolution had controlled magmatic exhalation and sedimentary evolution, and then controlled reservoir development. The major sources of sediment in this area are the uplifts on two sides, showing characteristics of near source, multi-source and juxtaposed source. The occurrence of igneous body can change source direction.
The study of sedimentary marker has established facies models of alluvial fan, fan delta, delta, fluvial and turbid flow, defined predominant sedimentary facies and reservoir development areas, and believed that the Es3low had developed alluvial fan - braided river-alluvial plain sedimentary system, Es3mid had developed alluvial fan - fan delta-lacustrine depositional system, Es3up North had developed alluvial fan braided river delta-lacustrine depositional system, and Es3up south had developed alluvial fan-river-delta-lacustrine depositional system, thus clearly defined the plane distribution of each sedimentary facies. The glutinite,turbidite, stream channel and point bar sand bodies are favorable hydrocarbon exploration area.
Sandstone reservoir distribution and physical property were controlled by sedimentary facies, diagenesis and lithogenous phase, etc;reservoirs of clastic rock and igneous rock had developed alternatively, which can attenuate the diagenesis of the sandstone underlying igneous rock and enhance reservoir property; the sandstone reservoir is comprehensively evaluated as low porosity-low permeability reservoir. The Es3up reservoir is mainly in the medium diagenesis stage of A_1, dominated by solutional diagenetic phase, solutional and partial recementing diagenetic phase, induced porosity was developed, reservoir property is good, mostly belonging to ClassⅡreservoir.
The igneous rock reservoirs mainly include trachyte (Rehetai-Huangshatuo area), diabase (Jiazhangsi, Qinglongtai areas), andesite (Dapingfang area), basalt, volcanic breccia (Hongxing area) and tuff, etc. Igneous rock reservoir is less affected by depth of burial and will be essential target of mid-depth exploration. Except volcanogenic and marginal facies, all the explosive facies, overflow facies and subvolcanic facies are favorable reservoir zones. Igneous rock reservoirs are classified into Class I, II, III and IV based on comprehensive consideration of lithofacies, physical property, deliverability, fissures development degree and other factors by integrating the results of lithology, lithofacies, fissures, well logging reservoir and seismic reservoir prediction. The control factors of hydrocarbon accumulation in igneous rock reservoir mainly include oil/gas conduction conditions, fissures development degree, and favorable facies,etc .
This paper has achieved new cognitions in respects of depositional pattern construction, the relationship of sedimentation and volcanic action, two-type reservoir development and oil/gas relationship research. The research findings are of certain application value to future oil and gas exploration.
通过大量沉积相标志的研究,建立了冲积扇、扇三角洲、三角洲、河流及浊流的相模式,确定优势沉积相带和优势储层发育区。研究认为沙三下亚段发育冲积扇-辫状河-冲积平原沉积体系,沙三中亚段发育冲积扇-扇三角洲-湖泊沉积体系,沙三上亚段北段发育冲积扇-辫状河三角洲-湖泊沉积体系,南段发育冲积扇-河流-三角洲-湖泊沉积体系,明确了各沉积相带的平面展布特征,沙三下、中、上亚段的砂砾岩体、浊积体、河道及滩坝砂体,是油气藏勘探的有利地区。
砂岩储层分布和物性受沉积相、成岩作用和成岩相等综合控制;碎屑岩与火成岩储层交互发育,可减弱火成岩下伏砂岩的成岩作用,提高储集性能;砂岩储层综合评价为低孔-低渗储层。沙三上亚段储层主要处于中成岩A_1期,以溶蚀成岩相、溶蚀及部分再胶结成岩相为主,次生孔隙较发育,储集性能较好,多为Ⅱ类储层。火成岩储层主要为粗面岩(热河台-黄沙坨地区)、辉绿岩(驾掌寺、青龙台地区)、安山岩(大平房地区)、玄武岩、火山角砾岩(红星地区)和凝灰岩等。火成岩储层受埋深影响较小,将是中深层勘探的重要目标。除火山沉积相和边缘相带外,爆发相、溢流相、次火山岩相均为有利储集相带。综合考虑岩相、物性、产能、裂缝发育程度等因素,综合岩性、岩相、裂缝、测井储层预测、地震储层预测的结果,将火成岩储层分为Ⅰ、Ⅱ、Ⅲ、Ⅳ类。控制火成岩成藏因素主要有:油气输导条件、裂缝发育程度、有利岩相带等。
论文在沉积模式建立、沉积作用与火山作用的关系、两类储层发育与油气的关系研究等方面取得了新认识。研究成果对今后的油气勘探具有一定的应用价值。
The Es3(The middle-late Eocene) in the Eastern Depression is at a stage of rift and fracture development. The structure belt is narrow and the sedimentation occurred alternatively with volcanic action, with sandstone and igneous rock reticulated, showing complex and conspicuous petroleum geology conditions. The lack of systematic research on sedimentation and reservoir has restricted oil and gas exploration in this area. This paper applies the new theory and method of sedimentology, sequence stratigraphy, petrology, reservoir geology and petroleum geology to guide the study on the Es3 sedimentation and overall reservoir research. Sedimentation and reservoir characteristics and oil/gas relationship are studied as per regional feature; depositional pattern and igneous rock development mode are constructed; the distribution of favorable reservoir is presented; and exploration deployment suggestion is proposed.
Structural evolution had controlled magmatic exhalation and sedimentary evolution, and then controlled reservoir development. The major sources of sediment in this area are the uplifts on two sides, showing characteristics of near source, multi-source and juxtaposed source. The occurrence of igneous body can change source direction.
The study of sedimentary marker has established facies models of alluvial fan, fan delta, delta, fluvial and turbid flow, defined predominant sedimentary facies and reservoir development areas, and believed that the Es3low had developed alluvial fan - braided river-alluvial plain sedimentary system, Es3mid had developed alluvial fan - fan delta-lacustrine depositional system, Es3up North had developed alluvial fan braided river delta-lacustrine depositional system, and Es3up south had developed alluvial fan-river-delta-lacustrine depositional system, thus clearly defined the plane distribution of each sedimentary facies. The glutinite,turbidite, stream channel and point bar sand bodies are favorable hydrocarbon exploration area.
Sandstone reservoir distribution and physical property were controlled by sedimentary facies, diagenesis and lithogenous phase, etc;reservoirs of clastic rock and igneous rock had developed alternatively, which can attenuate the diagenesis of the sandstone underlying igneous rock and enhance reservoir property; the sandstone reservoir is comprehensively evaluated as low porosity-low permeability reservoir. The Es3up reservoir is mainly in the medium diagenesis stage of A_1, dominated by solutional diagenetic phase, solutional and partial recementing diagenetic phase, induced porosity was developed, reservoir property is good, mostly belonging to ClassⅡreservoir.
The igneous rock reservoirs mainly include trachyte (Rehetai-Huangshatuo area), diabase (Jiazhangsi, Qinglongtai areas), andesite (Dapingfang area), basalt, volcanic breccia (Hongxing area) and tuff, etc. Igneous rock reservoir is less affected by depth of burial and will be essential target of mid-depth exploration. Except volcanogenic and marginal facies, all the explosive facies, overflow facies and subvolcanic facies are favorable reservoir zones. Igneous rock reservoirs are classified into Class I, II, III and IV based on comprehensive consideration of lithofacies, physical property, deliverability, fissures development degree and other factors by integrating the results of lithology, lithofacies, fissures, well logging reservoir and seismic reservoir prediction. The control factors of hydrocarbon accumulation in igneous rock reservoir mainly include oil/gas conduction conditions, fissures development degree, and favorable facies,etc .
This paper has achieved new cognitions in respects of depositional pattern construction, the relationship of sedimentation and volcanic action, two-type reservoir development and oil/gas relationship research. The research findings are of certain application value to future oil and gas exploration.
引文
[1]刘宝珺.沉积岩石学.北京:地质出版社,1979
[2]庞雯,郑浚茂.轮南地区三叠系辫状河三角洲沉积储层特征.西南石油大学学报(自然科学版),2008,30(1):58～62
[3]郑浚茂.陆源碎屑沉积环境的粒度标志(石油地质专业用).北京:武汉地质学院北京研究生部,1982
[4]郑浚茂,于兴河,谢承强,等.不同沉积环境储层的层内非均质性──以黄骅坳陷为例.现代地质,1995,9(4):501～508
[5]郑浚茂,吴仁龙.黄骅坳陷砂岩储层成岩作用与孔隙分带性,石油与天然气地质,1996,17(4):268～275
[6]于兴河,郑浚茂,宋立衡等.断陷盆地三角洲砂体的沉积作用与储层的层内非均质性特点[J].地球科学,中国地质大学学报,1997,22(1):51～56
[7]游俊,郑浚茂,周建生.深部地层异常压力与异常孔隙度及油气藏的关系.中国海上油气地质,1997,11(4):249～253
[8]于兴河.碎屑岩系油气储层沉积学.北京:石油工业出版社,2002
[9]何东博,应凤祥,郑浚茂,等.碎屑岩成岩作用数值模拟及其应用.石油勘探与开发,2004,31(6):66～68
[10]罗静兰,张晓莉,张云翔,等.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.沉积学报,2001,19(4):541～547
[11]吴胜和、熊琦华.油气储层地质学.北京:石油工业出版社,1998
[12]姚光庆,孙永传,李思田.油气储集层地质学研究体系.石油勘探与开发,2001,47(3):278～286
[13]鞠俊成,张凤莲,喻国凡,等.辽河盆地西部凹陷南部沙三段储层沉积特征及含油气性分析.古地理学报,2001,3(1):63～69
[14]邓宏文,王红亮,阎伟鹏等.河流相层序地层构成模式探讨.沉积学报,2004,22(3):373～379
[15]李丕龙等.陆相断陷盆地油气地质与勘探(卷二):陆相断陷盆地沉积体系与油气分布.北京.石油工业出版社/地质出版社,2003
[16]陆建林,王果寿,蔡进功,等.长岭断陷火山岩气藏勘探潜力.天然气工业,2007,27(8):13～15
[17]钟大康,朱筱敏,王红军.中国深层优质碎屑岩储层特征与形成机理分析.中国科学D辑,2008,38增刊:11～18
[18]舒萍,丁日新,曲延明,等.徐深气田火山岩储层岩性岩相模式.天然气工业,2008,27(8):23～27
[20]孙红军.辽河盆地东部凹陷含油气系统[D].辽河油田工作站,南京大学地质系,博士后论文,2000:15～42
[21]覃豪,李红娟,李军,等.徐深气田火山岩储层类型与主控因素研究.大庆石油地质与开发,2009,总第172期:15～18
[22]田景春,陈高武,窦伟坦,等.湖泊三角洲前缘砂体成因组合形式和分布规律-以鄂尔多斯盆地姬源白豹地区三叠系延长组为例.2004,31(6):637～640
[23]刘宝珺,韩作振,杨仁超.当代沉积学研究进展、前瞻与思考.特种油气藏,2006,13(5):1～5
[24]王国光.惠民凹陷西部古近系沙三段物源特征与沉积体系分布研究.[博士学位论文].广州:中国科学院广州地球化学研究所,2007
[25]张守仁,张遂安.松辽盆地深层断陷期地层展布特征及油气勘探意义.地学前缘,2009,16(1):335～343.
[26]姜在兴.沉积学.北京:石油工业出版社,2003
[27]张家政,赵广珍.红山嘴油田石炭系火山岩油藏综合研究.新疆石油天然气,2008,4(4):1～9
[28]姜在兴.扇三角洲高精度层序地层及其与油气聚集关系—以东营凹陷胜北断层下降盘坨76块为例.沉积与特提斯地质,2007,27(1):80～85
[29]薛叔浩,罗平,杨永泰等.辽河坳陷沉积体系与油气分布.石油勘探与开发,1997,24(4):19～22
[30]回雪峰,管守锐,张凤莲,等.辽河盆地东部凹陷中段深层沙河街组沉积相.古地理学报,2003,5(3):291～302
[31]鄢继华,陈世悦,姜在兴.三角洲前缘浊积体成因及分布规律研究.石油实验地质,2008,30(1):20～23
[32]冯有良,李思田.东营凹陷沙河街组三段层序低位域砂体沉积特征,地质论评,2001,47(3),278～286.
[33]钟大康,张崇军,文应初.砂岩储集层物性影响因素定量分析方法.石油与天然气地质,2000,21(2):130～132
[34]辽河油田石油地质志编辑委员会.辽河油田,中国石油地质志(三).北京:石油工业出版社,1993
[35]谢庆宾,朱筱敏,管守锐等.中国现代网状河流沉积特征和沉积模式.沉积学报,2003,21(20):219～227
[36]李潍莲,孙红军,唐文连.辽河盆地东部凹陷北段古近系层序地层特征及油气藏分布.石油大学学报(自然科学版),2004,28(5):1～6
[37]赵澄林,孟卫工,金春爽,等.辽河盆地东部凹陷火山岩与油气,北京:石油工业出版社,1999
[38]陈元勇,王振奇,邢成智,等.准噶尔盆地车排子地区火山岩储集层特征.断块油气田,2009,16(5):23～26
[39]陈永峤,于兴河,周新桂等.东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究.天然气地球科学,2004,15(1):68～74
[40]张金亮,司学强,梁杰等.陕甘宁盆地庆阳地区长8油层砂岩成岩作用及其对储层性质的影响,沉积学报,2004,22(2):225～233
[41]张新培,邓宏文,张吉昌,等.辽河坳陷东部凹陷欧-黄地区火山岩储集层特征及有利储层预测.石油天然气地质,2007,28(3):370～376
[42]张子枢、吴邦辉.国内外火成岩油气藏研究现状及勘探技术调研.开然气勘探与开发.1994,16(1):1～26
[43]裘亦楠、薛叔浩.油气储层评价技术.北京:石油工业出版社,2001
[44]裘亦楠.沉积方式与碎屑岩储层的层内非均质性.石油学报,1985,6(1):85～90
[45]祝彦贺,颜耀敏,王英民,等.碎屑岩与火山岩混积岩系层序地层学研究初探-以准噶尔盆地西北缘佳木河组为例.现代地质,2008,22(2):255～263
[46]张福功.辽河盆地东部凹陷中段火山岩岩性测井评价方法研究.海洋石油,2005,25(4):80～83
[47]陈昭年,陈晓巍,王明艳,等.内蒙古查干凹陷火山岩油藏成藏模式.现代地质,2008,22(4):628～632
[48]马全华.欧利坨子火山岩识别与浊积岩相模式研究.西北大学学报(自然科学版),2008,38(2):285～289
[49]张建龙,张方礼,蒋少涌,等.欧利坨子火山岩油藏原油特征及成因分析.地球学报,2007,28(4):369～376
[50]谭显春.徐深气田火山岩岩性岩相序列.天然气工业,2009,29(8):12～14
[51]徐正顺,王渝明,庞彦明,等.大庆徐深气田火山岩气藏储集层识别与评价.石油勘探与开发,2006,33(5):521～531
[52]李亚辉.高邮凹陷北斜坡辉绿岩与油气成藏,地质力学学报,2000,6(2):17～22
[53]邹才能,赵文智,贾承造,等.中国沉积盆地火山岩油气藏形成与分布.石油勘探与开发,2008,35(3):257～271
[54]赵文智,邹才能,冯志强,等.松辽盆地深层火山岩气藏地质特征及评价技术.石油勘探与开发,2008,35(2):129～142
[55]杨申谷,刘笑翠,胡志华,等.储层分析中火山岩岩性的测井识别.石油天然气学报(江汉石油学院学报),2007,29(6):33～37
[56]操应长,姜在兴,王留奇等.陆相断陷湖盆层序地层单元的划分及界面识别标志.石油大学学报(自然科学版),1996,20(4):1～5
[57]郑亚斌,王延斌,冉启全.枣35断块火山岩储层特征研究.石油学报,2006,27(4):54～58
[58]陈会军,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深层碎屑岩地层为例.石油勘探与开发,2001,28(6):28～31.
[59]陆建林,张玉明,徐宏节,等.松辽盆地长岭断陷火山岩储层形成特征研究.石油实验地质,2009,31(5):441～461
[60]张金亮,刘宝珺,毛凤鸣,等.苏北盆地高邮凹陷北斜坡阜宁组成岩作用及储层特征.石油学报,2003,24(2):43～49
[61]高山林,李学万,宋柏荣.辽河盆地欧利佗子地区火山岩储集空间特征,石油与天然气地质,2001,22(2):173～177
[62]罗静兰、邵红梅等,火山岩油气藏研究方法与勘探技术综述,石油学报,2003,24(1):31～38
[63]杨立民,邹才能,冉启全等.大港枣园油田火山岩裂缝性储层特征及其控制因素.沉积与特提斯地质,2007,27(1):86～912
[64]黄亮,彭军,周康,等,火山岩储层形成机制研究综述,特种油气藏,2009,16(1):1～5
[82] Sun Qiang,Xie Hongsen,Guo Jie,et al. Fluid inclusions in sedimentary basins generating petroleum and their application. Journal of Changchun University of Science and Technology,2000,30(1):42～45(in Chinese with English abstract)
[83] StreckerUwe,SteidtmannJR,SmithsonSB.A conceptual tectono strtigraphic model for seismic facies migration in fluvial-lacustrine extensional basin[J]. AAPG,Bull,1999,83(23):43～61
[84] Reynolds A D.Dimensions of paralic sandstone bodies.AAPG,Bull,1999,83(3):211～229
[85] Sruoga P,Rubinstein N. Processes controlling porosity and peimeability in volcanic reservoirs from the Austral and Neuquen basins,Argentina. AAPG Bull,2007,91(1):115～129
[86] Alan M,Salam S,Morad S, et al. Diagenesis and reservoir-quality evolution of fluvial sandstones during progressive burial and uplift: evidence from the Upper Jurassic Boipeba Member,Reconcavo basin, northeastern Brazil.AAPG Bulletin, 2000,84(7):1015～1040
[87] Luo J L,Morad S,Zhang X L. Reconstruction of the diagenesis of the fluvial-lacustrine-deltaic sandstones and its influence on the reservoir quality evolution. Science in China (Series D),2002,45(7):616～625
[88] Oelkers E H,Bjorkum P A, Murphy W m. A petrographic and computational investigation of quartz cemetation and porosity reduction in North Sea sandstones. American Journal of Science,1996,296: 420～452
[89] Michael L. Sweet and Larry T. Sumpter,Genesis field,Gulf of Mexico: Recognizing reservoir compartments on geologic and production time scales in deep-water reservoirs,AAPG Bulletin, Dec 2007,91: 1701～1729
[90] Haldorson HH,et al.Challenges in reservoir characterization .AAPG,1993,77(4):541～551
[91] Miall A D. Architectural elements and bounding surface in fluvial deposits: anatomy of the Kayente formation(lower Jurassic),southwest clorado.Sedimentary Geology.1988,55:233～262
[92]Stenen M Colman. Water-level changes in Lake Baikal, Siberia:Tectonic versusclimate.Geology,1998,26(6): 531～534
[93] Seemann U,Schere M. Volcaniclastics as potential hydrocarbon reservoirs. Clay Minerals,1984,19(9):457～470
[94] Vemik Lev. A new type reservoir rock in volcaniclastic sequences. AAPG Bulgy 1990,74( 6):830～836
[95] Hawland erHM. Diagenesis and reservoir potential of vol-canogenic sandstones-Cretaceous of the Surat Basin Australia.Sedimentary Geology,1990,66(3/4):181～195
[96] R L Gawthorpe, M R Leedert. Tectono-sedimentary evolution of active extensional basins.Basin Research,2000,12: 195～218
[97] Ramon,J.Cand Cross,T.A.Characterization and prediction of reservoir architecture and petrophysical properties in fluvial channel sandstones, Middle Magdalena Basin, Colombia:Ciencia, Tecnologia y Futuro,1997, v.1,no.3,p.19～46
[98] Perrin M,Plenier G,Dautria J M,et al.Rotation Of The Semail Ophiolite (Oman): Additional Paleomagnetic Data From The Volcanic Sequence,Mar Geophys Res V 21, Nos 3～4,2000,181～194
[99] De Carlo E H,Carmody R,Lackschewitz K K. Alteration Of Volcanic Matter In Sediments Of The Woodlark Basin,Abstr With Programs (Gsa) ,2001,33(6):234
[100] Blickwede J F,The Nazas Formation:A Detailed Look At The Early Mesozoic Convergent Margin Along The Western Rim Of The Gulf Of Mexico Basin,The Western Gulf Of Mexico Basin Tectonics,Sedimentary Basins,And Petroleum Systems [Aapg Mem No 75],The American Association Of Petroleum Geologists,2001,317～342
[101] Compston W. Effect Of Pb Loss On The Ages Of Reference Zircons Qgng And Sl13,And Of Volcanic Zircons From The Early Devonian Merrions And Turondale Formations,New South Wales,Australian J Earth Sci,2001,48(6):797～803
[102] Liu Z Y,Xiao S B,Jiang Z X. Volcanic Rocks Of Bohai Bay Basin In Tertiary And Their Genesis,J Univ Petrol,2001,China 25(1):22～26
[103] Jin Q.Volcanic Activities And Oil/Gas Accumulation In The Rift Basins Of Eastern China,J Univ Petrol,2001,China 25(1),27～33
[104] Sruoga P,RuSinstein N. Proccsscs controlling porosity and permeability in volcanic rescrvoirs from the Austral and Neuquen basins,Argentina.AAPG Bull, 2007,91(1):115～129
[105] Dutkiewicz A,Volk H,Ridlcy J. Geochemistry of oil in fluid inclusions in a middle Protcrozoic igncous intrusion implications for the sourced of hydrocarbons in crystallinc rocks.Organic Geochem istry 2004,35(8):937～957
[106] Lee A M,Hulen J B. Oil and igneous intrusions in Nevada. AAPG,1990,74(8):1313
[107]Stephen R. Occurrences of hydrocarbons in and around igneous rocks. Geol. Soc. Lon. Spec. Pub. 2003,214( 1):35～68
[108] Kawamoto T. Distribution and alteration of the volcanic reservoir in the Minami-Nagaoka gas field. Japan. Ass. Petroleum Tech. 2001,66( 1):46～55
[109] YuliMitsuhata,KoichiMatsuo,MatatoMinegishi. Magnetotelluric survey for exploration of a volcanic rock rescrvoir in the Yurihara oiland gas ficld,Japan. Geophysical Prospecing 1999,47(2):195～218
[110] Alvar Braathen1,Jan Tveranger,Haakon Fossen,et al.Fault facies and its application to sandstone reservoirs.AAPG Bulletin,2009,93(7):891～917;
[111] Anna Berger,Susanne Gier and Peter Krois. Porosity-preserving chlorite cements in shallow-marine volcaniclastic sandstones:Evidence from Cretaceous sandstones of the Sawan gas field,Pakistan.AAPG Bulletin,2009,93(5),595～615
[2]庞雯,郑浚茂.轮南地区三叠系辫状河三角洲沉积储层特征.西南石油大学学报(自然科学版),2008,30(1):58～62
[3]郑浚茂.陆源碎屑沉积环境的粒度标志(石油地质专业用).北京:武汉地质学院北京研究生部,1982
[4]郑浚茂,于兴河,谢承强,等.不同沉积环境储层的层内非均质性──以黄骅坳陷为例.现代地质,1995,9(4):501～508
[5]郑浚茂,吴仁龙.黄骅坳陷砂岩储层成岩作用与孔隙分带性,石油与天然气地质,1996,17(4):268～275
[6]于兴河,郑浚茂,宋立衡等.断陷盆地三角洲砂体的沉积作用与储层的层内非均质性特点[J].地球科学,中国地质大学学报,1997,22(1):51～56
[7]游俊,郑浚茂,周建生.深部地层异常压力与异常孔隙度及油气藏的关系.中国海上油气地质,1997,11(4):249～253
[8]于兴河.碎屑岩系油气储层沉积学.北京:石油工业出版社,2002
[9]何东博,应凤祥,郑浚茂,等.碎屑岩成岩作用数值模拟及其应用.石油勘探与开发,2004,31(6):66～68
[10]罗静兰,张晓莉,张云翔,等.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.沉积学报,2001,19(4):541～547
[11]吴胜和、熊琦华.油气储层地质学.北京:石油工业出版社,1998
[12]姚光庆,孙永传,李思田.油气储集层地质学研究体系.石油勘探与开发,2001,47(3):278～286
[13]鞠俊成,张凤莲,喻国凡,等.辽河盆地西部凹陷南部沙三段储层沉积特征及含油气性分析.古地理学报,2001,3(1):63～69
[14]邓宏文,王红亮,阎伟鹏等.河流相层序地层构成模式探讨.沉积学报,2004,22(3):373～379
[15]李丕龙等.陆相断陷盆地油气地质与勘探(卷二):陆相断陷盆地沉积体系与油气分布.北京.石油工业出版社/地质出版社,2003
[16]陆建林,王果寿,蔡进功,等.长岭断陷火山岩气藏勘探潜力.天然气工业,2007,27(8):13～15
[17]钟大康,朱筱敏,王红军.中国深层优质碎屑岩储层特征与形成机理分析.中国科学D辑,2008,38增刊:11～18
[18]舒萍,丁日新,曲延明,等.徐深气田火山岩储层岩性岩相模式.天然气工业,2008,27(8):23～27
[20]孙红军.辽河盆地东部凹陷含油气系统[D].辽河油田工作站,南京大学地质系,博士后论文,2000:15～42
[21]覃豪,李红娟,李军,等.徐深气田火山岩储层类型与主控因素研究.大庆石油地质与开发,2009,总第172期:15～18
[22]田景春,陈高武,窦伟坦,等.湖泊三角洲前缘砂体成因组合形式和分布规律-以鄂尔多斯盆地姬源白豹地区三叠系延长组为例.2004,31(6):637～640
[23]刘宝珺,韩作振,杨仁超.当代沉积学研究进展、前瞻与思考.特种油气藏,2006,13(5):1～5
[24]王国光.惠民凹陷西部古近系沙三段物源特征与沉积体系分布研究.[博士学位论文].广州:中国科学院广州地球化学研究所,2007
[25]张守仁,张遂安.松辽盆地深层断陷期地层展布特征及油气勘探意义.地学前缘,2009,16(1):335～343.
[26]姜在兴.沉积学.北京:石油工业出版社,2003
[27]张家政,赵广珍.红山嘴油田石炭系火山岩油藏综合研究.新疆石油天然气,2008,4(4):1～9
[28]姜在兴.扇三角洲高精度层序地层及其与油气聚集关系—以东营凹陷胜北断层下降盘坨76块为例.沉积与特提斯地质,2007,27(1):80～85
[29]薛叔浩,罗平,杨永泰等.辽河坳陷沉积体系与油气分布.石油勘探与开发,1997,24(4):19～22
[30]回雪峰,管守锐,张凤莲,等.辽河盆地东部凹陷中段深层沙河街组沉积相.古地理学报,2003,5(3):291～302
[31]鄢继华,陈世悦,姜在兴.三角洲前缘浊积体成因及分布规律研究.石油实验地质,2008,30(1):20～23
[32]冯有良,李思田.东营凹陷沙河街组三段层序低位域砂体沉积特征,地质论评,2001,47(3),278～286.
[33]钟大康,张崇军,文应初.砂岩储集层物性影响因素定量分析方法.石油与天然气地质,2000,21(2):130～132
[34]辽河油田石油地质志编辑委员会.辽河油田,中国石油地质志(三).北京:石油工业出版社,1993
[35]谢庆宾,朱筱敏,管守锐等.中国现代网状河流沉积特征和沉积模式.沉积学报,2003,21(20):219～227
[36]李潍莲,孙红军,唐文连.辽河盆地东部凹陷北段古近系层序地层特征及油气藏分布.石油大学学报(自然科学版),2004,28(5):1～6
[37]赵澄林,孟卫工,金春爽,等.辽河盆地东部凹陷火山岩与油气,北京:石油工业出版社,1999
[38]陈元勇,王振奇,邢成智,等.准噶尔盆地车排子地区火山岩储集层特征.断块油气田,2009,16(5):23～26
[39]陈永峤,于兴河,周新桂等.东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究.天然气地球科学,2004,15(1):68～74
[40]张金亮,司学强,梁杰等.陕甘宁盆地庆阳地区长8油层砂岩成岩作用及其对储层性质的影响,沉积学报,2004,22(2):225～233
[41]张新培,邓宏文,张吉昌,等.辽河坳陷东部凹陷欧-黄地区火山岩储集层特征及有利储层预测.石油天然气地质,2007,28(3):370～376
[42]张子枢、吴邦辉.国内外火成岩油气藏研究现状及勘探技术调研.开然气勘探与开发.1994,16(1):1～26
[43]裘亦楠、薛叔浩.油气储层评价技术.北京:石油工业出版社,2001
[44]裘亦楠.沉积方式与碎屑岩储层的层内非均质性.石油学报,1985,6(1):85～90
[45]祝彦贺,颜耀敏,王英民,等.碎屑岩与火山岩混积岩系层序地层学研究初探-以准噶尔盆地西北缘佳木河组为例.现代地质,2008,22(2):255～263
[46]张福功.辽河盆地东部凹陷中段火山岩岩性测井评价方法研究.海洋石油,2005,25(4):80～83
[47]陈昭年,陈晓巍,王明艳,等.内蒙古查干凹陷火山岩油藏成藏模式.现代地质,2008,22(4):628～632
[48]马全华.欧利坨子火山岩识别与浊积岩相模式研究.西北大学学报(自然科学版),2008,38(2):285～289
[49]张建龙,张方礼,蒋少涌,等.欧利坨子火山岩油藏原油特征及成因分析.地球学报,2007,28(4):369～376
[50]谭显春.徐深气田火山岩岩性岩相序列.天然气工业,2009,29(8):12～14
[51]徐正顺,王渝明,庞彦明,等.大庆徐深气田火山岩气藏储集层识别与评价.石油勘探与开发,2006,33(5):521～531
[52]李亚辉.高邮凹陷北斜坡辉绿岩与油气成藏,地质力学学报,2000,6(2):17～22
[53]邹才能,赵文智,贾承造,等.中国沉积盆地火山岩油气藏形成与分布.石油勘探与开发,2008,35(3):257～271
[54]赵文智,邹才能,冯志强,等.松辽盆地深层火山岩气藏地质特征及评价技术.石油勘探与开发,2008,35(2):129～142
[55]杨申谷,刘笑翠,胡志华,等.储层分析中火山岩岩性的测井识别.石油天然气学报(江汉石油学院学报),2007,29(6):33～37
[56]操应长,姜在兴,王留奇等.陆相断陷湖盆层序地层单元的划分及界面识别标志.石油大学学报(自然科学版),1996,20(4):1～5
[57]郑亚斌,王延斌,冉启全.枣35断块火山岩储层特征研究.石油学报,2006,27(4):54～58
[58]陈会军,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深层碎屑岩地层为例.石油勘探与开发,2001,28(6):28～31.
[59]陆建林,张玉明,徐宏节,等.松辽盆地长岭断陷火山岩储层形成特征研究.石油实验地质,2009,31(5):441～461
[60]张金亮,刘宝珺,毛凤鸣,等.苏北盆地高邮凹陷北斜坡阜宁组成岩作用及储层特征.石油学报,2003,24(2):43～49
[61]高山林,李学万,宋柏荣.辽河盆地欧利佗子地区火山岩储集空间特征,石油与天然气地质,2001,22(2):173～177
[62]罗静兰、邵红梅等,火山岩油气藏研究方法与勘探技术综述,石油学报,2003,24(1):31～38
[63]杨立民,邹才能,冉启全等.大港枣园油田火山岩裂缝性储层特征及其控制因素.沉积与特提斯地质,2007,27(1):86～912
[64]黄亮,彭军,周康,等,火山岩储层形成机制研究综述,特种油气藏,2009,16(1):1～5
[82] Sun Qiang,Xie Hongsen,Guo Jie,et al. Fluid inclusions in sedimentary basins generating petroleum and their application. Journal of Changchun University of Science and Technology,2000,30(1):42～45(in Chinese with English abstract)
[83] StreckerUwe,SteidtmannJR,SmithsonSB.A conceptual tectono strtigraphic model for seismic facies migration in fluvial-lacustrine extensional basin[J]. AAPG,Bull,1999,83(23):43～61
[84] Reynolds A D.Dimensions of paralic sandstone bodies.AAPG,Bull,1999,83(3):211～229
[85] Sruoga P,Rubinstein N. Processes controlling porosity and peimeability in volcanic reservoirs from the Austral and Neuquen basins,Argentina. AAPG Bull,2007,91(1):115～129
[86] Alan M,Salam S,Morad S, et al. Diagenesis and reservoir-quality evolution of fluvial sandstones during progressive burial and uplift: evidence from the Upper Jurassic Boipeba Member,Reconcavo basin, northeastern Brazil.AAPG Bulletin, 2000,84(7):1015～1040
[87] Luo J L,Morad S,Zhang X L. Reconstruction of the diagenesis of the fluvial-lacustrine-deltaic sandstones and its influence on the reservoir quality evolution. Science in China (Series D),2002,45(7):616～625
[88] Oelkers E H,Bjorkum P A, Murphy W m. A petrographic and computational investigation of quartz cemetation and porosity reduction in North Sea sandstones. American Journal of Science,1996,296: 420～452
[89] Michael L. Sweet and Larry T. Sumpter,Genesis field,Gulf of Mexico: Recognizing reservoir compartments on geologic and production time scales in deep-water reservoirs,AAPG Bulletin, Dec 2007,91: 1701～1729
[90] Haldorson HH,et al.Challenges in reservoir characterization .AAPG,1993,77(4):541～551
[91] Miall A D. Architectural elements and bounding surface in fluvial deposits: anatomy of the Kayente formation(lower Jurassic),southwest clorado.Sedimentary Geology.1988,55:233～262
[92]Stenen M Colman. Water-level changes in Lake Baikal, Siberia:Tectonic versusclimate.Geology,1998,26(6): 531～534
[93] Seemann U,Schere M. Volcaniclastics as potential hydrocarbon reservoirs. Clay Minerals,1984,19(9):457～470
[94] Vemik Lev. A new type reservoir rock in volcaniclastic sequences. AAPG Bulgy 1990,74( 6):830～836
[95] Hawland erHM. Diagenesis and reservoir potential of vol-canogenic sandstones-Cretaceous of the Surat Basin Australia.Sedimentary Geology,1990,66(3/4):181～195
[96] R L Gawthorpe, M R Leedert. Tectono-sedimentary evolution of active extensional basins.Basin Research,2000,12: 195～218
[97] Ramon,J.Cand Cross,T.A.Characterization and prediction of reservoir architecture and petrophysical properties in fluvial channel sandstones, Middle Magdalena Basin, Colombia:Ciencia, Tecnologia y Futuro,1997, v.1,no.3,p.19～46
[98] Perrin M,Plenier G,Dautria J M,et al.Rotation Of The Semail Ophiolite (Oman): Additional Paleomagnetic Data From The Volcanic Sequence,Mar Geophys Res V 21, Nos 3～4,2000,181～194
[99] De Carlo E H,Carmody R,Lackschewitz K K. Alteration Of Volcanic Matter In Sediments Of The Woodlark Basin,Abstr With Programs (Gsa) ,2001,33(6):234
[100] Blickwede J F,The Nazas Formation:A Detailed Look At The Early Mesozoic Convergent Margin Along The Western Rim Of The Gulf Of Mexico Basin,The Western Gulf Of Mexico Basin Tectonics,Sedimentary Basins,And Petroleum Systems [Aapg Mem No 75],The American Association Of Petroleum Geologists,2001,317～342
[101] Compston W. Effect Of Pb Loss On The Ages Of Reference Zircons Qgng And Sl13,And Of Volcanic Zircons From The Early Devonian Merrions And Turondale Formations,New South Wales,Australian J Earth Sci,2001,48(6):797～803
[102] Liu Z Y,Xiao S B,Jiang Z X. Volcanic Rocks Of Bohai Bay Basin In Tertiary And Their Genesis,J Univ Petrol,2001,China 25(1):22～26
[103] Jin Q.Volcanic Activities And Oil/Gas Accumulation In The Rift Basins Of Eastern China,J Univ Petrol,2001,China 25(1),27～33
[104] Sruoga P,RuSinstein N. Proccsscs controlling porosity and permeability in volcanic rescrvoirs from the Austral and Neuquen basins,Argentina.AAPG Bull, 2007,91(1):115～129
[105] Dutkiewicz A,Volk H,Ridlcy J. Geochemistry of oil in fluid inclusions in a middle Protcrozoic igncous intrusion implications for the sourced of hydrocarbons in crystallinc rocks.Organic Geochem istry 2004,35(8):937～957
[106] Lee A M,Hulen J B. Oil and igneous intrusions in Nevada. AAPG,1990,74(8):1313
[107]Stephen R. Occurrences of hydrocarbons in and around igneous rocks. Geol. Soc. Lon. Spec. Pub. 2003,214( 1):35～68
[108] Kawamoto T. Distribution and alteration of the volcanic reservoir in the Minami-Nagaoka gas field. Japan. Ass. Petroleum Tech. 2001,66( 1):46～55
[109] YuliMitsuhata,KoichiMatsuo,MatatoMinegishi. Magnetotelluric survey for exploration of a volcanic rock rescrvoir in the Yurihara oiland gas ficld,Japan. Geophysical Prospecing 1999,47(2):195～218
[110] Alvar Braathen1,Jan Tveranger,Haakon Fossen,et al.Fault facies and its application to sandstone reservoirs.AAPG Bulletin,2009,93(7):891～917;
[111] Anna Berger,Susanne Gier and Peter Krois. Porosity-preserving chlorite cements in shallow-marine volcaniclastic sandstones:Evidence from Cretaceous sandstones of the Sawan gas field,Pakistan.AAPG Bulletin,2009,93(5),595～615
© 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 |