松辽盆地北部中浅层成岩场分析及储层质量预测
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摘要
综合考虑时间、温度、流体、压力对成岩作用的影响,本文在原成岩作用数值模拟系统的基础上,对其模型进行了修改和完善,重新编译了成岩作用数值模拟系统。应用新的模拟系统对松辽盆地北部中浅层进行了成岩场分析和储层质量预测。
松辽盆地北部中浅层成岩作用数值模拟的结果表明,青一段有机质成熟区域集中在中央坳陷区,从嫩江组沉积时期开始,青一段有机质开始进入大量生烃时期,并且泥岩发生超压释放,下伏泉四段、泉三段储层处于中成岩阶段A1亚期和中成岩阶段A2亚期,以溶蚀相和溶蚀及部分再胶结相为主,次生孔隙发育,这一时期构造运动强烈,断层发育,是扶杨油层大规模成藏时期;明水组沉积时期泥岩超压再次达到最大值,生、储、盖层发育俱佳,扶杨油层再次大规模聚集成藏。现今成岩强度基本维持明末的状态,泉四段储层处于早成岩阶段～中成岩阶段A2亚期,储层质量较好;泉三段成岩作用较强,在埋藏较深的坳陷区已经进入中成岩阶段B期,储层物性较差。
沉积相和成岩作用共同决定储层现在的质量,在综合考虑这两个因素的基础上,建立了不同沉积微相的孔隙度、渗透率预测模型,对扶杨油层储层孔隙度、渗透率进行了预测。在平均填隙物含量约16%的条件下,孔隙度预测平均误差2.78%。在对扶杨油层油层物性重新统计分析的基础上,制定了扶杨油层有效储层的物性下限,并预测了有效油气储层的分布范围。预测结果表明,泉四段、泉三段上部储层大部分处于有效油气储层范围内,只有齐家古龙凹陷、三肇凹陷的部分地区,储层物性太差,失去了工业价值。
Considering effects of time, temperature, fluid medium and pressure on diageneses, Based on the old Diagenetic Modeling System, this paper modified and improved its geologic model, and recompiled the modeling system. This paper completed the diagenetic numerical modeling and the diagenetic field analyzes to the Middle-Shallow Strata of North Songliao Basin using the new modeling system.
The results of field analyze of the Middle-Shallow Strata of North Songliao Basin showed that the mature area of organic matter of K2qn1 centralizes in the Central Depression. The mature area of organic matter of K2qn1 came into great quantity hydrocarbon generation from the K2qn, and overpressure relief was happened. The reservoir of K1q4 and K1q3 is between middle diagenetic phase A1 and middle diagenetic phase A2 at deep area, and its diagenetic facies were dissolution facies and dissolution and cementation facies at that time, and secondary pores developed. On the side, tectonic movements were intensive, and developed lots of faults, and petroleum accumulated extensively of Fu-Yang Reservoir at that time. The overpressures of K2qn1 reached to the limited level and leaked off, and Fu-Yang Reservoir petroleum accumulated extensively again at K2m, when the source rocks and reservoirs were developed .The diagensis intensity at present keeps the state of K2m, and the reservoir of K1q4 is between early diagenetic phase and middle diagenetic phase A2, and have good quantity, while and the reservoir of K1q3 is middle diagenetic phase B at deep area, whose reservoir quantity is worse.
Reservoir quantity is mainly controlled by sedimentary facies and diagenses. Reservoir porosity and permeability prediction models were established on the base of considering the two the factors, and the reservoir quantity of K1q4 and K1q3 are predicted. The average error between measured and predicted porosities is 2.78% on condition that the average pore-fillings of the reservoir are 16%. Base on recounting the reservoir porosity and permeability data of Fu-Yang Reservoir, the limited porosity and permeability of commercial reservoirs of Fu-Yang Reservoir are determined and the effective reservoir areas are predicted. The results show that most of the reservoir of K1q4 and K1q3 develops effective reservoir, and the reservoirs at the deep area in Qijia-gulong depression and Sanzhao depression lost commercial value because of bad quantity.
松辽盆地北部中浅层成岩作用数值模拟的结果表明,青一段有机质成熟区域集中在中央坳陷区,从嫩江组沉积时期开始,青一段有机质开始进入大量生烃时期,并且泥岩发生超压释放,下伏泉四段、泉三段储层处于中成岩阶段A1亚期和中成岩阶段A2亚期,以溶蚀相和溶蚀及部分再胶结相为主,次生孔隙发育,这一时期构造运动强烈,断层发育,是扶杨油层大规模成藏时期;明水组沉积时期泥岩超压再次达到最大值,生、储、盖层发育俱佳,扶杨油层再次大规模聚集成藏。现今成岩强度基本维持明末的状态,泉四段储层处于早成岩阶段～中成岩阶段A2亚期,储层质量较好;泉三段成岩作用较强,在埋藏较深的坳陷区已经进入中成岩阶段B期,储层物性较差。
沉积相和成岩作用共同决定储层现在的质量,在综合考虑这两个因素的基础上,建立了不同沉积微相的孔隙度、渗透率预测模型,对扶杨油层储层孔隙度、渗透率进行了预测。在平均填隙物含量约16%的条件下,孔隙度预测平均误差2.78%。在对扶杨油层油层物性重新统计分析的基础上,制定了扶杨油层有效储层的物性下限,并预测了有效油气储层的分布范围。预测结果表明,泉四段、泉三段上部储层大部分处于有效油气储层范围内,只有齐家古龙凹陷、三肇凹陷的部分地区,储层物性太差,失去了工业价值。
Considering effects of time, temperature, fluid medium and pressure on diageneses, Based on the old Diagenetic Modeling System, this paper modified and improved its geologic model, and recompiled the modeling system. This paper completed the diagenetic numerical modeling and the diagenetic field analyzes to the Middle-Shallow Strata of North Songliao Basin using the new modeling system.
The results of field analyze of the Middle-Shallow Strata of North Songliao Basin showed that the mature area of organic matter of K2qn1 centralizes in the Central Depression. The mature area of organic matter of K2qn1 came into great quantity hydrocarbon generation from the K2qn, and overpressure relief was happened. The reservoir of K1q4 and K1q3 is between middle diagenetic phase A1 and middle diagenetic phase A2 at deep area, and its diagenetic facies were dissolution facies and dissolution and cementation facies at that time, and secondary pores developed. On the side, tectonic movements were intensive, and developed lots of faults, and petroleum accumulated extensively of Fu-Yang Reservoir at that time. The overpressures of K2qn1 reached to the limited level and leaked off, and Fu-Yang Reservoir petroleum accumulated extensively again at K2m, when the source rocks and reservoirs were developed .The diagensis intensity at present keeps the state of K2m, and the reservoir of K1q4 is between early diagenetic phase and middle diagenetic phase A2, and have good quantity, while and the reservoir of K1q3 is middle diagenetic phase B at deep area, whose reservoir quantity is worse.
Reservoir quantity is mainly controlled by sedimentary facies and diagenses. Reservoir porosity and permeability prediction models were established on the base of considering the two the factors, and the reservoir quantity of K1q4 and K1q3 are predicted. The average error between measured and predicted porosities is 2.78% on condition that the average pore-fillings of the reservoir are 16%. Base on recounting the reservoir porosity and permeability data of Fu-Yang Reservoir, the limited porosity and permeability of commercial reservoirs of Fu-Yang Reservoir are determined and the effective reservoir areas are predicted. The results show that most of the reservoir of K1q4 and K1q3 develops effective reservoir, and the reservoirs at the deep area in Qijia-gulong depression and Sanzhao depression lost commercial value because of bad quantity.
引文
[1]张昌民,胡明毅.松辽盆地北部泉三、四段层序地层、沉积相研究[R].武汉:长江大学,2007.
[2]王玉满,牛嘉玉,谯汉生等.渤海湾盆地深层油气资源潜力分析与认识[J].石油勘探与开发,2002,29(2):21～25.
[3]牛嘉玉,王玉满,谯汉生.中国东部老油区深层油气勘探潜力分析[J].中国石油勘探, 2004,9(1):33～40.
[4]孟元林,肖丽华,杨俊生等.成岩演化数值模拟及其应用[J].地学前缘,2000,7(4),430.
[5]孟元林,肖丽华,杨俊生等.渤海湾盆地老爷庙地区深层成岩作用的化学动力学分析[J].地球科学,2002,27(Suppl.):275～279.
[6]孟元林,黄文彪,肖丽华等.辽河坳陷西部斜坡带南段新生界成岩相分析与优质储层预测[J].古地理学报,2008,10(1):33～41.
[7]孟元林,肖丽华,杨俊生等.成岩作用过程综合模拟及其应用[J].石油实验地质,2003,25(2):211～215.
[8]孟元林.歧北凹陷沙河街组超压背景下的成岩作用研究与数值模拟[D].中国地质大学,博士论文,2004.
[9]孟元林,贺如,肖丽华等.成岩史模拟与成岩阶段预测—以黄骅坳陷碳酸盐为例[J].天然气工业,2006,26(7):5～7.
[10]孟元林,肖丽华,姜文亚等.辽河西部凹陷双清地区有利储集相预测与成藏史研究[R].秦皇岛:秦皇岛庆大科技有限公司,2007.
[11]肖丽华,孟元林,侯创业等.松辽盆地升平地区深层成岩作用数值模拟与次生孔隙带预测[J].地质论评,2003,49(5):544～551.
[12]肖丽华,孟元林,牛嘉玉等.歧口凹陷沙河街组成岩史分析和成岩阶段预测[J].地质科学,2005,40(3):346～362.
[13]解习农.松辽盆地层序地层格架和中浅层沉积体系研究.2007.
[14]孟元林,肖丽华.松辽盆地北部成岩演化及有利储层发育区带预测[R].大庆:大庆石油学院,2007.
[15] Hower J, et al..Mechanism of burial metamorphism of argillaceous sediments, I. Mineralogical and chemical evidence[J].G.S.A.Bull.,1976,87: 725～737.
[16] Smosna R and Bruner K R.Depositional controls over porosity development in lithic sandstones of the Appalachian Basin:reducing exploration risk,In J A Kupecz,J Gluyas and S Bloch,eds.,Reservoir quality prediction in sandstones and carbonates[J].AAPG Memoir 69,1997,249～265.
[17] Bloch S , FranksS G.Preservation of Shallow Plagioclase Dissolution Porosity During Burial:Implications for Porosity Prediction and Aluminum Mass Balance[J].AAPG Bull.,1993,9(9):1488～1501.
[18] Bloch S, Helmod K P.Appoaches to predicting reservoir quality in sandstones.AAPG Bulletin,1995,79:97～115.
[19] Byrnes A P.Empirical methods of reservoir quality prediction[A],In :Wilson W D,ed. Reservoir quality assessment and prediction in clastic rocks[C].SEPM Short Course,1994, 30:10～21.
[20]李思田,路风香,林畅松等.中国东部及邻区中、新生代盆地演化及地球动力学背景[M].北京:中国地质大学出版社,1997.
[21]裘怿楠,薛叔浩,应凤祥.中国陆相油气储集层[M].北京:石油工业出版社,1997,147～217.
[22] Anjos S M C,De Ros L F, De Souza R S, et al.Depositional and diagenetic control on the reservoir quality of Lower Cretaceous Pendencia sandstones,Potiguar rift basin,Brazil[J].AAPG Bull.,2000, 84 (11) :1719～1742.
[23]黄思静,侯中建.地下孔隙率和渗透率在空间和时间上的变化及影响因素[J].沉积学报,2001,19(2):224～232.
[24]薛书浩,刘文林,薛良清等.湖盆沉积地质与油气勘探[M].北京:石油工业出版社,2002,121～132.
[25]孟元林,刘德来,贺如等.岐北凹陷沙二段超压背景下的成岩场分析与储层孔隙度预测[J].沉积学报,2005,23(3):389～396.
[26] Wood J R and Byres A P.Alteration and emerging methodologies in geochemical and empirical modeling[A],In :Wilson W D,ed. Reservoir quality assessment and prediction in clastic rocks[C].SEPM Short Course,1994, 30:395～400.
[27] Kupecz J A,J Gluyas and S Bloch.Reservoir Quality Prediction in Sandstones and Carbonates:An Overview.[A]in Kupecz J A, Gluyas J G ,Bloch S eds.Reservoir quality prediction in Sandstones and Carbonates[C]:Tulsa,AAPG Memoir 69,1997,19～28.
[28]应凤祥.碎屑岩成岩阶段划分规范(中华人民共和国石油与天然气行业标准[S]).北京:石油工业出版社,2003.
[29]黄飞,辛茂安.中华人民共和国石油天然气行业标准并陆相烃源岩地球化学评价方法(SY/T5735-1995)[S].北京:石油工业出版社,1996,1～19.
[30]谢树艺.矢量分析与场论[M].北京:人民教育出版社,1979,136～139.
[31]杨乂,张家环,李汉瑜等.英汉石油大辞典石油地质分册[M].北京:石油工业出版社,1992.
[32]应凤祥,罗平,何东博等.中国含油气盆地碎屑岩储集层成岩作用与成岩作用数值模拟[M].北京:石油工业出版社,2004.
[33]庞雄奇,付广,万龙贵等.盖层封油气性综合定量评价—盆地模拟在盖层评价中的应用[M].北京:地质出版社,1993,14～16.
[34]李泰明.石油地质过程定量研究概论[M].东营:石油大学出版社,1989,4～10.
[35]孟元林,肖丽华,李泰明等.盆地模拟在油气田勘探初期阶段的应用[J].天然气工业,1994,14(4):6～9.
[36] Meng Yuanlin,Xiao Lihua,Cao Cheng Run,et al.Early basin modeling system EBMS and its application [A].In:Jang,B.A.Cheong,D.eds.Crustal evolution in northeast Asia:4th Korea-China joint geology symposium[C].ChuncheonKorea:Kingman Publishing Company,1997,125～132.
[37] Meng Yuanlin,Yang Junsheng,Xiao Lihua,et al.Diagenetic evolution modeling systemand its application[A].In:Hao Dongheng.ed.Treatises ofⅩⅢKerulien international conference of geology[C].Shijiazhuang,P.R.China:Shijiazhuang University of Economics,2001,25～27.
[38]石广仁.油气盆地数值模拟方法[M].北京:石油工业出版社,1994,12～40.
[39]石广仁.油气盆地数值模拟方法[M].北京:石油工业出版社,1999.
[40]郭秋麟,米石云,石广仁.盆地模拟原理方法[M].北京:石油工业出版社,1998.
[41]郝石生,黄志龙,杨家崎等.天然气运聚动平衡及其应用[M].北京:石油工业出版社,1994.
[42]庞雄奇,陈章明,陈景发.含油气盆地地史、热史、生留排烃史数值模拟研究与烃源岩定量评价[M].北京:地质出版社,1993,37～96.
[43]李景坤,刘伟,宋兰斌等.天然气扩散量方法研究[J].新疆石油地质,1999,50(5):383～386.
[44]付广,苏玉平.利用声波时差研究异常孔隙流体压力释放次数及深度的方法[J].石油物探,2006,45(1):21～24.
[45]孟元林,吕延防.地温史和有机质成岩史的一维模拟[J].大庆石油学院学报,1989,13(2):1～6.
[46] Domine F,Enguehard F.Kinetics of hexane pyrolysis at very high pressure -3[J].Application to geochemical modeling.Org.Geochem.,1992,18(1),41～49.
[47]姜峰,杜建国,王万青.高温高压模拟试验研究[J].沉积学报,1998,16(3):153～155.
[48] Hao Fang,Li Sitian,Sun Yongchuan,et al.Overpressure retardation of organic-matter maturation and hydrocarbon generation:a case study from the Yinghehai and Qiongdongnan basins,offshore South China Sea.AAPG Bulletin,1995,79:551～562.
[49] Sweeny J J and Burham A K.Evaluation of a simple model of vitrinite reflectance based on chemical kinetics[J].AAPG Bull.,1990,74:1559～1570.
[50] Marchand A M E,Smally P C,Haszeldine R S ,et al. Note on the importance of hydrocarbon fill for reservoir quality prediction in sandstones [J]. AAPG Bull., 2002, 86(9):1561～1571.
[51] Huang W L, Longo J M,David R P.An experimentally derived kinetic model for smectite-to-illite conversion and its use as a geothmometer[J].Clays and Minerals,1993,41(2):162～177.
[52] Huang W L.Experimental study of vitrinite maturation:effects of temperature,time,pressure,water,and hydrogen index.Org.Geochem.,1996,24(2):233～241.
[53]孟元林,肖丽华,王建国等.粘土矿物转化的化学动力学模型及其应用[J].沉积学报,1996,l4(2):110～116.
[54] Walderhaug O.Modeling quartz cementation and porosity in Middle Jurassic Brent Group sandstones of the Kvitebjφrn Field Northern North Sea[J].AAPG Bull.,2000,84:1325～1339.
[55] Colten-Bradley V A.Role of pressure in smectite dehydration-effects on geopressure and smectite-to-illite transformation.AAPG Bull.,1987,71:1414～1427.
[56] Mackenize A S, Mckenice D.Isomerization and aromatization of hydrocarbon in sedimentary basin formed by extension[J].Geo.Mag.,1983,120:417～470.
[57] Walderhaug O.Kinetic modeling of quartz cementation and porosity loss in deeply buried sandstone reservoirs[J].AAPG Bull.,1996, 80:731～745.
[58]杨俊生,孟元林,张宏等.石英胶结作用化学动力学模型及其应用[J].石油实验地质,2002,24(4):372～376.
[59] Hermanrud C.Basin modelling techniques─An overview,in :Basin modelling:Advances and application.NPF Special Publication 3,Elsevier,Amsterdam.,1993.
[60] Dow W G.Kerogen Studies and geological interpretation.Journal of Geochemical Exploration,1977,7:79～99.
[61]真柄钦次,陈立荷译.压实与流体运移[M].北京:石油工业出版社,1981,35～38.
[62]王英民,王贵文,李树青等.松辽盆地北部浅层次生油气藏形成条件与勘探方向研究[R].北京:中国石油大学,2007.
[63]李忠权,杭文艳,应丹琳等.松辽盆地北部构造地质特征及成盆动力学研究[R].成都:成都理工大学,2007.
[64]向才富,胡建武,马中振等.松辽大型陆相坳陷盆地北部晚期流体动力场演化与油气运聚规律剖面研究[R].北京:中国石油大学,2007.
[65]肖丽华,张靖,孟元林等,地热参数及边界条件的探讨[J].大庆石油学院学报,1996,20(2):28～31.
[66]王钧,黄尚瑶,黄歌山等.中国地温分布的基本特征[M].北京:地震出版社,1990,77～84.
[67]周平,要丹,刘伟.松辽盆地北部一维盆地模拟及资源量预测研究[R].大庆:大庆石油管理局勘探开发研究院,1990.
[68]邦特巴思著.(易志新,熊亮萍译).地热学导论[M].北京:地震出版社,1988,1～6
[69]王永玲,张忠义,汪集旸等.辽河断陷地热基本特征与油气资源[M].北京:中国科学院地质研究所,1984.
[70]吴乾蕃.松辽盆地地热场[J].地震研究,1991,14(1):31～40.
[71]肖丽华,孟元林,王建国等[J].碎屑岩成岩温度的数值模拟和成岩阶段的预测[J].中国海上油气(地质),1995,9(6):389～394.
[72]陈墨香.华北地热[M].北京:科学出版社,1988,11～12.
[73]张菊明等.有限单元法在地热研究中的应用[M].北京:科学出版社,1986,15～22.
[74] Horbury A D,Robinson A G.Diagenesis and basin development[J].AAPG Studies in Geology #36,1993,135～151.
[75]孙永传,李忠,李惠生等.中国东部含油气断陷盆地的成岩作用[M].北京:科学出版社,1996.
[76]刑顺洤，姜洪启．松辽盆地陆相砂岩储集层性质与成岩作用[M].哈尔滨:黑龙江科学技术出版社,1993,70～77.
[77]张顺,梁晓东等.松辽盆地北部中浅层成藏规律及勘探潜力再认识[R].大庆:大庆油田勘探开发研究院,2007.
[78]李延平,陈树民,宋永忠等.大庆长垣及以东泉三、四段扶杨油层浅水湖泊—三角洲体系沉积特征[M] .大庆石油地质与开发,2005,24(5):13～16.
[79] Evans J,Cade C,Bryant S.A geological approach to permeability prediction in clasdtic reservoir[J].AAPG Memoir,1997,69: 91～101.
[80] Osborne M J and Swarbrick R E.Diagenesis in North Sea HPHT classic reservoirs-consequences for porosity and overpressure prediction[J].Marine and Petroleum Geology,1999,16:337～353.
[81] Ramm M and Bjorlykke K.Porosity/depth trends in reservoir sandstones:assessing the quantitative effects of varying Pore-Pressure,Temperature History and Mineralogy,Norwegian Shelf Data[J].Clay Minerals,1994,29:475～490.
[82] Schmoker J M, Hester T C. Regional trends of sandstone porosity vs. vitrinite reflectance-a preliminary framework. Applications of thermal maturity studies to energy exploration[J]. Rocky Mountain Section of SEMP,1990,53～60.
[83] Wilson M D, Byrnes A P. Model design [A],In: Wilson W D,ed.Reservoir quality assessment and prediction in clastic rocks.SEPM Short Course,1994, 30:209～230.
[84] Sombra C L,Kiang C H.Burial history and porosity evolution of Brazilian Upper Jurassic to Tertiary sandstone reservoirs[A].In: Kupecz eds.Reservoir quality prediction in sandstones and carbonates. AAPG Memoir 69,1997,26:79～89.
[85] Gluyas J and Cade C A.Prediction of porosity in compacted sands. AAPG Memoir, 1997,69:19～27.
[86] Paxton ST, Szabo J O, Ajdukiewicz J M ,et al.Construction of an intergranular volume compaction curve for evaluating and predicting compaction and porosity loss in rigid-grain sandstone reservoirs[J].AAPG Bulletin,2002,86(12):2047～2069.
[87]罗平,裘怿楠,贾爱林等.中国油气储层地质研究面临的挑战和发展方向[J].沉积学报,2003,21(1):142～147.
[88]朱国华.碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3):114～121.
[89]姜培海,杨小丽.利用储层沉积学参数预测储层孔隙度[J].中国海上油气(地质),1997,11(4):261～267.
[90]武文来,周士科.渤海海域深部碎屑岩储层孔隙度预测[J].中国海上油气(地质),1997,11(4):241～248.
[91]寿建峰,朱国华.砂岩储层孔隙保存的定量预测研究[J].地质科学,1998,33(2):244～249.
[92]杨香华,叶加仁,周士科等.成岩动力学分析与深部储层孔隙度预测[J].现代地质,1998,12(1):108～114.
[93]王粤川,孟元林,贺如等.用时深效应指数预测储层孔隙度-以辽河西部凹陷沙三中亚段为例[J].中国海上油气,2007,18(5):308～312.
[2]王玉满,牛嘉玉,谯汉生等.渤海湾盆地深层油气资源潜力分析与认识[J].石油勘探与开发,2002,29(2):21～25.
[3]牛嘉玉,王玉满,谯汉生.中国东部老油区深层油气勘探潜力分析[J].中国石油勘探, 2004,9(1):33～40.
[4]孟元林,肖丽华,杨俊生等.成岩演化数值模拟及其应用[J].地学前缘,2000,7(4),430.
[5]孟元林,肖丽华,杨俊生等.渤海湾盆地老爷庙地区深层成岩作用的化学动力学分析[J].地球科学,2002,27(Suppl.):275～279.
[6]孟元林,黄文彪,肖丽华等.辽河坳陷西部斜坡带南段新生界成岩相分析与优质储层预测[J].古地理学报,2008,10(1):33～41.
[7]孟元林,肖丽华,杨俊生等.成岩作用过程综合模拟及其应用[J].石油实验地质,2003,25(2):211～215.
[8]孟元林.歧北凹陷沙河街组超压背景下的成岩作用研究与数值模拟[D].中国地质大学,博士论文,2004.
[9]孟元林,贺如,肖丽华等.成岩史模拟与成岩阶段预测—以黄骅坳陷碳酸盐为例[J].天然气工业,2006,26(7):5～7.
[10]孟元林,肖丽华,姜文亚等.辽河西部凹陷双清地区有利储集相预测与成藏史研究[R].秦皇岛:秦皇岛庆大科技有限公司,2007.
[11]肖丽华,孟元林,侯创业等.松辽盆地升平地区深层成岩作用数值模拟与次生孔隙带预测[J].地质论评,2003,49(5):544～551.
[12]肖丽华,孟元林,牛嘉玉等.歧口凹陷沙河街组成岩史分析和成岩阶段预测[J].地质科学,2005,40(3):346～362.
[13]解习农.松辽盆地层序地层格架和中浅层沉积体系研究.2007.
[14]孟元林,肖丽华.松辽盆地北部成岩演化及有利储层发育区带预测[R].大庆:大庆石油学院,2007.
[15] Hower J, et al..Mechanism of burial metamorphism of argillaceous sediments, I. Mineralogical and chemical evidence[J].G.S.A.Bull.,1976,87: 725～737.
[16] Smosna R and Bruner K R.Depositional controls over porosity development in lithic sandstones of the Appalachian Basin:reducing exploration risk,In J A Kupecz,J Gluyas and S Bloch,eds.,Reservoir quality prediction in sandstones and carbonates[J].AAPG Memoir 69,1997,249～265.
[17] Bloch S , FranksS G.Preservation of Shallow Plagioclase Dissolution Porosity During Burial:Implications for Porosity Prediction and Aluminum Mass Balance[J].AAPG Bull.,1993,9(9):1488～1501.
[18] Bloch S, Helmod K P.Appoaches to predicting reservoir quality in sandstones.AAPG Bulletin,1995,79:97～115.
[19] Byrnes A P.Empirical methods of reservoir quality prediction[A],In :Wilson W D,ed. Reservoir quality assessment and prediction in clastic rocks[C].SEPM Short Course,1994, 30:10～21.
[20]李思田,路风香,林畅松等.中国东部及邻区中、新生代盆地演化及地球动力学背景[M].北京:中国地质大学出版社,1997.
[21]裘怿楠,薛叔浩,应凤祥.中国陆相油气储集层[M].北京:石油工业出版社,1997,147～217.
[22] Anjos S M C,De Ros L F, De Souza R S, et al.Depositional and diagenetic control on the reservoir quality of Lower Cretaceous Pendencia sandstones,Potiguar rift basin,Brazil[J].AAPG Bull.,2000, 84 (11) :1719～1742.
[23]黄思静,侯中建.地下孔隙率和渗透率在空间和时间上的变化及影响因素[J].沉积学报,2001,19(2):224～232.
[24]薛书浩,刘文林,薛良清等.湖盆沉积地质与油气勘探[M].北京:石油工业出版社,2002,121～132.
[25]孟元林,刘德来,贺如等.岐北凹陷沙二段超压背景下的成岩场分析与储层孔隙度预测[J].沉积学报,2005,23(3):389～396.
[26] Wood J R and Byres A P.Alteration and emerging methodologies in geochemical and empirical modeling[A],In :Wilson W D,ed. Reservoir quality assessment and prediction in clastic rocks[C].SEPM Short Course,1994, 30:395～400.
[27] Kupecz J A,J Gluyas and S Bloch.Reservoir Quality Prediction in Sandstones and Carbonates:An Overview.[A]in Kupecz J A, Gluyas J G ,Bloch S eds.Reservoir quality prediction in Sandstones and Carbonates[C]:Tulsa,AAPG Memoir 69,1997,19～28.
[28]应凤祥.碎屑岩成岩阶段划分规范(中华人民共和国石油与天然气行业标准[S]).北京:石油工业出版社,2003.
[29]黄飞,辛茂安.中华人民共和国石油天然气行业标准并陆相烃源岩地球化学评价方法(SY/T5735-1995)[S].北京:石油工业出版社,1996,1～19.
[30]谢树艺.矢量分析与场论[M].北京:人民教育出版社,1979,136～139.
[31]杨乂,张家环,李汉瑜等.英汉石油大辞典石油地质分册[M].北京:石油工业出版社,1992.
[32]应凤祥,罗平,何东博等.中国含油气盆地碎屑岩储集层成岩作用与成岩作用数值模拟[M].北京:石油工业出版社,2004.
[33]庞雄奇,付广,万龙贵等.盖层封油气性综合定量评价—盆地模拟在盖层评价中的应用[M].北京:地质出版社,1993,14～16.
[34]李泰明.石油地质过程定量研究概论[M].东营:石油大学出版社,1989,4～10.
[35]孟元林,肖丽华,李泰明等.盆地模拟在油气田勘探初期阶段的应用[J].天然气工业,1994,14(4):6～9.
[36] Meng Yuanlin,Xiao Lihua,Cao Cheng Run,et al.Early basin modeling system EBMS and its application [A].In:Jang,B.A.Cheong,D.eds.Crustal evolution in northeast Asia:4th Korea-China joint geology symposium[C].ChuncheonKorea:Kingman Publishing Company,1997,125～132.
[37] Meng Yuanlin,Yang Junsheng,Xiao Lihua,et al.Diagenetic evolution modeling systemand its application[A].In:Hao Dongheng.ed.Treatises ofⅩⅢKerulien international conference of geology[C].Shijiazhuang,P.R.China:Shijiazhuang University of Economics,2001,25～27.
[38]石广仁.油气盆地数值模拟方法[M].北京:石油工业出版社,1994,12～40.
[39]石广仁.油气盆地数值模拟方法[M].北京:石油工业出版社,1999.
[40]郭秋麟,米石云,石广仁.盆地模拟原理方法[M].北京:石油工业出版社,1998.
[41]郝石生,黄志龙,杨家崎等.天然气运聚动平衡及其应用[M].北京:石油工业出版社,1994.
[42]庞雄奇,陈章明,陈景发.含油气盆地地史、热史、生留排烃史数值模拟研究与烃源岩定量评价[M].北京:地质出版社,1993,37～96.
[43]李景坤,刘伟,宋兰斌等.天然气扩散量方法研究[J].新疆石油地质,1999,50(5):383～386.
[44]付广,苏玉平.利用声波时差研究异常孔隙流体压力释放次数及深度的方法[J].石油物探,2006,45(1):21～24.
[45]孟元林,吕延防.地温史和有机质成岩史的一维模拟[J].大庆石油学院学报,1989,13(2):1～6.
[46] Domine F,Enguehard F.Kinetics of hexane pyrolysis at very high pressure -3[J].Application to geochemical modeling.Org.Geochem.,1992,18(1),41～49.
[47]姜峰,杜建国,王万青.高温高压模拟试验研究[J].沉积学报,1998,16(3):153～155.
[48] Hao Fang,Li Sitian,Sun Yongchuan,et al.Overpressure retardation of organic-matter maturation and hydrocarbon generation:a case study from the Yinghehai and Qiongdongnan basins,offshore South China Sea.AAPG Bulletin,1995,79:551～562.
[49] Sweeny J J and Burham A K.Evaluation of a simple model of vitrinite reflectance based on chemical kinetics[J].AAPG Bull.,1990,74:1559～1570.
[50] Marchand A M E,Smally P C,Haszeldine R S ,et al. Note on the importance of hydrocarbon fill for reservoir quality prediction in sandstones [J]. AAPG Bull., 2002, 86(9):1561～1571.
[51] Huang W L, Longo J M,David R P.An experimentally derived kinetic model for smectite-to-illite conversion and its use as a geothmometer[J].Clays and Minerals,1993,41(2):162～177.
[52] Huang W L.Experimental study of vitrinite maturation:effects of temperature,time,pressure,water,and hydrogen index.Org.Geochem.,1996,24(2):233～241.
[53]孟元林,肖丽华,王建国等.粘土矿物转化的化学动力学模型及其应用[J].沉积学报,1996,l4(2):110～116.
[54] Walderhaug O.Modeling quartz cementation and porosity in Middle Jurassic Brent Group sandstones of the Kvitebjφrn Field Northern North Sea[J].AAPG Bull.,2000,84:1325～1339.
[55] Colten-Bradley V A.Role of pressure in smectite dehydration-effects on geopressure and smectite-to-illite transformation.AAPG Bull.,1987,71:1414～1427.
[56] Mackenize A S, Mckenice D.Isomerization and aromatization of hydrocarbon in sedimentary basin formed by extension[J].Geo.Mag.,1983,120:417～470.
[57] Walderhaug O.Kinetic modeling of quartz cementation and porosity loss in deeply buried sandstone reservoirs[J].AAPG Bull.,1996, 80:731～745.
[58]杨俊生,孟元林,张宏等.石英胶结作用化学动力学模型及其应用[J].石油实验地质,2002,24(4):372～376.
[59] Hermanrud C.Basin modelling techniques─An overview,in :Basin modelling:Advances and application.NPF Special Publication 3,Elsevier,Amsterdam.,1993.
[60] Dow W G.Kerogen Studies and geological interpretation.Journal of Geochemical Exploration,1977,7:79～99.
[61]真柄钦次,陈立荷译.压实与流体运移[M].北京:石油工业出版社,1981,35～38.
[62]王英民,王贵文,李树青等.松辽盆地北部浅层次生油气藏形成条件与勘探方向研究[R].北京:中国石油大学,2007.
[63]李忠权,杭文艳,应丹琳等.松辽盆地北部构造地质特征及成盆动力学研究[R].成都:成都理工大学,2007.
[64]向才富,胡建武,马中振等.松辽大型陆相坳陷盆地北部晚期流体动力场演化与油气运聚规律剖面研究[R].北京:中国石油大学,2007.
[65]肖丽华,张靖,孟元林等,地热参数及边界条件的探讨[J].大庆石油学院学报,1996,20(2):28～31.
[66]王钧,黄尚瑶,黄歌山等.中国地温分布的基本特征[M].北京:地震出版社,1990,77～84.
[67]周平,要丹,刘伟.松辽盆地北部一维盆地模拟及资源量预测研究[R].大庆:大庆石油管理局勘探开发研究院,1990.
[68]邦特巴思著.(易志新,熊亮萍译).地热学导论[M].北京:地震出版社,1988,1～6
[69]王永玲,张忠义,汪集旸等.辽河断陷地热基本特征与油气资源[M].北京:中国科学院地质研究所,1984.
[70]吴乾蕃.松辽盆地地热场[J].地震研究,1991,14(1):31～40.
[71]肖丽华,孟元林,王建国等[J].碎屑岩成岩温度的数值模拟和成岩阶段的预测[J].中国海上油气(地质),1995,9(6):389～394.
[72]陈墨香.华北地热[M].北京:科学出版社,1988,11～12.
[73]张菊明等.有限单元法在地热研究中的应用[M].北京:科学出版社,1986,15～22.
[74] Horbury A D,Robinson A G.Diagenesis and basin development[J].AAPG Studies in Geology #36,1993,135～151.
[75]孙永传,李忠,李惠生等.中国东部含油气断陷盆地的成岩作用[M].北京:科学出版社,1996.
[76]刑顺洤，姜洪启．松辽盆地陆相砂岩储集层性质与成岩作用[M].哈尔滨:黑龙江科学技术出版社,1993,70～77.
[77]张顺,梁晓东等.松辽盆地北部中浅层成藏规律及勘探潜力再认识[R].大庆:大庆油田勘探开发研究院,2007.
[78]李延平,陈树民,宋永忠等.大庆长垣及以东泉三、四段扶杨油层浅水湖泊—三角洲体系沉积特征[M] .大庆石油地质与开发,2005,24(5):13～16.
[79] Evans J,Cade C,Bryant S.A geological approach to permeability prediction in clasdtic reservoir[J].AAPG Memoir,1997,69: 91～101.
[80] Osborne M J and Swarbrick R E.Diagenesis in North Sea HPHT classic reservoirs-consequences for porosity and overpressure prediction[J].Marine and Petroleum Geology,1999,16:337～353.
[81] Ramm M and Bjorlykke K.Porosity/depth trends in reservoir sandstones:assessing the quantitative effects of varying Pore-Pressure,Temperature History and Mineralogy,Norwegian Shelf Data[J].Clay Minerals,1994,29:475～490.
[82] Schmoker J M, Hester T C. Regional trends of sandstone porosity vs. vitrinite reflectance-a preliminary framework. Applications of thermal maturity studies to energy exploration[J]. Rocky Mountain Section of SEMP,1990,53～60.
[83] Wilson M D, Byrnes A P. Model design [A],In: Wilson W D,ed.Reservoir quality assessment and prediction in clastic rocks.SEPM Short Course,1994, 30:209～230.
[84] Sombra C L,Kiang C H.Burial history and porosity evolution of Brazilian Upper Jurassic to Tertiary sandstone reservoirs[A].In: Kupecz eds.Reservoir quality prediction in sandstones and carbonates. AAPG Memoir 69,1997,26:79～89.
[85] Gluyas J and Cade C A.Prediction of porosity in compacted sands. AAPG Memoir, 1997,69:19～27.
[86] Paxton ST, Szabo J O, Ajdukiewicz J M ,et al.Construction of an intergranular volume compaction curve for evaluating and predicting compaction and porosity loss in rigid-grain sandstone reservoirs[J].AAPG Bulletin,2002,86(12):2047～2069.
[87]罗平,裘怿楠,贾爱林等.中国油气储层地质研究面临的挑战和发展方向[J].沉积学报,2003,21(1):142～147.
[88]朱国华.碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3):114～121.
[89]姜培海,杨小丽.利用储层沉积学参数预测储层孔隙度[J].中国海上油气(地质),1997,11(4):261～267.
[90]武文来,周士科.渤海海域深部碎屑岩储层孔隙度预测[J].中国海上油气(地质),1997,11(4):241～248.
[91]寿建峰,朱国华.砂岩储层孔隙保存的定量预测研究[J].地质科学,1998,33(2):244～249.
[92]杨香华,叶加仁,周士科等.成岩动力学分析与深部储层孔隙度预测[J].现代地质,1998,12(1):108～114.
[93]王粤川,孟元林,贺如等.用时深效应指数预测储层孔隙度-以辽河西部凹陷沙三中亚段为例[J].中国海上油气,2007,18(5):308～312.