徐家围子断陷营城组火山岩储层特征研究
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摘要
徐家围子断陷特殊储层的勘探取得了良好的效果,展示了特殊储层良好的天然气勘探前景。本论文以火山岩岩石学、储层沉积学等理论为指导,认真分析和借鉴前人研究成果,以25口、17个项目300多块岩心样品的实验室室内岩心分析数据为基础,研究徐家围子断陷营城组火山岩储层特征,并对徐深1井进行单井评价。
研究过程中,采用了核磁和CT两项实验技术,用于确定岩心内部孔隙和裂缝的形态、展布,解决裂缝研究中遇到的问题。
通过制定火山岩天然气储层分类标准和确定的有效孔隙度勘探下限,解决了储量计算中遇到的问题,对生产起到指导作用。
对有利储层的岩性、岩相、孔隙类型和分布做了具体的分析,对成岩作用进行了深入研究,为深层天然气勘探提供依据。确定了火山岩好储层为流纹岩、安山岩、集块岩和风化淋滤带的晶屑凝灰岩,孔隙类型为气孔、杏仁孔、晶粒间孔、斑晶溶孔和构造裂缝、炸裂缝,发育地区以升平-兴城-肇州地区营城组为主。
按本文的分类标准,火山岩前三类储层压裂后具有工业产能,火山岩Ⅳ、Ⅴ类在目前工艺条件下压裂难获工业产能,有效储层孔隙度下限为4%,裂缝型储层孔隙度下限可以低于该值。
通过对火山岩相与火山岩孔隙和裂缝成因、类型及成岩演化规律等系统研究后认为,好的储层一般位于喷溢相的上部亚相或大段火山岩上部的风化淋滤带,主要地区为升平和肇州地区营城组。
确认了胶结和溶解作用是影响储层物性的主要因素以及胶结作用主要发生位置。
Exploration of the special reservoirs of Xujiaweizi fault depression have gained good effectiveness and show the cheerful prospect of gas exploration. This subject research on the volcanic reservoir characteristics of Yingcheng formation of Xujiaweizi fault depression, based on the laboratory core analysis data of 25 wells, 17 items more than 300 core samples.
Applying the two experimental techniques, NMR and CT, to determine the type and distribution of porosity and fraction in the reservoirs of volcanic rock.
This subject stablishes standard of evaluation and classification of reservoirs of volcanic rock, gives the lower limit value of effective porosity, that solve the difficult problems in the reserves calculation and guide the research and the production..
This subject provided an gist for the breakthrough of exploration for the deep-seated natural gas. A material prediction about lithology, lithofacies, type and distributing of pore and the study in-depth about diagenism of reservoir were worked out. Identified that, the better volcanic reservoirs are rhyolite, andesite, agglomerate and crystal tuff in the place of weathering and corrosion. The type of pore includes primary vesicular, inneramygdale pore, intercrystalline pore, phenocryst corroded pore and structure fracture, exploding fracture. The developed places lie in Yingcheng oil formation of Shengping-Xingcheng-Zhaozhou.
According to the standard of reservoir classification giving by this subject, the frontal three types of volcanic reservoirs can obtain industrial productivity after fracturing.Ⅳ,Ⅴvolcanic reservoirs can not obtain industrial productivity after fracturing in the actual technological conditions. The lower limit value of effective porosity is 4%. The lower limit value of fracture reservoir may be under this value.
Through the systems study for volcanic lithofacies and cause, type and diagenetic evolvement rule of pore and fracture, it can be obtained that better reservoirs mainly lie in the upper introfacies of eruptive facies or the zone of weathering and corrosion of the upper volcanic rock, Yingcheng oil formation of Shengping and Zhaozhou.
Confirmed the cementation and solution are the main factors influencing the especial reservoir quality, and the location of cementation mainly occurs.
研究过程中,采用了核磁和CT两项实验技术,用于确定岩心内部孔隙和裂缝的形态、展布,解决裂缝研究中遇到的问题。
通过制定火山岩天然气储层分类标准和确定的有效孔隙度勘探下限,解决了储量计算中遇到的问题,对生产起到指导作用。
对有利储层的岩性、岩相、孔隙类型和分布做了具体的分析,对成岩作用进行了深入研究,为深层天然气勘探提供依据。确定了火山岩好储层为流纹岩、安山岩、集块岩和风化淋滤带的晶屑凝灰岩,孔隙类型为气孔、杏仁孔、晶粒间孔、斑晶溶孔和构造裂缝、炸裂缝,发育地区以升平-兴城-肇州地区营城组为主。
按本文的分类标准,火山岩前三类储层压裂后具有工业产能,火山岩Ⅳ、Ⅴ类在目前工艺条件下压裂难获工业产能,有效储层孔隙度下限为4%,裂缝型储层孔隙度下限可以低于该值。
通过对火山岩相与火山岩孔隙和裂缝成因、类型及成岩演化规律等系统研究后认为,好的储层一般位于喷溢相的上部亚相或大段火山岩上部的风化淋滤带,主要地区为升平和肇州地区营城组。
确认了胶结和溶解作用是影响储层物性的主要因素以及胶结作用主要发生位置。
Exploration of the special reservoirs of Xujiaweizi fault depression have gained good effectiveness and show the cheerful prospect of gas exploration. This subject research on the volcanic reservoir characteristics of Yingcheng formation of Xujiaweizi fault depression, based on the laboratory core analysis data of 25 wells, 17 items more than 300 core samples.
Applying the two experimental techniques, NMR and CT, to determine the type and distribution of porosity and fraction in the reservoirs of volcanic rock.
This subject stablishes standard of evaluation and classification of reservoirs of volcanic rock, gives the lower limit value of effective porosity, that solve the difficult problems in the reserves calculation and guide the research and the production..
This subject provided an gist for the breakthrough of exploration for the deep-seated natural gas. A material prediction about lithology, lithofacies, type and distributing of pore and the study in-depth about diagenism of reservoir were worked out. Identified that, the better volcanic reservoirs are rhyolite, andesite, agglomerate and crystal tuff in the place of weathering and corrosion. The type of pore includes primary vesicular, inneramygdale pore, intercrystalline pore, phenocryst corroded pore and structure fracture, exploding fracture. The developed places lie in Yingcheng oil formation of Shengping-Xingcheng-Zhaozhou.
According to the standard of reservoir classification giving by this subject, the frontal three types of volcanic reservoirs can obtain industrial productivity after fracturing.Ⅳ,Ⅴvolcanic reservoirs can not obtain industrial productivity after fracturing in the actual technological conditions. The lower limit value of effective porosity is 4%. The lower limit value of fracture reservoir may be under this value.
Through the systems study for volcanic lithofacies and cause, type and diagenetic evolvement rule of pore and fracture, it can be obtained that better reservoirs mainly lie in the upper introfacies of eruptive facies or the zone of weathering and corrosion of the upper volcanic rock, Yingcheng oil formation of Shengping and Zhaozhou.
Confirmed the cementation and solution are the main factors influencing the especial reservoir quality, and the location of cementation mainly occurs.
引文
[1]钱伯章.当代天然气工业及其发展前景[J].天然气与石油, 2002, 20(2):16~20.
[2]张玉清,王晶. 2025年天然气消费量有可能超过石油[J].中国能源, 2004, 26(6):19.
[3]刘超,李俊岭等. 21世纪能源、环境与过程工程探讨[J].化工进展, 2002, 21(1):13~16.
[4]何文渊,刘晖等.加快我国天然气工业发展的建议[J].天然气工业, 2004, 24(6):4~7.
[5]张大伟.中国油气资源可持续供给战略与对策[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 38~44.
[6]杜灵通.中国天然气资源的分布特征及勘探前景[J].油气地质与采收率, 2005, 12(2):30~32.
[7]王庭斌.深化油气地质理论,实现油气资源可持续发展[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 68~79.
[8]邱中建.对我国油气资源可持续发展的一些看法[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 1~8.
[9]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].北京:石油工业出版社, 1997, 181~211.
[10]王永春.松辽盆地南部岩性油气藏的形成和分布[M].北京:石油工业出版社, 2001, 97~130.
[11]谢晓安,周卓明.松辽盆地深层天然气勘探实践与勘探领域[J].石油与天然气地质, 2008, 29(1):113~119.
[12]齐景顺.松辽盆地北部深层火山岩天然气勘探实践[J].石油与天然气地质, 2007, 28(5):590~596.
[13]冯志强.松辽盆地北部及海拉尔盆地油气勘探进展与潜力分析[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 110~117.
[14] Hunter B E, Davis D K.Distribution of volcanic sediments in the Golf coastal Province-significance to petroleum geology[J]. Transactions, Golf Coast Association of Geological Societies, 1979, 29(1):147-155.
[15] Homvc J F. Hydrocarbon Exploration Potential Within Intraplate Shear-Related Depocenters:Deseado And San Julian Basins,Southern Argentina[J]. AAPG BULL, 2001, 85(10):1795-1816.
[16] Hawlander H M. Diagenesis and reservoir potential of volcanogenic sandstone-Cretaceous of the Surat Basin,Australia[J]. Sedimentary Geology, 1990, 66(3/4):181-195.
[17]杜贤樾,肖焕钦.渤海湾盆地火成岩油气藏勘探研究进展[J].复式油气田, 1998,4:1~4.
[18]王惠民等.准噶尔盆地火山岩与构造热事件研究[J].新疆石油地质, 1999, 20:580~584.
[19]罗静兰,曲志浩等.风化店火山岩成因,储集孔隙类型及其火山岩相与油气的关系[J].石油学报, 1996, 17(1):32~39.
[20]刘惠民等.济阳坳陷下第三系火成岩油藏岩相研究[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004, 178~182.
[21]李丕龙.高勘探程度区隐蔽油气藏勘探-以济阳坳陷为例[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004, 12~16.
[22]刘泽容,信全麟等.山东惠民凹陷西部第三纪火山岩油藏形成条件与分布规律[J].地质学报, 1988, 62(3):210~222.
[23]陈岩.克拉玛依油田石炭系火山岩油藏剖析[J].新疆石油地质, 1988, 9(1):17~31.
[24]杨新明.闵桥油田火山岩油藏储层特征研究[J].江苏油气, 1993, 4(3):24~31.
[25]何琰,伍友佳等.火山岩油气藏研究[J].大庆石油地质与开发. 1998, 18(4):6~8.
[26]郎东升.大庆油区火成岩储层识别综合研究[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004:329~334
[27]石宝珩,张抗等.中国石油地质学五十年[J].江汉石油学院学报, 1999, 21(3):1~8.
[28]陈建文.一门新兴的边缘科学——火山岩储层地质学[J].海洋地质动态, 2002, 18(4):19~22.
[29] WANG P et al. Relationship Between Volcanic Facies and Volcanic Reservoirs in Songliao Basin[J]. Oil Gas Geol, 2003, 24(1):18~23。
[30]陈嵘,高楚桥等.交会图技术在识别三塘湖盆地火成岩岩性中的应用[J].测井技术, 2009, 21(3):94~97.
[31]范宜仁,黄隆基等.交会图技术在火山岩岩性与裂缝识别中的应用[J].测井技术, 1999, 23(1):53~56.
[32]卞德志,邱子刚.模糊数学识别火成岩岩性的方法及地质效果[C].测井资料的地质应用.北京:石油工业出版社, 1991, 57~67.
[33]景永奇,秦瑞宝.利用裂缝指示曲线判别花岗岩潜山纵向裂缝发育带[J].测井技术, 1999, 1:38~42.
[34]郝秀权,杨建军.裂缝指示曲线在花岗岩潜山裂缝评价中的应用[J].测井技术, 2001, 1:13~17.
[35]匡立春.克拉玛依油田5-8区二叠系佳木河组火成岩岩性识别[J].石油与天然气地质, 1990, 11(2):193~201.
[36]刘呈冰,史占国等.全面评价低孔裂缝/孔洞型碳酸盐岩及火成岩储层[J].测井技术, 1999, 23(6):457~465.
[37] Draxler J K. Estimation of the mineral content of crystalline rocks in theKTB-Oberpfalz VB[J]. Scientific Drilling, 1992, 3(3):115-125.
[38] Eberle D. Interpretation of multi-method geophysical borehole logging data from KTB Oberpfalz VB using multivariate statistical analyses[J]. Scientific Drilling, 1992, 3(3):16-26.
[39] Liu W. Comprehensive Evaluation of Volcanic Reservoir by Fuzzy Mathematics. Petrol Geol Recovery Efficiency, 2003, 10(2):9-10.
[40] Zimmermann G. Burkhard H.Estimation of porosity in crystalline rock by a multivariate statistical approach[J]. Scientific Drilling, 1992, 3(3):27-35.
[41]于星河,李剑锋.油气储层研究所面临的挑战与新动向[J].地学前缘, 1995, 2(4):213~220.
[42] Dai J S. Prediction of Volcanic Rock Fissure With Finite Deformation Method[J]. Jun Petrol,China, 2003, 27(1):1-3.
[43] Zhou F. Application of Nonlinear Deformation to Volcanic Fissure Prediction in Min 7 Block of JinHu Sag[J]. Recovery Efficiency, 2003, 10(1):12-13.
[44] Sobehrad J, Foote R S. Aerial Magnetic Reconnaissance Technique Finds Leads in Morocco[J]. Oil Gas, 2004, 102(4):44-48.
[45] Li Y. Discussion On Quantitative Prediction of Deep Volcanic Reservoir[J]. Oil Geophysical Prospecting, 2002, 37(2):175-179.
[46]裘亦楠,薛淑浩.油气储层评价技术[M].北京:石油工业出版社, 1997, 90~94.
[47]王德发,陈建文等.中国陆相储层表征与成藏型式[J].地学前缘, 2000, 7(4):363~369.
[48]冉建斌,康南昌等. AHDAB油田碳酸盐岩储层综合研究[J].石油地球物理勘探, 2004, 39(3):304~309.
[49]陈恭洋.碎屑岩储层随机建模的基本理论与实践[J].江汉石油学院学报, 2001, 23(4):1~4.
[50]于兴河,陈永峤.碎屑岩系的八大沉积作用与其油气储层表征[J].石油实验地质, 2004, 26(6):517~524.
[51] Van Riel P. The past, present, and future of quantitative reservoir characterization[J]. Leading Edge, 2000, 19(8):878-881.
[52]王志宏,罗霞等.松辽盆地北部深层有效烃源岩分布预测[J].天然气地球科学, 2008, 19(2):204~209.
[53]杨峰平.松辽盆地徐家围子断陷火山岩及天然气成藏研究[D].北京:中国地质大学(北京),2005.
[54]谭文化,李胜荣等.大庆徐家围子火山岩热释光特征与火山活动期次及岩性判别[J].岩石矿物学杂志, 2007, 26(3):247~252.
[55]侯启军.松辽盆地古龙地区天然气勘探方向[J].石油勘探与开发, 2005,32(5):38~41.
[56]宋宗平,姜传金等.兴城—丰乐地区深层火山岩储层识别[J].天然气工业, 2007, 27(8):28~30.
[57]曹宝军,李相方等.火山岩气藏开发难点与对策[J].天然气工业, 2007, 27(8):82~84.
[58]乐昌硕.岩石学[M].北京:地质出版社, 1984.
[59]窦立荣.油气藏地质学概论[M].石油工业出版社, 2001.
[60]赵澄林等.特殊油气储层[M].北京:石油工业出版社, 1997.
[61]张春露.火山岩含气储层有效孔隙度确定方法[J].国外测井技术, 2008, 23(1):25~27.
[62]魏斌,陈建文等.徐家围子断陷火山岩岩性的测井识别技术[J].特种油气藏, 2003, 10(1):73~75.
[63]袁云峰,秦启荣等.火山岩岩性识别技术发展现状研究[J].内蒙古石油化工, 2007,33(5):270~272.
[64]杨双玲,刘万洙等.松辽盆地火山岩储层储集空间特征及其成因[J].吉林大学学报:地球科学版, 2007,37(3):506~512.
[65]王璞珺,郑常青等.松辽盆地深层火山岩岩性分类方案[J].大庆石油地质与开发, 2007,26(4):17~22.
[66]舒萍,丁日新等.徐深气田火山岩储层岩性岩相模式[J].天然气工业, 2007,27(8):23~27.
[67]赵文智,邹才能等.松辽盆地深层火山岩气藏地质特征及评价技术[J].石油勘探与开发, 2008, 35(2):129~142.
[68]冯志强,王玉华等.松辽盆地深层火山岩气藏勘探技术与进展[J].天然气工业, 2007, 27(8):9~12.
[69]杨辉,宋吉杰等.火山岩岩性宏观预测方法—以松辽盆地北部徐家围子断陷为例[J].石油勘探与开发, 2007, 34(2):150~155.
[70]王璞珺,迟元林等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学, 2003, 33(4):449~456.
[71]王璞珺,吴河勇等.松辽盆地火山岩相:相序、相模式与储层物性的定量关系[J].吉林大学学报:地球科学版, 2006, 36(5):805~812.
[72]刘万洙,王璞珺等.松辽盆地北部深层火山岩储层特征[J].石油与天然气地质, 2003, 24(1):28~31.
[73]王拥军,胡永乐等.深层火山岩气藏储层裂缝发育程度评价[J].天然气工业, 2007, 27(8):31~34.
[74]王璞珺,陈树民等.松辽盆地火山岩相与火山岩储层的关系[J].石油与天然气地质, 2003, 24(1):18~23.
[75]王芙蓉,陈振林等.火山岩储集性研究[J].重庆石油高等专科学校学报, 2003, 5(3):44~46.
[76]文瑞霞等.火山岩储层地震特征及识别方法.中国地球物理学会第二十二届年会论文集[C].成都:四川科学技术出版社, 2006, 86.
[77]朱德丰等.松辽盆地北部深层天然气勘探突破方向研究[R].大庆:大庆油田有限责任公司勘探开发研究院,2003.4~16.
[78]彭彩珍,郭平等.流纹岩类火山岩储层物性特征研究[J].西南石油学院学报, 2004, 26(3):12-15.
[2]张玉清,王晶. 2025年天然气消费量有可能超过石油[J].中国能源, 2004, 26(6):19.
[3]刘超,李俊岭等. 21世纪能源、环境与过程工程探讨[J].化工进展, 2002, 21(1):13~16.
[4]何文渊,刘晖等.加快我国天然气工业发展的建议[J].天然气工业, 2004, 24(6):4~7.
[5]张大伟.中国油气资源可持续供给战略与对策[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 38~44.
[6]杜灵通.中国天然气资源的分布特征及勘探前景[J].油气地质与采收率, 2005, 12(2):30~32.
[7]王庭斌.深化油气地质理论,实现油气资源可持续发展[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 68~79.
[8]邱中建.对我国油气资源可持续发展的一些看法[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 1~8.
[9]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].北京:石油工业出版社, 1997, 181~211.
[10]王永春.松辽盆地南部岩性油气藏的形成和分布[M].北京:石油工业出版社, 2001, 97~130.
[11]谢晓安,周卓明.松辽盆地深层天然气勘探实践与勘探领域[J].石油与天然气地质, 2008, 29(1):113~119.
[12]齐景顺.松辽盆地北部深层火山岩天然气勘探实践[J].石油与天然气地质, 2007, 28(5):590~596.
[13]冯志强.松辽盆地北部及海拉尔盆地油气勘探进展与潜力分析[C].中国石油地质年会论文集.北京:石油工业出版社, 2004, 110~117.
[14] Hunter B E, Davis D K.Distribution of volcanic sediments in the Golf coastal Province-significance to petroleum geology[J]. Transactions, Golf Coast Association of Geological Societies, 1979, 29(1):147-155.
[15] Homvc J F. Hydrocarbon Exploration Potential Within Intraplate Shear-Related Depocenters:Deseado And San Julian Basins,Southern Argentina[J]. AAPG BULL, 2001, 85(10):1795-1816.
[16] Hawlander H M. Diagenesis and reservoir potential of volcanogenic sandstone-Cretaceous of the Surat Basin,Australia[J]. Sedimentary Geology, 1990, 66(3/4):181-195.
[17]杜贤樾,肖焕钦.渤海湾盆地火成岩油气藏勘探研究进展[J].复式油气田, 1998,4:1~4.
[18]王惠民等.准噶尔盆地火山岩与构造热事件研究[J].新疆石油地质, 1999, 20:580~584.
[19]罗静兰,曲志浩等.风化店火山岩成因,储集孔隙类型及其火山岩相与油气的关系[J].石油学报, 1996, 17(1):32~39.
[20]刘惠民等.济阳坳陷下第三系火成岩油藏岩相研究[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004, 178~182.
[21]李丕龙.高勘探程度区隐蔽油气藏勘探-以济阳坳陷为例[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004, 12~16.
[22]刘泽容,信全麟等.山东惠民凹陷西部第三纪火山岩油藏形成条件与分布规律[J].地质学报, 1988, 62(3):210~222.
[23]陈岩.克拉玛依油田石炭系火山岩油藏剖析[J].新疆石油地质, 1988, 9(1):17~31.
[24]杨新明.闵桥油田火山岩油藏储层特征研究[J].江苏油气, 1993, 4(3):24~31.
[25]何琰,伍友佳等.火山岩油气藏研究[J].大庆石油地质与开发. 1998, 18(4):6~8.
[26]郎东升.大庆油区火成岩储层识别综合研究[C].隐蔽油气藏形成机理与勘探实践,北京:石油工业出版社, 2004:329~334
[27]石宝珩,张抗等.中国石油地质学五十年[J].江汉石油学院学报, 1999, 21(3):1~8.
[28]陈建文.一门新兴的边缘科学——火山岩储层地质学[J].海洋地质动态, 2002, 18(4):19~22.
[29] WANG P et al. Relationship Between Volcanic Facies and Volcanic Reservoirs in Songliao Basin[J]. Oil Gas Geol, 2003, 24(1):18~23。
[30]陈嵘,高楚桥等.交会图技术在识别三塘湖盆地火成岩岩性中的应用[J].测井技术, 2009, 21(3):94~97.
[31]范宜仁,黄隆基等.交会图技术在火山岩岩性与裂缝识别中的应用[J].测井技术, 1999, 23(1):53~56.
[32]卞德志,邱子刚.模糊数学识别火成岩岩性的方法及地质效果[C].测井资料的地质应用.北京:石油工业出版社, 1991, 57~67.
[33]景永奇,秦瑞宝.利用裂缝指示曲线判别花岗岩潜山纵向裂缝发育带[J].测井技术, 1999, 1:38~42.
[34]郝秀权,杨建军.裂缝指示曲线在花岗岩潜山裂缝评价中的应用[J].测井技术, 2001, 1:13~17.
[35]匡立春.克拉玛依油田5-8区二叠系佳木河组火成岩岩性识别[J].石油与天然气地质, 1990, 11(2):193~201.
[36]刘呈冰,史占国等.全面评价低孔裂缝/孔洞型碳酸盐岩及火成岩储层[J].测井技术, 1999, 23(6):457~465.
[37] Draxler J K. Estimation of the mineral content of crystalline rocks in theKTB-Oberpfalz VB[J]. Scientific Drilling, 1992, 3(3):115-125.
[38] Eberle D. Interpretation of multi-method geophysical borehole logging data from KTB Oberpfalz VB using multivariate statistical analyses[J]. Scientific Drilling, 1992, 3(3):16-26.
[39] Liu W. Comprehensive Evaluation of Volcanic Reservoir by Fuzzy Mathematics. Petrol Geol Recovery Efficiency, 2003, 10(2):9-10.
[40] Zimmermann G. Burkhard H.Estimation of porosity in crystalline rock by a multivariate statistical approach[J]. Scientific Drilling, 1992, 3(3):27-35.
[41]于星河,李剑锋.油气储层研究所面临的挑战与新动向[J].地学前缘, 1995, 2(4):213~220.
[42] Dai J S. Prediction of Volcanic Rock Fissure With Finite Deformation Method[J]. Jun Petrol,China, 2003, 27(1):1-3.
[43] Zhou F. Application of Nonlinear Deformation to Volcanic Fissure Prediction in Min 7 Block of JinHu Sag[J]. Recovery Efficiency, 2003, 10(1):12-13.
[44] Sobehrad J, Foote R S. Aerial Magnetic Reconnaissance Technique Finds Leads in Morocco[J]. Oil Gas, 2004, 102(4):44-48.
[45] Li Y. Discussion On Quantitative Prediction of Deep Volcanic Reservoir[J]. Oil Geophysical Prospecting, 2002, 37(2):175-179.
[46]裘亦楠,薛淑浩.油气储层评价技术[M].北京:石油工业出版社, 1997, 90~94.
[47]王德发,陈建文等.中国陆相储层表征与成藏型式[J].地学前缘, 2000, 7(4):363~369.
[48]冉建斌,康南昌等. AHDAB油田碳酸盐岩储层综合研究[J].石油地球物理勘探, 2004, 39(3):304~309.
[49]陈恭洋.碎屑岩储层随机建模的基本理论与实践[J].江汉石油学院学报, 2001, 23(4):1~4.
[50]于兴河,陈永峤.碎屑岩系的八大沉积作用与其油气储层表征[J].石油实验地质, 2004, 26(6):517~524.
[51] Van Riel P. The past, present, and future of quantitative reservoir characterization[J]. Leading Edge, 2000, 19(8):878-881.
[52]王志宏,罗霞等.松辽盆地北部深层有效烃源岩分布预测[J].天然气地球科学, 2008, 19(2):204~209.
[53]杨峰平.松辽盆地徐家围子断陷火山岩及天然气成藏研究[D].北京:中国地质大学(北京),2005.
[54]谭文化,李胜荣等.大庆徐家围子火山岩热释光特征与火山活动期次及岩性判别[J].岩石矿物学杂志, 2007, 26(3):247~252.
[55]侯启军.松辽盆地古龙地区天然气勘探方向[J].石油勘探与开发, 2005,32(5):38~41.
[56]宋宗平,姜传金等.兴城—丰乐地区深层火山岩储层识别[J].天然气工业, 2007, 27(8):28~30.
[57]曹宝军,李相方等.火山岩气藏开发难点与对策[J].天然气工业, 2007, 27(8):82~84.
[58]乐昌硕.岩石学[M].北京:地质出版社, 1984.
[59]窦立荣.油气藏地质学概论[M].石油工业出版社, 2001.
[60]赵澄林等.特殊油气储层[M].北京:石油工业出版社, 1997.
[61]张春露.火山岩含气储层有效孔隙度确定方法[J].国外测井技术, 2008, 23(1):25~27.
[62]魏斌,陈建文等.徐家围子断陷火山岩岩性的测井识别技术[J].特种油气藏, 2003, 10(1):73~75.
[63]袁云峰,秦启荣等.火山岩岩性识别技术发展现状研究[J].内蒙古石油化工, 2007,33(5):270~272.
[64]杨双玲,刘万洙等.松辽盆地火山岩储层储集空间特征及其成因[J].吉林大学学报:地球科学版, 2007,37(3):506~512.
[65]王璞珺,郑常青等.松辽盆地深层火山岩岩性分类方案[J].大庆石油地质与开发, 2007,26(4):17~22.
[66]舒萍,丁日新等.徐深气田火山岩储层岩性岩相模式[J].天然气工业, 2007,27(8):23~27.
[67]赵文智,邹才能等.松辽盆地深层火山岩气藏地质特征及评价技术[J].石油勘探与开发, 2008, 35(2):129~142.
[68]冯志强,王玉华等.松辽盆地深层火山岩气藏勘探技术与进展[J].天然气工业, 2007, 27(8):9~12.
[69]杨辉,宋吉杰等.火山岩岩性宏观预测方法—以松辽盆地北部徐家围子断陷为例[J].石油勘探与开发, 2007, 34(2):150~155.
[70]王璞珺,迟元林等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学, 2003, 33(4):449~456.
[71]王璞珺,吴河勇等.松辽盆地火山岩相:相序、相模式与储层物性的定量关系[J].吉林大学学报:地球科学版, 2006, 36(5):805~812.
[72]刘万洙,王璞珺等.松辽盆地北部深层火山岩储层特征[J].石油与天然气地质, 2003, 24(1):28~31.
[73]王拥军,胡永乐等.深层火山岩气藏储层裂缝发育程度评价[J].天然气工业, 2007, 27(8):31~34.
[74]王璞珺,陈树民等.松辽盆地火山岩相与火山岩储层的关系[J].石油与天然气地质, 2003, 24(1):18~23.
[75]王芙蓉,陈振林等.火山岩储集性研究[J].重庆石油高等专科学校学报, 2003, 5(3):44~46.
[76]文瑞霞等.火山岩储层地震特征及识别方法.中国地球物理学会第二十二届年会论文集[C].成都:四川科学技术出版社, 2006, 86.
[77]朱德丰等.松辽盆地北部深层天然气勘探突破方向研究[R].大庆:大庆油田有限责任公司勘探开发研究院,2003.4~16.
[78]彭彩珍,郭平等.流纹岩类火山岩储层物性特征研究[J].西南石油学院学报, 2004, 26(3):12-15.