上覆优质源岩对上生下储式致密油成藏的控制作用——以松南中央坳陷区青一段泥岩为例
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摘要
基于优质源岩在致密油成藏过程中的作用越来越显著,以松南中央坳陷区青一段泥岩为例,综合运用测井、录井及地球化学测试等资料,提出由排烃角度建立源岩评价标准,在此基础上,综合优质源岩的供烃能力、古超压发育特征及封盖能力等因素,详细阐述其对下伏泉四段致密油成藏的控制作用.研究结果表明:青一段暗色泥岩有机质类型以I型和II_1型为主,具有丰度高、类型好、生烃潜力大的特征,其中,TOC>2.0%,Ro>0.9%的泥岩排烃量明显增大,为优质烃源岩;优质烃源岩厚度由湖盆边缘向沉积中心逐渐增加,纵向上主要集中在青一段下段,平面上以长岭凹陷中、北部和红岗阶地东部海坨子地区最为发育;研究区青一段优质源岩的展布范围控制了泉四段致密油藏的分布格局;其累计厚度及生、排烃强度控制油源充足程度,使得石油最大下排深度达160m;青一段古超压是石油下排的充注动力,其与油源断层的配置关系控制了泉四段下部砂组的油气富集程度;此外,青一下亚段的优质源岩为泉四段致密油藏的保存提供有效封盖.
Based on the more and more significant function of high-quality source rocks in the process of tight oil reservoir,this paper studied the mudstone in Q_(n1) formation at central depression in southern Songliao basin,by using logging data and geochemical analysis data,and proposed the viewpoint of establishing the evaluation standard of source rocks from the angle of hydrocarbon expulsion.On these foundations,this paper elaborated its controlling function ontight oil reservoir in Q_4 formation,by colligating the hydrocarbon supplying ability,ancient overpressure characteristics and sealing ability of high-quality source rocks in Q_(n1) formation.The results show that the types of dark mudstone's organic matter in Q_(n1) formation mainly are I and II1 type,which have the characteristics of high abundance,good types and great potential of hydrocarbon generation.Among them,the mudstone whose TOC>2.0% and Ro>0.9%and has an obvious increase of the hydrocarbon expulsion is high-quality source rocks and its thickness increases gradually from the edge to the sedimentary center of the lake basin.Highquality source rocks mainly distributes in lower Qn1 formation in the vertical and mostly develops in northern and central of Changling depression and Haituozi area in Honggang terrace on the plane.In these study areas,the distribution range of high-quality source rocks in Q_(n1) formation controls the distribution pattern of tight oil reservoir in Q_4 formation.The high-quality source rocks' cumulative thickness,generation and expulsion intensity of hydrocarbon controls the degree of oil source,which prompts the maximum downward-migration depth of oil in Q_4 formation reach to 160 m.The ancient overpressure in Q_(n1) formation is filling power for oil's downward migration,whose match relationship with source faults controls the oiliness of lower sand group in Q_4 formation.What's more,the high-quality source rocks in lower Q_(n1) formation provides effective sealing for tight oil reservoir in Q_4 formation.
Based on the more and more significant function of high-quality source rocks in the process of tight oil reservoir,this paper studied the mudstone in Q_(n1) formation at central depression in southern Songliao basin,by using logging data and geochemical analysis data,and proposed the viewpoint of establishing the evaluation standard of source rocks from the angle of hydrocarbon expulsion.On these foundations,this paper elaborated its controlling function ontight oil reservoir in Q_4 formation,by colligating the hydrocarbon supplying ability,ancient overpressure characteristics and sealing ability of high-quality source rocks in Q_(n1) formation.The results show that the types of dark mudstone's organic matter in Q_(n1) formation mainly are I and II1 type,which have the characteristics of high abundance,good types and great potential of hydrocarbon generation.Among them,the mudstone whose TOC>2.0% and Ro>0.9%and has an obvious increase of the hydrocarbon expulsion is high-quality source rocks and its thickness increases gradually from the edge to the sedimentary center of the lake basin.Highquality source rocks mainly distributes in lower Qn1 formation in the vertical and mostly develops in northern and central of Changling depression and Haituozi area in Honggang terrace on the plane.In these study areas,the distribution range of high-quality source rocks in Q_(n1) formation controls the distribution pattern of tight oil reservoir in Q_4 formation.The high-quality source rocks' cumulative thickness,generation and expulsion intensity of hydrocarbon controls the degree of oil source,which prompts the maximum downward-migration depth of oil in Q_4 formation reach to 160 m.The ancient overpressure in Q_(n1) formation is filling power for oil's downward migration,whose match relationship with source faults controls the oiliness of lower sand group in Q_4 formation.What's more,the high-quality source rocks in lower Q_(n1) formation provides effective sealing for tight oil reservoir in Q_4 formation.
引文
[1]US Energy Information Administration.Annual energy outlook 2012,with projections to 2035[R].Washington D C:Energy Information Administration,2012.
[2]贾承造,郑民,张永峰.中国非常规油气资源与勘探开发前景[J].石油勘探与开发,2012,39(2):129-136.JIA Chengzao,ZHENG Min,ZHANG Yongfeng.Unconventional hydrocarbon resources in China and the prospect of exploration and development[J].Petroleum Exploration and Development,2012,39(2):129-136.
[3]祝海华,钟大康,姚泾利,等.鄂尔多斯西南地区长7段致密油储层微观特征及成因机理[J].中国矿业大学学报,2014,43(5):853-862.ZHU Haihua,ZHONG Dakang,YAO Jingli,et al.Microscopic characteristics and formation mechanism of Upper Triassic Chang7tight oil reservoir in the southwest Ordos basin[J].Journal of China University of Mining&Technology,2014,43(5):853-862.
[4]邹才能,朱如凯,吴松涛,等.常规与非常规油气聚集类型、特征、机理及展望:以中国致密油和致密气为例[J].石油学报,2012,33(2):173-187.ZOU Caineng,ZHU Rukai,WU Songtao,et al.Types,characteristics,genesis and prospects of conventional and unconventional hydrocarbon accumulations:taking tight oil and tight gas in China as an instance[J].Acta Petrolei Sinica,2012,33(2):173-187.
[5]ANONYMOUS.HIS:World's tight oil resources hold large potential[J].Oil&Gas Journal,2013,111(9d):27.
[6]SNOW,NICK.A coming tight oil bonanza[J].Oil&Gas Journal,2011,109(19b):22.
[7]YAO Jingli,DENG Xiuqin,ZHAO Yande,et al.Characteristics of tight oil in Triassic Yanchang formation,Ordos basin[J].Petroleum Exploration and Development,2013,Vol.40(2):161-169.
[8]马中振,戴国威,盛晓峰,等.松辽盆地北部连续型致密砂岩油藏的认识及其地质意义[J].中国矿业大学学报,2013,42(2):221-229.MA Zhongzhen,DAI Guowei,SHENG Xiaofeng,et al.Tight sand oil reservoir of continuous type in northern Songliao basin and its geological significance[J].Journal of China University of Mining&Technology,2013,42(2):221-229.
[9]张妮妮,刘洛夫,苏天喜,等.鄂尔多斯盆地延长组长7段与威利斯顿盆地Bakken组致密油形成条件的对比及其意义[J].现代地质,2013,27(5):1120-1130.ZHANG Nini,LIU Luofu,SU Tianxi,et al.Comparison of Chang 7member of Yanchang formation in Ordos basin with Bakken formation in Williston basin and its significance[J].Geoscience,2013,27(5):1120-1130.
[10]宋岩,姜林,马行陟.非常规油气藏的形成及其分布特征[J].古地理学报,2013,15(5):605-614.SONG Yan,JIANG Lin,MA Xingzhi.Formation and distribution characteristics of unconventional oil and gas reservoirs[J].Journal of Palaeogeography,2013,15(5):605-614.
[11]中石油吉林油田勘探研究院.松南扶余油层致密油成藏规律研究[R].松原:中石油吉林油田勘探研究院,2014.
[12]金强,朱光有,王娟.咸化湖盆优质烃源岩的形成和分布[J].中国石油大学学报(自然科学版),2008,32(4):19-24.JIN Qiang,ZHU Guangyou,WANG Juan.Depositon and distribution of high-potiential source rocks in saline lacustrine environments[J].Journal of China University of Petroleum(Natural Science Edition),2008,32(4):19-24.
[13]付金华,李士祥,刘显阳.鄂尔多斯盆地石油勘探地质理论与实践[J].天然气地球科学,2013,24(16):1091-1101.FU Jinhua,LI Shixiang,LIU Xianyang.Geological theory and practice of petroleum exploration in the Ordos basin[J].Natural Gas Geoscience,2013,24(16):1091-1101.
[14]卢双舫,马延伶,曹瑞成,等.优质烃源岩评价标准及其应用:以海拉尔盆地乌尔逊凹陷为例[J].地球科学(中国地质大学学报),2012,37(3):535-544.LU Shuangfang,MA Yanling,CAO Ruicheng,et al.Evaluation criteria of high-quality source rocks and its application:taking the Wuerxun sag in Hailaer basin as an example[J].Earth Science(Journal of China University of Geosciences),2012,37(3):535-544.
[15]WEBSTER R L.Petroleum source rocks and stratigraphy of Bakken formation innorth Dakota[J].AAPG Bulletin,1984,68(7):593.
[16]白玉彬,赵靖舟,赵子龙,等.鄂尔多斯盆地志丹地区延长组长7致密油成藏条件与成藏特征[J].石油与天然气地质,2013,34(5):631-639.BAI Yubin,ZHAO Jingzhou,ZHAO Zilong,et al.Accumulation conditions and characteristics of the Chang 7tight oil reservoir of the Yanchang formation in Zhidan area,Ordos basin[J].Oil&Gas Geology,2013,34(5):631-639.
[17]付锁堂,张道伟,薛建勤,等.柴达木盆地致密油形成的地质条件及勘探潜力分析[J].沉积学报,2013,31(4):672-681.FU Suotang,ZHANG Daowei,XUE Jianqin,et al.Exploration potential and geological conditions of tight oil in the Qaidam basin[J].Acta Sedimentologica Sinica,2013,31(4):672-681.
[18]黄薇,梁江平,赵波,等.松辽盆地北部白垩系泉头组扶余油层致密油成藏主控因素[J].古地理学报,2013,15(5):635-644.HUANG Wei,LIANG Jiangping,ZHAO Bo,et al.Main controlling factors of tight oil accumulation in the Fuyu layer of cretaceous Quantou formation in northern Songliao basin[J].Journal of Palaeogeography,2013,15(5):635-644.
[19]王力,金强,林腊梅,等.柴达木盆地西部古近系—新近系优质烃源岩特征[J].天然气工业,2009,29(2):23-26.WANG Li,JIN Qiang,LIN Lamei,et al.Characteristics of quality Tertiary source rocks in west Qaidam basin[J].Natural Gas Industry,2009,29(2):23-26.
[20]郑红菊,董月霞,朱光有,等.南堡凹陷优质烃源岩的新发现[J].石油勘探与开发,2007,34(4):385-391.ZHENG Hongju,DONG Yuexia,ZHU Guangyou,et al.High-quality source rocks in Nanpu sag[J].Petroleum Exploration and Development,2007,34(4):385-391.
[21]侯杜杰,张善文,肖建新,等.济阳坳陷优质烃源岩特征与隐蔽油气藏的关系分析[J].地学前缘,2008,15(2):137-146.HOU Dujie,ZHANG Shanwen,XIAO Jianxin,et al.The excellent source rocks and accumulation of stratigraphic and lithologic traps in the Jiyang depression,Bohai bay basin,China[J].Earth Science Frontiers,2008,15(2):137-146.
[22]刘新颖,邓宏文,邸永香,等.海拉尔盆地乌尔逊凹陷南屯组优质烃源岩发育特征[J].石油实验地质,2009,31(1):68-73.LIU Xinying,DENG Hongwen,DI Yongxiang,et al.High-quality source rocks of Nantun formation in Wuerxun depression,Hailaer basin[J].Petroleum Geology&Experiment,2009,31(1):68-73.
[23]黄文彪,邓守伟,卢双舫,等.泥页岩有机非均执行评价及其在页岩油资源评价中的应用:以松辽盆地南部青山口组为例[J].石油与天然气地质,2014,35(5):704-711.HUANG Wenbiao,DENG Shouwei,LU Shuangfang,et al.Shale organic heterogeneity evalution method and its application to shale oil resource evaluation:a case study from Qingshankou formation,southern Songliao basin[J].Oil&Gas Geology,2014,35(5):704-711.
[24]孙雨,陈晨,马世忠,等.松辽盆地扶新隆起带南部扶余油层油气运移机制与成藏模式研究[J].地质论评,2013,59(3):501-509.SUN Yu,CHEN Chen,MA Shizhong,et al.Hydrocarbon migration mechanism and accumulation models of the Fuyu oil layer in southern Fuxin uplift,Songliao basin[J].Geological Review,2013,59(3):501-509.
[25]陶士振,邹才能,袁选俊,等.流体包裹体在油气勘探中的应用:以吉林油田扶新隆起扶余油层为例[J].中国石油勘探,2006(4):46-51.TAO Shizhen,ZOU Caineng,YUAN Xuanjun,et al.Application of fluid inclusion in oil-gas exploration[J].PetroChina Research Institute of Petroleum Exploration and Development,2006(4):46-51.
[26]王子文,赵锡嘏,卢双舫,等.原始有机质丰度的恢复及其意义[J].大庆石油地质与开发,1991,10(4):20-26.WANG Ziwen,ZHAO Xigu,LU Shuangfang,et al.The recovery of original abundance of organic matter and its significance[J].Petroleum Geology and Oilfield Development in Daqing,1991,10(4):20-26.
[27]卢双舫,刘晓艳,曲佳燕,等.海拉尔盆地呼和湖凹陷烃源岩原始生烃潜力和原始有机碳的恢复[J].大庆石油学院学报,1995,19(1):31-33.LU Shuangfang,LIU Xiaoyan,QU Jiayan,et al.Restoring of original hydrocarbon potential and original organic carbon of source rocks in Huhehu depression,Hailar basin[J].Journal of Daqing Petroleum Institute,1995,19(1):31-33.
[28]庞雄奇,李素梅,金之钧,等.排烃门限存在的地质地球化学证据及其应用[J].地球科学(中国地质大学学报),2004,29(4):384-390.PANG Xiongqi,LI Sumei,JIN Zhijun,et al.Geochemical evidences of hydrocarbon expulsion threshold and its application[J].Earth Science(Journal of China University of Geosciences),2004,29(4):384-390.
[29]范柏江,董月霞,庞雄奇.有效源岩的精确厘定及其排烃量:以南堡凹陷为例[J].中南大学学报(自然科学版),2012,43(1):229-237.FAN Bojiang,DONG Yuexia,PANG Xiongqi.Establishment of effective source rock and hydrocarbon expulsion quantity:taking Nanpu sag for example[J].Journal of Central South University(Science and Technology),2012,43(1):229-237.
[30]蔡希源.湖相烃源岩生排烃机制及生排烃效率差异性:以渤海湾盆地东营凹陷为例[J].石油与天然气地质,2012,33(3):329-334.CAI Xiyuan.Hydrocarbon generation-expulsion mechanisms and efficiencies of lacustrine source rocks:a case study from the Dongying sag,Bohai Bay basin[J].Oil&Gas Geology,2012,33(3):329-334.
[31]陈建平,梁狄刚,张水昌,等.中国古生界海相烃源岩生烃潜力评价与方法[J].地质学报,2012,86(7):1132-1142.CHEN Jianping,LIANG Digang,ZHANG Shuichang,et al.Evaluation criterion and methods of the hydrocarbon generation potential for China’s Paleozoic marine source rocks[J].Acta Geologica Sinica,2012,86(7):1132-1142.
[32]姜福杰,庞雄奇,姜振学,等.渤海海域沙三段烃源岩评价及排烃特征[J].石油学报,2010,31(6):906-912.JIANG Fujie,PANG Xiongqi,JIANG Zhenxue,et al.The quality evaluation and hydrocarbon-expilsion characters of source rocks in the 3rd member of Shahejie formation in the Bohai sea[J].Acta Petrolei Sinica,2010,31(6):906-912.
[33]卢双舫,李娇娜,刘绍军,等.松辽盆地生油门限重新厘定及其意义[J].石油勘探与开发,2009,36(2):166-173.LU Shuangfang,LI Jiaona,LIU Shaojun,et al.Oil generation threshold depth of Songliao basin:revision and its significance[J].Petroleum Exploration and Development,2009,36(2):166-173.
[34]赵志魁,张金亮,赵占银,等.松辽盆地南部坳陷湖盆沉积相和储层研究[M].北京:石油工业出版社,2009:209-212.
[35]徐思煌,朱义清.烃源岩有机碳含量的测井响应特征与定量预测模型:以珠江口盆地文昌组烃源岩为例[J].石油实验地质,2010,32(3):290-300.XU Sihuang,ZHU Yiqing.Well logs response and prediction model of organic carbon content in source rocks:A case study from the source rock of Wenchang formation in the pearl Mouth basin[J].Petroleum Geology&Experiment,2010,32(3):290-300.
[36]李丹,董春梅,林承焰,等.松辽盆地南部让字井斜坡带超压特征及其对源下油藏运聚模式的控制[J].天然气地球科学,2014,25(3):326-332.LI Dan,DONG Chunmei,LIN Chengyan,et al.Characteristic of overpressure and its control on migration and accumulation for hydrocarbon reservoirs below source rocks in Rangzijing slope zone of southern Songliao basin[J].Natural Gas Geoscience,2014,25(3):326-332.
[37]杨伟伟,柳广弟,刘显阳,等.鄂尔多斯盆地陇东地区延长组低渗透砂岩油藏成藏机理与成藏模式[J].地学前缘,2013,20(2):132-139.YANG Weiwei,LIU Guangdi,LIU Xianyang,et al.The accumulation mechanism and accumulation models of oil in low permeability reservoir of Yanchang formation in Longdong area,Ordos basin[J].Earth Science Frontiers,2013,20(2):132-139.
[38]郭小文,何生,郑伦举,等.生油增压定量模型及影响因素[J].石油学报,2011,32(4):637-644.GUO Xiaowen,HE Sheng,ZHENG Lunju,et al.A quantitative model for the overpressure caused by oil generation and its influential factors[J].Acta Petrolei Sinica,2011,32(4):637-644.
[39]李星,黄文娟,孙旭东,等.东营凹陷地层异常压力的成因机制与动态模拟[J].地质科技情报,2012,31(6):28-33.LI Xing,HUANG Wenjuan,SUN Xudong,et al.Formation mechanism and dynamic simulation of abnormal formation pressure of Dongying depression[J].Geological Science and Technology Infoamation,2012,31(6):28-33.
[40]王雅春,王胜男.源岩、超压和断裂空间匹配对三肇凹陷扶杨油层油成藏的控制作用[J].吉林大学学报(地球科学版),2009,39(4):656-661.WANG Yachun,WANG Shengnan.Controlling of the match of source rock,overpressure and fault on oil accumulation of Fu-Yang oil layer in Sanzhao Depression[J].Journal of Jilin University(Earth Science Edition),2009,39(4):656-661.
[41]陈子炓,姚根顺,楼章华,等.桂中坳陷及周缘油气保存条件分析[J].中国矿业大学学报,2011,40(1):80-87.CHEN Ziliao,YAO Genshun,LOU Zhanghua,et al.Study of hydrocarbon preservation condition in Guizhong depression and the margin[J].Journal of China University of Mining&Technology,2011,40(1):80-87.
[2]贾承造,郑民,张永峰.中国非常规油气资源与勘探开发前景[J].石油勘探与开发,2012,39(2):129-136.JIA Chengzao,ZHENG Min,ZHANG Yongfeng.Unconventional hydrocarbon resources in China and the prospect of exploration and development[J].Petroleum Exploration and Development,2012,39(2):129-136.
[3]祝海华,钟大康,姚泾利,等.鄂尔多斯西南地区长7段致密油储层微观特征及成因机理[J].中国矿业大学学报,2014,43(5):853-862.ZHU Haihua,ZHONG Dakang,YAO Jingli,et al.Microscopic characteristics and formation mechanism of Upper Triassic Chang7tight oil reservoir in the southwest Ordos basin[J].Journal of China University of Mining&Technology,2014,43(5):853-862.
[4]邹才能,朱如凯,吴松涛,等.常规与非常规油气聚集类型、特征、机理及展望:以中国致密油和致密气为例[J].石油学报,2012,33(2):173-187.ZOU Caineng,ZHU Rukai,WU Songtao,et al.Types,characteristics,genesis and prospects of conventional and unconventional hydrocarbon accumulations:taking tight oil and tight gas in China as an instance[J].Acta Petrolei Sinica,2012,33(2):173-187.
[5]ANONYMOUS.HIS:World's tight oil resources hold large potential[J].Oil&Gas Journal,2013,111(9d):27.
[6]SNOW,NICK.A coming tight oil bonanza[J].Oil&Gas Journal,2011,109(19b):22.
[7]YAO Jingli,DENG Xiuqin,ZHAO Yande,et al.Characteristics of tight oil in Triassic Yanchang formation,Ordos basin[J].Petroleum Exploration and Development,2013,Vol.40(2):161-169.
[8]马中振,戴国威,盛晓峰,等.松辽盆地北部连续型致密砂岩油藏的认识及其地质意义[J].中国矿业大学学报,2013,42(2):221-229.MA Zhongzhen,DAI Guowei,SHENG Xiaofeng,et al.Tight sand oil reservoir of continuous type in northern Songliao basin and its geological significance[J].Journal of China University of Mining&Technology,2013,42(2):221-229.
[9]张妮妮,刘洛夫,苏天喜,等.鄂尔多斯盆地延长组长7段与威利斯顿盆地Bakken组致密油形成条件的对比及其意义[J].现代地质,2013,27(5):1120-1130.ZHANG Nini,LIU Luofu,SU Tianxi,et al.Comparison of Chang 7member of Yanchang formation in Ordos basin with Bakken formation in Williston basin and its significance[J].Geoscience,2013,27(5):1120-1130.
[10]宋岩,姜林,马行陟.非常规油气藏的形成及其分布特征[J].古地理学报,2013,15(5):605-614.SONG Yan,JIANG Lin,MA Xingzhi.Formation and distribution characteristics of unconventional oil and gas reservoirs[J].Journal of Palaeogeography,2013,15(5):605-614.
[11]中石油吉林油田勘探研究院.松南扶余油层致密油成藏规律研究[R].松原:中石油吉林油田勘探研究院,2014.
[12]金强,朱光有,王娟.咸化湖盆优质烃源岩的形成和分布[J].中国石油大学学报(自然科学版),2008,32(4):19-24.JIN Qiang,ZHU Guangyou,WANG Juan.Depositon and distribution of high-potiential source rocks in saline lacustrine environments[J].Journal of China University of Petroleum(Natural Science Edition),2008,32(4):19-24.
[13]付金华,李士祥,刘显阳.鄂尔多斯盆地石油勘探地质理论与实践[J].天然气地球科学,2013,24(16):1091-1101.FU Jinhua,LI Shixiang,LIU Xianyang.Geological theory and practice of petroleum exploration in the Ordos basin[J].Natural Gas Geoscience,2013,24(16):1091-1101.
[14]卢双舫,马延伶,曹瑞成,等.优质烃源岩评价标准及其应用:以海拉尔盆地乌尔逊凹陷为例[J].地球科学(中国地质大学学报),2012,37(3):535-544.LU Shuangfang,MA Yanling,CAO Ruicheng,et al.Evaluation criteria of high-quality source rocks and its application:taking the Wuerxun sag in Hailaer basin as an example[J].Earth Science(Journal of China University of Geosciences),2012,37(3):535-544.
[15]WEBSTER R L.Petroleum source rocks and stratigraphy of Bakken formation innorth Dakota[J].AAPG Bulletin,1984,68(7):593.
[16]白玉彬,赵靖舟,赵子龙,等.鄂尔多斯盆地志丹地区延长组长7致密油成藏条件与成藏特征[J].石油与天然气地质,2013,34(5):631-639.BAI Yubin,ZHAO Jingzhou,ZHAO Zilong,et al.Accumulation conditions and characteristics of the Chang 7tight oil reservoir of the Yanchang formation in Zhidan area,Ordos basin[J].Oil&Gas Geology,2013,34(5):631-639.
[17]付锁堂,张道伟,薛建勤,等.柴达木盆地致密油形成的地质条件及勘探潜力分析[J].沉积学报,2013,31(4):672-681.FU Suotang,ZHANG Daowei,XUE Jianqin,et al.Exploration potential and geological conditions of tight oil in the Qaidam basin[J].Acta Sedimentologica Sinica,2013,31(4):672-681.
[18]黄薇,梁江平,赵波,等.松辽盆地北部白垩系泉头组扶余油层致密油成藏主控因素[J].古地理学报,2013,15(5):635-644.HUANG Wei,LIANG Jiangping,ZHAO Bo,et al.Main controlling factors of tight oil accumulation in the Fuyu layer of cretaceous Quantou formation in northern Songliao basin[J].Journal of Palaeogeography,2013,15(5):635-644.
[19]王力,金强,林腊梅,等.柴达木盆地西部古近系—新近系优质烃源岩特征[J].天然气工业,2009,29(2):23-26.WANG Li,JIN Qiang,LIN Lamei,et al.Characteristics of quality Tertiary source rocks in west Qaidam basin[J].Natural Gas Industry,2009,29(2):23-26.
[20]郑红菊,董月霞,朱光有,等.南堡凹陷优质烃源岩的新发现[J].石油勘探与开发,2007,34(4):385-391.ZHENG Hongju,DONG Yuexia,ZHU Guangyou,et al.High-quality source rocks in Nanpu sag[J].Petroleum Exploration and Development,2007,34(4):385-391.
[21]侯杜杰,张善文,肖建新,等.济阳坳陷优质烃源岩特征与隐蔽油气藏的关系分析[J].地学前缘,2008,15(2):137-146.HOU Dujie,ZHANG Shanwen,XIAO Jianxin,et al.The excellent source rocks and accumulation of stratigraphic and lithologic traps in the Jiyang depression,Bohai bay basin,China[J].Earth Science Frontiers,2008,15(2):137-146.
[22]刘新颖,邓宏文,邸永香,等.海拉尔盆地乌尔逊凹陷南屯组优质烃源岩发育特征[J].石油实验地质,2009,31(1):68-73.LIU Xinying,DENG Hongwen,DI Yongxiang,et al.High-quality source rocks of Nantun formation in Wuerxun depression,Hailaer basin[J].Petroleum Geology&Experiment,2009,31(1):68-73.
[23]黄文彪,邓守伟,卢双舫,等.泥页岩有机非均执行评价及其在页岩油资源评价中的应用:以松辽盆地南部青山口组为例[J].石油与天然气地质,2014,35(5):704-711.HUANG Wenbiao,DENG Shouwei,LU Shuangfang,et al.Shale organic heterogeneity evalution method and its application to shale oil resource evaluation:a case study from Qingshankou formation,southern Songliao basin[J].Oil&Gas Geology,2014,35(5):704-711.
[24]孙雨,陈晨,马世忠,等.松辽盆地扶新隆起带南部扶余油层油气运移机制与成藏模式研究[J].地质论评,2013,59(3):501-509.SUN Yu,CHEN Chen,MA Shizhong,et al.Hydrocarbon migration mechanism and accumulation models of the Fuyu oil layer in southern Fuxin uplift,Songliao basin[J].Geological Review,2013,59(3):501-509.
[25]陶士振,邹才能,袁选俊,等.流体包裹体在油气勘探中的应用:以吉林油田扶新隆起扶余油层为例[J].中国石油勘探,2006(4):46-51.TAO Shizhen,ZOU Caineng,YUAN Xuanjun,et al.Application of fluid inclusion in oil-gas exploration[J].PetroChina Research Institute of Petroleum Exploration and Development,2006(4):46-51.
[26]王子文,赵锡嘏,卢双舫,等.原始有机质丰度的恢复及其意义[J].大庆石油地质与开发,1991,10(4):20-26.WANG Ziwen,ZHAO Xigu,LU Shuangfang,et al.The recovery of original abundance of organic matter and its significance[J].Petroleum Geology and Oilfield Development in Daqing,1991,10(4):20-26.
[27]卢双舫,刘晓艳,曲佳燕,等.海拉尔盆地呼和湖凹陷烃源岩原始生烃潜力和原始有机碳的恢复[J].大庆石油学院学报,1995,19(1):31-33.LU Shuangfang,LIU Xiaoyan,QU Jiayan,et al.Restoring of original hydrocarbon potential and original organic carbon of source rocks in Huhehu depression,Hailar basin[J].Journal of Daqing Petroleum Institute,1995,19(1):31-33.
[28]庞雄奇,李素梅,金之钧,等.排烃门限存在的地质地球化学证据及其应用[J].地球科学(中国地质大学学报),2004,29(4):384-390.PANG Xiongqi,LI Sumei,JIN Zhijun,et al.Geochemical evidences of hydrocarbon expulsion threshold and its application[J].Earth Science(Journal of China University of Geosciences),2004,29(4):384-390.
[29]范柏江,董月霞,庞雄奇.有效源岩的精确厘定及其排烃量:以南堡凹陷为例[J].中南大学学报(自然科学版),2012,43(1):229-237.FAN Bojiang,DONG Yuexia,PANG Xiongqi.Establishment of effective source rock and hydrocarbon expulsion quantity:taking Nanpu sag for example[J].Journal of Central South University(Science and Technology),2012,43(1):229-237.
[30]蔡希源.湖相烃源岩生排烃机制及生排烃效率差异性:以渤海湾盆地东营凹陷为例[J].石油与天然气地质,2012,33(3):329-334.CAI Xiyuan.Hydrocarbon generation-expulsion mechanisms and efficiencies of lacustrine source rocks:a case study from the Dongying sag,Bohai Bay basin[J].Oil&Gas Geology,2012,33(3):329-334.
[31]陈建平,梁狄刚,张水昌,等.中国古生界海相烃源岩生烃潜力评价与方法[J].地质学报,2012,86(7):1132-1142.CHEN Jianping,LIANG Digang,ZHANG Shuichang,et al.Evaluation criterion and methods of the hydrocarbon generation potential for China’s Paleozoic marine source rocks[J].Acta Geologica Sinica,2012,86(7):1132-1142.
[32]姜福杰,庞雄奇,姜振学,等.渤海海域沙三段烃源岩评价及排烃特征[J].石油学报,2010,31(6):906-912.JIANG Fujie,PANG Xiongqi,JIANG Zhenxue,et al.The quality evaluation and hydrocarbon-expilsion characters of source rocks in the 3rd member of Shahejie formation in the Bohai sea[J].Acta Petrolei Sinica,2010,31(6):906-912.
[33]卢双舫,李娇娜,刘绍军,等.松辽盆地生油门限重新厘定及其意义[J].石油勘探与开发,2009,36(2):166-173.LU Shuangfang,LI Jiaona,LIU Shaojun,et al.Oil generation threshold depth of Songliao basin:revision and its significance[J].Petroleum Exploration and Development,2009,36(2):166-173.
[34]赵志魁,张金亮,赵占银,等.松辽盆地南部坳陷湖盆沉积相和储层研究[M].北京:石油工业出版社,2009:209-212.
[35]徐思煌,朱义清.烃源岩有机碳含量的测井响应特征与定量预测模型:以珠江口盆地文昌组烃源岩为例[J].石油实验地质,2010,32(3):290-300.XU Sihuang,ZHU Yiqing.Well logs response and prediction model of organic carbon content in source rocks:A case study from the source rock of Wenchang formation in the pearl Mouth basin[J].Petroleum Geology&Experiment,2010,32(3):290-300.
[36]李丹,董春梅,林承焰,等.松辽盆地南部让字井斜坡带超压特征及其对源下油藏运聚模式的控制[J].天然气地球科学,2014,25(3):326-332.LI Dan,DONG Chunmei,LIN Chengyan,et al.Characteristic of overpressure and its control on migration and accumulation for hydrocarbon reservoirs below source rocks in Rangzijing slope zone of southern Songliao basin[J].Natural Gas Geoscience,2014,25(3):326-332.
[37]杨伟伟,柳广弟,刘显阳,等.鄂尔多斯盆地陇东地区延长组低渗透砂岩油藏成藏机理与成藏模式[J].地学前缘,2013,20(2):132-139.YANG Weiwei,LIU Guangdi,LIU Xianyang,et al.The accumulation mechanism and accumulation models of oil in low permeability reservoir of Yanchang formation in Longdong area,Ordos basin[J].Earth Science Frontiers,2013,20(2):132-139.
[38]郭小文,何生,郑伦举,等.生油增压定量模型及影响因素[J].石油学报,2011,32(4):637-644.GUO Xiaowen,HE Sheng,ZHENG Lunju,et al.A quantitative model for the overpressure caused by oil generation and its influential factors[J].Acta Petrolei Sinica,2011,32(4):637-644.
[39]李星,黄文娟,孙旭东,等.东营凹陷地层异常压力的成因机制与动态模拟[J].地质科技情报,2012,31(6):28-33.LI Xing,HUANG Wenjuan,SUN Xudong,et al.Formation mechanism and dynamic simulation of abnormal formation pressure of Dongying depression[J].Geological Science and Technology Infoamation,2012,31(6):28-33.
[40]王雅春,王胜男.源岩、超压和断裂空间匹配对三肇凹陷扶杨油层油成藏的控制作用[J].吉林大学学报(地球科学版),2009,39(4):656-661.WANG Yachun,WANG Shengnan.Controlling of the match of source rock,overpressure and fault on oil accumulation of Fu-Yang oil layer in Sanzhao Depression[J].Journal of Jilin University(Earth Science Edition),2009,39(4):656-661.
[41]陈子炓,姚根顺,楼章华,等.桂中坳陷及周缘油气保存条件分析[J].中国矿业大学学报,2011,40(1):80-87.CHEN Ziliao,YAO Genshun,LOU Zhanghua,et al.Study of hydrocarbon preservation condition in Guizhong depression and the margin[J].Journal of China University of Mining&Technology,2011,40(1):80-87.