坳陷湖盆烃源岩发育样式及其对石油聚集的控制——以鄂尔多斯盆地三叠系延长组长7油层组为例
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摘要
鄂尔多斯盆地中生界T—J1含油系统,石油富集程度、主力产层和烃源岩分布均具有较强的地区差异性,对该差异性缺少系统研究。对盆地内不同区域8口长取心井长7油层组烃源层开展系统的地球化学分析,结合测井ΔLogR法计算出300口井长7油层组总有机碳丰度与纵向分布,依据工业油流井和低产井划定长8、长7和长6油层组油藏有利分布区。研究发现烃源岩纵向上存在5种分布样式并存在较强的区域性差异:湖盆西北部姬塬地区以底部富集型和全段富集型为主;东北部陕北地区主要以中部富集型和顶部富集型为主;盆地中部地区主要以互层型为主;西南部陇东地区主要为底部富集型为主。源岩类型和石油有利区综合分析,揭示出源岩发育样式对石油分布具有控制性作用。姬塬地区底部富集型源下聚集、全段富集型源上源下双向聚集,长6油层组和长8油层组油层组多层系含油;陕北地区顶部富集型和中部富集型源上聚集,长6油层组为主力产层;陇东地区底部富集型源下聚集,长8油层组原油为主力产层,湖盆中部互层型多层复合成藏,源内致密油和源上源下多层系含油。烃源岩纵向分布样式与石油聚集关系不仅是陆相湖盆源藏分布规律的提升,对优选近源—源内油气勘探领域也具有重要意义。
In the Mesozoic T-J1 oil system of Ordos Basin,the degree of oil enrichment,main production layer and source rock distribution have strong regional differences,and there is no systematic study on this difference.The total organic carbon abundance and vertical distribution of the Chang 7 oil formation source layers of 8 long core wells in different areas of the basin were calculated by means ofΔLogR method.According to the industrial oil well and the low production well,the favorable oil distribution areas of Chang8,Chang 7 and Chang 6 oil formation reservoirs are demarcated.The study found that there are five distribution styles and strong regional differences in the longitudinal direction of source rocks.The Jiyuan area in the northwestern part of the lake basin is dominated by the bottom rich type and the full section rich type.The northeastern Shaanxi region is mainly dominated by the middle rich type and the top rich type.The central area of the basin is mainly the interlayered type,and the southwestern Longdong region is mainly the bottom rich type.The comprehensive analysis of source rock type and oil favorable zone reveals that source rock type has a controlling effect on crude oil distribution.Bottom rich type and the full section rich type are dominant in the Jiyuan area,and multiple layers have oil.In northern Shaanxi,the top rich type and middle rich type accumulate to the upper,and the Chang 6 oil formation was the main production layer.The bottom rich type of the Longdong area accumulates under the source,and the Chang 8 oil formation is the main production layer.The central part of the lake basin is dominated by the interlayered type with multiple layers of production oil.The relationship between the distribution pattern of source rock and oil accumulation is not only an improvement of the distribution law of the continental lake,but also has important significance for the optimization of the field of near-source-in-source oil and gas exploration.
In the Mesozoic T-J1 oil system of Ordos Basin,the degree of oil enrichment,main production layer and source rock distribution have strong regional differences,and there is no systematic study on this difference.The total organic carbon abundance and vertical distribution of the Chang 7 oil formation source layers of 8 long core wells in different areas of the basin were calculated by means ofΔLogR method.According to the industrial oil well and the low production well,the favorable oil distribution areas of Chang8,Chang 7 and Chang 6 oil formation reservoirs are demarcated.The study found that there are five distribution styles and strong regional differences in the longitudinal direction of source rocks.The Jiyuan area in the northwestern part of the lake basin is dominated by the bottom rich type and the full section rich type.The northeastern Shaanxi region is mainly dominated by the middle rich type and the top rich type.The central area of the basin is mainly the interlayered type,and the southwestern Longdong region is mainly the bottom rich type.The comprehensive analysis of source rock type and oil favorable zone reveals that source rock type has a controlling effect on crude oil distribution.Bottom rich type and the full section rich type are dominant in the Jiyuan area,and multiple layers have oil.In northern Shaanxi,the top rich type and middle rich type accumulate to the upper,and the Chang 6 oil formation was the main production layer.The bottom rich type of the Longdong area accumulates under the source,and the Chang 8 oil formation is the main production layer.The central part of the lake basin is dominated by the interlayered type with multiple layers of production oil.The relationship between the distribution pattern of source rock and oil accumulation is not only an improvement of the distribution law of the continental lake,but also has important significance for the optimization of the field of near-source-in-source oil and gas exploration.
引文
[1]Dai Jinxing,Wang Tingbin,Song Yan,et al.Formation Conditions and Distribution Regularity of Large and Medium Scale Natural Gas Field in China[M].Beijing:Geological Publishing House,1997:20-27.戴金星,王廷斌,宋岩,等.中国大中型天然气田形成条件与分布规律[M].北京:地质出版社,1997:20-27.
[2]Zhang Wenzheng,Yang Hua,Yang Yihua,et al.Petrology and element geochemistry and development environment of Yanchang Formation Chang-7high quality source rocks in Ordos Basin[J].Geochimica,2008,37(1):59-64.张文正,杨华,杨奕华,等.鄂尔多斯盆地长7优质烃源岩的岩石学,元素地球化学特征及发育环境[J].地球化学,2008,37(1):59-64.
[3]Yang Hua,Li Shixiang,Liu Xianyang.Characteristics and resource prospects of tight oil and shale oil in Ordos Basin[J].Acta Petrolei Sinica,2013,34(1):1-11.杨华,李士祥,刘显阳.鄂尔多斯盆地致密油、页岩油特征及资源潜力[J].石油学报,2013,34(1):1-11.
[4]Liu Wenhou,Pang Jungang,Cao Hongxia,et al.Depositional system and paleogeographic evolution of the Late Triassic Yanchang stage in Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2009,39(3):501-506.李文厚,庞军刚,曹红霞,等.鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化[J].西北大学学报:自然科学版,2009,39(3):501-506.
[5]Hu Chaoyuan.An approach on regional controlling factors of oil-gas field distribution in offshore sedimentary basins of China[J].Marine Geology&Quaternary Geology,1986,6(4):23-29.胡朝元.我国海上沉积盆地油气田分布区域控制因素的探讨[J].海洋地质与第四纪地质,1986,6(4):23-29.
[6]Hu Chaoyuan.Research on the appliance extent of source control theory by semi-quantitative statistics characteristics of oil and gas migration distance[J].Natural Gas Industry,2005,25(10):1-3.胡朝元.“源控论”适用范围量化分析[J].天然气工业,2005,25(10):1-3.
[7]Zou Caineng,Tao Shizhen,Hou Lianhua,et al.Unconventional Oil and Gas Geology[M].Second Edition.Beijing:Geological Publishing House,2013:9-14.邹才能,陶士振,侯连华,等.非常规油气地质[M].第二版.北京:地质出版社,2013:9-14.
[8]Cui Jingwei,Zhu Rukai,Wu Songtao,et al.Heterogeneity and lower oily limits for tight sandstones:A case study on Chang-7oil layers of the Yanchang Formation,Ordos Basin[J].Acta Petrolei Sinica,2013,34(5):877-882.崔景伟,朱如凯,吴松涛,等.致密砂岩层内非均质性及含油下限---以鄂尔多斯盆地三叠系延长组长7段为例[J].石油学报,2013,34(5):877-882.
[9]Cui Jingwei,Zhu Rukai,Li Shixiang,et al.Movable oil and its controlling factors in tight sandstones:A case study of the Triassic Chang 7reservoir,Yanchang Formation,Ordos Basin[J].Petroleum Geology&Experiment,2016,38(4):536-542.崔景伟,朱如凯,李士祥,等.致密砂岩油可动量及其主控因素---以鄂尔多斯盆地三叠系延长组长7为例[J].石油实验地质,2016,38(4):536-542.
[10]Tian Jingchun,Chen Gaowu,Dou Weitan,et al.Origin and association types of lake delta front sandstones and their distribution patterns of Triassic Yanchang Formation in Ordos Basin,China[J].Journal of Chengdu University of Technology,Science&Technology Edition,2004,31(6):636-640.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---以鄂尔多斯盆地姬塬白豹地区三叠系延长组为例[J].成都理工大学学报:自然科学版,2004,31(6):636-640.
[11]China National Standardizing Committee.GB/T19145-2003Determination of Total Organic Carbon in Sedimentary Rock[S].Beijing:Standards Press of China,2003.中国国家标准化管理委员会.GB/T19145-2003沉积岩中总有机碳的测定标准[S].北京:中国标准出版社,2003.
[12]China National Standardizing Committee.GB/T18602-2012RockPyrolysis Analysis[S].Beijing:Standards Press of China,2012.中国国家标准化管理委员会.GB/T18602-2012岩石热解分析[S].北京:中国标准出版社,2012.
[13]Behar F,Beaumont V,Penteado H L D B.Rock-Eval 6technology:Performances and developments[J].Oil&Gas Science and Technology,2001,56(2):111-134.
[14]China National Standardizing Committee.GB/T6948-2008Method of Determining Microscopically the Reflectance ofVitrinite in Coal[S].Beijing:Standards Press of China,2008.中国国家标准化管理委员会.GB/T6948-2008煤的镜质体反射率显微镜测定方法[S].北京:中国标准出版社,2008.
[15]Zou C N,Zhu R K,Chen Z Q,et al.Organic-matter-rich shales of China[J].Earth-Science Reviews,2019,189:51-78.
[16]Zhu Guangyou,Jin Qiang,Zhou Jianlin,et al.Source rock characters of cyclic deep-lake facies in the Dongying Depression[J].Chinese Journal of Geology,2003,38(2):254-262.朱光有,金强,周建林,等.东营凹陷旋回式深湖相烃源岩研究[J].地质科学,2003,38(2):254-262.
[17]Zhang Shuichang,Zhang Baoming,Wang Feiyu,et al.The organic matter properties,environment and controlling factors of the two set of marine source rock in Tarim Basin[J].Advance in Natural Science,2001,11(3):261-268.张水昌,张保民,王飞宇,等.塔里木盆地两套海相有效烃源岩层-Ⅰ.有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261-268.
[18]Yang Minghui,Xia Wenchen,Zhang Bingshan,et al.Parasequence-shale organic facies variations and its significance in Nonmarine Basin[J].Acta Sedimentologica Sinica,2000,18(2):297-301.杨明慧,夏文臣,张兵山,等.非海相盆地准层序级别的有机相变化及其地质意义[J].沉积学报,2000,18(2):297-301.
[19]Shi Zhiqiang,Han Yonglin,Zhao Junxing,et al.Depositional system and paleogeographic evolution of the Middle Jurassic Yan’anian stage in the central and southern Ordos Basin[J].Acta Geoscientia Sinica,2003,24(1):49-54.时志强,韩永林,赵俊兴,等.鄂尔多斯盆地中南部中侏罗世延安期沉积体系及岩相古地理演化[J].地球学报,2003,24(1):49-54.
[20]Wang Lei.The Recovery of the Paleoproductivity in the Period of Chang 7in Ordos Basin and Its Control Factors[D].Xi’an:Northwest University,2015.王磊.鄂尔多斯盆地延长组长7期湖盆古生产力恢复及其控制因素[D].西安:西北大学,2015.
[21]Zhu Guangyou,Jin Qiang.Study on source rock heterogeneityA case of Niu-38Well in Dongying depression[J].Acta Petrolei Sinica,2002,23(5):34-39.朱光有,金强.烃源岩的非均质性研究-以东营凹陷牛38井为例[J].石油学报,2002,23(5):34-39.
[22]Wang Huizhong,Mei Hongming.Paleolimnological information from the oil shale in the lower part of Sha 3Formation,in Dongying Depression[J].Journal Of Tongji University,1998,26(3):315-319.王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315-319.
[23]Zhang Wenzheng,Yang Hua,Peng Ping’an,et al.The influence of Late Triassic volcanism on the development of Chang7high grade hydrocarbon source rock in Ordos Basin[J].Geochimica,2009,38(6):573-582.张文正,杨华,彭平安,等.晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响[J].地球化学,2009,38(6):573-582.
[24]Cui J W,Zhu R K,Luo Z,et al.Sedimentary and geochemical characteristics of Triassic Chang 7 member Shale in Southeastern Ordos Basin,Central China[J].Petroleum Science,2019,16(2):285-297.
[25]Carroll A R,Bohacs K M.Lake-type controls on petroleum source rock potential in nonmarine basins[J].AAPG Bulletin,2001,85(6):1033-1053.
[26]Liu Qun,Yuan Xuanjun,Lin Senhu,et al.Depositional environment and characteristic comparison between lacustrine mudstone and shale:A case study from the Chang 7member of the Yanchang Formation,Ordos Basin[J].Oil&Gas Geology,2018,39(3):531-540.刘群,袁选俊,林森虎,等.湖相泥岩、页岩的沉积环境和特征对比---以鄂尔多斯盆地延长组7段为例[J].石油与天然气地质,2018,39(3):531-540.
[27]Yuan Xuanjun,Lin Senhu,Liu Qun,et al.Lacustrine finegrained sedimentary features and organic-rich shale distribution pattern:A case study of Chang 7 member of Triassic Yanchang Formation in Ordos Basin,NW China[J].Petroleum Exporation and Development,2015,42(1):34-43.袁选俊,林森虎,刘群,等.湖盆细粒沉积特征与富有机质页岩分布模式---以鄂尔多斯盆地延长组长7油层组为例[J].石油勘探与开发,2015,42(1):34-43.
[28]Ren Zhanli,Zhang Sheng,Gao Shengli,et al.Research on region of maturation anomaly and formation time in Ordos Basin[J].Acta Geologica Sinica,2006,80(5):674-684.任战利,张盛,高胜利,等.鄂尔多斯盆地热演化程度异常分布区及形成时期探讨[J].地质学报,2006,80(5):674-684.
[29]Passey Q R,Creaney S,Kulla J B,et al.A practical model for organic richness from porosity and resistivity logs[J].AAPGBulletin,1990,74(12):1777-1794.
[30]Wang Lan,Li Wenhou,Lin Tong,et al.Diagenesis and its influence factors of the Chang 6interval of Upper Triassic Yanchang Formation in Ordos Basin[J].Journal of Palaeogeography,2012,14(3):311-320.王岚,李文厚,林潼,等.鄂尔多斯盆地上三叠统延长组长6油层组储集层成岩作用及其影响因素[J].古地理学报,2012,14(3):311-320.
[31]Bai Yubin,Gao Zhendong,Li Zhongfeng,et al.Geochemical characteristics of crude oil and oil-source correlation in Yanchang Formation in Xingzichuan Oilfield,Ordos Basin[J].Petroleum Geology&Experiment,2013,35(5):552-558.白玉彬,高振东,李忠锋,等.鄂尔多斯盆地杏子川油田延长组原油地球化学特征与油源探讨[J].石油实验地质,2013,35(5):552-558.
[32]Du Jiangmin,Wang Qingchun,Zhao Yande,et al.Geochemical characteristics and source analysis of the Chang 6crude oil in Shanbei area,Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2018,48(2):246-254.杜江民,王青春,赵彦德,等.鄂尔多斯盆地陕北地区延长组长6原油地球化学特征及油源分析[J].西北大学学报:自然科学版,2018,48(2):246-254.
[33]Wang Xiaomei,Wang Zhenliang,Guan Hong,et al.A study on hydrocarbon migration and accumulation in Yanchang area of the Ordos Basin[J].Natural Gas Geoscience,2006,17(4):485-489.王晓梅,王震亮,管红,等.鄂尔多斯盆地延长矿区油气运移成藏研究[J].天然气地球科学,2006,17(4):485-489.
[34]Yao Jingli,Gao Gang,Pang Jinlian,et al.Development characteristics of non-main effective source rocks of the Yanchang Formation in eastern Gansu Province of Ordos Basin[J].Earth Science Frontiers,2013,20(2):116-124.姚泾利,高岗,庞锦莲,等.鄂尔多斯盆地陇东地区延长组非主力有效烃源岩发育特征[J].地学前缘,2013,20(2):116-124.
[35]Liu Guangdi,Yang Weiwei,Feng Yuan,et al.Geochemical characteristics and genetic types of crude oil from Yanchang Formation in Longdong area,Ordos Basin[J].Earth Science Frontiers,2013,20(2):108-115.柳广弟,杨伟伟,冯渊,等.鄂尔多斯盆地陇东地区延长组原油地球化学特征及成因类型划分[J].地学前缘,2013,20(2):108-115.
[36]Zheng Rongcai,Niu Xiaobing,Liang Xiaowei,et al.Study on the property and origin of crude oil of Yanchang Formation in Jiyuan Oilfield,Ordos Basin[J].Journal of Earth Sciences and Environment,2011,33(2):142-145.郑荣才,牛小兵,梁晓伟,等.鄂尔多斯盆地姬塬油田延长组原油性质与来源分析[J].地球科学与环境学报,2011,33(2):142-145.
[37]Wang Ruogu,Li Wenhou,Liao Youyun,et al.Provenance analysis of Chang 7 member of Triassic Yanchang Formation in Ordos Basin[J].Geological Bulletin of China,2013,32(4):671-684.王若谷,李文厚,廖友运,等.鄂尔多斯盆地三叠系延长组长7段物源区分析[J].地质通报,2013,32(4):671-684.
[38]Zhang Dongyang.Sedimentary Facies of Chang 8Oil Formation of the Triassic Yancahng Formation in Ordos Basin[D].Xi’an:Northwest University,2008.张东阳.鄂尔多斯盆地三叠系延长组长8油层组沉积相研究[D].西安:西北大学,2008.
[39]Chu Meijuan,Li Shixiang,Liu Xianyang,et al.Accumulation mechanisms and modes of Yanchang Formation Chang 9interval hydrocarbons in Ordos Basin[J].Acta Sedimentologica Sinica,2013,31(4):683-692.楚美娟,李士祥,刘显阳,等.鄂尔多斯盆地延长组长8油层组石油成藏机理及成藏模式[J].沉积学报,2013,31(4):683-692.
[40]Zhang Xiaoli,Duan Yi,He Jinxian,et al.Analysis of reservoir forming conditions of Chang 8Formation in Huaqing area,Ordos Basin[J].Geological Science and Technology Information,2013,32(4):127-132.张晓丽,段毅,何金先,等.鄂尔多斯盆地华庆地区三叠系延长组长8油层组油气成藏条件分析[J].地质科技情报,2013,32(4):127-132.
[41]Duan Yi,Wu Baoxiang,Zhang Hui,et al.Geochemistry and Genesis of crude oils of Xifeng Oilfield in the Ordos Basin[J].Acta Geological Sinica,2006,80(2):301-310.段毅,吴保祥,张辉,等.鄂尔多斯盆地西峰油田原油地球化学特征及其成因[J].地质学报,2006,80(2):301-310.
[42]Luo Xiaorong,Zhang Liuping,Yang Hua,et al.Oil accumulation process in the low-permeability Chang 81 member of Longdong area,the Ordos Basin[J].Oil&Gas Geology,2010,31(6):770-778.罗晓容,张刘平,杨华,等.鄂尔多斯盆地陇东地区长81段低渗油藏成藏过程[J].石油与天然气地质,2010,31(6):770-778.
[43]Duan Yi,Wu Baoxiang,Zheng Chaoyang,et al.Pool-forming dynamic properties of Xifeng Oilfield in Ordos Basin[J].Acta Petrolei Sinica,2005,26(4):29-33.段毅,吴保祥,郑朝阳,等.鄂尔多斯盆地西峰油田油气成藏动力学特征[J].石油学报,2005,26(4):29-33.
[44]Deng Xiuqin,Yao Jingli,Hu Xifeng,et al.Characteristics and geological significance of hydrodynamic system on ultra-low permeability reservoir of Yanchang Formation in Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2011,41(6):1044-1050.邓秀芹,姚泾利,胡喜锋,等.鄂尔多斯盆地延长组超低渗透岩性油藏成藏流体动力系统特征及其意义[J].西北大学学报:自然科学版,2011,41(6):1044-1050.
[45]Wang Xiangzeng,Ren Laiyi,Zhang Lixia,et al.Oil and source rock correlation of lower assemblage of Yanchang Formation in Wuqi and Dingbian areas,Ordos Basin[J].Petroleum Geology&Experiment,2013(4):426-431.王香增,任来义,张丽霞,等.鄂尔多斯盆地吴起-定边地区延长组下组合油源对比研究[J].石油实验地质,2013(4):426-431.
[46]Fu Jinhua,Li Shixiang,Liu Xianyang,et al.Multi-layer composite accumulation mechanism and exploration significance of Jiyuan Oilfield,Ordos Basin[J].China Petroleum Exploration,2013,18(5):1-9.付金华,李士祥,刘显阳,等.鄂尔多斯盆地姬塬大油田多层系复合成藏机理及勘探意义[J].中国石油勘探,2013,18(5):1-9.
[47]Zhou Jingao,Yao Genshun,Deng Hongying,et al.Exploration potential of Chang 9 member,Yanchang Formation,Ordos Basin[J].Petroleum Exploration and Development,2008,35(3):289-293.周进高,姚根顺,邓红婴,等.鄂尔多斯盆地延长组长9油层组勘探潜力分析[J].石油勘探与开发,2008,35(3):289-293.
[48]Shi Baohong,Yao Jingli,Zhang Yan,et al.Geologic conditions for hydrocarbon accumulation in Chang 9oil reservoir of the Yanchang Formation,Ordos Basin[J].Oil&Gas Geology,2013,34(3):294-300.时保宏,姚泾利,张艳,等.鄂尔多斯盆地延长组长9油层组成藏地质条件[J].石油与天然气地质,2013,34(3):294-300.
[49]Wu Baoxiang,Duan Yi,Zheng Chaoyang,et al.Fluid overpressure and migration of oil and gas from Chang 9 member in Gufengzhuang-Wangwazi area,Ordos Basin[J].Acta Geological Sinica,2008,82(6):844-849.吴保祥,段毅,郑朝阳,等.鄂尔多斯盆地古峰庄-王洼子地区长9油层组流体过剩压力与油气运移研究[J].地质学报,2008,82(6):844-849.
[50]Johnson R L.The Pronghorn Member of the Bakken Formation,Williston Basin,USA:Lithology,Stratigraphy,Reservoir Properties[C].AAPG Annual Convention and Exhibition,Pittsburgh,Pennsylvania,2013.
[51]Skinner O,Canter L,Sonnenfeld M D,et al.Discovery of“Pronghorn”and“Lewis and Clark”Fields:Sweet-Spots within the Bakken Petroleum System Producing from the Sanish/Pronghorn Member NOT the Middle Bakken or Three Forks[C].AAPG Annual Convention and Exhibition,Long Beach,California,USA,2012.
[2]Zhang Wenzheng,Yang Hua,Yang Yihua,et al.Petrology and element geochemistry and development environment of Yanchang Formation Chang-7high quality source rocks in Ordos Basin[J].Geochimica,2008,37(1):59-64.张文正,杨华,杨奕华,等.鄂尔多斯盆地长7优质烃源岩的岩石学,元素地球化学特征及发育环境[J].地球化学,2008,37(1):59-64.
[3]Yang Hua,Li Shixiang,Liu Xianyang.Characteristics and resource prospects of tight oil and shale oil in Ordos Basin[J].Acta Petrolei Sinica,2013,34(1):1-11.杨华,李士祥,刘显阳.鄂尔多斯盆地致密油、页岩油特征及资源潜力[J].石油学报,2013,34(1):1-11.
[4]Liu Wenhou,Pang Jungang,Cao Hongxia,et al.Depositional system and paleogeographic evolution of the Late Triassic Yanchang stage in Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2009,39(3):501-506.李文厚,庞军刚,曹红霞,等.鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化[J].西北大学学报:自然科学版,2009,39(3):501-506.
[5]Hu Chaoyuan.An approach on regional controlling factors of oil-gas field distribution in offshore sedimentary basins of China[J].Marine Geology&Quaternary Geology,1986,6(4):23-29.胡朝元.我国海上沉积盆地油气田分布区域控制因素的探讨[J].海洋地质与第四纪地质,1986,6(4):23-29.
[6]Hu Chaoyuan.Research on the appliance extent of source control theory by semi-quantitative statistics characteristics of oil and gas migration distance[J].Natural Gas Industry,2005,25(10):1-3.胡朝元.“源控论”适用范围量化分析[J].天然气工业,2005,25(10):1-3.
[7]Zou Caineng,Tao Shizhen,Hou Lianhua,et al.Unconventional Oil and Gas Geology[M].Second Edition.Beijing:Geological Publishing House,2013:9-14.邹才能,陶士振,侯连华,等.非常规油气地质[M].第二版.北京:地质出版社,2013:9-14.
[8]Cui Jingwei,Zhu Rukai,Wu Songtao,et al.Heterogeneity and lower oily limits for tight sandstones:A case study on Chang-7oil layers of the Yanchang Formation,Ordos Basin[J].Acta Petrolei Sinica,2013,34(5):877-882.崔景伟,朱如凯,吴松涛,等.致密砂岩层内非均质性及含油下限---以鄂尔多斯盆地三叠系延长组长7段为例[J].石油学报,2013,34(5):877-882.
[9]Cui Jingwei,Zhu Rukai,Li Shixiang,et al.Movable oil and its controlling factors in tight sandstones:A case study of the Triassic Chang 7reservoir,Yanchang Formation,Ordos Basin[J].Petroleum Geology&Experiment,2016,38(4):536-542.崔景伟,朱如凯,李士祥,等.致密砂岩油可动量及其主控因素---以鄂尔多斯盆地三叠系延长组长7为例[J].石油实验地质,2016,38(4):536-542.
[10]Tian Jingchun,Chen Gaowu,Dou Weitan,et al.Origin and association types of lake delta front sandstones and their distribution patterns of Triassic Yanchang Formation in Ordos Basin,China[J].Journal of Chengdu University of Technology,Science&Technology Edition,2004,31(6):636-640.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---以鄂尔多斯盆地姬塬白豹地区三叠系延长组为例[J].成都理工大学学报:自然科学版,2004,31(6):636-640.
[11]China National Standardizing Committee.GB/T19145-2003Determination of Total Organic Carbon in Sedimentary Rock[S].Beijing:Standards Press of China,2003.中国国家标准化管理委员会.GB/T19145-2003沉积岩中总有机碳的测定标准[S].北京:中国标准出版社,2003.
[12]China National Standardizing Committee.GB/T18602-2012RockPyrolysis Analysis[S].Beijing:Standards Press of China,2012.中国国家标准化管理委员会.GB/T18602-2012岩石热解分析[S].北京:中国标准出版社,2012.
[13]Behar F,Beaumont V,Penteado H L D B.Rock-Eval 6technology:Performances and developments[J].Oil&Gas Science and Technology,2001,56(2):111-134.
[14]China National Standardizing Committee.GB/T6948-2008Method of Determining Microscopically the Reflectance ofVitrinite in Coal[S].Beijing:Standards Press of China,2008.中国国家标准化管理委员会.GB/T6948-2008煤的镜质体反射率显微镜测定方法[S].北京:中国标准出版社,2008.
[15]Zou C N,Zhu R K,Chen Z Q,et al.Organic-matter-rich shales of China[J].Earth-Science Reviews,2019,189:51-78.
[16]Zhu Guangyou,Jin Qiang,Zhou Jianlin,et al.Source rock characters of cyclic deep-lake facies in the Dongying Depression[J].Chinese Journal of Geology,2003,38(2):254-262.朱光有,金强,周建林,等.东营凹陷旋回式深湖相烃源岩研究[J].地质科学,2003,38(2):254-262.
[17]Zhang Shuichang,Zhang Baoming,Wang Feiyu,et al.The organic matter properties,environment and controlling factors of the two set of marine source rock in Tarim Basin[J].Advance in Natural Science,2001,11(3):261-268.张水昌,张保民,王飞宇,等.塔里木盆地两套海相有效烃源岩层-Ⅰ.有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261-268.
[18]Yang Minghui,Xia Wenchen,Zhang Bingshan,et al.Parasequence-shale organic facies variations and its significance in Nonmarine Basin[J].Acta Sedimentologica Sinica,2000,18(2):297-301.杨明慧,夏文臣,张兵山,等.非海相盆地准层序级别的有机相变化及其地质意义[J].沉积学报,2000,18(2):297-301.
[19]Shi Zhiqiang,Han Yonglin,Zhao Junxing,et al.Depositional system and paleogeographic evolution of the Middle Jurassic Yan’anian stage in the central and southern Ordos Basin[J].Acta Geoscientia Sinica,2003,24(1):49-54.时志强,韩永林,赵俊兴,等.鄂尔多斯盆地中南部中侏罗世延安期沉积体系及岩相古地理演化[J].地球学报,2003,24(1):49-54.
[20]Wang Lei.The Recovery of the Paleoproductivity in the Period of Chang 7in Ordos Basin and Its Control Factors[D].Xi’an:Northwest University,2015.王磊.鄂尔多斯盆地延长组长7期湖盆古生产力恢复及其控制因素[D].西安:西北大学,2015.
[21]Zhu Guangyou,Jin Qiang.Study on source rock heterogeneityA case of Niu-38Well in Dongying depression[J].Acta Petrolei Sinica,2002,23(5):34-39.朱光有,金强.烃源岩的非均质性研究-以东营凹陷牛38井为例[J].石油学报,2002,23(5):34-39.
[22]Wang Huizhong,Mei Hongming.Paleolimnological information from the oil shale in the lower part of Sha 3Formation,in Dongying Depression[J].Journal Of Tongji University,1998,26(3):315-319.王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315-319.
[23]Zhang Wenzheng,Yang Hua,Peng Ping’an,et al.The influence of Late Triassic volcanism on the development of Chang7high grade hydrocarbon source rock in Ordos Basin[J].Geochimica,2009,38(6):573-582.张文正,杨华,彭平安,等.晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响[J].地球化学,2009,38(6):573-582.
[24]Cui J W,Zhu R K,Luo Z,et al.Sedimentary and geochemical characteristics of Triassic Chang 7 member Shale in Southeastern Ordos Basin,Central China[J].Petroleum Science,2019,16(2):285-297.
[25]Carroll A R,Bohacs K M.Lake-type controls on petroleum source rock potential in nonmarine basins[J].AAPG Bulletin,2001,85(6):1033-1053.
[26]Liu Qun,Yuan Xuanjun,Lin Senhu,et al.Depositional environment and characteristic comparison between lacustrine mudstone and shale:A case study from the Chang 7member of the Yanchang Formation,Ordos Basin[J].Oil&Gas Geology,2018,39(3):531-540.刘群,袁选俊,林森虎,等.湖相泥岩、页岩的沉积环境和特征对比---以鄂尔多斯盆地延长组7段为例[J].石油与天然气地质,2018,39(3):531-540.
[27]Yuan Xuanjun,Lin Senhu,Liu Qun,et al.Lacustrine finegrained sedimentary features and organic-rich shale distribution pattern:A case study of Chang 7 member of Triassic Yanchang Formation in Ordos Basin,NW China[J].Petroleum Exporation and Development,2015,42(1):34-43.袁选俊,林森虎,刘群,等.湖盆细粒沉积特征与富有机质页岩分布模式---以鄂尔多斯盆地延长组长7油层组为例[J].石油勘探与开发,2015,42(1):34-43.
[28]Ren Zhanli,Zhang Sheng,Gao Shengli,et al.Research on region of maturation anomaly and formation time in Ordos Basin[J].Acta Geologica Sinica,2006,80(5):674-684.任战利,张盛,高胜利,等.鄂尔多斯盆地热演化程度异常分布区及形成时期探讨[J].地质学报,2006,80(5):674-684.
[29]Passey Q R,Creaney S,Kulla J B,et al.A practical model for organic richness from porosity and resistivity logs[J].AAPGBulletin,1990,74(12):1777-1794.
[30]Wang Lan,Li Wenhou,Lin Tong,et al.Diagenesis and its influence factors of the Chang 6interval of Upper Triassic Yanchang Formation in Ordos Basin[J].Journal of Palaeogeography,2012,14(3):311-320.王岚,李文厚,林潼,等.鄂尔多斯盆地上三叠统延长组长6油层组储集层成岩作用及其影响因素[J].古地理学报,2012,14(3):311-320.
[31]Bai Yubin,Gao Zhendong,Li Zhongfeng,et al.Geochemical characteristics of crude oil and oil-source correlation in Yanchang Formation in Xingzichuan Oilfield,Ordos Basin[J].Petroleum Geology&Experiment,2013,35(5):552-558.白玉彬,高振东,李忠锋,等.鄂尔多斯盆地杏子川油田延长组原油地球化学特征与油源探讨[J].石油实验地质,2013,35(5):552-558.
[32]Du Jiangmin,Wang Qingchun,Zhao Yande,et al.Geochemical characteristics and source analysis of the Chang 6crude oil in Shanbei area,Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2018,48(2):246-254.杜江民,王青春,赵彦德,等.鄂尔多斯盆地陕北地区延长组长6原油地球化学特征及油源分析[J].西北大学学报:自然科学版,2018,48(2):246-254.
[33]Wang Xiaomei,Wang Zhenliang,Guan Hong,et al.A study on hydrocarbon migration and accumulation in Yanchang area of the Ordos Basin[J].Natural Gas Geoscience,2006,17(4):485-489.王晓梅,王震亮,管红,等.鄂尔多斯盆地延长矿区油气运移成藏研究[J].天然气地球科学,2006,17(4):485-489.
[34]Yao Jingli,Gao Gang,Pang Jinlian,et al.Development characteristics of non-main effective source rocks of the Yanchang Formation in eastern Gansu Province of Ordos Basin[J].Earth Science Frontiers,2013,20(2):116-124.姚泾利,高岗,庞锦莲,等.鄂尔多斯盆地陇东地区延长组非主力有效烃源岩发育特征[J].地学前缘,2013,20(2):116-124.
[35]Liu Guangdi,Yang Weiwei,Feng Yuan,et al.Geochemical characteristics and genetic types of crude oil from Yanchang Formation in Longdong area,Ordos Basin[J].Earth Science Frontiers,2013,20(2):108-115.柳广弟,杨伟伟,冯渊,等.鄂尔多斯盆地陇东地区延长组原油地球化学特征及成因类型划分[J].地学前缘,2013,20(2):108-115.
[36]Zheng Rongcai,Niu Xiaobing,Liang Xiaowei,et al.Study on the property and origin of crude oil of Yanchang Formation in Jiyuan Oilfield,Ordos Basin[J].Journal of Earth Sciences and Environment,2011,33(2):142-145.郑荣才,牛小兵,梁晓伟,等.鄂尔多斯盆地姬塬油田延长组原油性质与来源分析[J].地球科学与环境学报,2011,33(2):142-145.
[37]Wang Ruogu,Li Wenhou,Liao Youyun,et al.Provenance analysis of Chang 7 member of Triassic Yanchang Formation in Ordos Basin[J].Geological Bulletin of China,2013,32(4):671-684.王若谷,李文厚,廖友运,等.鄂尔多斯盆地三叠系延长组长7段物源区分析[J].地质通报,2013,32(4):671-684.
[38]Zhang Dongyang.Sedimentary Facies of Chang 8Oil Formation of the Triassic Yancahng Formation in Ordos Basin[D].Xi’an:Northwest University,2008.张东阳.鄂尔多斯盆地三叠系延长组长8油层组沉积相研究[D].西安:西北大学,2008.
[39]Chu Meijuan,Li Shixiang,Liu Xianyang,et al.Accumulation mechanisms and modes of Yanchang Formation Chang 9interval hydrocarbons in Ordos Basin[J].Acta Sedimentologica Sinica,2013,31(4):683-692.楚美娟,李士祥,刘显阳,等.鄂尔多斯盆地延长组长8油层组石油成藏机理及成藏模式[J].沉积学报,2013,31(4):683-692.
[40]Zhang Xiaoli,Duan Yi,He Jinxian,et al.Analysis of reservoir forming conditions of Chang 8Formation in Huaqing area,Ordos Basin[J].Geological Science and Technology Information,2013,32(4):127-132.张晓丽,段毅,何金先,等.鄂尔多斯盆地华庆地区三叠系延长组长8油层组油气成藏条件分析[J].地质科技情报,2013,32(4):127-132.
[41]Duan Yi,Wu Baoxiang,Zhang Hui,et al.Geochemistry and Genesis of crude oils of Xifeng Oilfield in the Ordos Basin[J].Acta Geological Sinica,2006,80(2):301-310.段毅,吴保祥,张辉,等.鄂尔多斯盆地西峰油田原油地球化学特征及其成因[J].地质学报,2006,80(2):301-310.
[42]Luo Xiaorong,Zhang Liuping,Yang Hua,et al.Oil accumulation process in the low-permeability Chang 81 member of Longdong area,the Ordos Basin[J].Oil&Gas Geology,2010,31(6):770-778.罗晓容,张刘平,杨华,等.鄂尔多斯盆地陇东地区长81段低渗油藏成藏过程[J].石油与天然气地质,2010,31(6):770-778.
[43]Duan Yi,Wu Baoxiang,Zheng Chaoyang,et al.Pool-forming dynamic properties of Xifeng Oilfield in Ordos Basin[J].Acta Petrolei Sinica,2005,26(4):29-33.段毅,吴保祥,郑朝阳,等.鄂尔多斯盆地西峰油田油气成藏动力学特征[J].石油学报,2005,26(4):29-33.
[44]Deng Xiuqin,Yao Jingli,Hu Xifeng,et al.Characteristics and geological significance of hydrodynamic system on ultra-low permeability reservoir of Yanchang Formation in Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2011,41(6):1044-1050.邓秀芹,姚泾利,胡喜锋,等.鄂尔多斯盆地延长组超低渗透岩性油藏成藏流体动力系统特征及其意义[J].西北大学学报:自然科学版,2011,41(6):1044-1050.
[45]Wang Xiangzeng,Ren Laiyi,Zhang Lixia,et al.Oil and source rock correlation of lower assemblage of Yanchang Formation in Wuqi and Dingbian areas,Ordos Basin[J].Petroleum Geology&Experiment,2013(4):426-431.王香增,任来义,张丽霞,等.鄂尔多斯盆地吴起-定边地区延长组下组合油源对比研究[J].石油实验地质,2013(4):426-431.
[46]Fu Jinhua,Li Shixiang,Liu Xianyang,et al.Multi-layer composite accumulation mechanism and exploration significance of Jiyuan Oilfield,Ordos Basin[J].China Petroleum Exploration,2013,18(5):1-9.付金华,李士祥,刘显阳,等.鄂尔多斯盆地姬塬大油田多层系复合成藏机理及勘探意义[J].中国石油勘探,2013,18(5):1-9.
[47]Zhou Jingao,Yao Genshun,Deng Hongying,et al.Exploration potential of Chang 9 member,Yanchang Formation,Ordos Basin[J].Petroleum Exploration and Development,2008,35(3):289-293.周进高,姚根顺,邓红婴,等.鄂尔多斯盆地延长组长9油层组勘探潜力分析[J].石油勘探与开发,2008,35(3):289-293.
[48]Shi Baohong,Yao Jingli,Zhang Yan,et al.Geologic conditions for hydrocarbon accumulation in Chang 9oil reservoir of the Yanchang Formation,Ordos Basin[J].Oil&Gas Geology,2013,34(3):294-300.时保宏,姚泾利,张艳,等.鄂尔多斯盆地延长组长9油层组成藏地质条件[J].石油与天然气地质,2013,34(3):294-300.
[49]Wu Baoxiang,Duan Yi,Zheng Chaoyang,et al.Fluid overpressure and migration of oil and gas from Chang 9 member in Gufengzhuang-Wangwazi area,Ordos Basin[J].Acta Geological Sinica,2008,82(6):844-849.吴保祥,段毅,郑朝阳,等.鄂尔多斯盆地古峰庄-王洼子地区长9油层组流体过剩压力与油气运移研究[J].地质学报,2008,82(6):844-849.
[50]Johnson R L.The Pronghorn Member of the Bakken Formation,Williston Basin,USA:Lithology,Stratigraphy,Reservoir Properties[C].AAPG Annual Convention and Exhibition,Pittsburgh,Pennsylvania,2013.
[51]Skinner O,Canter L,Sonnenfeld M D,et al.Discovery of“Pronghorn”and“Lewis and Clark”Fields:Sweet-Spots within the Bakken Petroleum System Producing from the Sanish/Pronghorn Member NOT the Middle Bakken or Three Forks[C].AAPG Annual Convention and Exhibition,Long Beach,California,USA,2012.