作者:李庆;姜在兴;由雪莲;赵贤正;张锐锋; 时间:2016-01-01 点击数:
李庆;姜在兴;由雪莲;赵贤正;张锐锋;
1:中国石油大学(北京)地球科学学院
2:中国石油大学(北京)油气资源与探测国家重点实验室
3:中国地质大学(北京)能源学院
4:中国地质大学(北京)海洋学院
摘要(Abstract):
为分析有机相对非常规油气储层的影响并对储层进行评价,以束鹿凹陷富有机质泥灰岩储层为例,根据岩石热解参数、干酪根元素组成和有机质来源等划分有机相类型,确定储层评价参数及标准。结果表明,有机质在热演化过程中生成有机质孔隙,在排烃过程中产生的酸性流体和异常高压等形成溶蚀孔隙及裂缝,可以改善储集性能。研究区有机相包括AB、B、BC、C、CD及D六种类型,缺少A类型发育。有机相变化对储层的储集性能具有重要控制作用,可作为非常规油气储层评价的参数。束鹿凹陷沙三下亚段层序2的坡折带及洼槽区部位发育具有优质有机相AB类型的高有机质泥灰岩,储集性能较好,为有利目标区。该结果对评价页岩油气等非常规油气储层具有指导意义。
关键词(KeyWords):有机相;非常规油气;储层评价;页岩油气;泥灰岩;束鹿凹陷
Abstract:
Keywords:
基金项目(Foundation):国家科技重大专项(2016ZX05049006-001-002);; 中国石油大学(北京)科研基金项目(2462015YJRC022)
作者(Author):李庆;姜在兴;由雪莲;赵贤正;张锐锋;
Email:
参考文献(References):
[1]Jarvie D M,Hill R J,Ruble T E,et al.Unconventional shale-gas systems:The Mississippian Barnett shale of north-central Texas as one model for thermogenic shale-gas assessment[J].AAPG Bulletin,2007,91(4):475-499.
[2]Loucks R G,Reed R M,Ruppel S C,et al.Spectrum of pore types and networks in mudrocks and a descriptive classification for matrix-related mudrock pores[J].AAPG Bulletin,2012,96(6):1071-1098.
[3]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.
[4]久凯,丁文龙,黄文辉,等.渤海湾盆地济阳拗陷沙三段页岩气地质条件分析[J].大庆石油学院学报,2012,36(2):65-70.Jiu Kai,Ding Wenlong,Huang Wenhui,et al.Analysis of geological condition of the formation of Shahejie shale gas in Jiyang depression in Bohai Bay basin[J].Journal of Daqing Petroleum Institute,2012,36(2):65-70.
[5]梁超,姜在兴,郭岭,等.陆棚相黑色泥岩发育特征、沉积演化及页岩气勘探前景——以瓮安永和剖面牛蹄塘组为例[J].大庆石油学院学报,2011,35(6):13-21.Liang Chao,Jiang Zaixing,Guo ling,et al.Characteristics of black shale,sedimentary evolution and shale gas exploration prospect of shelf face taking Weng'an Yonghe profile Niutitang group as an example[J].Journal of Daqing Petroleum Institute,2011,35(6):13-21.
[6]单衍胜,张金川,李晓光,等.辽河盆地东部凸起太原组页岩气聚集条件及有利区预测[J].大庆石油学院学报,2012,36(1):1-7.Shan Yansheng,Zhang Jinchuan,Li Xiaoguang,et al.Shale gas accumulation factors and prediction of favorable area of Taiyuan formation in Liaohe eastern uplift[J].Journal of Daqing Petroleum Institute,2012,36(1):1-7.
[7]邹才能,杨智,陶士振,等.纳米油气与源储共生型油气聚集[J].石油勘探与开发,2012,39(1):13-26.Zou Caineng,Yang Zhi,Tao Shizhen,et al.Nano-hydrocarbon and the accumulation in coexisting source and reservoir[J].Petroleum Exploration and Development,2012,39(1):13-26.
[8]姜在兴,张文昭,梁超,等.页岩油储层基本特征及评价要素[J].石油学报,2014,35(1):184-196.Jiang Zaixing,Zhang Wenzhao,Liang Chao,et al.Characteristics and evaluation elements of shale oil reservoir[J].Acta Petrolei Sinica,2014,35(1):184-196.
[9]于炳松.页岩气储层的特殊性及其评价思路和内容[J].地学前缘,2012,19(3):252-258.Yu Bingsong.Particularity of shale gas reservoir and its evaluation[C].Earth Science Frontiers,2012,19(3):252-258.
[10]Rogers M A.Application of organic facies concept to hydrocarbon source rock evaluation[J].Bucharest:The 10th World Petrolum Congress,1979.
[11]郝芳,陈建渝,孙永传,等.有机相研究及其在盆地分析中的应用[J].沉积学报,1994,12(4):77-86.Hao Fang,Chen Jianyu,Sun Yongchuan,et al.Organic facies studies and their use in sedimentary basin analysis[J].Acta Sedimentologica Sinica,1994,12(4):77-86.
[12]Filho J G M,Menezes T R,de Oliveira Mendon a J,et al.Organic facies:Palynofacies and organic geochemistry approaches[M].Rijeka:INTECH Open Access Publisher,2012.
[13]Tyson R V.Sedimentary organic matter,organic facies and palynofacies[M].London:Chapman and Hall,1995.
[14]Hao F,Zhou X,Zhu Y,et al.Lacustrine source rock deposition in response to co-evolution of environments and organisms controlled by tectonic subsidence and climate,Bohai Bay basin,China[J].Organic Geochemistry,2011,42(4):323-339.
[15]金凤鸣,韩春元,王吉茂,等.有机地球化学参数在层序划分对比中的应用——以冀中坳陷束鹿凹陷沙三下亚段为例[J].沉积学报,2008,26(1):86-91.Jin Fengming,Han Chunyuan,Wang Jimao,et al.Application of organic geochemical parameters in sequence classification and correlation:A case study from lower Es3in Shulu sag,Jizhong depression[J].Acta Sedimentologica Sinica,2008,26(1):86-91.
[16]梁宏斌,旷红伟,刘俊奇,等.冀中坳陷束鹿凹陷古近系沙河街组三段泥灰岩成因探讨[J].古地理学报,2007,9(2):167-174.Liang Hongbin,Kuang Hongwei,Liu Junqi,et al.Discussion on origin for marls of the member 3of Shahejie formation of Paleogene in Shulu sag of central Hebei depression[J].Journal of Palaeogeography,2007,9(2):167-174.
[17]Jiang Z,Chen D,Qiu L,et al.Source-controlled carbonates in a small Eocene half-graben lake basin(Shulu sag)in central Hebei province,north China[J].Sedimentology,2007,54(2):265-292.
[18]Zheng L,Jiang Z,Liu H,et al.Core evidence of paleoseismic events in Paleogene deposits of the Shulu sag in the Bohai Bay basin,east China,and their petroleum geologic significance[J].Sedimentary Geology,2015,328:33-54.
[19]Zhao X,Li Q,Jiang Z,et al.Organic geochemistry and reservoir characterization of the organic matter-rich calcilutite in the Shulu sag,Bohai Bay basin,north China[J].Marine and Petroleum Geology,2014,51:239-255.
[20]Fishman N S,Hackley P C,Lowers H A,et al.The nature of porosity in organic-rich mudstones of the upper Jurassic Kimmeridge Clay formation,North sea,offshore United Kingdom[J].International Journal of Coal Geology,2012,103:32-50.
[21]Milliken K L,Rudnicki M,Awwiller D N,et al.Organic matter-hosted pore system Marcellus formation(Devonian)Pennsylvania[J].AAPG Bulletin,2013,97(2):177-200.
[22]Loucks R G,Reed R M,Ruppel S C,et al.Morphology genesis and distribution of nanometer-scale pores in siliceous mudstones of the Mississippian Barnett shale[J].Journal of Sedimentary Research,2009,79(12):848-861.
[23]Curtis M E,Ambrose R J,Sondergeld C S,et al.Structural characterization of gas shales on the micro and nano scales[C].Calgary:Canadian Unconventional Resources and International Petroleum Conference.2010:SPE 137693.
[24]Bernard S,Wirth R,Schreiber A,et al.Formation of nanoporous pyrobitumen residues during maturation of the Barnett shale(Fort Worth basin)[J].International Journal of Coal Geology,2012,103:3-11.
[25]Jarvie D M.Shale resource systems for oil and gas:Part 1:Shale-gas resource systems,in shale reservoirs:Giant resources for the21st century[J].AAPG Memoir,2012,97:69-87.
[26]Modica C J,Lapierre S G.Estimation of kerogen porosity in source rocks as a function of thermal transformation:Example from the Mowry shale in the Powder River basin of Wyoming[J].AAPG Bulletin,2012,96(1):87-108.
[27]Romero-Sarmiento M F,Ducros M,Carpentier B,et al.Quantitative evaluation of TOC,organic porosity and gas retention distribution in a gas shale play using petroleum system modeling,application to the Mississippian Barnett shale[J].Marine and Petroleum Geology,2013,45:315-330.
[28]Millard M,Ruble T.Utilizing hydrocarbon yield determinations to evaluate source/reservoir relationships in the Bakken/Three Forks of the Williston basin ND[C].Denver:Unconventional Resources Technology Conference(URTEC),2014.
[29]Curtis M E,Cardott B J,Sondergeld C H,et al.Development of organic porosity in the Woodford shale with increasing thermal maturity[J].International Journal of Coal Geology,2012,103:26-31.
[30]Ambrose R J,Hartman R C,Diaz-Campos M,et al.Shale gas-in-place calculations part I:New pore-scale considerations[J].SPE Journal,2012,17(1):219-229.
[31]Sondergeld C H,Ambrose R J,Rai C S,et al.Micro-structural studies of gas shales[C].SPE Unconventional Gas Conference.2010,MS-131771.
[32]Surdam R C,Boese S,Crossey L J.Role of organic and inorganic reactions in development of secondary porosity in sandstones[J].AAPG Bulletin,1982,66:635-635.
[33]MacGowan D B,Surdam R C.Carboxylic acid anions in formation waters San Joaquin basin and Louisiana Gulf Coast,USA:Implications for clastic diagenesis[J].Applied Geochemistry,1990,5:687-701.
[34]Schieber J.Common themes in the formation and preservation of intrinsic porosity in shales and mudstones-illustrated with examples across the Phanerozoic[J].Pittsburgh:SPE Unconventional Gas Conference,2010.
[35]Parnell J,Carey P F.Emplacement of bitumen(asphaltite)veins in the Neuquén basin,Argentina[J].AAPG Bulletin,1995,79:1798-1815.
[36]Parnell J,Honghan C,Middleton D,et al.Significance of fibrous mineral veins in hydrocarbon migration:fluid inclusion studies[J].Journal of Geochemical Exploration,2000,69:623-627.
[37]Hubbert M K,Willis D G.Mechanics of hydraulic fracturing[J].AIME Petroleum Trans,1957,210:153-163.
[38]Snarsky A N.Die primare migration des Erdols[M].[s.l.]Freiburger Forschungsh,1962.
[39]Pasley M A.Organic matter variation within depositional sequences stratigraphic significance of implication to petroleum source rock prediction[D].Louisiana:The Louisiana State University and agricultural and Mechanical Col Louisiana(USA)PhD Thesis,1991.
[40]Jones R W.Organic facies[M]//Welte D.Advances in Petroleum Geochemistry II Brooks J.London:Academic press,1987,1-90.
2019 版权所有©东北石油大学 | 地址:黑龙江省大庆市高新技术产业开发区学府街99号 | 邮政编码:163318
信息维护:学报 | 技术支持:现代教育技术中心
网站访问量: