油气田开发中构造地质成因分析进展
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摘要
构造地质成因分析,在油气田开发中具有十分重要的作用。文章从国内外研究现状入手,在文献调研基础上详细对比了油气田开发中构造地质成因分析的优缺点。总结了构造地质成因分析研究内容:(1)通过构造演化历史分析和地应力场等研究,确定断裂体系构造地质成因。(2)井震结合开展精细的构造解释,分析构造地质成因。(3)对构造地质成因研究方法进行探索和改进。(4)综合动静态资料,开展储层地质成因分析。(5)与沉积相研究和成岩作用研究等紧密结合。(6)加强地质成因分析成果应用,为油气田开发提供基础。(7)裂缝表征和建模。(8)微构造地质成因分析。油气田开发中构造地质成因分析的方法主要包括:基础地质研究、野外露头观察描述、岩心观察和描述、镜下薄片观察、物理模拟、各种测井解释、地震解释、各种分析测试统计、地质建模、动态监测和生产动态分析方法等。结合研究实践,对每一种方法的优缺点进行分析。在此基础上,指出了油气田开发中构造地质成因分析存在的8方面主要问题和发展趋势。
The genesis analysis of structural geology plays an important role in the oil and gas field development. Based on the research advances in China and abroad, the advantages and disadvantages of the study in this field are compared in detail. There are eight research directions in general. First, the structural geological genesis of fault system is determined through the analysis of structural evolution history and stress field. Second, the genesis of geological structure was analyzed by means of detailed structural interpretation. Third, explore and improve the research methods of structural geological genesis. Fourth, the geological genesis analysis of reservoir is carried out based on comprehensive dynamic and static data. Fifth, structural geological genesis is studied by close combination with sedimentary facies research and diagenesis research. Sixth, application of metallogenic analysis results should be strengthened to provide a basis for the development of oil and gas fields. Seventh, microfracture characterization and modeling. Eighth,microstructural geological genesis analysis. Methods of structural geological genesis analysis in oil and gas field development mainly include: basic geological research, field description of outcrop observation, core observation and description, microscopic thin-section observation, physical simulation, well logging, seismic interpretation, geochemical analysis and testing, geological modeling, dynamic monitoring and dynamic analysis of production. The advantages and disadvantages of each method are analyzed based on case studies.On this basis, it is concluded that there are eight main issues and eight future research directions in the study of the genesis of structural geology in the oil and gas field development.
The genesis analysis of structural geology plays an important role in the oil and gas field development. Based on the research advances in China and abroad, the advantages and disadvantages of the study in this field are compared in detail. There are eight research directions in general. First, the structural geological genesis of fault system is determined through the analysis of structural evolution history and stress field. Second, the genesis of geological structure was analyzed by means of detailed structural interpretation. Third, explore and improve the research methods of structural geological genesis. Fourth, the geological genesis analysis of reservoir is carried out based on comprehensive dynamic and static data. Fifth, structural geological genesis is studied by close combination with sedimentary facies research and diagenesis research. Sixth, application of metallogenic analysis results should be strengthened to provide a basis for the development of oil and gas fields. Seventh, microfracture characterization and modeling. Eighth,microstructural geological genesis analysis. Methods of structural geological genesis analysis in oil and gas field development mainly include: basic geological research, field description of outcrop observation, core observation and description, microscopic thin-section observation, physical simulation, well logging, seismic interpretation, geochemical analysis and testing, geological modeling, dynamic monitoring and dynamic analysis of production. The advantages and disadvantages of each method are analyzed based on case studies.On this basis, it is concluded that there are eight main issues and eight future research directions in the study of the genesis of structural geology in the oil and gas field development.
引文
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胡秋媛,董大伟,赵利,等.2016.准噶尔盆地车排子凸起构造演化特征及其成因[J].石油与天然气地质,37(4):556-564.
李伟,任健,刘一鸣,李春锐.2015.辽东湾坳陷东部新生代构造发育与成因机制[J].地质科技情报,34(6):58-63.
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王珂,张荣虎,戴俊生,等.2017.塔里木盆地克深2气田储层构造裂缝成因与演化[J].中南大学学报(自然科学版),48(5):1242-1251.
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张继标,云金表,张仲培,等.2014.塔里木盆地玉北地区奥陶系储层构造裂缝成因模式[J].地质力学学报,20(4):413-423.
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张卫海,王韬,何畅,等.2015.金湖凹陷铜城断层构造特征与成因分析[J].中国石油大学学报(自然科学版),39(5):18-26.
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Alexander K,Augusto S A,Francisco H R B,et al.2016.Hypogenic origin,geologic controls and functional organization of a giant cave system in Precambrian carbonates,Brazil[J].Geomorphology,253:385-405.
Arthur P C L,Juliette L,Arnaud G,et al.2013.Tectonic versus diagenetic origin of fractures in a naturally fractured carbonate reservoir analog(Nerthe anticline,southeastern France)[J].AAPG Bulletin,97(12):2207-2232.
Botros N S.2015.The role of the granite emplacement and structural setting on the genesis of gold mineralization in Egypt[J].Ore Geology Reviews,70:173-187.
Casas-Sainz A M and Vicente G de.2009.On the tectonic origin of Iberian topography[J].Tectonophysics,474:214-235.
Emily H G C,Natalie H R,Jaime D B,et al.2018.Tectonic origin of serpentinites on Syros,Greece:Geochemical signatures of abyssal origin preserved in a HP/LT subduction complex[J].Lithos,296-299:352-364.
Franc esc S,Bemadi G,Antonio R,et al.2011.Geological structure and evolution of Majorca:Implications for the origin of the Western Medilerranean[J].Tectonophysics,510:217-238.
Francesco D P,Andrea F and Andrea I.2007.Interaction of tectonic,sedimentary,and diapiric processes in the origin of chaotic sediments:An example from the Messinian of Torino Hill(Tertiary Piedmont Basin,northwestern Italy)[J].GSA Bulletin,119(9/10):1107-1119.
Gavin R T W and Hugh C J.2004.The age,origin and tectonic significance of Mesozoic sediment-filled fissures in the Mendip Hills(SW England):implications for extension models and Jurassic sea-level curves[J].Geol.Mag.,141(4):471-504.
Giulio M,Kostitsyn Y,Preinfalk C,et al.2010.The genesis of the amethyst geodes at Artigas(Uruguay)and the paleohydrology of the Guarani aquifer:structural, geochemical,oxygen,carbon,strontium isotope and fluid inclusion study[J].International Journal of Earth Sciences,99:927-947.
Gregory D and Lyal B H.2013.Tectonic models for the origin of regional transverse structures in the Grenville Province of SW Quebec interpreted from regional gravity[J].Journal of Geodynamics,64:15-39.
Hassan I,Andre M,Andre C,et al.2014.Tectonic-karstic origin of the alleged"impact crater"of Lake Isli(Imilchil district,High Atlas,Morocco)[J].C.R.Geoscience,346:82-89.
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Iain N,Jennifer A G,Alan R H,et al.2010.Origin of the volcanic complexes of LaDesirade,Lesser Antilles:Implications for tectonic reconstructionof the Late Jurassic to Cretaceous Pacific-proto Caribbean margin[J].Lithos,120:407-420.
Jack E D and Phyllis A C.2006.Sedimentologic and tectonic origin of an incised-valley-fill sequence along an extensional marginal-lacustrine system in the Basin and Range province,United States:Implications for predictive models of the location of incised valleys[J].AAPG B ulletin,90(2):209-235.
Jacques C, Liangshu S,Michel F,et al.2010.Structural development of the Lower Paleozoic belt of South China:Genesisof an intracontinental orogen[J].Journal of Asian Earth Sciences,39:309-330.
J ames N P,Bone Y,Carter R M,et al.2006.Origin of the Late Neogene Roe Plains and their calcarenite veneer:implications for sedimentology and tectonics in the Great Australian Bight[J].Australian Journal of Earth Sciences,53:407-419.
Juan J and Luis M N.2008.Geochemical and mineralogical evidence of tectonic and sedimentary factors controlling the origin of ferromanganese crusts associated to stratigraphic discontinuities(Betic Cordilleras,SE of Spain)[J].Chemie der Erde,68:323-336.
Li Q,Simo J A,McGowran B,et al.2004.The eustatic and tectonic origin of Neogene unconformities from the Great Australian Bight[J].Marine Geology,203:57-81.
Maarten P C,Harry D and Jan D V W.2009.Classification of rifted sedimentary basins of the Pannonian Basin System according to the structural genesis,evolutionary history and hydrocarbon maturation zones[J].Marine and Petroleum Geology,26:1452-1464.
Margot M.2007.Nature,origin and tectonic significance of anomalous transverse structures,southeastern Skeena Fold Belt,British Columbia[J].Bulletin of Candian petroleum geology,55(4):262-274.
Martin-Izard A,Gumiel P,Arias M,et al.2009.Genesis and evolution of the structurally controlled vein mineralization(Sb-Hg)in the Escarlati deposit(Leon,Spain):Evidence from fault population analysis methods,fluid-inclusion research and stable isotope data[J].Journal of Geochemical Exploration,100:51-66.
Mualla C C and i N O.2010.The origin of Neogene tectonic rotations in the Galatean volcanic massif,central Anatolia[J].International Journal of Earth Sciences,99:413-426.Richard I C,Mike P S and Rolf B P.2001.Tectonic setting,origin,and
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葛君,张泽坤,倪金龙,等.2015.牟平-即墨断裂带南端断裂构造特征及动力学成因[J].现代地质,29(4):747-753.
韩大匡.2010.关于高含水油田二次开发理念、对策和技术路线的探讨[J].石油勘探与开发,37(5):583-591.
胡秋媛,董大伟,赵利,等.2016.准噶尔盆地车排子凸起构造演化特征及其成因[J].石油与天然气地质,37(4):556-564.
李伟,任健,刘一鸣,李春锐.2015.辽东湾坳陷东部新生代构造发育与成因机制[J].地质科技情报,34(6):58-63.
李新红,王萍,胡景双,等.2009.高集油田微构造特征及成因类型分析[J].复杂油气藏,2(2):16-19.
李相博,姚泾利,刘化清,等.2013.鄂尔多斯盆地中生界低幅度隆起构造成因类型及其对油气分布的控制作用[J].现代地质,27(4):755-764,773.
李阳.2001.复杂断块油藏构造表征[M].北京:石油工业出版社.
刘寅,陈清华,胡凯,等.2014.渤海湾盆地与苏北-南黄海盆地构造特征和成因对比[J].大地构造与成矿学,38(1):38-51.
刘泽容,信荃麟,邓俊国,等.1998.断块群油气藏形成机制和构造模式[M].北京:石油工业出版社.
王建民,张三.2018.鄂尔多斯盆地伊陕斜坡上的低幅度构造特征及成因探讨[J].地学前缘,25(2):246-253.
王珂,张荣虎,戴俊生,等.2017.塔里木盆地克深2气田储层构造裂缝成因与演化[J].中南大学学报(自然科学版),48(5):1242-1251.
吴林,陈清华.2015.苏北盆地高邮凹陷基底断裂构造特征及成因演化[J].天然气地球科学,26(4):689-699.
谢建华.2006.南海新生代构造演化及其成因数值模拟[D].广州:中国科学院广州地球化学研究所.
徐睿,奥立德.2016.北加蓬次盆白垩系盐构造发育特征及成因分析[J].中国石油勘探,21(5):70-74.
薛雁,林会喜,张奎华,等.2017.哈拉阿拉特山地区构造特征及成因机制模拟[J].大地构造与成矿学,41(5):843-852.
杨传胜,杨长清,张剑,等.2017.东海陆架盆地中生界构造样式及其动力学成因探讨[J].海洋通报,36(4):431-439.
袁士义,宋新民,冉启全.2004.裂缝性油藏开发技术[M].北京:石油工业出版社.
曾联波,柯式镇,刘洋.2010.低渗透油气储层裂缝研究方法[M].北京:石油工业出版社.
张继标,云金表,张仲培,等.2014.塔里木盆地玉北地区奥陶系储层构造裂缝成因模式[J].地质力学学报,20(4):413-423.
张金亮,谢俊.2011.油田开发地质学[M].北京:石油工业出版社.
张勤,翟伟,彭建兵,等.2012.渭河盆地地裂缝群发机理及东、西部地裂缝分布不均衡构造成因研究[J].地球物理学报,55(8):2589-2597.
张卫海,王韬,何畅,等.2015.金湖凹陷铜城断层构造特征与成因分析[J].中国石油大学学报(自然科学版),39(5):18-26.
张学汝,陈和平、张吉昌,等.1999.变质岩储集层构造裂缝研究技术[M].北京:石油工业出版社.
Alexander K,Augusto S A,Francisco H R B,et al.2016.Hypogenic origin,geologic controls and functional organization of a giant cave system in Precambrian carbonates,Brazil[J].Geomorphology,253:385-405.
Arthur P C L,Juliette L,Arnaud G,et al.2013.Tectonic versus diagenetic origin of fractures in a naturally fractured carbonate reservoir analog(Nerthe anticline,southeastern France)[J].AAPG Bulletin,97(12):2207-2232.
Botros N S.2015.The role of the granite emplacement and structural setting on the genesis of gold mineralization in Egypt[J].Ore Geology Reviews,70:173-187.
Casas-Sainz A M and Vicente G de.2009.On the tectonic origin of Iberian topography[J].Tectonophysics,474:214-235.
Emily H G C,Natalie H R,Jaime D B,et al.2018.Tectonic origin of serpentinites on Syros,Greece:Geochemical signatures of abyssal origin preserved in a HP/LT subduction complex[J].Lithos,296-299:352-364.
Franc esc S,Bemadi G,Antonio R,et al.2011.Geological structure and evolution of Majorca:Implications for the origin of the Western Medilerranean[J].Tectonophysics,510:217-238.
Francesco D P,Andrea F and Andrea I.2007.Interaction of tectonic,sedimentary,and diapiric processes in the origin of chaotic sediments:An example from the Messinian of Torino Hill(Tertiary Piedmont Basin,northwestern Italy)[J].GSA Bulletin,119(9/10):1107-1119.
Gavin R T W and Hugh C J.2004.The age,origin and tectonic significance of Mesozoic sediment-filled fissures in the Mendip Hills(SW England):implications for extension models and Jurassic sea-level curves[J].Geol.Mag.,141(4):471-504.
Giulio M,Kostitsyn Y,Preinfalk C,et al.2010.The genesis of the amethyst geodes at Artigas(Uruguay)and the paleohydrology of the Guarani aquifer:structural, geochemical,oxygen,carbon,strontium isotope and fluid inclusion study[J].International Journal of Earth Sciences,99:927-947.
Gregory D and Lyal B H.2013.Tectonic models for the origin of regional transverse structures in the Grenville Province of SW Quebec interpreted from regional gravity[J].Journal of Geodynamics,64:15-39.
Hassan I,Andre M,Andre C,et al.2014.Tectonic-karstic origin of the alleged"impact crater"of Lake Isli(Imilchil district,High Atlas,Morocco)[J].C.R.Geoscience,346:82-89.
Hofmann A,Dirks P H G M,Jelsma H A,et al.2003.A tectonic origin for ironstone horizons in the Zimbabwe craton and their significance for greenstone belt geology[J].Journal of the geological society,London,160:83-97.
Iain N,Jennifer A G,Alan R H,et al.2010.Origin of the volcanic complexes of LaDesirade,Lesser Antilles:Implications for tectonic reconstructionof the Late Jurassic to Cretaceous Pacific-proto Caribbean margin[J].Lithos,120:407-420.
Jack E D and Phyllis A C.2006.Sedimentologic and tectonic origin of an incised-valley-fill sequence along an extensional marginal-lacustrine system in the Basin and Range province,United States:Implications for predictive models of the location of incised valleys[J].AAPG B ulletin,90(2):209-235.
Jacques C, Liangshu S,Michel F,et al.2010.Structural development of the Lower Paleozoic belt of South China:Genesisof an intracontinental orogen[J].Journal of Asian Earth Sciences,39:309-330.
J ames N P,Bone Y,Carter R M,et al.2006.Origin of the Late Neogene Roe Plains and their calcarenite veneer:implications for sedimentology and tectonics in the Great Australian Bight[J].Australian Journal of Earth Sciences,53:407-419.
Juan J and Luis M N.2008.Geochemical and mineralogical evidence of tectonic and sedimentary factors controlling the origin of ferromanganese crusts associated to stratigraphic discontinuities(Betic Cordilleras,SE of Spain)[J].Chemie der Erde,68:323-336.
Li Q,Simo J A,McGowran B,et al.2004.The eustatic and tectonic origin of Neogene unconformities from the Great Australian Bight[J].Marine Geology,203:57-81.
Maarten P C,Harry D and Jan D V W.2009.Classification of rifted sedimentary basins of the Pannonian Basin System according to the structural genesis,evolutionary history and hydrocarbon maturation zones[J].Marine and Petroleum Geology,26:1452-1464.
Margot M.2007.Nature,origin and tectonic significance of anomalous transverse structures,southeastern Skeena Fold Belt,British Columbia[J].Bulletin of Candian petroleum geology,55(4):262-274.
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