北部湾盆地福山凹陷古近系流沙港组层序地层样式及其研究意义
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摘要
为探究北部湾盆地福山凹陷古近系流沙港组层序地层样式,运用钻井、测井、地震等资料,建立了流沙港组等时层序地层格架,在此基础上,综合考虑构造活动、盆缘背景、物源供给等影响因素,并结合福山凹陷在不同构造部位、不同层段以及层序发育的时空差异性特点,将流沙港组层序构成样式总结为4种:断控陡坡型、多级断阶带型、挠曲坡折带型和斜坡型.通过对以上层序样式特征及其内部沉积特点的研究,总结了在不同层序构成样式控制下发育的油气藏圈闭类型,为福山凹陷油气藏勘探提供了重要的指导意义.
To explore the sequence stratigraphic architecture of Paleogene Liushagang Formation(Els)in the Fushan sag of Beibuwan basin,by using drilling,logging,seismic data,the isochronous sequence stratigraphic framework in systems tracts level has been established.Aiming at different tectonic units in Elsof Fushan sag,with comprehensive consideration of tectonic activities,basin marginal background,provenance supply,etc.,sequence strata architecture of Els can be extracted into four types,namely,fault controlling steep type,multi-stage fault terrace type,flexure break type,and gentle slope break type. The features of sequence architecture,different types of traps developed in different sequence architecture.It is of great significance to the hydrocarbon exploration in Els,Fushan sag.
To explore the sequence stratigraphic architecture of Paleogene Liushagang Formation(Els)in the Fushan sag of Beibuwan basin,by using drilling,logging,seismic data,the isochronous sequence stratigraphic framework in systems tracts level has been established.Aiming at different tectonic units in Elsof Fushan sag,with comprehensive consideration of tectonic activities,basin marginal background,provenance supply,etc.,sequence strata architecture of Els can be extracted into four types,namely,fault controlling steep type,multi-stage fault terrace type,flexure break type,and gentle slope break type. The features of sequence architecture,different types of traps developed in different sequence architecture.It is of great significance to the hydrocarbon exploration in Els,Fushan sag.
引文
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Fan,T.L.,Li,W.D.,1999.A successful case on sequencestratigraphy applied to the prediction of non-marine oilreservoir.Acta Petrolei Sinica,20(2):12-17(in Chi-nese with English abstract).
Frimmel,H.E.,Filling,P.G.,Eriksson,P.G.,2002.Neo-proterozoic tectonic and climatic evolution recorded inthe Cariep belt,Namibia and South Africa.Basin Re-search,14(1):55-67.doi:10.1046/j.1365-2117.2002.00166.x
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Huang,C.Y.,Wang,H.,Zhou,L.H.,et al.,2010.Sequencepattern controlled by structural evolution of Jiannanburied-hill in Huanghua depression.Journal of CentralSouth University(Science and Technology),41(2):692-699(in Chinese with English abstract).
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Lin,C.S.,Zheng,H.R.,Ren,J.Y.,et al.,2004.The controlof syndepositional faulting on the Eogene sedimentarybasin fills of Dongying and Zhanhua sags,Bohai bay ba-sin.Science in China(Ser.D),47(9):769-782.doi:10.1360/03yd.0203
Liu,L.J.,Kuang,H.W.,Tong,Y.M.,et al.,2003.Sedi-mentary systems and evolution characteristics of LowerTertiary Liushagang Formation in Fushan sag.Oil andGas Geology,24(2):140-145(in Chinese with Eng-lish abstract).
Luo,J.X.,He,Y.B.,Gao,Z.Z.,et al.,2007.Gravity flowdeposits of Paleogene Liushagang Formation in Fushansag,Hainan Province.Offshore Oil,27(3):13-21(inChinese with English abstract).
Luo,Q.,Pang,X.Q.,2008.Reservoir controlling mechanismand petroleum accumulation model for consequent faultand antithetic fault in Fushan depression of Hainanarea.Acta Petrolei Sinica,29(3):363-367(in Chi-nese with English abstract).
Posamentier,H.W.,Vail,P.R.,1988.Eustatic controls onclastic depositionⅡ:sequence and systems tract mod-els.In:Wilgus,C.K.,Hastings,B.S.,Van Wagoner,J.,et al.,eds.,Sea level changes:an integrated ap-proach.SEPM Special Publication,42:125-154.doi:10.2110/pec.88.01.0125
Posamentier,H.W.,Weimer,P.,1993.Siliciclastic sequencestratigraphy and petroleum geology:where to fromhere?AAPG Bulletin,77(5):731-742.doi:10.1306/BDFF8D3A-1718-11D7-8645000102C1865D
Qiu,Z.J.,Gong,Z.S.,1999.Hydrocarbon exploration inChina,vol.4,near shore hydrocarbon area.GeologyPress,Petroleum Industry Press,Beijing(in Chinese).
Ren,J.Y.,Lu,Y.C.,Zhang,Q.L.,2004.Forming mecha-nism of structural slope-break and its control on se-quence style in faulted basin.Earth Science—Journalof China University of Geosciences,29(5):596-602(in Chinese with English abstract).
Shi,Y.M.,Liu,J.,Zhang,M.Z.,et al.,2007.Experience andunderstand in oil and gas exploration in Fushan sag,HainanProvince.South China Journal of Seismology,27(3):57-68(in Chinese with English abstract).
Smith,G.J.,Jacobi,R.D.,2001.Tectonic and eustatic sig-nals in the sequence stratigraphy of the Upper DevonianCanadaway Group,New York State.AAPG Bulletin,85(2):325-357.doi:10.1306/8626C7D5-173B-11D7-8645000102C1865D
Yan,D.T.,Wang,H.,Wang,J.H.,et al.,2006.Analysis ofthe Cretaceous sequence-stratigraphic pattern and con-trolling factors in Kuna foreland basin.Acta Sedimento logica Sinica,24(6):841-848(in Chinese with Eng-lish abstract).
Zhang,C.,Wei,K.S.,2005.Sequence characteristics andreservoir formation condition in the southern Wuerxundepression.Acta Petrolei Sinica,26(2):47-52(inChinese with English abstract).
丁卫星,王文军,马英俊,2003.北部湾盆地福山凹陷流沙港组含油气系统特征.海洋石油,23(2):1-6.
樊太亮,李卫东,1999.层序地层应用于陆相油藏预测的成功实例.石油学报,20(2):12-17.
郭巍,刘招君,董清水,等,2002.断陷湖盆层序地层格架中的油气聚集规律——以松辽盆地为例.吉林大学学报(地球科学版),32(3):233-237.
黄传炎,王华,周立宏,等,2010.黄骅坳陷涧南潜山构造演化对层序样式的控制.中南大学学报(自然科学版),41(2):692-699.
李思田,林畅松,解习农,等,1995.大型陆相盆地层序地层学研究——以鄂尔多斯中生代盆地为例.地学前缘,2(3-4):133-136.
林畅松,潘元林,肖建新,等,2000.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学——中国地质大学学报,25(3):260-265.
刘丽君,旷红伟,佟彦明,等,2003.福山凹陷下第三系流沙港组沉积体系及演化特征.石油与天然气地质,24(2):140-145.
罗进雄,何幼斌,高振中,等,2007.海南福山凹陷古近系流沙港组重力流沉积研究.海洋石油,27(3):13-21.
罗群,庞雄奇,2008.海南福山凹陷顺向和反向断裂控藏机理及油气聚集模式.石油学报,29(3):363-367.
邱中建,龚再升,1999.中国油气勘探,第四卷,近海油气区.北京:地质出版社、石油工业出版社.
任建业,陆永潮,张青林,2004.断陷盆地构造坡折带形成机制及其对层序发育样式的控制.地球科学——中国地质大学学报,29(5):596-602.
石彦民,刘菊,张梅珠,等,2007.海南福山凹陷油气勘探实践与认识.华南地震,27(3):57-68.
严德天,王华,王家豪,等,2006.库车前陆盆地白垩系层序地层样式及控制因素分析.沉积学报,24(6):841-848.
张成,魏魁生,2005.乌尔逊凹陷南部层序地层特征及成藏条件.石油学报,26(2):47-52.
Ding,W.X.,Wang,W.J.,Ma,Y.J.,2003.Characteristics ofLiushagang Formation petroleum system in Fushan de-pression of Beibuwan basin.Offshore Oil,23(2):1-6(in Chinese with English abstract).
Fan,T.L.,Li,W.D.,1999.A successful case on sequencestratigraphy applied to the prediction of non-marine oilreservoir.Acta Petrolei Sinica,20(2):12-17(in Chi-nese with English abstract).
Frimmel,H.E.,Filling,P.G.,Eriksson,P.G.,2002.Neo-proterozoic tectonic and climatic evolution recorded inthe Cariep belt,Namibia and South Africa.Basin Re-search,14(1):55-67.doi:10.1046/j.1365-2117.2002.00166.x
Guo,W.,Liu,Z.J.,Dong,Q.S.,et al.,2002.Oil and gasgathering rule in the sequence stratigraphic frame offault depression Lacustrine basin:an example fromSongtao basin.Journal of Jilin University(Earth Sci-ence Edition),32(3):233-237(in Chinese with Eng-lish abstract).
Huang,C.Y.,Wang,H.,Zhou,L.H.,et al.,2010.Sequencepattern controlled by structural evolution of Jiannanburied-hill in Huanghua depression.Journal of CentralSouth University(Science and Technology),41(2):692-699(in Chinese with English abstract).
Li,S.T.,Lin,C.S.,Xie,X.N.,et al.,1995.Approaches ofnon-marine sequence stratigraphy:a case study on theMesozoic Ordos basin.Earth Science Frontiers,2(3-4):133-136(in Chinese with English abstract).
Lin,C.S.,Eriksson,K.,Li,S.T.,et al.,2001.Sequence ar-chitecture,depositional systems,and controls on devel-opment of Lacustrine basin fills in part of the Erlian ba-sin,northeast China.AAPG Bulletin,85(11):2017-2043.doi:10.1306/8626D0DB-173B-11D7-8645000102C1865D
Lin,C.S.,Pan,Y.L.,Xiao,J.X.,et al.,2000.Structuralslope-break zone:key concept for stratigraphic se-quence analysis and petroleum forecasting in fault sub-sidence basins.Earth Science—Journal of China Uni-versity of Geosciences,25(3):260-265(in Chinesewith English abstract).
Lin,C.S.,Zheng,H.R.,Ren,J.Y.,et al.,2004.The controlof syndepositional faulting on the Eogene sedimentarybasin fills of Dongying and Zhanhua sags,Bohai bay ba-sin.Science in China(Ser.D),47(9):769-782.doi:10.1360/03yd.0203
Liu,L.J.,Kuang,H.W.,Tong,Y.M.,et al.,2003.Sedi-mentary systems and evolution characteristics of LowerTertiary Liushagang Formation in Fushan sag.Oil andGas Geology,24(2):140-145(in Chinese with Eng-lish abstract).
Luo,J.X.,He,Y.B.,Gao,Z.Z.,et al.,2007.Gravity flowdeposits of Paleogene Liushagang Formation in Fushansag,Hainan Province.Offshore Oil,27(3):13-21(inChinese with English abstract).
Luo,Q.,Pang,X.Q.,2008.Reservoir controlling mechanismand petroleum accumulation model for consequent faultand antithetic fault in Fushan depression of Hainanarea.Acta Petrolei Sinica,29(3):363-367(in Chi-nese with English abstract).
Posamentier,H.W.,Vail,P.R.,1988.Eustatic controls onclastic depositionⅡ:sequence and systems tract mod-els.In:Wilgus,C.K.,Hastings,B.S.,Van Wagoner,J.,et al.,eds.,Sea level changes:an integrated ap-proach.SEPM Special Publication,42:125-154.doi:10.2110/pec.88.01.0125
Posamentier,H.W.,Weimer,P.,1993.Siliciclastic sequencestratigraphy and petroleum geology:where to fromhere?AAPG Bulletin,77(5):731-742.doi:10.1306/BDFF8D3A-1718-11D7-8645000102C1865D
Qiu,Z.J.,Gong,Z.S.,1999.Hydrocarbon exploration inChina,vol.4,near shore hydrocarbon area.GeologyPress,Petroleum Industry Press,Beijing(in Chinese).
Ren,J.Y.,Lu,Y.C.,Zhang,Q.L.,2004.Forming mecha-nism of structural slope-break and its control on se-quence style in faulted basin.Earth Science—Journalof China University of Geosciences,29(5):596-602(in Chinese with English abstract).
Shi,Y.M.,Liu,J.,Zhang,M.Z.,et al.,2007.Experience andunderstand in oil and gas exploration in Fushan sag,HainanProvince.South China Journal of Seismology,27(3):57-68(in Chinese with English abstract).
Smith,G.J.,Jacobi,R.D.,2001.Tectonic and eustatic sig-nals in the sequence stratigraphy of the Upper DevonianCanadaway Group,New York State.AAPG Bulletin,85(2):325-357.doi:10.1306/8626C7D5-173B-11D7-8645000102C1865D
Yan,D.T.,Wang,H.,Wang,J.H.,et al.,2006.Analysis ofthe Cretaceous sequence-stratigraphic pattern and con-trolling factors in Kuna foreland basin.Acta Sedimento logica Sinica,24(6):841-848(in Chinese with Eng-lish abstract).
Zhang,C.,Wei,K.S.,2005.Sequence characteristics andreservoir formation condition in the southern Wuerxundepression.Acta Petrolei Sinica,26(2):47-52(inChinese with English abstract).
丁卫星,王文军,马英俊,2003.北部湾盆地福山凹陷流沙港组含油气系统特征.海洋石油,23(2):1-6.
樊太亮,李卫东,1999.层序地层应用于陆相油藏预测的成功实例.石油学报,20(2):12-17.
郭巍,刘招君,董清水,等,2002.断陷湖盆层序地层格架中的油气聚集规律——以松辽盆地为例.吉林大学学报(地球科学版),32(3):233-237.
黄传炎,王华,周立宏,等,2010.黄骅坳陷涧南潜山构造演化对层序样式的控制.中南大学学报(自然科学版),41(2):692-699.
李思田,林畅松,解习农,等,1995.大型陆相盆地层序地层学研究——以鄂尔多斯中生代盆地为例.地学前缘,2(3-4):133-136.
林畅松,潘元林,肖建新,等,2000.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学——中国地质大学学报,25(3):260-265.
刘丽君,旷红伟,佟彦明,等,2003.福山凹陷下第三系流沙港组沉积体系及演化特征.石油与天然气地质,24(2):140-145.
罗进雄,何幼斌,高振中,等,2007.海南福山凹陷古近系流沙港组重力流沉积研究.海洋石油,27(3):13-21.
罗群,庞雄奇,2008.海南福山凹陷顺向和反向断裂控藏机理及油气聚集模式.石油学报,29(3):363-367.
邱中建,龚再升,1999.中国油气勘探,第四卷,近海油气区.北京:地质出版社、石油工业出版社.
任建业,陆永潮,张青林,2004.断陷盆地构造坡折带形成机制及其对层序发育样式的控制.地球科学——中国地质大学学报,29(5):596-602.
石彦民,刘菊,张梅珠,等,2007.海南福山凹陷油气勘探实践与认识.华南地震,27(3):57-68.
严德天,王华,王家豪,等,2006.库车前陆盆地白垩系层序地层样式及控制因素分析.沉积学报,24(6):841-848.
张成,魏魁生,2005.乌尔逊凹陷南部层序地层特征及成藏条件.石油学报,26(2):47-52.
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