歧口凹陷古近纪东营期古物源体系重建与应用
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摘要
以沉积盆地分析、层序地层研究和油气勘探实践中急待解决的古物源体系分析为切入点,以歧口凹陷东营组研究为例,阐述了古物源体系研究的途径、方法与技术路线;初步总结出应用轻-重矿物时空配置关系、地震前积反射结构特征、古地貌恢复与沟谷展布特征、盆地内部骨架砂体形态与时空配置以及盆地边缘及内部层序界面上大型下切谷的空间展布特征,即"五位合一"法来判断沉积盆地的古物源体系.该分析方法可为同领域的研究提供借鉴作用.
The paleoprovenance system analysis is critical in terms of present sedimentary basin analysis,sequence stratigraphy study,and petroleum exploration practice.In this paper,we present a preliminarily summary of applying the "five-in-one" method to study provenace system of the Dongying Formation in the Qikou depression.The so-called "five-in-one" method is a compositive analysis of light-heavy minerals,seismic progradational reflection structure features,paleogeomorphy and gully expansion features,skeleton sand body forms within the basin and the time-space expansion and matching rules analysis,and basin margin and the spatial expansion features analysis of large-scale incised valley developed in its internal sequence boundary.This method undoubtedly provides a reference for the researches of other basins within the same field.However,we know that provenace analysis of sedimentary basin is a complicated job.With the development of science and technology,and the increase of basin data obtained,it will apply on the field together with more effective methods and technologies.It will also further approach the real status of provenace system,and provide better service for petroleum exploration.
The paleoprovenance system analysis is critical in terms of present sedimentary basin analysis,sequence stratigraphy study,and petroleum exploration practice.In this paper,we present a preliminarily summary of applying the "five-in-one" method to study provenace system of the Dongying Formation in the Qikou depression.The so-called "five-in-one" method is a compositive analysis of light-heavy minerals,seismic progradational reflection structure features,paleogeomorphy and gully expansion features,skeleton sand body forms within the basin and the time-space expansion and matching rules analysis,and basin margin and the spatial expansion features analysis of large-scale incised valley developed in its internal sequence boundary.This method undoubtedly provides a reference for the researches of other basins within the same field.However,we know that provenace analysis of sedimentary basin is a complicated job.With the development of science and technology,and the increase of basin data obtained,it will apply on the field together with more effective methods and technologies.It will also further approach the real status of provenace system,and provide better service for petroleum exploration.
引文
Bai,Y.F.,Wang,Z.S.,Wei,A.J.,et al.,2008.Ti me andspace distribution characteristics and material resourcesystem of heavy minerals in Dongying Formation ofHuanghua depression.Petroleum Geology&OilfieldDevelopment in Daqing,27(2):39-42(in Chinesewith English abstract).
Bai,Y.F.,Zhang,B.,Wang,H.,et al.,2006.Research onthe source direction of Palaeogene Dongying Formationin Huanghua depression.Journal of Oil and Gas Tech-nology,28(3):17-19(in Chinese with Englishabstract).
Bonjour,J.L.,Dabard,M.P.,1990.Ti/Nb ratios of clasticterrigenous sedi ments used as an indicator of prove-nance.Chemical Geology,91(3):257-267.
Chen,C.F.,Zheng,J.M.,Wang,D.F.,2001.Depositionalsystems and source provenance of the third member ofShahejie Formation in Banqiao sag.Journal of Palaeo-geography,3(1):55-62(in Chinese with Englishabstract).
Deng,H.W.,Wang,H.L.,Wang,D.Z.,2001.Control ofpaleo-morphology to stratigraphic sequence in continen-tal rift basins:Take Lower Tertiary of western slope inBozhong depression as an example.Oil and Gas Geolo-gy,22(4):293-296,303(in Chinese with Englishabstract).
Dickinson,W.R.,1985.Interpreting provenance relationsfromdetrital modes of sandstones.In:Zuffa,G.G.,ed.,Provenance of arenites.NATO-ASI Series.D.Reidel.,Dordrecht,148:333-361.
Haughton,P.D.W.,Morton,A.C.,Todd,S.P.,1991.De-velopments in sedi mentary provenance studies.The Ge-ological Society of London,London.
He,Z.H.,Liu,Z.J.,Zhang,F.,2001.Latest progress ofheavy mineral researchin the basin analysis.GeologicalScience and Technology Information,20(4):29-32(in Chinese with English abstract).
Jiao,Y.Q.,Li,Z.,Zhou,H.M.,1998.The integrated studyof sedi ment sources in sedi mentary basins:An examplefromthe Eocene Nanpu rift subbasin.Sedi mentary Fa-cies and Palaeogeography,18(5):16-20(in Chinesewith English abstract).
Johnson,C.M.,Winter,B.L.,1999.Provenance analysis ofLower Paleozoic cratonic quartz arenites of the NorthAmerican midcontinent region:U-Pb and Sm-Ndisotopegeochemistry.Geological Society of American Bulle-tin,111(11):1723-1738.
Li,Z.,Jiao,Y.Q.,Liu,C.H.,et al.,1998.Source analysis ofheavy mineral in Gaoliu area,Huanghua depression.Pe-troleumExploration and Development,25(6):5-7(inChinese with English abstract).
Lin,C.S.,2006.Tectono-stratigraphic analysis of sedi menta-ry basins:Acase study on the inland tectonically activebasins in China.Geoscience,20(2):185-194(in Chi-nese with English abstract).
Liu,L.,Hu,C.Y.,1991.Provenance significance of the maindetrital composition in sandstone.Sedi mentary Faciesand Palaeogeography,11(6):48-53(in Chinese withEnglish abstract).
McLennan,S.M.,Hemming,S.,McDaniel,D.K.,et al.,1993.Geochemical approaches to sedi mentation,prove-nance,and tectonics.Special Paper-Geological Societyof America,284:21-40.
Morton,A.,Hurst,A.,1995.Correlation of sandstonesusing heavy minerals:An example from the StatfjordFormation of the Snorre Field,northern North Sea.In:Dunay,R.E.,Hail wood,E.A.,eds.,Non-biostrati-graphical methods of dating and correlation.GeologicalSociety Special Publication,89:3-22.
Ravnas,R.,Steel,R.J.,1998.Architecture of marine rift-ba-sin successions.AAPG Bulletin,82:110-146.
Sambridge,M.S.,Compston,W.,1994.Mixture modeling ofmulti-component data sets with application to ion-probezircon ages.Earthand Planetary Science Letters,128(3-4):373-390.
Sherlock,S.C.,Jones,K.A.,Jones,J.A.,2000.A CentralEuropean variscide source for Upper Carboniferous sed-i ments in SW England:40Ar/39Ar detrital white micaages fromthe Forest of Dean basin.Journal ofthe Geo-logical Society,157(5):905-908.
Stevenson,R.K.,Whittaker,S.,Mountjoy,E.W.,2000.Ge-ochemical and Nd isotopic evidence for sedi mentary-source changes in the Devonian miogeocline of thesouthern Canadian Cordillera.Geological Society ofAmerican Bulletin,112:531-539.
Taylor,S.R.,McLennan,S.M.,1985.The continentalcrust:Its composition and evolution.Blackwell ScientificPublication,Oxford.
Wang,J.H.,Wang,H.,Zhao,Z.X.,et al.,2003.Sequencestratigraphy in paleogeomorphy analysis:An examplefrom Tahe oilfield.Earth Science—Journal of ChinaUniversity of Geosciences,28(4):425-430(in Chinesewith English abstract).
Wang,Z.J.,Chen,H.D.,Zhang,J.Q.,2000.The researchand prospect in provenance analysis.Sedi mentary Geol-ogy and Tethyan Geology,20(4):104-110(in Chinesewith English abstract).
Wang,Z.Y.,Qi,J.F.,Lu,K.Z.,2000.Analysis of Cenozoictectonic subsidence history of the east tectonic belts inHuanghua depression.Oil and Gas Geology,21(2):127-129,167(in Chinese with English abstract).
Yan,Y.,Lin,G.,Wang,Y.J.,et al.,2002.The indication ofcontinental detrital sedi ment to tectonic setting.Ad-vance in Earth Sciences,17(1):85-90(in Chinese withEnglish abstract).
Zhang,J.L.,Lin,C.S.,Zheng,H.R.,2002.Controlling ac-tion of fractures,palaeogeomorphology and materialsources of rift lake basin on sedi mentary system—Tak-ing Es3Gubei subsag as example.Petroleum Geologyand Recovery Efficiency,9(4):24-27(in Chinesewith English abstract).
Zhao,J.X.,Chen,H.D.,Shi,Z.Q.,2001.The way and i m-plications of rebuilding palaeogeomorphology,taking theresearch of palaeogeomorphology of the Ordos basin be-fore Jurassic deposition as example.Journal of Cheng-du University of Technology,28(3):260-266(in Chi-nese with English abstract).
白云风,王振升,韦阿娟,等,2008.黄骅坳陷东营组重矿物时空展布特征及物源体系分析.大庆石油地质与开发,27(2):39-42.
白云风,张兵,王华,等,2006.黄骅坳陷古近纪东营组物源方向研究.石油天然气学报,28(3):17-19.
陈纯芳,郑浚茂,王德发,2001.板桥凹陷沙三段沉积体系与物源分析.古地理学报,3(1):55-62.
邓宏文,王红亮,王敦则,2001.古地貌对陆相裂谷盆地层序充填特征的控制——以渤中凹陷西斜坡区下第三系为例.石油与天然气地质,22(4):293-296,303.
和钟铧,刘招君,张峰,2001.重矿物分析在盆地中的应用研究进展.地质科技情报,20(4):29-32.
焦养泉,李珍,周海民,1998.沉积盆地物质来源综合研究——以南堡老第三纪亚断陷盆地为例.岩相古地理,18(5):16-20.
李珍,焦养泉,刘春华,等,1998.黄骅坳陷高柳地区重矿物物源分析.石油勘探与开发,25(6):5-7.
林畅松,2006.沉积盆地的构造地层分析——以中国构造活动盆地研究为例.现代地质,20(2):185-194.
刘立,胡春燕,1991.砂岩中主要碎屑成分的物源区意义.岩相古地理,11(6):48-53.
王家豪,王华,赵忠新,等,2003.层序地层学应用于古地貌分析——以塔河油田为例.地球科学——中国地质大学学报,28(4):425-430.
汪正江,陈洪德,张锦泉,2000.物源分析的研究与展望.沉积与特提斯地质,20(4):104-110.
王子煜,漆家福,陆克政,2000.黄骅坳陷东部构造带新生代构造沉降史分析.石油与天然气地质,21(2):127-129,167.
闫义,林舸,王岳军,等,2002.盆地陆源碎屑沉积物对源区构造背景的指示意义.地球科学进展,17(1):85-90.
张建林,林畅松,郑和荣,2002.断裂湖盆断裂、古地貌及物源对沉积体系的控制作用——以孤北洼陷沙三段为例.油气地质与采收率,9(4):24-27.
赵俊兴,陈洪德,时志强,2001.古地貌恢复技术方法及其研究意义——以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例.成都理工学院学报,28(3):260-266.
Bai,Y.F.,Zhang,B.,Wang,H.,et al.,2006.Research onthe source direction of Palaeogene Dongying Formationin Huanghua depression.Journal of Oil and Gas Tech-nology,28(3):17-19(in Chinese with Englishabstract).
Bonjour,J.L.,Dabard,M.P.,1990.Ti/Nb ratios of clasticterrigenous sedi ments used as an indicator of prove-nance.Chemical Geology,91(3):257-267.
Chen,C.F.,Zheng,J.M.,Wang,D.F.,2001.Depositionalsystems and source provenance of the third member ofShahejie Formation in Banqiao sag.Journal of Palaeo-geography,3(1):55-62(in Chinese with Englishabstract).
Deng,H.W.,Wang,H.L.,Wang,D.Z.,2001.Control ofpaleo-morphology to stratigraphic sequence in continen-tal rift basins:Take Lower Tertiary of western slope inBozhong depression as an example.Oil and Gas Geolo-gy,22(4):293-296,303(in Chinese with Englishabstract).
Dickinson,W.R.,1985.Interpreting provenance relationsfromdetrital modes of sandstones.In:Zuffa,G.G.,ed.,Provenance of arenites.NATO-ASI Series.D.Reidel.,Dordrecht,148:333-361.
Haughton,P.D.W.,Morton,A.C.,Todd,S.P.,1991.De-velopments in sedi mentary provenance studies.The Ge-ological Society of London,London.
He,Z.H.,Liu,Z.J.,Zhang,F.,2001.Latest progress ofheavy mineral researchin the basin analysis.GeologicalScience and Technology Information,20(4):29-32(in Chinese with English abstract).
Jiao,Y.Q.,Li,Z.,Zhou,H.M.,1998.The integrated studyof sedi ment sources in sedi mentary basins:An examplefromthe Eocene Nanpu rift subbasin.Sedi mentary Fa-cies and Palaeogeography,18(5):16-20(in Chinesewith English abstract).
Johnson,C.M.,Winter,B.L.,1999.Provenance analysis ofLower Paleozoic cratonic quartz arenites of the NorthAmerican midcontinent region:U-Pb and Sm-Ndisotopegeochemistry.Geological Society of American Bulle-tin,111(11):1723-1738.
Li,Z.,Jiao,Y.Q.,Liu,C.H.,et al.,1998.Source analysis ofheavy mineral in Gaoliu area,Huanghua depression.Pe-troleumExploration and Development,25(6):5-7(inChinese with English abstract).
Lin,C.S.,2006.Tectono-stratigraphic analysis of sedi menta-ry basins:Acase study on the inland tectonically activebasins in China.Geoscience,20(2):185-194(in Chi-nese with English abstract).
Liu,L.,Hu,C.Y.,1991.Provenance significance of the maindetrital composition in sandstone.Sedi mentary Faciesand Palaeogeography,11(6):48-53(in Chinese withEnglish abstract).
McLennan,S.M.,Hemming,S.,McDaniel,D.K.,et al.,1993.Geochemical approaches to sedi mentation,prove-nance,and tectonics.Special Paper-Geological Societyof America,284:21-40.
Morton,A.,Hurst,A.,1995.Correlation of sandstonesusing heavy minerals:An example from the StatfjordFormation of the Snorre Field,northern North Sea.In:Dunay,R.E.,Hail wood,E.A.,eds.,Non-biostrati-graphical methods of dating and correlation.GeologicalSociety Special Publication,89:3-22.
Ravnas,R.,Steel,R.J.,1998.Architecture of marine rift-ba-sin successions.AAPG Bulletin,82:110-146.
Sambridge,M.S.,Compston,W.,1994.Mixture modeling ofmulti-component data sets with application to ion-probezircon ages.Earthand Planetary Science Letters,128(3-4):373-390.
Sherlock,S.C.,Jones,K.A.,Jones,J.A.,2000.A CentralEuropean variscide source for Upper Carboniferous sed-i ments in SW England:40Ar/39Ar detrital white micaages fromthe Forest of Dean basin.Journal ofthe Geo-logical Society,157(5):905-908.
Stevenson,R.K.,Whittaker,S.,Mountjoy,E.W.,2000.Ge-ochemical and Nd isotopic evidence for sedi mentary-source changes in the Devonian miogeocline of thesouthern Canadian Cordillera.Geological Society ofAmerican Bulletin,112:531-539.
Taylor,S.R.,McLennan,S.M.,1985.The continentalcrust:Its composition and evolution.Blackwell ScientificPublication,Oxford.
Wang,J.H.,Wang,H.,Zhao,Z.X.,et al.,2003.Sequencestratigraphy in paleogeomorphy analysis:An examplefrom Tahe oilfield.Earth Science—Journal of ChinaUniversity of Geosciences,28(4):425-430(in Chinesewith English abstract).
Wang,Z.J.,Chen,H.D.,Zhang,J.Q.,2000.The researchand prospect in provenance analysis.Sedi mentary Geol-ogy and Tethyan Geology,20(4):104-110(in Chinesewith English abstract).
Wang,Z.Y.,Qi,J.F.,Lu,K.Z.,2000.Analysis of Cenozoictectonic subsidence history of the east tectonic belts inHuanghua depression.Oil and Gas Geology,21(2):127-129,167(in Chinese with English abstract).
Yan,Y.,Lin,G.,Wang,Y.J.,et al.,2002.The indication ofcontinental detrital sedi ment to tectonic setting.Ad-vance in Earth Sciences,17(1):85-90(in Chinese withEnglish abstract).
Zhang,J.L.,Lin,C.S.,Zheng,H.R.,2002.Controlling ac-tion of fractures,palaeogeomorphology and materialsources of rift lake basin on sedi mentary system—Tak-ing Es3Gubei subsag as example.Petroleum Geologyand Recovery Efficiency,9(4):24-27(in Chinesewith English abstract).
Zhao,J.X.,Chen,H.D.,Shi,Z.Q.,2001.The way and i m-plications of rebuilding palaeogeomorphology,taking theresearch of palaeogeomorphology of the Ordos basin be-fore Jurassic deposition as example.Journal of Cheng-du University of Technology,28(3):260-266(in Chi-nese with English abstract).
白云风,王振升,韦阿娟,等,2008.黄骅坳陷东营组重矿物时空展布特征及物源体系分析.大庆石油地质与开发,27(2):39-42.
白云风,张兵,王华,等,2006.黄骅坳陷古近纪东营组物源方向研究.石油天然气学报,28(3):17-19.
陈纯芳,郑浚茂,王德发,2001.板桥凹陷沙三段沉积体系与物源分析.古地理学报,3(1):55-62.
邓宏文,王红亮,王敦则,2001.古地貌对陆相裂谷盆地层序充填特征的控制——以渤中凹陷西斜坡区下第三系为例.石油与天然气地质,22(4):293-296,303.
和钟铧,刘招君,张峰,2001.重矿物分析在盆地中的应用研究进展.地质科技情报,20(4):29-32.
焦养泉,李珍,周海民,1998.沉积盆地物质来源综合研究——以南堡老第三纪亚断陷盆地为例.岩相古地理,18(5):16-20.
李珍,焦养泉,刘春华,等,1998.黄骅坳陷高柳地区重矿物物源分析.石油勘探与开发,25(6):5-7.
林畅松,2006.沉积盆地的构造地层分析——以中国构造活动盆地研究为例.现代地质,20(2):185-194.
刘立,胡春燕,1991.砂岩中主要碎屑成分的物源区意义.岩相古地理,11(6):48-53.
王家豪,王华,赵忠新,等,2003.层序地层学应用于古地貌分析——以塔河油田为例.地球科学——中国地质大学学报,28(4):425-430.
汪正江,陈洪德,张锦泉,2000.物源分析的研究与展望.沉积与特提斯地质,20(4):104-110.
王子煜,漆家福,陆克政,2000.黄骅坳陷东部构造带新生代构造沉降史分析.石油与天然气地质,21(2):127-129,167.
闫义,林舸,王岳军,等,2002.盆地陆源碎屑沉积物对源区构造背景的指示意义.地球科学进展,17(1):85-90.
张建林,林畅松,郑和荣,2002.断裂湖盆断裂、古地貌及物源对沉积体系的控制作用——以孤北洼陷沙三段为例.油气地质与采收率,9(4):24-27.
赵俊兴,陈洪德,时志强,2001.古地貌恢复技术方法及其研究意义——以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例.成都理工学院学报,28(3):260-266.
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