松辽盆地深部地质特征及其盆地动力学演化
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摘要
对松辽盆地深反射地震资料的分析表明 ,该盆地地壳不仅具有层圈结构 ,而且具有明显的块断构造 ,这些块断的边界是深部热流体的网络通道。以深反射地震资料研究为基础 ,结合区域地震层析成像、火山岩地球化学等对壳幔相互作用的研究成果 ,通过地壳层圈与块断结构、构造变形史以及盆地构造与深部构造之间的关系研究 ,认为松辽盆地的形成过程是 :库拉 -太平洋板块向欧亚大陆之下俯冲作用导致的地幔隆起促使地壳拆沉减薄、地壳“三明治”结构形成 ,同时导致上地壳伸展沉降及其后期的热沉降。正因如此 ,盆地整体凹陷与地幔凸起成镜像关系 ,而断陷与拆离带凸起成偏镜像关系。强烈的壳幔作用是形成松辽盆地大规模沉降的动力学基础 ,也是盆地油气 (包括无机物质 )富集的重要原因。
The Songliao basin located in Northeast China is a large Mesozoic rift basin. A lot of work has been done on the geological characteristics, formation and evolution of the basin, as well as the accumulation regularity of oil and gas in this basin. However, the question about the formation of the basin is still a point at issue, and has attracted the great attention of many geologists. Various models have been proposed so far for the formation of the basin, such as continent rift, back arc rift, and pull apart models. Basing on deep seismic reflection data, this paper discusses the type of the basin and the geodynamic cause of its formation. Deep seismic reflection profiling has revealed that the crust of the Songliao basin is characterized by both layered and fault block structures. The crust can be divided into three layers: the upper crust, middle crust and lower crust. Parallel reflections in shallow layer and oblique reflections at above 6s twt represent the upper crust. The strong reflection belt below the upper crust represents the detachment zone between the upper and middle crust. Most of the faults in the upper crust terminate in this zone. The analysis shows that the faults in the upper crust are extensional syn sedimentary faults formed during late Jurassic to early Cretaceous and thrust system formed in late Paleozoic era. The middle crust at about 6~8s twt not only has a lot of discontinuous parallel reflections and rhombic reflections, but also a small quantity of "crocodile mouth" reflectors. The former represents extensional reformation formed in late Mesozoic era, and the later represents compressional structure formed in late Paleozoic era. The middle crust is also a low velocity and high conductivity layer. The lower crust is located at about 8～11s twt, and is characterized by rhombic reflection events. The Moho below the lower crust appears as a strong reflection belt, beneath which the layer is transparent. The reflection structure of the Songliao basin is similar to that of typical rift basin. Boundary faults between blocks were the passage of upward transferring of hot fluid from the middle lower crust or mantle to the basin. "Mushroom cloud" reflections at the deep part of the boundary faults might be the reflections of hot fluid diapir. Mirror symmetry between the down warped basin and mantle uplift is the main evidence for the rift origin of the Songliao basin. Deep seismic reflection data indicate that the main factor at depth that affected the subsidence of the basin was not only the uplift of the mantle, but also the "low velocity high conductivity" layer in the upper middle crust and hot fluid diapirs. The former caused the subsidence in later stage, while the later caused the subsidence in early stage. Regional geology and geophysical data indicate that this area is located in back arc formed by the subduction of the Kula pacific plate into the Eurasia plate in Mesozoic. Mesozoic volcanic rock system in this area is mainly of CA series, with a few exception of a small amount of A and Th type. Geochemical analysis reveals that the volcanic rocks here are characterized not only by high SiO 2 and K 2O contents and enrichment in LREE, but also by EMII type mantle, indicating back arc environment disturbed by plate subduction. However, seismic tomography data have revealed that the Songliao basin is located in disturbed area of continental mantle, rather than back arc area. It is suggested, therefore, that formation and evolution of the Songliao basin was the result of the subduction of Kula Pacific plate into the Eurasian plate. The plate subduction has led to the uplift and diapir of the mantle, and the detachment of the crust. Strong crust mantle interaction has led to the delimitation and extension of the crust, resulting in the formation of sandwich structure and large scale subsidence of the crust. It was the afore mentioned factors that caused the formation of mirror symmetry between the downwarping part of the basin and the uplifting part of the mantle, a
The Songliao basin located in Northeast China is a large Mesozoic rift basin. A lot of work has been done on the geological characteristics, formation and evolution of the basin, as well as the accumulation regularity of oil and gas in this basin. However, the question about the formation of the basin is still a point at issue, and has attracted the great attention of many geologists. Various models have been proposed so far for the formation of the basin, such as continent rift, back arc rift, and pull apart models. Basing on deep seismic reflection data, this paper discusses the type of the basin and the geodynamic cause of its formation. Deep seismic reflection profiling has revealed that the crust of the Songliao basin is characterized by both layered and fault block structures. The crust can be divided into three layers: the upper crust, middle crust and lower crust. Parallel reflections in shallow layer and oblique reflections at above 6s twt represent the upper crust. The strong reflection belt below the upper crust represents the detachment zone between the upper and middle crust. Most of the faults in the upper crust terminate in this zone. The analysis shows that the faults in the upper crust are extensional syn sedimentary faults formed during late Jurassic to early Cretaceous and thrust system formed in late Paleozoic era. The middle crust at about 6~8s twt not only has a lot of discontinuous parallel reflections and rhombic reflections, but also a small quantity of "crocodile mouth" reflectors. The former represents extensional reformation formed in late Mesozoic era, and the later represents compressional structure formed in late Paleozoic era. The middle crust is also a low velocity and high conductivity layer. The lower crust is located at about 8～11s twt, and is characterized by rhombic reflection events. The Moho below the lower crust appears as a strong reflection belt, beneath which the layer is transparent. The reflection structure of the Songliao basin is similar to that of typical rift basin. Boundary faults between blocks were the passage of upward transferring of hot fluid from the middle lower crust or mantle to the basin. "Mushroom cloud" reflections at the deep part of the boundary faults might be the reflections of hot fluid diapir. Mirror symmetry between the down warped basin and mantle uplift is the main evidence for the rift origin of the Songliao basin. Deep seismic reflection data indicate that the main factor at depth that affected the subsidence of the basin was not only the uplift of the mantle, but also the "low velocity high conductivity" layer in the upper middle crust and hot fluid diapirs. The former caused the subsidence in later stage, while the later caused the subsidence in early stage. Regional geology and geophysical data indicate that this area is located in back arc formed by the subduction of the Kula pacific plate into the Eurasia plate in Mesozoic. Mesozoic volcanic rock system in this area is mainly of CA series, with a few exception of a small amount of A and Th type. Geochemical analysis reveals that the volcanic rocks here are characterized not only by high SiO 2 and K 2O contents and enrichment in LREE, but also by EMII type mantle, indicating back arc environment disturbed by plate subduction. However, seismic tomography data have revealed that the Songliao basin is located in disturbed area of continental mantle, rather than back arc area. It is suggested, therefore, that formation and evolution of the Songliao basin was the result of the subduction of Kula Pacific plate into the Eurasian plate. The plate subduction has led to the uplift and diapir of the mantle, and the detachment of the crust. Strong crust mantle interaction has led to the delimitation and extension of the crust, resulting in the formation of sandwich structure and large scale subsidence of the crust. It was the afore mentioned factors that caused the formation of mirror symmetry between the downwarping part of the basin and the uplifting part of the mantle, a
引文
①大庆石油勘探开发研究院,1999,徐家围子深层火山岩特征研究。
①大庆石油勘探开发研究院,1999,徐家围子深层火山岩特征研究。
①大庆石油勘探开发研究院,2000,深部与基底构造研究。
迟元林,云金表,蒙启安.2002.松辽盆地深部结构及盆地动力学与油气聚集〔M〕.北京:石油工业出版社.
CHIYUAN lin,YUNJin biao,MENGQi an.2002.DeepStructureandDynamicsofSongliaoBasinandHydrocar bonAccumulation〔M〕.PetroleumIndustryPress,Beijing(inChinese).
高明修.1983.中国东部中新生代盆地与北美西部盆岭省对比研究〔A〕.见:朱夏主编.中国中新生代盆地构造和演化.北京:科学出版社.
GAOMing xiu.1983.ComparisonbetweenMesozocicCenozoicbasinsineastChinaandBasinRangeProvinceinA marica〔A〕.In:ZHUXia(ed).TectonicsandEvolutionoftheMesozoicBasinsinChina〔M〕.SciencePress,Beijing(inChinese).
高瑞祺,蔡希源.1997.松辽盆地油气田形成条件与分布规律〔M〕.北京:石油工业出版社.
GAORui qi,CAIXi yuan.1997.TheConditionandDistributionofOilandGasFieldsinSongliaobasin〔M〕.PetroleumIndustryPress,Beijing(inChinese).
葛文春,林强,孙德有,等.1999.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据〔J〕.岩石学报,15(3):396—407.
GEWen chun,LINQiang,SUNDe you,etal.1999.GeochemicalcharacteristicsoftheMesozoicbasaltinDaHingganYanshanarea:evidenceofinteractionbetweenthecrustandmantle〔J〕.ActaPetrologicaSinica,15(3):396—407(inChinese).
郭占谦,刘文龙,王先彬,等.1994.松辽盆地无机成因气的成藏特征〔J〕.中国科学(D辑),(27)2:143—148.
GUOZhan qian,LIUWen long,WANGXian bin.1994.Characteristicofnon organismgasreservoirinSongliaobasin〔J〕.ScienceinChina(SeriesD),27(2):143—148(inChinese).
李四光.地质力学概论〔M〕.1974.北京:科学出版社.LISi guang.1974.IntruductiontoGeomechanics〔M〕.SciencePress,Beijing(inChinese).
李思田.1983.东北中生代断陷盆地群分布规律与形成机制〔A〕.见:朱夏主编.中国中新生代盆地构造和演化〔M〕.北京:科学出版社.
LISi tian.1983.Distributionandformationmechanismofthefaultdepressionbasins〔A〕.In:ZHUXia(ed).Tec tonicsandEvolutionoftheMesozoicBasinsinChina〔M〕.SciencePress,Beijing(inChinese).
李思田,路凤香,林畅松.1997.中国东部及邻区中、新生代盆地演化及地球动力学背景〔M〕.北京:中国地质大学出版社.
LISi tian,LUFeng xiang,LINChang song.1997.EvolutionandGeodynamicBackgroundoftheMesozoicandCenozoicBasinsineasternChinaanditsAdjacentAreas〔M〕.ChinaUniversityofGeosciencesPress,Beijing(inChinese).
林强,葛文春,孙德有,等.1998.中国东北地区中生代火山岩的大地构造意义〔J〕.地质科学,33(2):129—139.
LINQiang,GEWen chun,SUNDe you,etal.1998.TectonicsignificanceofMesozoicvolcanicrocksinnorth easternChina〔J〕.ScientiaGeologicaSinica,33(2):129—139(inChinese).
刘德来,马莉.1998.松辽盆地裂谷期前火山岩与裂谷盆地关系及动力学过程〔J〕.地质论评,44(2):130—135.
LIUDe lai,MaLi.1998.RelationshipbetweenvolcanicrocksinpostriftstagesandriftanddynamicsprocessesonSongliaobasin.〔J〕GeologicalReview,44(2):130—135(inChinese).
路凤香,郑建平,李伍平,等.2000.中国东部显生宙地幔化的主要样式:“蘑菇云”模型〔J〕.地学前缘,7(1):97—107.
LUFeng xiang,ZHENGJian ping,LIWu ping,etal.2000.ThemainevolutionpatternofphanerozoicmantleintheeasternChina:the“mushroomcloud”model〔J〕.EarthScienceFrontiers,7(1):97—107(inChinese).
B .C .沃里沃夫斯基,H .C .沃里沃夫斯基1988.“双层砖”大陆地壳模式与巨型油气藏的关系评述〔J〕.任俞译.1995.世界石油工业,2(4):13—19.
RENYu(translator).1995.Reviewonrelationshipbetween”sandwich”modelofthecontinentalcrustandgigantichydrocarbonreservoir〔J〕.WorldPetroleumIndustry,2(4):13—19(inChinese).
任纪舜,陈廷愚,牛宝贵,等.1990.中国东部及邻区大陆岩石圈的构造演化与成矿〔M〕.北京:科学出版社.
RENJi shun,CHENTing yu,NIUBao gui,etal.1990.TectonicEvolutionofContinentalLithosphereandMet allogenyinEasternChinaandAdjacentAreas〔M〕.SciencePress,Beijing(inChinese).
任纪舜,姜春发,张正坤,等.1980.中国大地构造及其演化〔M〕.北京:科学出版社.
RENJi shun,JIANGChun fa,ZHANGZheng kun,etal.1980.TectonicEvolutionofChina〔M〕.SciencePress,Beijing(inChinese).
邵济安,刘福田,陈辉,等.2001.大兴安岭燕山晚中生代岩浆活动与俯冲作用关系〔J〕.地质学报,75(1):56—63.
SHAOji an,LIUFu tian,Chen hui,etal.2001.RelationshipbetweenMesozoicmagmatismandsubductioninDaHingganYanshanarea〔J〕.ActaGeologicaSinica,75(1):56—63(inChinese).
水谷伸治郎,邵
①大庆石油勘探开发研究院,1999,徐家围子深层火山岩特征研究。
①大庆石油勘探开发研究院,2000,深部与基底构造研究。
迟元林,云金表,蒙启安.2002.松辽盆地深部结构及盆地动力学与油气聚集〔M〕.北京:石油工业出版社.
CHIYUAN lin,YUNJin biao,MENGQi an.2002.DeepStructureandDynamicsofSongliaoBasinandHydrocar bonAccumulation〔M〕.PetroleumIndustryPress,Beijing(inChinese).
高明修.1983.中国东部中新生代盆地与北美西部盆岭省对比研究〔A〕.见:朱夏主编.中国中新生代盆地构造和演化.北京:科学出版社.
GAOMing xiu.1983.ComparisonbetweenMesozocicCenozoicbasinsineastChinaandBasinRangeProvinceinA marica〔A〕.In:ZHUXia(ed).TectonicsandEvolutionoftheMesozoicBasinsinChina〔M〕.SciencePress,Beijing(inChinese).
高瑞祺,蔡希源.1997.松辽盆地油气田形成条件与分布规律〔M〕.北京:石油工业出版社.
GAORui qi,CAIXi yuan.1997.TheConditionandDistributionofOilandGasFieldsinSongliaobasin〔M〕.PetroleumIndustryPress,Beijing(inChinese).
葛文春,林强,孙德有,等.1999.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据〔J〕.岩石学报,15(3):396—407.
GEWen chun,LINQiang,SUNDe you,etal.1999.GeochemicalcharacteristicsoftheMesozoicbasaltinDaHingganYanshanarea:evidenceofinteractionbetweenthecrustandmantle〔J〕.ActaPetrologicaSinica,15(3):396—407(inChinese).
郭占谦,刘文龙,王先彬,等.1994.松辽盆地无机成因气的成藏特征〔J〕.中国科学(D辑),(27)2:143—148.
GUOZhan qian,LIUWen long,WANGXian bin.1994.Characteristicofnon organismgasreservoirinSongliaobasin〔J〕.ScienceinChina(SeriesD),27(2):143—148(inChinese).
李四光.地质力学概论〔M〕.1974.北京:科学出版社.LISi guang.1974.IntruductiontoGeomechanics〔M〕.SciencePress,Beijing(inChinese).
李思田.1983.东北中生代断陷盆地群分布规律与形成机制〔A〕.见:朱夏主编.中国中新生代盆地构造和演化〔M〕.北京:科学出版社.
LISi tian.1983.Distributionandformationmechanismofthefaultdepressionbasins〔A〕.In:ZHUXia(ed).Tec tonicsandEvolutionoftheMesozoicBasinsinChina〔M〕.SciencePress,Beijing(inChinese).
李思田,路凤香,林畅松.1997.中国东部及邻区中、新生代盆地演化及地球动力学背景〔M〕.北京:中国地质大学出版社.
LISi tian,LUFeng xiang,LINChang song.1997.EvolutionandGeodynamicBackgroundoftheMesozoicandCenozoicBasinsineasternChinaanditsAdjacentAreas〔M〕.ChinaUniversityofGeosciencesPress,Beijing(inChinese).
林强,葛文春,孙德有,等.1998.中国东北地区中生代火山岩的大地构造意义〔J〕.地质科学,33(2):129—139.
LINQiang,GEWen chun,SUNDe you,etal.1998.TectonicsignificanceofMesozoicvolcanicrocksinnorth easternChina〔J〕.ScientiaGeologicaSinica,33(2):129—139(inChinese).
刘德来,马莉.1998.松辽盆地裂谷期前火山岩与裂谷盆地关系及动力学过程〔J〕.地质论评,44(2):130—135.
LIUDe lai,MaLi.1998.RelationshipbetweenvolcanicrocksinpostriftstagesandriftanddynamicsprocessesonSongliaobasin.〔J〕GeologicalReview,44(2):130—135(inChinese).
路凤香,郑建平,李伍平,等.2000.中国东部显生宙地幔化的主要样式:“蘑菇云”模型〔J〕.地学前缘,7(1):97—107.
LUFeng xiang,ZHENGJian ping,LIWu ping,etal.2000.ThemainevolutionpatternofphanerozoicmantleintheeasternChina:the“mushroomcloud”model〔J〕.EarthScienceFrontiers,7(1):97—107(inChinese).
B .C .沃里沃夫斯基,H .C .沃里沃夫斯基1988.“双层砖”大陆地壳模式与巨型油气藏的关系评述〔J〕.任俞译.1995.世界石油工业,2(4):13—19.
RENYu(translator).1995.Reviewonrelationshipbetween”sandwich”modelofthecontinentalcrustandgigantichydrocarbonreservoir〔J〕.WorldPetroleumIndustry,2(4):13—19(inChinese).
任纪舜,陈廷愚,牛宝贵,等.1990.中国东部及邻区大陆岩石圈的构造演化与成矿〔M〕.北京:科学出版社.
RENJi shun,CHENTing yu,NIUBao gui,etal.1990.TectonicEvolutionofContinentalLithosphereandMet allogenyinEasternChinaandAdjacentAreas〔M〕.SciencePress,Beijing(inChinese).
任纪舜,姜春发,张正坤,等.1980.中国大地构造及其演化〔M〕.北京:科学出版社.
RENJi shun,JIANGChun fa,ZHANGZheng kun,etal.1980.TectonicEvolutionofChina〔M〕.SciencePress,Beijing(inChinese).
邵济安,刘福田,陈辉,等.2001.大兴安岭燕山晚中生代岩浆活动与俯冲作用关系〔J〕.地质学报,75(1):56—63.
SHAOji an,LIUFu tian,Chen hui,etal.2001.RelationshipbetweenMesozoicmagmatismandsubductioninDaHingganYanshanarea〔J〕.ActaGeologicaSinica,75(1):56—63(inChinese).
水谷伸治郎,邵
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