松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究
|
摘要
通过对晚白垩世松辽盆地南部西部斜坡区的综合研究,从基底构造、古地理位置、地层产状和厚度、钻井和地震资料特征及构造发育情况等方面表明,该区在青山口组-嫩江组坳陷期发育侵蚀坡折带、沉积坡折带和构造坡折带。由于多种类型坡折带的存在,制约着盆地充填可容空间的变化,控制了区内的层序发育、沉积体系展布和非构造圈闭类型。松辽盆地南部西部斜坡区湖盆坡折带附近是非构造油气藏发育的有利部位,可以应用坡折带理论指导本区的隐蔽油气藏勘探。
The study is carried out by a comprehensive analysis of the basement structure, palaeo-(geographic) location, occurrence and thickness of stratigraphy, structure development and of the well log and seismic data of the western slope of the southern sector of the Songliao basin in the late Cretaceous period. Three types of slope breaks developed during the depression period from the Qingshankou to Nenjiang Formations based on the present research: erodent, sedimentary and structural. It is evident these different types of slope breaks not only have restricted changes of compatible space filling in basin, but also have an important control on the sequence, development of sedimentary system and types of non-structural traps. Consequently it is obvious that the western slope of the Southern sector of the Songliao basin is a favorable area for non-structural traps and subtle reservoir exploration. The theory of slope breaks is also important in directing the further exploration and reserves prediction.
The study is carried out by a comprehensive analysis of the basement structure, palaeo-(geographic) location, occurrence and thickness of stratigraphy, structure development and of the well log and seismic data of the western slope of the southern sector of the Songliao basin in the late Cretaceous period. Three types of slope breaks developed during the depression period from the Qingshankou to Nenjiang Formations based on the present research: erodent, sedimentary and structural. It is evident these different types of slope breaks not only have restricted changes of compatible space filling in basin, but also have an important control on the sequence, development of sedimentary system and types of non-structural traps. Consequently it is obvious that the western slope of the Southern sector of the Songliao basin is a favorable area for non-structural traps and subtle reservoir exploration. The theory of slope breaks is also important in directing the further exploration and reserves prediction.
引文
[1]VailP R.Seismic stratigraphy interpretation using se quence stratigrapthy,Part1:Seismic stratigraphy inter pretation procedure[J].AAPG Studies inGeology,1987,27:110.
[2]VanWagonerJ C.Siliciclastic sequence stratigraphy inwell logs, cores and outcrops: concepts for high reso lution correlation of time and facies[M].Oklahoma:AmericanAssociation ofPetroleumGeologists,1990.
[3] VanWagonerJ C.Sequence stratigraphy and marine tonon marine facies architecture of foreland basin strata[J].AAPG Memoir,1995,64:137223.
[4]刘招君,董清水,王嗣敏,等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002.LIU Zhao jun,DONG Qing shui,WANG Si min,et al.Introduction to continental sequence stratigraphy andapplication[M].Beijing:PetroleumIndustryPress,2002.
[5]徐怀大.陆相层序地层学研究中的某些问题[J].石油与天然气地质,1997,18(2):8389.XU Huai da.Some problems in study of continental se quence stratigraphy[J].Oil andGasGeology,1997,18(2):8389.
[6]薛良清.湖相盆地中的层序、体系域与隐蔽油气藏[J].石油与天然气地质,2002,23(2):115120.XUE Liang qing.Sequence, system tracts and subtlehyudrocarbon pools in lacustrine basins[J].Oil andGasGeology,2002,23(2):115120.
[7]VanWagonerJ C,PosamentierH W,MitchumR M,etal.An overview of the fundamentals of sequence stra tigraphy and key definitions[J].SEPM SpecialPublica tion,1988,42:3945.
[8]BrownL F Jr,BemspmJ M,BrinkG J, et al.Se quence stratigraphy in offshoreSouthAfrican divergentbasin[J].AAPG Studies inGeology,1995,41:1184.
[9]ShawH,HockS C,SitohongE P.Extensional fault-bend folding and synrift deposition, an example fromthe centralSumutraBasin,Indonesia[J].AAPG Bulle tin,1997,81(3):367379.
[10]姜秀芳,宗国洪,郭玉新,等.断裂坡折带低位扇成因及成藏特征[J].石油与天然气地质,2002,23(2):143144.JIANG Xiu fang,ZONG Guo hong,GUO Yu xin, etal.Origin of lowstand fan in faulted topographic breakand play’s characteristics[J].Oil andGasGeology,2002,23(2):143144.
[11]冯有良,李思田.东营凹陷沙河街组三段层序低位域砂体沉积特征[J].地质论评,2001,47(3):279286.FENG You liang,LI Si tian.Sand body depositionalcharacteristics of low standard system sequence inShahejieFormation ofDongying depression[J].Geo logicalReview,2001,47(3):279286.
[12]邓宏文,王洪亮,王敦则.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[J].石油与天然气地质,2001,22(4):293296.DENG Hong wen,WANG Hong liang,WANG Dun ze.Control of paleo morphology to stratigraphic se quence in continental rift basins:Take lowerTertiaryof western slope inBozhong depression as an example[J].Oil andGasGeology,2001,22(4):293296.
[13]樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2):1217.FAN Tai liang,LI Wei dong.A successful case onsequence stratigraphy applied to the prediction of non marine oil reservoir[J].ActaPetroleiSinica,1999,20(2):1217.
[14]林畅松,潘元林,肖建新,等.“构造坡折带”———断陷盆地层序分析和油气预测的重要概念[J].地球科学中国地质大学学报,2000,25(3):260266.LIN Chang song,PAN Yuan lin,XIAO Jian xin, etal.Structural slope break zone:Key concept for stra tigraphic sequence analysis and petroleum prospectingin fault subsidence basins[J ].EarthScienceJournal ofChinaUniversity ofGeosciences,2000,25(3):260266.
[15]魏魁生,徐怀大,雷怀玉,等.非海相层序地层学———以松辽盆地为例[M].北京:地质出版社,1996.WEI Kui sheng,XU Huai da,LEI Huai yu, et al.Se quence stratigraphy of nonmarine facier———TakeSongliao basin as an example[M].Beijing:GeologicalPublishingHouse,1996.
[16]朱筱敏,康安,王贵文.陆相坳陷型和断陷型湖盆层序地层样式探讨[J].沉积学报,2003,31(2):283287.ZHU Xiao min,KANG An,WANG Gui wen.Se quence stratigraphic models of depression and faulted down lake basins[J].ActaSedimentologicaSinica,2003,31(2):283287.
[17]赵玉光,丘东洲.西准噶尔界山前陆盆地晚期(T-J)层序地层与油气勘探[J].新疆石油地质,1993,14(4):323331.ZHAO Yu guang,QIU Dong zhou.Sequence strati graphy and petroleum exploration in the late stage offorland basin, western mountain ofJunggar basin[J].XinjiangPetroleumGeology,1993,14(4):323331.
[18]王英民,刘豪,李立诚,等.准噶尔大型坳陷湖盆坡折带的类型和分布特征[J].地球科学中国地质大学学报,2002,27(6):683688.WANG Ying min,LIU Hao,LI Li cheng,et al.Typesand distribution characteristics of slope breaks oflarge type down warped lake basins[J].EarthScienceJournal ofChinaUniversity ofGeosciences,2002,27(6):683688.
[19]王英民,金武弟,刘书会,等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义[J].石油与天然气地质,2003,24(3):199204.WANG Ying min,JIN Wu di,LIU Shu hui,et al.Ge netic types, distribution and exploration significanceof multistage slope breaks in rift lacustrine basin[J].Oil andGasGeology,2003,24(3):199204.
[20]何汉漪.二十一世纪的地震勘探技术[J].地学前缘,2000,7(3):267273.HE Han yi.The seismic technology in the21st centu ry[J].EarthScienceFrontiers,2000,7(3):267273.
[21]张功成,徐宏,朱德丰.松辽盆地构造特征与油气[A].见:张功成,徐宏,等主编.中国含油气盆地构造[C].北京:石油工业出版社,1999:111125.ZHANG Gong cheng,XU Hong,ZHU De feng.Thestructure characteristics and oil ofSongliao basin[A].In:ZHANG Gong cheng,XU Hong,et al, eds.Tectonics and structural style of petroliferous basinsinChina[C].Beijing:PetroleumIndustryPress,1999:111125.
[22]郭巍,刘招君,董清水,等.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[J].吉林大学学报(地球科学版),2002,32(3):233237.GUO Wei,LIU Zhao jun,DONG Qing shui,et al.Oiland gas gathering rule in the sequence stritagraphicframe of fault depression lacustrine basinAn ex ample fromSongliao basin[J].Journal ofJilinUniver sity(EarthScienceEdition),2002,32(3):233237.
[2]VanWagonerJ C.Siliciclastic sequence stratigraphy inwell logs, cores and outcrops: concepts for high reso lution correlation of time and facies[M].Oklahoma:AmericanAssociation ofPetroleumGeologists,1990.
[3] VanWagonerJ C.Sequence stratigraphy and marine tonon marine facies architecture of foreland basin strata[J].AAPG Memoir,1995,64:137223.
[4]刘招君,董清水,王嗣敏,等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002.LIU Zhao jun,DONG Qing shui,WANG Si min,et al.Introduction to continental sequence stratigraphy andapplication[M].Beijing:PetroleumIndustryPress,2002.
[5]徐怀大.陆相层序地层学研究中的某些问题[J].石油与天然气地质,1997,18(2):8389.XU Huai da.Some problems in study of continental se quence stratigraphy[J].Oil andGasGeology,1997,18(2):8389.
[6]薛良清.湖相盆地中的层序、体系域与隐蔽油气藏[J].石油与天然气地质,2002,23(2):115120.XUE Liang qing.Sequence, system tracts and subtlehyudrocarbon pools in lacustrine basins[J].Oil andGasGeology,2002,23(2):115120.
[7]VanWagonerJ C,PosamentierH W,MitchumR M,etal.An overview of the fundamentals of sequence stra tigraphy and key definitions[J].SEPM SpecialPublica tion,1988,42:3945.
[8]BrownL F Jr,BemspmJ M,BrinkG J, et al.Se quence stratigraphy in offshoreSouthAfrican divergentbasin[J].AAPG Studies inGeology,1995,41:1184.
[9]ShawH,HockS C,SitohongE P.Extensional fault-bend folding and synrift deposition, an example fromthe centralSumutraBasin,Indonesia[J].AAPG Bulle tin,1997,81(3):367379.
[10]姜秀芳,宗国洪,郭玉新,等.断裂坡折带低位扇成因及成藏特征[J].石油与天然气地质,2002,23(2):143144.JIANG Xiu fang,ZONG Guo hong,GUO Yu xin, etal.Origin of lowstand fan in faulted topographic breakand play’s characteristics[J].Oil andGasGeology,2002,23(2):143144.
[11]冯有良,李思田.东营凹陷沙河街组三段层序低位域砂体沉积特征[J].地质论评,2001,47(3):279286.FENG You liang,LI Si tian.Sand body depositionalcharacteristics of low standard system sequence inShahejieFormation ofDongying depression[J].Geo logicalReview,2001,47(3):279286.
[12]邓宏文,王洪亮,王敦则.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[J].石油与天然气地质,2001,22(4):293296.DENG Hong wen,WANG Hong liang,WANG Dun ze.Control of paleo morphology to stratigraphic se quence in continental rift basins:Take lowerTertiaryof western slope inBozhong depression as an example[J].Oil andGasGeology,2001,22(4):293296.
[13]樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2):1217.FAN Tai liang,LI Wei dong.A successful case onsequence stratigraphy applied to the prediction of non marine oil reservoir[J].ActaPetroleiSinica,1999,20(2):1217.
[14]林畅松,潘元林,肖建新,等.“构造坡折带”———断陷盆地层序分析和油气预测的重要概念[J].地球科学中国地质大学学报,2000,25(3):260266.LIN Chang song,PAN Yuan lin,XIAO Jian xin, etal.Structural slope break zone:Key concept for stra tigraphic sequence analysis and petroleum prospectingin fault subsidence basins[J ].EarthScienceJournal ofChinaUniversity ofGeosciences,2000,25(3):260266.
[15]魏魁生,徐怀大,雷怀玉,等.非海相层序地层学———以松辽盆地为例[M].北京:地质出版社,1996.WEI Kui sheng,XU Huai da,LEI Huai yu, et al.Se quence stratigraphy of nonmarine facier———TakeSongliao basin as an example[M].Beijing:GeologicalPublishingHouse,1996.
[16]朱筱敏,康安,王贵文.陆相坳陷型和断陷型湖盆层序地层样式探讨[J].沉积学报,2003,31(2):283287.ZHU Xiao min,KANG An,WANG Gui wen.Se quence stratigraphic models of depression and faulted down lake basins[J].ActaSedimentologicaSinica,2003,31(2):283287.
[17]赵玉光,丘东洲.西准噶尔界山前陆盆地晚期(T-J)层序地层与油气勘探[J].新疆石油地质,1993,14(4):323331.ZHAO Yu guang,QIU Dong zhou.Sequence strati graphy and petroleum exploration in the late stage offorland basin, western mountain ofJunggar basin[J].XinjiangPetroleumGeology,1993,14(4):323331.
[18]王英民,刘豪,李立诚,等.准噶尔大型坳陷湖盆坡折带的类型和分布特征[J].地球科学中国地质大学学报,2002,27(6):683688.WANG Ying min,LIU Hao,LI Li cheng,et al.Typesand distribution characteristics of slope breaks oflarge type down warped lake basins[J].EarthScienceJournal ofChinaUniversity ofGeosciences,2002,27(6):683688.
[19]王英民,金武弟,刘书会,等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义[J].石油与天然气地质,2003,24(3):199204.WANG Ying min,JIN Wu di,LIU Shu hui,et al.Ge netic types, distribution and exploration significanceof multistage slope breaks in rift lacustrine basin[J].Oil andGasGeology,2003,24(3):199204.
[20]何汉漪.二十一世纪的地震勘探技术[J].地学前缘,2000,7(3):267273.HE Han yi.The seismic technology in the21st centu ry[J].EarthScienceFrontiers,2000,7(3):267273.
[21]张功成,徐宏,朱德丰.松辽盆地构造特征与油气[A].见:张功成,徐宏,等主编.中国含油气盆地构造[C].北京:石油工业出版社,1999:111125.ZHANG Gong cheng,XU Hong,ZHU De feng.Thestructure characteristics and oil ofSongliao basin[A].In:ZHANG Gong cheng,XU Hong,et al, eds.Tectonics and structural style of petroliferous basinsinChina[C].Beijing:PetroleumIndustryPress,1999:111125.
[22]郭巍,刘招君,董清水,等.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[J].吉林大学学报(地球科学版),2002,32(3):233237.GUO Wei,LIU Zhao jun,DONG Qing shui,et al.Oiland gas gathering rule in the sequence stritagraphicframe of fault depression lacustrine basinAn ex ample fromSongliao basin[J].Journal ofJilinUniver sity(EarthScienceEdition),2002,32(3):233237.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心