基于地震资料的陆相湖盆物源通道特征分析:以渤中凹陷西斜坡东营组为例
摘要
针对渤中凹陷西斜坡无井、少井的地质特征,基于最新的三维地震资料,讨论了沙垒田凸起、石臼坨凸起之间的古物源搬运通道及其控制沉积的差异性.研究结果表明,渤中凹陷西斜坡东营组发育3种类型的沉积物搬运通道:古沟谷物源通道、断槽物源通道、构造转换带物源通道.研究区的沉积主要受到源于沙垒田凸起NEE向条带状展布的断槽物源通道控制;古沟谷物源搬运通道控制的沉积主要分布石臼坨凸起南部的局部地区;构造转换带物源通道控制的沉积主要分布在沙垒田凸起东南缘的局部地区.研究区发育的这3种物源搬运通道,代表陆相湖盆物源从源区到沉积区的搬运途径,并分别对应不同的源-渠-汇的空间耦合模式.研究区源于沙垒田凸起的断槽物源通道模式观点的提出,改变了传统上认为沙垒田凸起东缘为近源快速堆积的扇三角洲为主的认识,为寻找有利的储层和油气分布建立了指导模式.
Due to insufficient well data,the diversity of sediment transport pathway and their controlling deposits was analyzed using the recent 3Dseismic data in the western slope of Bozhong sag.The results show that there are three types of sediment transport pathway in Dongying formation of the western slope of Bozhong sag,including sediment transport pathway of Paleochannel,faulted trough and structural transfer zones.The deposits of study area were controlled mainly by faulted trough sediment transport pathway derived from Shaleitian uplift,with the belted distribution in NEE direction.The deposits controlled by paleo-channel sediment transport pathway occurred in the local area of southern Shijiutuo uplift.The deposits controlled by structural transfer zones sediment transport pathway are focused on the local area of southeast Shaleitian uplift.Three types of sediment transport pathway display the overall sediment transport methods from the source area to the deposits area in the continental lacustrine basins,and formed three types corresponding coupling patterns of the source area-transport pathway-deposit area.Structural transfer zones sediment transport pathway is considered one special style of faulted trough sediment transport pathway.The presence of faulted trough sediment transport pathway derived from the Shaleitian uplift changes the past understanding that it is the fan delta with proximal and rapid deposit in the eastern Shaleitian uplift,and provides an effective model for seeking potential reservoir.
Due to insufficient well data,the diversity of sediment transport pathway and their controlling deposits was analyzed using the recent 3Dseismic data in the western slope of Bozhong sag.The results show that there are three types of sediment transport pathway in Dongying formation of the western slope of Bozhong sag,including sediment transport pathway of Paleochannel,faulted trough and structural transfer zones.The deposits of study area were controlled mainly by faulted trough sediment transport pathway derived from Shaleitian uplift,with the belted distribution in NEE direction.The deposits controlled by paleo-channel sediment transport pathway occurred in the local area of southern Shijiutuo uplift.The deposits controlled by structural transfer zones sediment transport pathway are focused on the local area of southeast Shaleitian uplift.Three types of sediment transport pathway display the overall sediment transport methods from the source area to the deposits area in the continental lacustrine basins,and formed three types corresponding coupling patterns of the source area-transport pathway-deposit area.Structural transfer zones sediment transport pathway is considered one special style of faulted trough sediment transport pathway.The presence of faulted trough sediment transport pathway derived from the Shaleitian uplift changes the past understanding that it is the fan delta with proximal and rapid deposit in the eastern Shaleitian uplift,and provides an effective model for seeking potential reservoir.
引文
Cheng,R.H.,Zhu,D.F.,Wang,H.Y.,et al.,2006.Struc-tural Sub-Division and Depositional Systems of LindianFault Depression in the North Songliao Basin duringShahezi Stage of Early Cretaceous.Journal of JilinUniversity(Earth Science Edition),36(5):793-798(in Chinese with English abstract).
Chi,Y.L.,Zhao,W.Z.,2000.Strike-Slip Deformation duringthe Cenozoic and Its Influence on Hydrocarbon Accu-mulation in the Bohai Bay Basin.Acta Petrolei Sinica,21(2):14-20(in Chinese with English abstract).
Chu,Q.Z.,Zhang,S.L.,Huang,X.W.,2002.Study on the Re-lation between Associated Gas Accumulation and StructuralCharacteristics of Cenozioc Faulted Structure in BozhongDepression.Journal of Xinjiang Petroleum Institute,14(2):9-13(in Chinese with English abstract).
Dahlstrom,C.D.A.,1970.Structural Geology in the EasternMargin of the Canadian Rocky Mountain.Bulletin ofCanadian Petroleum Geology,18(3):332-406.
Faulds,J.E.,Varga,R.J.,1998.The Role of AccommodationZone and Transfer Zone in the Regional Segmentation ofExtended Terranes.In:Faulds,J.E.,Stewart,J.H.,eds.,Accommodation Zones and Transfer Zones:The RegionalSegmentation of the Basin and Range Provinces.GeologicalSociety of America Special Paper,USA,1-45.
Feng,Y.L.,Xu,X.S.,2006.Syndepositional StructuralSlope-break Zone Controls on Lithologic Reservoirs—ACase from Paleogene Bohai Bay Basin.Petroleum Ex-ploration and Development,33(1):22-25(in Chinesewith English abstract).
Li,H.,Wang,L.J.,Wang,K.,2001.The Early Tertiary Shahe-jie Faulted Trough in Eastern Liaohe Basin and Its Implica-tions to Oil and Gas Resource.Acta Geoscientia Sinica,22(5):437-440(in Chinese with English abstract).
Lin,C.S.,Zhang,Y.M.,Li,S.T.,et al.,2004.Episodic Rif-ting Dynamic Process and Quantitative Model of Meso-zoic-Cenozoic Faulted Basins in Eastern China.Earth Science—Journal of China University of Geosciences,29(5):583-588(in Chinese with English abstract).
Mouslopoulou,V.,Nicol,A.,Little,T.A.,et al.,2007.Displace-ment Transfer between Intersecting Regional Strike-Slip andExtensional Fault Systems.Journal of Structural Geology,29(1):100-116.doi:10.1016/j.jsg.2006.08.002
Moustafa,A.R.,2002.Controls on the Geometry of TransferZones in the Suez Rift and Northwest Red Sea:Implica-tions for the Structural Geometry of Rift Systems.AAPG Bulletin,86(6):979-1002.doi:10.1306/61EEDC06-173E-11D7-8645000102C1865D
Peacock,D.C.P.,Sanderson,D.J.,1994.Geometry and De-velopment of Relay Ramps in Normal Fault Systems.AAPG Bulletin,78(2):147-165.doi:10.1306/BD-FF9046-1718-11D7-8645000102C1865D
Qi,J.F.,2007.Structural Transfer Zones and Significancefor Hydrocarbon Accumulation in Rifting Basins.Ma-rine Origin Petroleum Geology,12(4):43-50(in Chi-nese with English abstract).
Soliva,R.,Benedicto,A.,2004.A Linkage Criterion for Seg-mented Normal Faults.Journal of Structural Geology,26(12):2251-2267.doi:10.1016/j.jsg.2004.06.008
Sun,Y.H.,Qi,J.F.,Lv,Y.F.,et al.2008.Characteristics ofFault Structure and Its Control to Hydrocarbon inBozhong Depression.Acta Petrolei Sinica,29(5):669-675(in Chinese with English abstract).
Wan,G.M.,Tang,L.J.,Zhou,X.H.,et al.,2009.Zonationof Structural Pattern in the Bozhong Depression and ItsAdjacent Area.Marine Geology and Quaternary Geolo-gy,29(2):9-13(in Chinese with English abstract).
Wang,Z.J.,Chen,H.D.,Zhang,J.Q.,2000.The Research andProspect in Provenance Analysis.Sedimentary Geologyand Tethyan Geology,20(4):104-110(in Chinese).
Wu,L.,Xu,H.M.,Ji,H.C.,2006.Evolution of Sedimenta-ry System and Analysis of Sedimentary Source in Paleo-gene of Bozhong Sag,Bohai Bay.Marine Geology andQuaternary Geology,26(1):81-88(in Chinese withEnglish abstract).
Xu,C.G.,Yu,S.,Lin,C.S.,et al.,2008.Structural Stylesof the Paleogene Lacustrine Basin Margin and TheirControl on Sedimentary Sequences in Bohai Sea Area.Journal of Palaeogeography,10(6):627-635(inChinese with English abstract).
Xu,Y.J,Du,Y.S.,Yang,J.H.,2007.Prospects of SedimentProvenance Analysis.Geological Science and Technolo-gy Information,26(3):26-32(in Chinese with Eng-lish abstract).
Yu,Y.X.,Zhou,X.H.,Wei,G.,et al.,2008.Structural Transfer Zones and Their Hydrocarbon Significances inBohai Bay Area.Journal of Palaeogeography,10(5):555-560(in Chinese with English abstract).
Zhang,J.N.,Yu,J.G.,2006.The Indetermination Analysison the Seismic Attribute Application.GeophysicalProspecting for Petroleum,45(4):373-379(in Chi-nese with English abstract).
Zhao,G.L.,Zhao,C.L.,2002.Study on the Seismic-Sedimenta-ry Facies of the Bozhong Subsidence.Journal of Chen DuUniversity of Tecnology(Science&Technology Edi-tion),29(1):41-48(in Chinese with English abstract).
Zhao,G.L.,Zhao,C.L.,Ye,L.J.,2005.Sedimentary Sys-tem of“Four Fans and One Channel”in the Bohai GulfBasin and Its Significance for Petroleum Exploration.Journal of Geomechanics,11(3):245-258(in Chinesewith English abstract).
Zhao,H.G.,Liu,C.Y.,2003.Approaches and Prospects ofProvenance Analysis.Acta Sedimentologica Sinica,21(3):409-415(in Chinese with English abstract).
Zhou,S.K.,Wei,Z.D.,Deng,H.W.,et al.,2006.A Studyon Paleogene Tectonic Sequences in Bozhong Sag.ChinaOffshore Oil and Gas,18(4):236-240(in Chinesewith English abstract).
Zhou,S.K.,Xu,C.G.,2006.One Kind of Important Deep-water Reservoir:The Longitudinal Gravity CurrentsSediments—A Case Study in Mingyuefeng Formation inLishui Sag,East China Sea Basin.Geological Scienceand Technology Information,25(5):57-62(in Chi-nese with English abstract).
Zhu,H.T.,Du,Y.S.,Liu,K.Y.,et al.,2008.SequenceStratigraphic Delineation and Correlation of the Dongy-ing Formation in the Nearshore and Adjacent Sea Are-as,Bohai Bay Basin.Earth Science—Journal of ChinaUniversity of Geosciences,19(1):54-64.
Zhu,H.T.,Yang,X.H.,Zhou,X.H.,et al.,2011.High Reso-lution Three-Dimensional Facies Architecture DelineationUsing Sequence Stratigraphy,Seismic Sedimentology:Ex-ample from Dongying Formation in BZ3-1Block of WesternSlope of Bozhong Sag,Bohai Bay Basin.Earth Science—Journal of China University of Geosciences,36(6):1073-1084(in Chinese with English abstract).
程日辉,朱德丰,王洪艳,等,2006.松辽盆地林甸断陷白垩纪沙河子期盆地次级构造单元与沉积体系.吉林大学学报(地球科学版),36(5):793-798.
池英柳,赵文智.2000.渤海湾盆地新生代走滑构造与油气聚集.石油学报,21(2):14-20.
褚庆忠,张树林,黄雄伟,2002.渤中坳陷断裂构造特征与油气运聚关系研究.新疆石油学院学报,14(2):9-13.
冯有良,徐秀生,2006.同沉积构造坡折带对岩性油气藏富集带的控制作用——以渤海湾盆地古近系为例.石油勘探与开发,33(1):22-25.
李虹,王立军,王凯,2001.辽河坳陷下第三系沙三段深断槽发育特点及其油气勘探意义.地球学报,22(5):437-440.
林畅松,张燕梅,李思田,等,2004.中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型.地球科学——中国地质大学学报,29(5):583-588.
漆家福,2007.裂陷盆地中的构造变换带及其石油地质意义.海相油气地质,12(4):43-50.
孙永河,漆家福,吕延防,等,2008.渤中坳陷断裂构造特征及其对油气的控制.石油学报,29(5):669-675.
万桂梅,汤良杰,周心怀,等,2009.渤中坳陷及邻区构造分带变形特征.海洋地质与第四纪地质,29(2):9-13.
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.
吴磊,徐怀民,季汉成,2006.渤海湾盆地渤中凹陷古近系沉积体系演化及物源分析.海洋地质与第四纪地质,26(1):81-88.
徐长贵,于水,林畅松,等,2008.渤海海域古近系湖盆边缘构造样式及其对沉积层序的控制作用.古地理学报,10(6):627-635.
徐亚军,杜远生,杨江海,2007.沉积物物源分析研究进展.地质科技情报,26(3):26-32.
余一欣,周心怀,魏刚,等,2008.渤海湾地区构造变换带及油气意义.古地理学报,10(5):555-560.
张建宁,于建国,2006.地震属性应用中的不确定性分析.石油物探,45(4):373-379.
赵国连,赵澄林,叶连俊,2005.渤海湾盆地“四扇一沟”沉积体系及其油气意义.地质力学学报,11(3):245-258.
赵国连,赵澄林,2002.渤中凹陷地震-沉积相研究.成都理工学院学报,29(1):41-48.
赵红格,刘池洋,2003.物源分析方法及研究进展.沉积学报,21(3):409-415.
周士科,魏泽典,邓宏文,等,2006.渤中凹陷古近系构造层序研究.中国海上油气,18(4):236-240.
周士科,徐长贵,2006.轴向重力流沉积:一种重要的深水储层—以东海盆地丽水凹陷明月峰组为例.地质科技情报,25(5):57-62.
朱红涛,杨香华,周心怀,等,2011.基于层序地层学和地震沉积学的高精度三维沉积体系:以渤中凹陷西斜坡BZ3-1区块东营组为例.地球科学——中国地质大学学报,36(6):1073-1084.
Chi,Y.L.,Zhao,W.Z.,2000.Strike-Slip Deformation duringthe Cenozoic and Its Influence on Hydrocarbon Accu-mulation in the Bohai Bay Basin.Acta Petrolei Sinica,21(2):14-20(in Chinese with English abstract).
Chu,Q.Z.,Zhang,S.L.,Huang,X.W.,2002.Study on the Re-lation between Associated Gas Accumulation and StructuralCharacteristics of Cenozioc Faulted Structure in BozhongDepression.Journal of Xinjiang Petroleum Institute,14(2):9-13(in Chinese with English abstract).
Dahlstrom,C.D.A.,1970.Structural Geology in the EasternMargin of the Canadian Rocky Mountain.Bulletin ofCanadian Petroleum Geology,18(3):332-406.
Faulds,J.E.,Varga,R.J.,1998.The Role of AccommodationZone and Transfer Zone in the Regional Segmentation ofExtended Terranes.In:Faulds,J.E.,Stewart,J.H.,eds.,Accommodation Zones and Transfer Zones:The RegionalSegmentation of the Basin and Range Provinces.GeologicalSociety of America Special Paper,USA,1-45.
Feng,Y.L.,Xu,X.S.,2006.Syndepositional StructuralSlope-break Zone Controls on Lithologic Reservoirs—ACase from Paleogene Bohai Bay Basin.Petroleum Ex-ploration and Development,33(1):22-25(in Chinesewith English abstract).
Li,H.,Wang,L.J.,Wang,K.,2001.The Early Tertiary Shahe-jie Faulted Trough in Eastern Liaohe Basin and Its Implica-tions to Oil and Gas Resource.Acta Geoscientia Sinica,22(5):437-440(in Chinese with English abstract).
Lin,C.S.,Zhang,Y.M.,Li,S.T.,et al.,2004.Episodic Rif-ting Dynamic Process and Quantitative Model of Meso-zoic-Cenozoic Faulted Basins in Eastern China.Earth Science—Journal of China University of Geosciences,29(5):583-588(in Chinese with English abstract).
Mouslopoulou,V.,Nicol,A.,Little,T.A.,et al.,2007.Displace-ment Transfer between Intersecting Regional Strike-Slip andExtensional Fault Systems.Journal of Structural Geology,29(1):100-116.doi:10.1016/j.jsg.2006.08.002
Moustafa,A.R.,2002.Controls on the Geometry of TransferZones in the Suez Rift and Northwest Red Sea:Implica-tions for the Structural Geometry of Rift Systems.AAPG Bulletin,86(6):979-1002.doi:10.1306/61EEDC06-173E-11D7-8645000102C1865D
Peacock,D.C.P.,Sanderson,D.J.,1994.Geometry and De-velopment of Relay Ramps in Normal Fault Systems.AAPG Bulletin,78(2):147-165.doi:10.1306/BD-FF9046-1718-11D7-8645000102C1865D
Qi,J.F.,2007.Structural Transfer Zones and Significancefor Hydrocarbon Accumulation in Rifting Basins.Ma-rine Origin Petroleum Geology,12(4):43-50(in Chi-nese with English abstract).
Soliva,R.,Benedicto,A.,2004.A Linkage Criterion for Seg-mented Normal Faults.Journal of Structural Geology,26(12):2251-2267.doi:10.1016/j.jsg.2004.06.008
Sun,Y.H.,Qi,J.F.,Lv,Y.F.,et al.2008.Characteristics ofFault Structure and Its Control to Hydrocarbon inBozhong Depression.Acta Petrolei Sinica,29(5):669-675(in Chinese with English abstract).
Wan,G.M.,Tang,L.J.,Zhou,X.H.,et al.,2009.Zonationof Structural Pattern in the Bozhong Depression and ItsAdjacent Area.Marine Geology and Quaternary Geolo-gy,29(2):9-13(in Chinese with English abstract).
Wang,Z.J.,Chen,H.D.,Zhang,J.Q.,2000.The Research andProspect in Provenance Analysis.Sedimentary Geologyand Tethyan Geology,20(4):104-110(in Chinese).
Wu,L.,Xu,H.M.,Ji,H.C.,2006.Evolution of Sedimenta-ry System and Analysis of Sedimentary Source in Paleo-gene of Bozhong Sag,Bohai Bay.Marine Geology andQuaternary Geology,26(1):81-88(in Chinese withEnglish abstract).
Xu,C.G.,Yu,S.,Lin,C.S.,et al.,2008.Structural Stylesof the Paleogene Lacustrine Basin Margin and TheirControl on Sedimentary Sequences in Bohai Sea Area.Journal of Palaeogeography,10(6):627-635(inChinese with English abstract).
Xu,Y.J,Du,Y.S.,Yang,J.H.,2007.Prospects of SedimentProvenance Analysis.Geological Science and Technolo-gy Information,26(3):26-32(in Chinese with Eng-lish abstract).
Yu,Y.X.,Zhou,X.H.,Wei,G.,et al.,2008.Structural Transfer Zones and Their Hydrocarbon Significances inBohai Bay Area.Journal of Palaeogeography,10(5):555-560(in Chinese with English abstract).
Zhang,J.N.,Yu,J.G.,2006.The Indetermination Analysison the Seismic Attribute Application.GeophysicalProspecting for Petroleum,45(4):373-379(in Chi-nese with English abstract).
Zhao,G.L.,Zhao,C.L.,2002.Study on the Seismic-Sedimenta-ry Facies of the Bozhong Subsidence.Journal of Chen DuUniversity of Tecnology(Science&Technology Edi-tion),29(1):41-48(in Chinese with English abstract).
Zhao,G.L.,Zhao,C.L.,Ye,L.J.,2005.Sedimentary Sys-tem of“Four Fans and One Channel”in the Bohai GulfBasin and Its Significance for Petroleum Exploration.Journal of Geomechanics,11(3):245-258(in Chinesewith English abstract).
Zhao,H.G.,Liu,C.Y.,2003.Approaches and Prospects ofProvenance Analysis.Acta Sedimentologica Sinica,21(3):409-415(in Chinese with English abstract).
Zhou,S.K.,Wei,Z.D.,Deng,H.W.,et al.,2006.A Studyon Paleogene Tectonic Sequences in Bozhong Sag.ChinaOffshore Oil and Gas,18(4):236-240(in Chinesewith English abstract).
Zhou,S.K.,Xu,C.G.,2006.One Kind of Important Deep-water Reservoir:The Longitudinal Gravity CurrentsSediments—A Case Study in Mingyuefeng Formation inLishui Sag,East China Sea Basin.Geological Scienceand Technology Information,25(5):57-62(in Chi-nese with English abstract).
Zhu,H.T.,Du,Y.S.,Liu,K.Y.,et al.,2008.SequenceStratigraphic Delineation and Correlation of the Dongy-ing Formation in the Nearshore and Adjacent Sea Are-as,Bohai Bay Basin.Earth Science—Journal of ChinaUniversity of Geosciences,19(1):54-64.
Zhu,H.T.,Yang,X.H.,Zhou,X.H.,et al.,2011.High Reso-lution Three-Dimensional Facies Architecture DelineationUsing Sequence Stratigraphy,Seismic Sedimentology:Ex-ample from Dongying Formation in BZ3-1Block of WesternSlope of Bozhong Sag,Bohai Bay Basin.Earth Science—Journal of China University of Geosciences,36(6):1073-1084(in Chinese with English abstract).
程日辉,朱德丰,王洪艳,等,2006.松辽盆地林甸断陷白垩纪沙河子期盆地次级构造单元与沉积体系.吉林大学学报(地球科学版),36(5):793-798.
池英柳,赵文智.2000.渤海湾盆地新生代走滑构造与油气聚集.石油学报,21(2):14-20.
褚庆忠,张树林,黄雄伟,2002.渤中坳陷断裂构造特征与油气运聚关系研究.新疆石油学院学报,14(2):9-13.
冯有良,徐秀生,2006.同沉积构造坡折带对岩性油气藏富集带的控制作用——以渤海湾盆地古近系为例.石油勘探与开发,33(1):22-25.
李虹,王立军,王凯,2001.辽河坳陷下第三系沙三段深断槽发育特点及其油气勘探意义.地球学报,22(5):437-440.
林畅松,张燕梅,李思田,等,2004.中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型.地球科学——中国地质大学学报,29(5):583-588.
漆家福,2007.裂陷盆地中的构造变换带及其石油地质意义.海相油气地质,12(4):43-50.
孙永河,漆家福,吕延防,等,2008.渤中坳陷断裂构造特征及其对油气的控制.石油学报,29(5):669-675.
万桂梅,汤良杰,周心怀,等,2009.渤中坳陷及邻区构造分带变形特征.海洋地质与第四纪地质,29(2):9-13.
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.
吴磊,徐怀民,季汉成,2006.渤海湾盆地渤中凹陷古近系沉积体系演化及物源分析.海洋地质与第四纪地质,26(1):81-88.
徐长贵,于水,林畅松,等,2008.渤海海域古近系湖盆边缘构造样式及其对沉积层序的控制作用.古地理学报,10(6):627-635.
徐亚军,杜远生,杨江海,2007.沉积物物源分析研究进展.地质科技情报,26(3):26-32.
余一欣,周心怀,魏刚,等,2008.渤海湾地区构造变换带及油气意义.古地理学报,10(5):555-560.
张建宁,于建国,2006.地震属性应用中的不确定性分析.石油物探,45(4):373-379.
赵国连,赵澄林,叶连俊,2005.渤海湾盆地“四扇一沟”沉积体系及其油气意义.地质力学学报,11(3):245-258.
赵国连,赵澄林,2002.渤中凹陷地震-沉积相研究.成都理工学院学报,29(1):41-48.
赵红格,刘池洋,2003.物源分析方法及研究进展.沉积学报,21(3):409-415.
周士科,魏泽典,邓宏文,等,2006.渤中凹陷古近系构造层序研究.中国海上油气,18(4):236-240.
周士科,徐长贵,2006.轴向重力流沉积:一种重要的深水储层—以东海盆地丽水凹陷明月峰组为例.地质科技情报,25(5):57-62.
朱红涛,杨香华,周心怀,等,2011.基于层序地层学和地震沉积学的高精度三维沉积体系:以渤中凹陷西斜坡BZ3-1区块东营组为例.地球科学——中国地质大学学报,36(6):1073-1084.
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