塔里木盆地巴楚隆起西段边界断层联接及变形特征
摘要
在前人研究的基础上,利用最新的地震和钻井资料,分析了巴楚隆起西段与麦盖提斜坡过渡区色力布亚、康塔库木两条边界断层的构造特征.色力布亚和康塔库木断层均表现为基底卷入型逆冲断层,两条断层之间通过软联接的形式发生相互作用.色力布亚断层沿其走向往南东方向位移量逐渐减小并终止,康塔库木断层沿其走向往南东方向位移量逐渐增大.构造转换带传递了色力布亚断层和康塔库木断层的位移量,使巴楚隆起西段边界断层总位移量保持一致.该转换带属于同向倾斜型构造转换带,现今处于转换带复杂阶段.转换带内发育次级断层和走向裂缝,有利于形成裂缝型油气藏,也是油气运移的有利通道,是巴楚地区未来油气勘探的重要目标.
Based on the interpretation of the new drilling and seismic data,the structural characteristics of the Selibuya fault and Kangtakumu fault,which are the boundary faults between the western Bachu uplift and Maigaiti slope,are analyzed in this paper.The Selibuya and Kangtakumu faults are basement-involved thrust faults interacting by soft-linkage.Along the SE strike,the displacement of the Selibuya fault gradually decreases,while the displacement of the Kangtakumu fault increases.The transform zone between the two faults transferred their displacements,and kept the conservation of fault displacements in western part of the Bachu Uplift.The transform zone belongs to the synthetic overlapping zone which is in the evolution stage of complex.There are much secondary faults and fractures,which is good basis for the formation of fractured-type reservoirs and hydrocarbon migration.The transform zone is the favorable objective for petroleum exploration in the Bachu area.
Based on the interpretation of the new drilling and seismic data,the structural characteristics of the Selibuya fault and Kangtakumu fault,which are the boundary faults between the western Bachu uplift and Maigaiti slope,are analyzed in this paper.The Selibuya and Kangtakumu faults are basement-involved thrust faults interacting by soft-linkage.Along the SE strike,the displacement of the Selibuya fault gradually decreases,while the displacement of the Kangtakumu fault increases.The transform zone between the two faults transferred their displacements,and kept the conservation of fault displacements in western part of the Bachu Uplift.The transform zone belongs to the synthetic overlapping zone which is in the evolution stage of complex.There are much secondary faults and fractures,which is good basis for the formation of fractured-type reservoirs and hydrocarbon migration.The transform zone is the favorable objective for petroleum exploration in the Bachu area.
引文
Davis,K.,Burbank,D.W.,Fisher,D.,et al.,2005.Thrust-FaultGrowth and Segment Linkage in the Active Ostler FaultZone,New Zealand.JournalofStructuralGeology,27(6):1528-1546.doi:10.1016/j.jsg.2005.04.011
Guan,S.W.,Wang,X.,Yang,S.F.,et al.,2004.Two ConceptModels of Displacement Transfer and Examples.Science inChina(Ser.D),34(9):807-817(in Chinese).
He,W.Y.,Li,J.H.,Qian,X.L.,et al.,2000.The Meso-Cenozoic Evolution of Bachu Fault-Uplift in Tarim Ba-sin.Acta Scientiarum Naturalium,36(4):539-546(in Chinese with English abstract).
Higgins,S.,Davies,R.J.,Clarke,B.,2007.Antithetic FaultLinkages in a Deep Water Fold and Thrust Belt.Jour-nal of Structural Geology,29(12):1900-1914.doi:10.1016/j.jsg.2007.09.004
Hus,R.,Batist,M.D.,Klerkx,J.,et al.,2006.Fault Link-age in Continental Rifts:Structure and Evolution of aLarge Relay Ramp in Zavarotny;Lake Baikal(Russia).Journal of Structural Geology,28(5):1338-1351.doi:10.1016/j.jsg.2006.03.031
Kim,Y.S.,Peacock,D.C.P.,Sanderson,D.J.,2004.FaultDamage Zones.Journal of Structural Geology,26(1):503-517.doi:10.1016/j.jsg.2003.08.002
Kim,Y.S.,Sanderson,D.J.,2005.The Relationship be-tween Displacement and Length of Faults:A Review.Earth Science Reviews,68(3-4):317-334.doi:10.1016/j.earscirev.2004.06.003
Meng,Q.L.,Li,Y.J.,Shi,J.,et al.,2008.Main Charactersand Active Ages of the Serikbuya and Kangxi Faults inthe Western Tarim Basin.Chinese Journal of Geology,43(2):282-293(in Chinese with English abstract).
Ning,F.,Tang,L.J.,Zhu,C.L.,et al.,2009.Types of Structural Transfer Zone in Compressional Area and ItsSignificance of Petroleum Geology.Geoscience,23(3):394-400(in Chinese with English abstract).
Ravaglia,A.,Turrini,C.,Seno,S.,2004.Mechanical Stratig-raphy as a Factor Controlling the Development of aSandbox Transfer Zone:A Three-Dimensional Analy-sis.Journal of Structural Geology,26(12):2269-2283.doi:10.1016/j.jsg.2004.04.009
Ren,J.Y.,Zhang,J.X.,Yang,H.Z.,et al.,2011.Analysisof Fault Systems in the Central Uplift Tarim Basin.Ac-ta Petrologica Sinica,27(1):219-230(in Chinesewith English abstract).
Rotevatn,A.,Fossen,H.,2011.Simulating the Effect ofSubseismic Fault Tails and Process Zones in a Siliciclas-tic Reservoir Analogue:Implications for Aquifer Sup-port and Trap Definition.Marine and Petroleum Geolo-gy,28(7):1648-1662.doi:10.1016/j.marpetgeo.2011.07.005
She,X.Y.,Shi,Z.J.,Liu,G.B.,et al.,2004.MigrationPathway of Hydrocarbon Dynamic Accumulation in Ba-chu-Markit Area,Xinjiang,China.Jouranal of ChenduUniversity of Technology(Science&Technology Edi-tion),31(3):291-296(in Chinese with English ab-stract).
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,S.M.,Peng,S.M.,Wang,X.W.,et al.,2003.The Charac-teristic of Relay Ramps in Fault System of the Placanticlinein Dongpu Sag and Their Relevance to Hydrocarbon Explo-ration.Petroleum Exploration and Development,30(1):22-24(in Chinese with English abstract).
Wang,H.Y.,Fan,T.L.,Wei,F.J.,et al.,2004.Develop-mental Characterististics of Cambrian Subsalt Struc-tures in Central Bachu Area,Tarim Basin.Oil&GasGeology,25(5):554-557(in Chinese with English ab-stract).
Xiao,A.C.,Yang,S.F.,Li,Y.J.,et al.,2005.Mian Periodfor Creation of Fracture System in The Bachu Uplift,Tarim Basin.Chinese Journal of Geology,40(2):291-302(in Chinese with English abstract).
Yang,M.H.,Jin,Z.J.,Lv,X.X.,et al.,2007.Basement-Involved Transpressional Structure and the Formationof the Bachu Uplift,Tarim Basin,Northwestern China.Acta Geologica Sinica,81(2):158-165(in Chinesewith English abstract).
Yu,Y.X.,Zhou,X.H.,Tang,L.J.,et al.,2009.Linkage of Normal and Transfer Zones in the Liaodongwan De-pression,Offshore Bohai Bay Basin.Geological Review,55(1):79-83(in Chinese with English abstract).
Zhang,G.Y.,1997.Tectionic Transfer Style and Its Originin Northern Tarim Basin.Geoscience,11(4):453-459(in Chinese with English abstract).
Zhang,Q.L.,Hou,G.Y.,Pan,W.Q.,et al.,2010.Develop-ment of Fractures in Carbonate Rocks under the Influ-ence of Strike-Slip Faults in Bachu Area,Xinjiang,Chi-na.Geological Bulletin of China,29(8):1160-1167(in Chinese with English abstract).
管树巍,汪新,杨树锋,等,2004.位移转换的两种概念模型与实例.中国科学(D辑),34(9):807-817.
何文渊,李江海,钱祥麟,等,2000.塔里木盆地巴楚断隆中新生代的构造演化.北京大学学报(自然科学版),36(4):539-546.
孟庆龙,李曰俊,师骏,等,2008.塔里木盆地西部色力布亚断裂和康西断裂的主要特征及活动时代.地质科学,43(2):282-293.
宁飞,汤良杰,朱传玲,等,2009.挤压区局部构造转换带类型及石油地质意义.现代地质,23(3):394-400.
任建业,张俊霞,阳怀忠,等,2011.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219-230.
佘晓宇,施泽进,刘高波,等,2004.巴楚-麦盖提地区油气动态成藏的运移通道.成都理工大学学报(自然科学版),31(3):291-296.
孙思敏,彭仕宓,汪新文,等,2003.东濮凹陷长垣断层系中转换斜坡的特征与油气勘探.石油勘探与开发,30(1):22-24.
王宏语,樊太亮,魏福军,等,2004.塔里木盆地巴楚中部地区寒武系盐下构造发育特征.石油与天然气地质,25(5):554-557.
肖安成,杨树锋,李曰俊,等,2005.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识.地质科学,40(2):291-302.
杨明慧,金之钧,吕修祥,等,2007.塔里木盆地基底卷入扭压构造与巴楚隆起的形成.地质学报,81(2):158-165.
余一欣,周心怀,汤良杰,等,2009.渤海海域辽东湾坳陷正断层联接及其转换带特征.地质评论,55(1):79-83.
张光亚,1997.塔里木盆地北部构造转换形式及其成因.现代地质,11(4):453-459.
张庆莲,侯贵廷,潘文庆,等,2010.新疆巴楚地区走滑断裂对碳酸盐岩构造裂缝发育的控制.地质通报,29(8):1160-1167.
Guan,S.W.,Wang,X.,Yang,S.F.,et al.,2004.Two ConceptModels of Displacement Transfer and Examples.Science inChina(Ser.D),34(9):807-817(in Chinese).
He,W.Y.,Li,J.H.,Qian,X.L.,et al.,2000.The Meso-Cenozoic Evolution of Bachu Fault-Uplift in Tarim Ba-sin.Acta Scientiarum Naturalium,36(4):539-546(in Chinese with English abstract).
Higgins,S.,Davies,R.J.,Clarke,B.,2007.Antithetic FaultLinkages in a Deep Water Fold and Thrust Belt.Jour-nal of Structural Geology,29(12):1900-1914.doi:10.1016/j.jsg.2007.09.004
Hus,R.,Batist,M.D.,Klerkx,J.,et al.,2006.Fault Link-age in Continental Rifts:Structure and Evolution of aLarge Relay Ramp in Zavarotny;Lake Baikal(Russia).Journal of Structural Geology,28(5):1338-1351.doi:10.1016/j.jsg.2006.03.031
Kim,Y.S.,Peacock,D.C.P.,Sanderson,D.J.,2004.FaultDamage Zones.Journal of Structural Geology,26(1):503-517.doi:10.1016/j.jsg.2003.08.002
Kim,Y.S.,Sanderson,D.J.,2005.The Relationship be-tween Displacement and Length of Faults:A Review.Earth Science Reviews,68(3-4):317-334.doi:10.1016/j.earscirev.2004.06.003
Meng,Q.L.,Li,Y.J.,Shi,J.,et al.,2008.Main Charactersand Active Ages of the Serikbuya and Kangxi Faults inthe Western Tarim Basin.Chinese Journal of Geology,43(2):282-293(in Chinese with English abstract).
Ning,F.,Tang,L.J.,Zhu,C.L.,et al.,2009.Types of Structural Transfer Zone in Compressional Area and ItsSignificance of Petroleum Geology.Geoscience,23(3):394-400(in Chinese with English abstract).
Ravaglia,A.,Turrini,C.,Seno,S.,2004.Mechanical Stratig-raphy as a Factor Controlling the Development of aSandbox Transfer Zone:A Three-Dimensional Analy-sis.Journal of Structural Geology,26(12):2269-2283.doi:10.1016/j.jsg.2004.04.009
Ren,J.Y.,Zhang,J.X.,Yang,H.Z.,et al.,2011.Analysisof Fault Systems in the Central Uplift Tarim Basin.Ac-ta Petrologica Sinica,27(1):219-230(in Chinesewith English abstract).
Rotevatn,A.,Fossen,H.,2011.Simulating the Effect ofSubseismic Fault Tails and Process Zones in a Siliciclas-tic Reservoir Analogue:Implications for Aquifer Sup-port and Trap Definition.Marine and Petroleum Geolo-gy,28(7):1648-1662.doi:10.1016/j.marpetgeo.2011.07.005
She,X.Y.,Shi,Z.J.,Liu,G.B.,et al.,2004.MigrationPathway of Hydrocarbon Dynamic Accumulation in Ba-chu-Markit Area,Xinjiang,China.Jouranal of ChenduUniversity of Technology(Science&Technology Edi-tion),31(3):291-296(in Chinese with English ab-stract).
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,S.M.,Peng,S.M.,Wang,X.W.,et al.,2003.The Charac-teristic of Relay Ramps in Fault System of the Placanticlinein Dongpu Sag and Their Relevance to Hydrocarbon Explo-ration.Petroleum Exploration and Development,30(1):22-24(in Chinese with English abstract).
Wang,H.Y.,Fan,T.L.,Wei,F.J.,et al.,2004.Develop-mental Characterististics of Cambrian Subsalt Struc-tures in Central Bachu Area,Tarim Basin.Oil&GasGeology,25(5):554-557(in Chinese with English ab-stract).
Xiao,A.C.,Yang,S.F.,Li,Y.J.,et al.,2005.Mian Periodfor Creation of Fracture System in The Bachu Uplift,Tarim Basin.Chinese Journal of Geology,40(2):291-302(in Chinese with English abstract).
Yang,M.H.,Jin,Z.J.,Lv,X.X.,et al.,2007.Basement-Involved Transpressional Structure and the Formationof the Bachu Uplift,Tarim Basin,Northwestern China.Acta Geologica Sinica,81(2):158-165(in Chinesewith English abstract).
Yu,Y.X.,Zhou,X.H.,Tang,L.J.,et al.,2009.Linkage of Normal and Transfer Zones in the Liaodongwan De-pression,Offshore Bohai Bay Basin.Geological Review,55(1):79-83(in Chinese with English abstract).
Zhang,G.Y.,1997.Tectionic Transfer Style and Its Originin Northern Tarim Basin.Geoscience,11(4):453-459(in Chinese with English abstract).
Zhang,Q.L.,Hou,G.Y.,Pan,W.Q.,et al.,2010.Develop-ment of Fractures in Carbonate Rocks under the Influ-ence of Strike-Slip Faults in Bachu Area,Xinjiang,Chi-na.Geological Bulletin of China,29(8):1160-1167(in Chinese with English abstract).
管树巍,汪新,杨树锋,等,2004.位移转换的两种概念模型与实例.中国科学(D辑),34(9):807-817.
何文渊,李江海,钱祥麟,等,2000.塔里木盆地巴楚断隆中新生代的构造演化.北京大学学报(自然科学版),36(4):539-546.
孟庆龙,李曰俊,师骏,等,2008.塔里木盆地西部色力布亚断裂和康西断裂的主要特征及活动时代.地质科学,43(2):282-293.
宁飞,汤良杰,朱传玲,等,2009.挤压区局部构造转换带类型及石油地质意义.现代地质,23(3):394-400.
任建业,张俊霞,阳怀忠,等,2011.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219-230.
佘晓宇,施泽进,刘高波,等,2004.巴楚-麦盖提地区油气动态成藏的运移通道.成都理工大学学报(自然科学版),31(3):291-296.
孙思敏,彭仕宓,汪新文,等,2003.东濮凹陷长垣断层系中转换斜坡的特征与油气勘探.石油勘探与开发,30(1):22-24.
王宏语,樊太亮,魏福军,等,2004.塔里木盆地巴楚中部地区寒武系盐下构造发育特征.石油与天然气地质,25(5):554-557.
肖安成,杨树锋,李曰俊,等,2005.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识.地质科学,40(2):291-302.
杨明慧,金之钧,吕修祥,等,2007.塔里木盆地基底卷入扭压构造与巴楚隆起的形成.地质学报,81(2):158-165.
余一欣,周心怀,汤良杰,等,2009.渤海海域辽东湾坳陷正断层联接及其转换带特征.地质评论,55(1):79-83.
张光亚,1997.塔里木盆地北部构造转换形式及其成因.现代地质,11(4):453-459.
张庆莲,侯贵廷,潘文庆,等,2010.新疆巴楚地区走滑断裂对碳酸盐岩构造裂缝发育的控制.地质通报,29(8):1160-1167.
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