渤海湾盆地辽西低凸起传递斜坡构造特征与潜山油气聚集
摘要
传递斜坡是调节区域构造应变平衡的一类重要的构造样式。根据新的三维地震资料解释和断层位移-距离关系以及相干体切片分析,探讨了渤海湾盆地辽西低凸起传递斜坡的特征,并简要分析传递斜坡与潜山油气聚集的关系。地震剖面解释表明,辽西低凸起潜山带的传递斜坡连接辽西1号断层的下盘和辽西2号断层的上盘;在数据体相干切片上,辽西1号和2号断层呈清晰的侧接形态;而位移-距离关系显示,辽西1号断层的位移沿着断层走向自南向北逐渐传递到辽西2号断层,断层位移在传递斜坡内部基本保持守恒。传递斜坡对潜山油气聚集的意义主要表现在对储层形成和改造方面,优质储层发育是JZ25-1S潜山大油气田的重要成藏要素。
Relay ramp is an important structural style to accommodate regional strain balance.According to new 3-D seismic data interpretation,fault displacement-distance relation and seismic coherence slice analysis,this paper discussed some features of the relay ramp in Liaoxi low-uplift,Bohai bay basin,and briefly analyzed the relationship between relay ramp and hydrocarbon accumulation of buried-hill reservoir.The seismic profile interpretation indicates that the relay ramp of buried-hill belt in Liaoxi low-uplift connects footwall of Liaoxi No.1 fault and hangingwall of Liaoxi No.2 fault.On the seismic coherence slices,lateral connection with Liaoxi No.1 fault and Liaoxi No.2 fault is very clear.However,according to the fault displacement-distance relation,Liaoxi No.1 fault displacement is gradually transferred to Liaoxi No.2 fault along the faults strike.At the same time,this displacement is fundamental to maintain conservation in relay ramp.The relay ramp's significance for hydrocarbon accumulation is mainly exhibited in the formation and transformation of buried-hill reservoir.High quality reservoir is the material base of JZ25-1S buried-hill hydrocarbon reservoir.
Relay ramp is an important structural style to accommodate regional strain balance.According to new 3-D seismic data interpretation,fault displacement-distance relation and seismic coherence slice analysis,this paper discussed some features of the relay ramp in Liaoxi low-uplift,Bohai bay basin,and briefly analyzed the relationship between relay ramp and hydrocarbon accumulation of buried-hill reservoir.The seismic profile interpretation indicates that the relay ramp of buried-hill belt in Liaoxi low-uplift connects footwall of Liaoxi No.1 fault and hangingwall of Liaoxi No.2 fault.On the seismic coherence slices,lateral connection with Liaoxi No.1 fault and Liaoxi No.2 fault is very clear.However,according to the fault displacement-distance relation,Liaoxi No.1 fault displacement is gradually transferred to Liaoxi No.2 fault along the faults strike.At the same time,this displacement is fundamental to maintain conservation in relay ramp.The relay ramp's significance for hydrocarbon accumulation is mainly exhibited in the formation and transformation of buried-hill reservoir.High quality reservoir is the material base of JZ25-1S buried-hill hydrocarbon reservoir.
引文
[1]Jackson C A L,Gawthorpe R L,Sharp I A.Growth and linkageof the East Tanka fault zone,Suez rift:structural style and syn-rift stratigraphic response[J].Journal of the Geological Societyof London,2002,159:175-187.
[2]Segall P,Pollard D D.Mechanics of discontinuous faults[J].Journal of Geophysical Research,1980,85:4337-4350.
[3]Peacock D C P,Sanderson D J.Displacements,segment linkageand relay ramps in normal fault zones[J].Journal of StructuralGeology,1991,13:721-733.
[4]Cartwright J A,Mansfield C,Trudgill B.The growth of normalfaults by segment linkage[M]//Buchanan P G,Nieuwland DA.Modern Developments in Structural Geology,Interpretation,Validation and Modeling:Geological Society Special Publication.London:Geological Society of London,1996:163-177.
[5]Morley C K,Nelson R A,Patton T L,et al.Transfer zones inthe East African Rift System and their relevance to hydrocarbonexploration in rifts[J].Bulletin of the American Association ofPetroleum Geologists,1990,74:1234-1253.
[6]Peacock D C P,Sanderson D J.Geometry and development ofrelay ramps in normal fault systems[J].Bulletin of the Ameri-can Association of Petroleum Geologists,1994,78:147-165.
[7]Coskun B.Oil and gas fields—transfer zone relationships,ThraceBasin,NW Turkey[J].Marine and Petroleum Geology,1997,14:401-416.
[8]万天丰,王明明,殷秀兰,等.渤海湾不同方向断裂带的封闭性[J].现代地质,2004,18(2):157-164.
[9]付兆辉,高喜龙,陆友朋,等.渤海湾盆地垦东凸起构造特征与油气聚集[J].现代地质,2008,22(4):619-628.
[10]王家豪,王华,周海民,等.河北南堡凹陷老爷庙油田构造活动与油气富集[J].现代地质,2002,16(2):205-209.
[11]周建生,杨池银,陈发景,等.黄骅坳陷横向变换带的构造特征及成因[J].现代地质,1997,11(4):425-433.
[12]杨明慧,刘池阳,杨斌谊,等.冀中坳陷早第三纪的伸展构造[J].地质论评,2002,48(1):58-67.
[13]宗国洪,李常宝,孙红蕾.断裂体系中的调节带——以济阳坳陷为例[J].复式油气田,1995,6(3):7-10.
[14]孙思敏,彭仕宓,黄述旺.渤海湾盆地东濮凹陷横向调节带特征、成因及其区域分段作用[J].地质力学学报,2006,12(1):55-63.
[15]Hsiao LY,Stephan AG,Tilander N.Seismic reflection imagingof a major strike-slip fault zone in a rift system:Paleogene struc-ture and evolution of the Tan-Lu fault system,Liaodong Bay,Bo-hai,offshore China[J].Bulletin of the American Association ofPetroleum Geologists,2004,88:71-97.
[16]Nicol A,Watterson J,Walsh J J,et al.The shapes,major axisorientations and displacement patterns of fault surfaces[J].Journal of Structural Geology,1996,18:235-248.
[17]Manighetti I,King G C P,Gaudemer Y,et al.Slip accumula-tion and lateral propagation of active normal faults in Afar[J].Journal of Geophysical Research,2001,106:13667-13696.
[18]Hus R,De Batist M,Klerkx J,et al.Fault linkage in continen-tal rifts:structure and evolution of a large relay ramp in Zavarot-ny,Lake Baikal(Russia)[J].Journal of Structural Geology,2006,28:1338-1351.
[19]Yang Minghui,Zhou Xinhuai,Wei Gang,et al.Segment,link-age,and extensional fault-related fold in the western Liaodong baysubbasin,northeastern Bohai sea,China[J].Journal of ChinaUniversity of Geosciences,2008,19(6):602-610.
[20]杨明慧.渤海湾盆地变换构造特征及其成藏意义[J].石油学报,2009,30(6):816-823.
[21]项华,周心怀,魏刚,等.渤海海域锦州25-1南基岩古潜山油气成藏特征分析[J].石油天然气学报,2007,29(5):32-35.
[22]薛永安,项华,李思田.锦州25-1S大型混合花岗岩潜山油藏发现的启示[J].石油天然气学报,2006,28(3):29-31.
[23]吕丁友,杨明慧,周心怀,等.辽东湾坳陷辽西低凸起潜山构造特征与油气聚集[J].石油与天然气地质,2009,30(4):490-496.
[24]周心怀,项华,于水,等.渤海锦州南变质岩潜山油藏储集层特征与发育控制因素[J].石油勘探与开发,2005,32(6):17-20.
[25]刘乐,杨明慧,李春霞,等.辽西低凸起变质岩潜山裂缝储层及评价预测[J].石油与天然气地质,2009,30(2):188-194.
[2]Segall P,Pollard D D.Mechanics of discontinuous faults[J].Journal of Geophysical Research,1980,85:4337-4350.
[3]Peacock D C P,Sanderson D J.Displacements,segment linkageand relay ramps in normal fault zones[J].Journal of StructuralGeology,1991,13:721-733.
[4]Cartwright J A,Mansfield C,Trudgill B.The growth of normalfaults by segment linkage[M]//Buchanan P G,Nieuwland DA.Modern Developments in Structural Geology,Interpretation,Validation and Modeling:Geological Society Special Publication.London:Geological Society of London,1996:163-177.
[5]Morley C K,Nelson R A,Patton T L,et al.Transfer zones inthe East African Rift System and their relevance to hydrocarbonexploration in rifts[J].Bulletin of the American Association ofPetroleum Geologists,1990,74:1234-1253.
[6]Peacock D C P,Sanderson D J.Geometry and development ofrelay ramps in normal fault systems[J].Bulletin of the Ameri-can Association of Petroleum Geologists,1994,78:147-165.
[7]Coskun B.Oil and gas fields—transfer zone relationships,ThraceBasin,NW Turkey[J].Marine and Petroleum Geology,1997,14:401-416.
[8]万天丰,王明明,殷秀兰,等.渤海湾不同方向断裂带的封闭性[J].现代地质,2004,18(2):157-164.
[9]付兆辉,高喜龙,陆友朋,等.渤海湾盆地垦东凸起构造特征与油气聚集[J].现代地质,2008,22(4):619-628.
[10]王家豪,王华,周海民,等.河北南堡凹陷老爷庙油田构造活动与油气富集[J].现代地质,2002,16(2):205-209.
[11]周建生,杨池银,陈发景,等.黄骅坳陷横向变换带的构造特征及成因[J].现代地质,1997,11(4):425-433.
[12]杨明慧,刘池阳,杨斌谊,等.冀中坳陷早第三纪的伸展构造[J].地质论评,2002,48(1):58-67.
[13]宗国洪,李常宝,孙红蕾.断裂体系中的调节带——以济阳坳陷为例[J].复式油气田,1995,6(3):7-10.
[14]孙思敏,彭仕宓,黄述旺.渤海湾盆地东濮凹陷横向调节带特征、成因及其区域分段作用[J].地质力学学报,2006,12(1):55-63.
[15]Hsiao LY,Stephan AG,Tilander N.Seismic reflection imagingof a major strike-slip fault zone in a rift system:Paleogene struc-ture and evolution of the Tan-Lu fault system,Liaodong Bay,Bo-hai,offshore China[J].Bulletin of the American Association ofPetroleum Geologists,2004,88:71-97.
[16]Nicol A,Watterson J,Walsh J J,et al.The shapes,major axisorientations and displacement patterns of fault surfaces[J].Journal of Structural Geology,1996,18:235-248.
[17]Manighetti I,King G C P,Gaudemer Y,et al.Slip accumula-tion and lateral propagation of active normal faults in Afar[J].Journal of Geophysical Research,2001,106:13667-13696.
[18]Hus R,De Batist M,Klerkx J,et al.Fault linkage in continen-tal rifts:structure and evolution of a large relay ramp in Zavarot-ny,Lake Baikal(Russia)[J].Journal of Structural Geology,2006,28:1338-1351.
[19]Yang Minghui,Zhou Xinhuai,Wei Gang,et al.Segment,link-age,and extensional fault-related fold in the western Liaodong baysubbasin,northeastern Bohai sea,China[J].Journal of ChinaUniversity of Geosciences,2008,19(6):602-610.
[20]杨明慧.渤海湾盆地变换构造特征及其成藏意义[J].石油学报,2009,30(6):816-823.
[21]项华,周心怀,魏刚,等.渤海海域锦州25-1南基岩古潜山油气成藏特征分析[J].石油天然气学报,2007,29(5):32-35.
[22]薛永安,项华,李思田.锦州25-1S大型混合花岗岩潜山油藏发现的启示[J].石油天然气学报,2006,28(3):29-31.
[23]吕丁友,杨明慧,周心怀,等.辽东湾坳陷辽西低凸起潜山构造特征与油气聚集[J].石油与天然气地质,2009,30(4):490-496.
[24]周心怀,项华,于水,等.渤海锦州南变质岩潜山油藏储集层特征与发育控制因素[J].石油勘探与开发,2005,32(6):17-20.
[25]刘乐,杨明慧,李春霞,等.辽西低凸起变质岩潜山裂缝储层及评价预测[J].石油与天然气地质,2009,30(2):188-194.
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