梁家—万昌地区同沉积断层对奢岭组沉积的控制作用
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摘要
陆相盆地油气勘探表明,同沉积断层对沉积体的分布具有明显的控制作用。伊通盆地为一走滑为主的盆地,其中始新世西北缘边界断层的右旋走滑运动控制了盆地的形成和演化,走滑运动必然会在盆内派生出一系列次级伸展断层。本文从西北缘走滑断裂活动时间、走滑派生的次级断层的展布及活动时间等方面对同沉积断层进行剖析;同时阐述了同沉积断层对沉积的控制作用,得出三点结论:①盆内边界断层的走滑控制了盆内次级伸展断层的分布特征及活动时间;②分布于万昌围斜带的同沉积断层对沉积体主要起疏导作用,沉积体沿着同沉积断层之间夹持的地带沉积;③分布在梁家地区的同沉积断层控制了沉积体的分布范围,沉积体基本不越过同沉积断层的上升盘进行沉积。
Global exploration of oil and gas in continental basins has already indicated that contemporaneous faults have significant effects on the distribution of depositional body.The research of oil and gas exploration shows that Yitong Basin has been implied to be a strike-slip fault basin.Basin formation and evolution are controlled by the dextral rotation and strike-slip movement of the boundary fault in the northwestern margin of the Eocene.Strike-slip movement is bound to derive a series of contemporaneous fault in the basin.From the aspect of strike-slip fault active time in the northwest edge,distribution and activity time of the secondary faults derived from strike-slip movement,this paper determines the contemporaneous fault and also analyzes its controlling action on the deposition.Three conclusions made are stated below.①The strike-slip movement of boundary faults controls the distribution and active time of secondary tensile faults in the basin.②The contemporaneous fault located in Wanchang slope area has a leading control on the depositional bodies which are deposited along clamp zone between the contemporaneous faults.③The contemporaneous faults located in Liangjia district control the distribution of depositional bodies.Depositional bodies basically do not cross over the upthrow of contemporaneous faults in the deposition process.
Global exploration of oil and gas in continental basins has already indicated that contemporaneous faults have significant effects on the distribution of depositional body.The research of oil and gas exploration shows that Yitong Basin has been implied to be a strike-slip fault basin.Basin formation and evolution are controlled by the dextral rotation and strike-slip movement of the boundary fault in the northwestern margin of the Eocene.Strike-slip movement is bound to derive a series of contemporaneous fault in the basin.From the aspect of strike-slip fault active time in the northwest edge,distribution and activity time of the secondary faults derived from strike-slip movement,this paper determines the contemporaneous fault and also analyzes its controlling action on the deposition.Three conclusions made are stated below.①The strike-slip movement of boundary faults controls the distribution and active time of secondary tensile faults in the basin.②The contemporaneous fault located in Wanchang slope area has a leading control on the depositional bodies which are deposited along clamp zone between the contemporaneous faults.③The contemporaneous faults located in Liangjia district control the distribution of depositional bodies.Depositional bodies basically do not cross over the upthrow of contemporaneous faults in the deposition process.
引文
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[5]唐大卿,何生,陈红汉等.伊通盆地断裂体系特征及其演化历史.吉林大学学报(地球科学版),2009,39(3):386～396Tang Daqing,He Sheng,Chen Honghan et al.Faultsystem′s characteristics of Yitong basin and its evolu-tion.Journal of Jilin University(Earth Science Edi-tion),2009,39(3):386～396
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[9]王剑,徐翔军,陈秀艳等.伊通地堑岔路河断陷南段构造—沉积特征与油气藏类型.世界地质,2007,26(2):240～244Wang Jian,Xu Xiangjun,Chen Xiuyan et al.Structu-ral and sedimentary features and types of hydrocar-bon reservoir in southern Chaluhe fault depression ofYitong Graben.Global Geology,2007,26(2):240～244
[10]梁富康,于兴河,李先平等.冀中坳陷深县凹陷的生长断层特点及其对沉积的控制作用.中国地质,2011,38(2):263～270Liang Fukang,Yu Xinghe,Li Xianping et al.Growthfaults in Shenxian depression and their control overthe sedimentation.Geology in China,2011,38(2):263～270
[11]石万忠,孔敏,宋志峰.伊通盆地梁家地区奢岭组混源扇三角洲内幕结构.地球科学——中国地质大学学报,2008,33(3):365～370Shi Wanzhong,Kong Min,Song Zhifeng.Multi-prov-enance fan delta in the Sheling Formation,LiangjiaArea,Yitong Basin,China.Earth Science(Journal ofChina University of Geosciences),2008,33(3):365～370
[12]李本才,孙凯,白洪彬等.伊通盆地层序地层格架与层序构成分析.岩性油气藏,2009,21(4):28～31Li Bencai,Sun Kai,Bai Hongbin et al.Sequence stra-tigraphic framework and sequence components of theYitong Basin.Lithologic Reservoirs,2009,21(4):28～31
[13]唐大卿,陈红汉,孙家振等.郯庐断裂带伊通段新生代构造演化特征及其控盆机制.大地构造与成矿学,2010,34(3):340～348Tang Daqing,Chen Honghan,Sun Jiazhen et al.Ce-nozoic tectonic evolution of the Yitong part of the TanLu Fault zone and its control on Yitong Basin.Geo-tectonica Et Metallogenia,2010,34(3):340～348
[14]李献甫,陈全茂,张学海等.伊通地堑一走滑断陷盆地的构造特征及演化.石油实验地质,2002,24(1):19～24Li Xianfu,Chen Quanmao,Zhang Xuehai et al.TheYitong graben-the structural features and evolutionof a strike-slip fault basin.Petroleum Geology&Ex-periment,2002,24(1):19～24
[15]丁增勇,王良书,钟铠等.渤海湾盆地新生界残留地层分布特征及其构造意义.高校地质学报,2008,14(3):405～413Ding Zengyong,Wang Liangshu,Zhong Kai et al.Distribution characteristics and tectonic significance ofCenozoic remnant formation,BaHai Bay Basin.Geo-logical Journal of China Universities,2008,14(3):405～413
[16]池英柳,赵文智.渤海湾盆地新生代走滑构造与油气聚集.石油学报,2000,21(2):14～20Chi Yingliu,Zhao Wenzhi.Strike-slip deformationduring the Cenozoic and its influence on hydrocarbonaccumulation in the BoHai bay basin.Acta PetroleiSinica,2000,21(2):14～20
[17]张亚敏,刘池洋,王婧韫.M盆地走滑特征与油气富集规律.西北大学学报(自然科学版),2002,32(3):275～280Zhang Yamin,Liu Chiyang,Wang Jingyun et al.Stike-slip characteristics and hydrocarbon accumula-tion of M basin.Journal of Northwest University(Natural Science Edition),2002,32(3):275～280
[18]吴根耀,马力,里群等.继承性构造与新生构造并存的时空发育特征——“盆”“山”耦合理论指导油气勘探的一个切入点.石油实验地质,2010,32(1):1～9Wu Genyao,Ma Li,Li Qun et al.Time-spatial devel-oping features of co-existed inherited and neogenicstructures.Petroleum Geology&Experiment,2010,32(1):1～9
[19]刘力辉,王绪本.双域、双面沉积体解释方法在L区的应用.石油物探,2011,50(2):155～159Liu Lihui,Wang Xuben.Application of double-do-main and double-plane interpretation method on sedi-mentary bodies in L block.GPP,2011,50(2):155～159
[20]廖瑞君.江西吉安—泰和陆相红色盆地沉积体研究.中国区域地质,2000,19(2):181～186Liao Ruijun.Study on sedimentary deposits in the redcontinental basin of Ji’an-Taihe,Jiangxi.RegionalGeology of China,2000,19(2):181～186
[21]Shi Wanzhong,Zhao Zhikui,Jiang Tao et al.Identi-fying updip pinch-out sandstone in nearshore suba-queous fans using acoustic impedance and the instan-taneous phase in the Liangjia area,Yitong Basin,Chi-na.Marine and Petroleum Geology,2012,30:32～42
[22]Nath S K,Dewangan P.Detection of seismic reflec-tions from seismic attributes through fractal analysis.Geophysical Prospecting,2002,50(3):341～360
[23]Chen Q,Sideney S.Seismic attribute technology forreservoir forecasting and monitoring.The LeadingEdge,1997,16(5):445～456
[24]Zahrani A A,Neves F.Interpretation and mapping ofa stratigraphic play using 3Dseismic data and attrib-utes in central Saudi Arabia.Petroleum Geoscience,2008,14(3):245～251
[25]Gao J,Wang J M,Yun M H.Seismic attributes opti-mization and application in reservoir predication.App-lied Geophysics,2006,3(4):243～247
[26]李明,侯连华,邹才能等.岩性地层油气藏地球物理勘探技术与应用.北京:石油工业出版社,2005:52～146
[27]于京波,潘红卫,郭增虎.松辽盆地南部岩性圈闭识别技术及效果.石油地球物理勘探,2006,41(增刊):57～61Yu Jingbo,Pan Hongwei,Guo Zenghu.Identificationof lithologic traps in south Songliao basin and effects.OGP,2006,41(Sup):57～61
[28]张立恩,陈少峰,姜继莲等.MT法在地热勘探中的应用.石油地球物理勘探,2004,39(增刊):66～70Zhang Lien,Chen Shaofeng,Jiang Jilian et al.Appli-cations of MT method for geothermal exploration.OGP,2004,39(Sup):66～70
[29]魏小东,张延庆,曹丽丽等.地震资料振幅谱梯度属性在WC地区储层评价中的应用.石油地球物理勘探,2011,46(2):281～284Wei Xiaodong,Zhang Yanqing,Cao Lili et al.Appli-cations of amplitude spectrum gradient for reservoirevaluation in WC project.OGP,2011,46(2):281～284
[2]Yu Zhaohua,Wu Shiguo,Zou Dongbo et al.Seismicprofiles across the middle Tan-Lu fault zone inLaizhou Bay,Bohai Sea,Eastern China.Journal ofAsian Earth Sciences,2008,33(5,6):383～394
[3]江涛,邱玉超,宋立斌等.伊通盆地西北缘断裂带的性质.现代地质,2009,23(5):860～864Jiang Tao,Qiu Yuchao,Song Libin et al.Fault natureof North-West fault zone in Yitong basin and its rela-tion with reservoir accumulation.Geoscience,2009,23(5):860～864
[4]童亨茂.伊通地堑边界断裂的性质与演化.地质力学学报,2002,8(1):35～42Tong Hengmao.The property and evolution ofboundary faults of Yitong graben.Journal of Geome-chanics,2002,8(1):35～42
[5]唐大卿,何生,陈红汉等.伊通盆地断裂体系特征及其演化历史.吉林大学学报(地球科学版),2009,39(3):386～396Tang Daqing,He Sheng,Chen Honghan et al.Faultsystem′s characteristics of Yitong basin and its evolu-tion.Journal of Jilin University(Earth Science Edi-tion),2009,39(3):386～396
[6]唐大卿,何生,陈红汉等.伊通盆地新近纪以来的反转构造特征.石油学报,2009,30(4):506～512Tang Daqing,He Sheng,Chen Honghan et al.Char-acteristics of inversion structures in Yitong Basinsince Neogene.Acta Petrolei Sinica,2009,30(4):506～512
[7]王燮培,费琪,张家骅.石油勘探构造分析.中国地质大学出版社,1990:132～139
[8]王旭丽,周江羽,马良等.伊通盆地岔路河断陷重力流沉积特征及油气勘探意义.石油实验地质,2008,30(1):26～31Wang Xuli,Zhou Jiangyu,Ma Liang et al.Gravityflow sedimentary characteristics and the significanceof petroleum exploration in the Chaluhe fault depres-sion,the Yitong basin.Petroleum Geology&Expe-riment,2008,30(1):26～31
[9]王剑,徐翔军,陈秀艳等.伊通地堑岔路河断陷南段构造—沉积特征与油气藏类型.世界地质,2007,26(2):240～244Wang Jian,Xu Xiangjun,Chen Xiuyan et al.Structu-ral and sedimentary features and types of hydrocar-bon reservoir in southern Chaluhe fault depression ofYitong Graben.Global Geology,2007,26(2):240～244
[10]梁富康,于兴河,李先平等.冀中坳陷深县凹陷的生长断层特点及其对沉积的控制作用.中国地质,2011,38(2):263～270Liang Fukang,Yu Xinghe,Li Xianping et al.Growthfaults in Shenxian depression and their control overthe sedimentation.Geology in China,2011,38(2):263～270
[11]石万忠,孔敏,宋志峰.伊通盆地梁家地区奢岭组混源扇三角洲内幕结构.地球科学——中国地质大学学报,2008,33(3):365～370Shi Wanzhong,Kong Min,Song Zhifeng.Multi-prov-enance fan delta in the Sheling Formation,LiangjiaArea,Yitong Basin,China.Earth Science(Journal ofChina University of Geosciences),2008,33(3):365～370
[12]李本才,孙凯,白洪彬等.伊通盆地层序地层格架与层序构成分析.岩性油气藏,2009,21(4):28～31Li Bencai,Sun Kai,Bai Hongbin et al.Sequence stra-tigraphic framework and sequence components of theYitong Basin.Lithologic Reservoirs,2009,21(4):28～31
[13]唐大卿,陈红汉,孙家振等.郯庐断裂带伊通段新生代构造演化特征及其控盆机制.大地构造与成矿学,2010,34(3):340～348Tang Daqing,Chen Honghan,Sun Jiazhen et al.Ce-nozoic tectonic evolution of the Yitong part of the TanLu Fault zone and its control on Yitong Basin.Geo-tectonica Et Metallogenia,2010,34(3):340～348
[14]李献甫,陈全茂,张学海等.伊通地堑一走滑断陷盆地的构造特征及演化.石油实验地质,2002,24(1):19～24Li Xianfu,Chen Quanmao,Zhang Xuehai et al.TheYitong graben-the structural features and evolutionof a strike-slip fault basin.Petroleum Geology&Ex-periment,2002,24(1):19～24
[15]丁增勇,王良书,钟铠等.渤海湾盆地新生界残留地层分布特征及其构造意义.高校地质学报,2008,14(3):405～413Ding Zengyong,Wang Liangshu,Zhong Kai et al.Distribution characteristics and tectonic significance ofCenozoic remnant formation,BaHai Bay Basin.Geo-logical Journal of China Universities,2008,14(3):405～413
[16]池英柳,赵文智.渤海湾盆地新生代走滑构造与油气聚集.石油学报,2000,21(2):14～20Chi Yingliu,Zhao Wenzhi.Strike-slip deformationduring the Cenozoic and its influence on hydrocarbonaccumulation in the BoHai bay basin.Acta PetroleiSinica,2000,21(2):14～20
[17]张亚敏,刘池洋,王婧韫.M盆地走滑特征与油气富集规律.西北大学学报(自然科学版),2002,32(3):275～280Zhang Yamin,Liu Chiyang,Wang Jingyun et al.Stike-slip characteristics and hydrocarbon accumula-tion of M basin.Journal of Northwest University(Natural Science Edition),2002,32(3):275～280
[18]吴根耀,马力,里群等.继承性构造与新生构造并存的时空发育特征——“盆”“山”耦合理论指导油气勘探的一个切入点.石油实验地质,2010,32(1):1～9Wu Genyao,Ma Li,Li Qun et al.Time-spatial devel-oping features of co-existed inherited and neogenicstructures.Petroleum Geology&Experiment,2010,32(1):1～9
[19]刘力辉,王绪本.双域、双面沉积体解释方法在L区的应用.石油物探,2011,50(2):155～159Liu Lihui,Wang Xuben.Application of double-do-main and double-plane interpretation method on sedi-mentary bodies in L block.GPP,2011,50(2):155～159
[20]廖瑞君.江西吉安—泰和陆相红色盆地沉积体研究.中国区域地质,2000,19(2):181～186Liao Ruijun.Study on sedimentary deposits in the redcontinental basin of Ji’an-Taihe,Jiangxi.RegionalGeology of China,2000,19(2):181～186
[21]Shi Wanzhong,Zhao Zhikui,Jiang Tao et al.Identi-fying updip pinch-out sandstone in nearshore suba-queous fans using acoustic impedance and the instan-taneous phase in the Liangjia area,Yitong Basin,Chi-na.Marine and Petroleum Geology,2012,30:32～42
[22]Nath S K,Dewangan P.Detection of seismic reflec-tions from seismic attributes through fractal analysis.Geophysical Prospecting,2002,50(3):341～360
[23]Chen Q,Sideney S.Seismic attribute technology forreservoir forecasting and monitoring.The LeadingEdge,1997,16(5):445～456
[24]Zahrani A A,Neves F.Interpretation and mapping ofa stratigraphic play using 3Dseismic data and attrib-utes in central Saudi Arabia.Petroleum Geoscience,2008,14(3):245～251
[25]Gao J,Wang J M,Yun M H.Seismic attributes opti-mization and application in reservoir predication.App-lied Geophysics,2006,3(4):243～247
[26]李明,侯连华,邹才能等.岩性地层油气藏地球物理勘探技术与应用.北京:石油工业出版社,2005:52～146
[27]于京波,潘红卫,郭增虎.松辽盆地南部岩性圈闭识别技术及效果.石油地球物理勘探,2006,41(增刊):57～61Yu Jingbo,Pan Hongwei,Guo Zenghu.Identificationof lithologic traps in south Songliao basin and effects.OGP,2006,41(Sup):57～61
[28]张立恩,陈少峰,姜继莲等.MT法在地热勘探中的应用.石油地球物理勘探,2004,39(增刊):66～70Zhang Lien,Chen Shaofeng,Jiang Jilian et al.Appli-cations of MT method for geothermal exploration.OGP,2004,39(Sup):66～70
[29]魏小东,张延庆,曹丽丽等.地震资料振幅谱梯度属性在WC地区储层评价中的应用.石油地球物理勘探,2011,46(2):281～284Wei Xiaodong,Zhang Yanqing,Cao Lili et al.Appli-cations of amplitude spectrum gradient for reservoirevaluation in WC project.OGP,2011,46(2):281～284
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