伊通盆地断裂体系特征及其演化历史
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摘要
综合利用最新的地震、航磁、钻井等资料,对伊通盆地断裂体系进行了重新认识,并对断裂演化及其油气成藏的控制作用进行了综合分析。伊通盆地主要是受西北缘走滑断裂控制的新生代走滑-伸展盆地;断裂的性质、特征及演化极其复杂,按断裂特征及规模可划分为3个级别。一级断裂为西北缘和东南缘控盆边界断裂;二级断裂为早期张扭作用形成的呈雁列展布的马鞍山断裂,2号、3号、4号断裂和晚期压扭作用形成的西北缘逆冲断裂;三级断裂为盆地演化过程中形成的众多次级断裂。伊通盆地断裂演化特征与太平洋板块的俯冲作用、印度板块和欧亚大陆碰撞作用以及盆缘大黑山地垒和那丹哈达岭地体挤压位置与隆升强度密切相关,断裂演化经历了古近纪成盆期的右旋张扭作用阶段和新近纪反转期的右旋压扭及基底隆升作用阶段;新近纪反转期压扭作用形成的西北缘断褶带具有良好的油气勘探潜力。
According to the data of seismic,aeromagnetic,well drilling,etc,the authors restudy the characteristics of the fault system in Yitong basin,analyzes its evolution and the control effect on the hydrocarbon accumulation.Yitong basin is a strike-slip stretching basin which is controlled mostly by the strike-slip fault of the north-west boundary in Cenozoic.The features and evolution of the basin's faults are very complex,the faults can be classified as three distinction based on their characteristics and sizes.The first distinction faults include the north-west boundary fault and the south-east boundary fault;the second distinction faults include the stretching faults such as Maanshan fault,number 2 fault,number 3 fault,number 4 fault and the thrust fault along the north-west edge;the third distinction faults include the rest faults of the basin.The faults' evolution features in Yitong basin took place in the regional dynamic setting that back-arc spreading caused by westward subduction of the Pacific plate,and the collision from the Indian plate also played a partial role in the E-W compression in the East China.Besides this,the distribution and uplift strength of rigid plates of Daheishan and Nadanhadaling Mountain play a great role on the fault evolution.The fault evolution includes two stages: the early dextral strike-slip stretching stage and the dextral strike-slip compressing stage in basin's reverse period.The dextral strike-slip compressing forms the fault-folds belt by the north-west edge and it has great potential for hydrocarbon exploration.
According to the data of seismic,aeromagnetic,well drilling,etc,the authors restudy the characteristics of the fault system in Yitong basin,analyzes its evolution and the control effect on the hydrocarbon accumulation.Yitong basin is a strike-slip stretching basin which is controlled mostly by the strike-slip fault of the north-west boundary in Cenozoic.The features and evolution of the basin's faults are very complex,the faults can be classified as three distinction based on their characteristics and sizes.The first distinction faults include the north-west boundary fault and the south-east boundary fault;the second distinction faults include the stretching faults such as Maanshan fault,number 2 fault,number 3 fault,number 4 fault and the thrust fault along the north-west edge;the third distinction faults include the rest faults of the basin.The faults' evolution features in Yitong basin took place in the regional dynamic setting that back-arc spreading caused by westward subduction of the Pacific plate,and the collision from the Indian plate also played a partial role in the E-W compression in the East China.Besides this,the distribution and uplift strength of rigid plates of Daheishan and Nadanhadaling Mountain play a great role on the fault evolution.The fault evolution includes two stages: the early dextral strike-slip stretching stage and the dextral strike-slip compressing stage in basin's reverse period.The dextral strike-slip compressing forms the fault-folds belt by the north-west edge and it has great potential for hydrocarbon exploration.
引文
[1]王永春.伊通地堑含油气系统与油气成藏[M].北京:石油工业出版社,2001:119-129.WANG Yong-chun.The petroleum system and hydro-carbon accumulation in Yitong graben[M].Beijing:Petroleum Industry Press,2001:119-129.
[2]张世红,程学儒,李安锋.论依—舒地堑伸展构造的深部机制[J].石油物探,1993,32(3):96-102.ZHANG Shi-hong,CHENG Xue-ru,LI An-feng.Mechanism of Yi-Shu graben in the depth of the earth[J].Geophysical Prospecting for Petroleum,1993,32(3):96-102.
[3]李献甫,陈全茂,张学海,等.伊通地堑——走滑断陷盆地的构造特征及演化[J].石油实验地质,2002,24(1):19-30.LI Xian-fu,CHEN Quan-mao,ZHANG Xue-hai,et al.The Yitong graben—the structural features and evolu-tion of a strike slip fault basin[J].Petroleum Geology&Experiment,2002,24(1):19-30.
[4]朱光,刘国生,宋传中,等.郯庐断裂带的脉动式伸展活动[J].高校地质学报,2000,6(3):396-404.ZHU Guang,LIU Guo-sheng,SONG Chuan-zhong,et al.Pulsative extensional activities of the Tan-Lufault zone[J].Geological Journal of China Universi-ties,2000,6(3):396-404.
[5]朱光,王道轩,刘国生,等.郯庐断裂带的伸展活动及其动力学背景[J].地质科学,2001,36(3):269-278.ZHU Guang,WANG Dao-xuan,LIU Guo-sheng,etal.Extensional activities along the Tan-Lu fault zoneand its geodynamic setting[J].Chinese Journal ofGeology,2001,36(3):269-278.
[6]许浚远.依舒地堑新生代构造演化[J].地球科学——中国地质大学学报,1997,22(4):407-410.XU Jun-yuan.Tectonic evolution of Yishu graben inCenozoic[J].Earth Science—Journal of China Univer-sity of Geosciences,1997,22(4):407-410.
[7]朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学,2004,39(1):36-49.ZHU Guang,WANG Dao-xuan,LIU Guo-sheng,etal.Evolution of the Tan-Lu fault zone and its respon-ses to plate movements in west Pacific basin[J].Chi-nese Journal of Geology,2004,39(1):36-49.
[8]Yu Zhao-hua,Wu Shi-guo,Zou Dong-bo,et al.Seis-mic profiles across the middle Tan-Lu fault zone inLaizhou Bay,Bohai Sea,Eastern China[J].Journal ofAsian Earth Sciences,2008,33:383-394.
[9]刘国生,朱光,宋传中,等.郯庐断裂带新近纪以来的挤压构造与合肥盆地的反转[J].安徽地质,2002,12(2):81-84.LIU Guo-sheng,ZHU Guang,SONG Chuan-zhong,et al.Compressional structures of the Tan-Lu faultzone and inversion of the Hefei basin since Neogene[J].Geology of Anhui,2002,12(2):81-84.
[10]殷敬红,雷安贵,方炳钟,等.辽河外围中生代盆地“下洼找油气”理念[J].石油勘探与开发,2008,35(1):6-10.YIN Jing-hong,LEI An-gui,FANG Bing-zhong,etal.Concept of“seeking for oil and gas deep down de-pressions”in Liaohe peripheral Mesozoic basin[J].Petroleum Exploration and Development,2008,35(1):6-10.
[11]张大立,石殿志,崔斗烈.郯庐断裂北延问题的探讨[J].吉林地质,1982,6(4):47-54.ZHANG Da-li,SHI Dian-zhi,CUI Dou-lie.Discus-sion on northern part of Tan-Lu fault zone[J].JilinGeology,1982,6(4):47-54.
[12]程捷,万天丰.郯庐断裂带在新生代的演化[J].地质科技情报,1996,15(3):35-42.CHENG Jie,WAN Tian-feng.On the activity of theTancheng-Lujiang fault zone during Cenozoic[J].Ge-ological Science and Technology Information,1996,15(3):35-42.
[13]卢华复,俞鸿年,丁幼文,等.试论郯庐断裂带中段新构造期构造应力场的演化[C]//构造地质论丛(三).北京:地质出版社,1984:107-115.LU Hua-fu,YU Hong-nian,DING You-wen,et al.On the evolution of the structural stress fields in thearea of the middle segment of the Tancheng-Lujiangfracture zone in new tectonic period[C]//Collection ofstructural geology(3).Beijing:Geological Publi-shing House,1984:107-115.
[14]荆凤,申旭辉,洪顺英,等.基于遥感技术研究依兰—伊通断裂带[J].地震,2006,26(3):79-84.JING Feng,SHEN Xu-hui,HONG Shun-ying,et al.A study on Yilan-Yitong fault zone based on remotesensing technology[J].Earthquake,2006,26(3):79-84.
[15]刘茂强,杨丙中,邓俊国,等.伊通—舒兰地堑地质构造特征及其演化[M].北京:地质出版社,1993.LIU Mao-qiang,YANG Bing-zhong,DENG Jun-guo,et al.Geological tectonic features and evolutionof Yitong-Shulan graben[M].Beijing:GeologicalPublishing House,1993:42-84.
[16]童亨茂.伊通地堑边界断裂的性质与演化[J].地质力学学报,2002,8(1):35-42.TONG Heng-mao.The property and evolution ofboundary faults of Yitong graben[J].Journal of Geo-mechanics,2002,8(1):35-42.
[17]孙晓猛,龙胜祥,张梅生.佳木斯—伊通断裂带大型逆冲构造带的发现及形成时代[J].石油与天然气地质,2006,27(5):637-643.SUN Xiao-meng,LONG Sheng-xiang,ZHANG Mei-sheng,et al.Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone[J].Oil&Gas Geol-ogy,2006,27(5):637-643.
[18]孙万军,刘宝柱,李本才,等.伊通地堑断层系统与构造样式[J].现代地质,2004,18(4):505-510.SUN Wan-jun,LIU Bao-zhu,LI Ben-cai,et al.Faultsystem and tectonic style of the Yitong graben[J].Geoscience,2004,18(4):505-510.
[19]李洪革,李本才,韩龙,等.伊通地堑二号断层几何学特征及其与油气关系[J].石油地球物理勘探,2004,39(5):614-618.LI Hong-ge,LI Ben-cai,HAN Long,et al.Geomet-ric feature of No.2 fault in Yitong graben and its rela-tion to oil-gas[J].Oil Geophysical Prospecting,2004,39(5):614-618.
[20]江涛,邱玉超,王立武,等.伊通盆地二号断层与西拉木伦河断裂带及油气的关系[J].吉林大学学报:地球科学版,2008,38(3):411-416.JIANG Tao,QIU Yu-chao,WANG Li-wu,et al.Relationship between No.2 fault in Yitong basin andXilamulun River fault and its significances for petrole-um[J].Journal of Jilin University:Earth Science Edi-tion,2008,38(3):411-416.
[21]孔祥星.准噶尔盆地南缘西部山前断褶带油源分析[J].石油勘探与开发,2007,34(4):413-418.KONG Xiang-xing.Oil source of foothill fault-foldstructural belt in western part of the southern mar-gin,Junggar basin[J].Petroleum Exploration andDevelopment,2007,34(4):413-418.
[22]刘顺,刘树根,李智武,等.南大巴山褶断带西段中新生代构造应力场的节理研究[J].成都理工大学学报:自然科学版,2005,32(4):345-350.LIU Shun,LIU Shu-gen,LI Zhi-wu,et al.Analysisof joints from the Meso-Cenozoic tectonic stress fieldin the west section of south Dabashan fault-fold beltin China[J].Journal of Chengdu University of Tech-nology:Science&Technology Edition,2005,32(4):345-350.
[23]何登发,贾承造,童晓光,等.含油气区构造学研究进展[J].石油勘探与开发,2004,31(5):1-7.HE Deng-fa,JIA Cheng-zao,TONG Xiao-guang,etal.Advances in studies of petroliferous structures andtectonics[J].Petroleum Exploration and Develop-ment,2004,31(5):1-7.
[24]周玉琦,周荔青,郭念发.中国东部新生代盆地油气地质[M].北京:石油工业出版社,2004:130-141.ZHOU Yu-qi,ZHOU Li-qing,GUO Nian-fa.Petro-leum geology of Cenozoic basins in East China[M].Beijing:Petroleum Industry Press,2004:130-141.
[25]XU J W.The Tangcheng-Lujiang wrench fault sys-tem[M].London:John Wiley&Sons,1993:1-74.
[26]朱光,刘国生,牛漫兰,等.郯庐断裂带晚第三纪以来的浅部挤压活动与深部过程[J].地震地质,2002,24(2):265-277.ZHU Guang,LIU Guo-sheng,NIU Man-lan,et al.Post-Eogene compressive activities on the Tan-Lufault zone and their deep processes[J].Seismologyand Geology,2002,24(2):265-277.
[27]陈全茂,李忠飞.辽河盆地东部凹陷构造及含油气性分析[M].北京:地质出版社,1998:141-148.CHEN Quan-mao,LI Zhong-fei.Structures of eastdepression in Liaohe basin and petroliferous analysis[M].Beijing:Geological Publishing House,1998:141-148.
[28]程有义,李晓清,汪泽成,等.潍北拉分盆地形成演化及其对成油气条件的控制[J].石油勘探与开发,2004,31(6):32-35.CHENG You-yi,LI Xiao-qing,WANG Ze-cheng,etal.Tectonic evolution and its controlling on petrole-um generation in Weibei basin[J].Petroleum Explo-ration and Development,2004,31(6):32-35.
[29]陈义贤.辽河裂谷盆地断裂演化序次和油气藏形成模式[J].石油学报,1985,6(2):1-11.CHEN Yi-xian.The evolution of faults and formationof oil and gas reservoirs in the Liaohe rift valley[J].Acta Petrolei Sinica,1985,6(2):1-11.
[30]刘祥.中国东北地区新生代火山活动构造控制及火山灾害[J].世界地质,1999(2):23-29.LIU Xiang.Tectonic control of Cenozoic volcanism inNortheastern China[J].World Geology,1999(2):23-29.
[31]马宗晋,张进,任金卫,等.全球GPS矢量场的分区描述及规律性分析[J].地质学报,2006,80(8):1089-1100.MA Zong-jin,ZHANG Jin,REN Jin-wei,et al.Sub-regional descriptions of global GPS vector fieldand its geodynamic significance[J].Acta GeologicaSinica,2006,80(8):1089-1100.
[2]张世红,程学儒,李安锋.论依—舒地堑伸展构造的深部机制[J].石油物探,1993,32(3):96-102.ZHANG Shi-hong,CHENG Xue-ru,LI An-feng.Mechanism of Yi-Shu graben in the depth of the earth[J].Geophysical Prospecting for Petroleum,1993,32(3):96-102.
[3]李献甫,陈全茂,张学海,等.伊通地堑——走滑断陷盆地的构造特征及演化[J].石油实验地质,2002,24(1):19-30.LI Xian-fu,CHEN Quan-mao,ZHANG Xue-hai,et al.The Yitong graben—the structural features and evolu-tion of a strike slip fault basin[J].Petroleum Geology&Experiment,2002,24(1):19-30.
[4]朱光,刘国生,宋传中,等.郯庐断裂带的脉动式伸展活动[J].高校地质学报,2000,6(3):396-404.ZHU Guang,LIU Guo-sheng,SONG Chuan-zhong,et al.Pulsative extensional activities of the Tan-Lufault zone[J].Geological Journal of China Universi-ties,2000,6(3):396-404.
[5]朱光,王道轩,刘国生,等.郯庐断裂带的伸展活动及其动力学背景[J].地质科学,2001,36(3):269-278.ZHU Guang,WANG Dao-xuan,LIU Guo-sheng,etal.Extensional activities along the Tan-Lu fault zoneand its geodynamic setting[J].Chinese Journal ofGeology,2001,36(3):269-278.
[6]许浚远.依舒地堑新生代构造演化[J].地球科学——中国地质大学学报,1997,22(4):407-410.XU Jun-yuan.Tectonic evolution of Yishu graben inCenozoic[J].Earth Science—Journal of China Univer-sity of Geosciences,1997,22(4):407-410.
[7]朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学,2004,39(1):36-49.ZHU Guang,WANG Dao-xuan,LIU Guo-sheng,etal.Evolution of the Tan-Lu fault zone and its respon-ses to plate movements in west Pacific basin[J].Chi-nese Journal of Geology,2004,39(1):36-49.
[8]Yu Zhao-hua,Wu Shi-guo,Zou Dong-bo,et al.Seis-mic profiles across the middle Tan-Lu fault zone inLaizhou Bay,Bohai Sea,Eastern China[J].Journal ofAsian Earth Sciences,2008,33:383-394.
[9]刘国生,朱光,宋传中,等.郯庐断裂带新近纪以来的挤压构造与合肥盆地的反转[J].安徽地质,2002,12(2):81-84.LIU Guo-sheng,ZHU Guang,SONG Chuan-zhong,et al.Compressional structures of the Tan-Lu faultzone and inversion of the Hefei basin since Neogene[J].Geology of Anhui,2002,12(2):81-84.
[10]殷敬红,雷安贵,方炳钟,等.辽河外围中生代盆地“下洼找油气”理念[J].石油勘探与开发,2008,35(1):6-10.YIN Jing-hong,LEI An-gui,FANG Bing-zhong,etal.Concept of“seeking for oil and gas deep down de-pressions”in Liaohe peripheral Mesozoic basin[J].Petroleum Exploration and Development,2008,35(1):6-10.
[11]张大立,石殿志,崔斗烈.郯庐断裂北延问题的探讨[J].吉林地质,1982,6(4):47-54.ZHANG Da-li,SHI Dian-zhi,CUI Dou-lie.Discus-sion on northern part of Tan-Lu fault zone[J].JilinGeology,1982,6(4):47-54.
[12]程捷,万天丰.郯庐断裂带在新生代的演化[J].地质科技情报,1996,15(3):35-42.CHENG Jie,WAN Tian-feng.On the activity of theTancheng-Lujiang fault zone during Cenozoic[J].Ge-ological Science and Technology Information,1996,15(3):35-42.
[13]卢华复,俞鸿年,丁幼文,等.试论郯庐断裂带中段新构造期构造应力场的演化[C]//构造地质论丛(三).北京:地质出版社,1984:107-115.LU Hua-fu,YU Hong-nian,DING You-wen,et al.On the evolution of the structural stress fields in thearea of the middle segment of the Tancheng-Lujiangfracture zone in new tectonic period[C]//Collection ofstructural geology(3).Beijing:Geological Publi-shing House,1984:107-115.
[14]荆凤,申旭辉,洪顺英,等.基于遥感技术研究依兰—伊通断裂带[J].地震,2006,26(3):79-84.JING Feng,SHEN Xu-hui,HONG Shun-ying,et al.A study on Yilan-Yitong fault zone based on remotesensing technology[J].Earthquake,2006,26(3):79-84.
[15]刘茂强,杨丙中,邓俊国,等.伊通—舒兰地堑地质构造特征及其演化[M].北京:地质出版社,1993.LIU Mao-qiang,YANG Bing-zhong,DENG Jun-guo,et al.Geological tectonic features and evolutionof Yitong-Shulan graben[M].Beijing:GeologicalPublishing House,1993:42-84.
[16]童亨茂.伊通地堑边界断裂的性质与演化[J].地质力学学报,2002,8(1):35-42.TONG Heng-mao.The property and evolution ofboundary faults of Yitong graben[J].Journal of Geo-mechanics,2002,8(1):35-42.
[17]孙晓猛,龙胜祥,张梅生.佳木斯—伊通断裂带大型逆冲构造带的发现及形成时代[J].石油与天然气地质,2006,27(5):637-643.SUN Xiao-meng,LONG Sheng-xiang,ZHANG Mei-sheng,et al.Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone[J].Oil&Gas Geol-ogy,2006,27(5):637-643.
[18]孙万军,刘宝柱,李本才,等.伊通地堑断层系统与构造样式[J].现代地质,2004,18(4):505-510.SUN Wan-jun,LIU Bao-zhu,LI Ben-cai,et al.Faultsystem and tectonic style of the Yitong graben[J].Geoscience,2004,18(4):505-510.
[19]李洪革,李本才,韩龙,等.伊通地堑二号断层几何学特征及其与油气关系[J].石油地球物理勘探,2004,39(5):614-618.LI Hong-ge,LI Ben-cai,HAN Long,et al.Geomet-ric feature of No.2 fault in Yitong graben and its rela-tion to oil-gas[J].Oil Geophysical Prospecting,2004,39(5):614-618.
[20]江涛,邱玉超,王立武,等.伊通盆地二号断层与西拉木伦河断裂带及油气的关系[J].吉林大学学报:地球科学版,2008,38(3):411-416.JIANG Tao,QIU Yu-chao,WANG Li-wu,et al.Relationship between No.2 fault in Yitong basin andXilamulun River fault and its significances for petrole-um[J].Journal of Jilin University:Earth Science Edi-tion,2008,38(3):411-416.
[21]孔祥星.准噶尔盆地南缘西部山前断褶带油源分析[J].石油勘探与开发,2007,34(4):413-418.KONG Xiang-xing.Oil source of foothill fault-foldstructural belt in western part of the southern mar-gin,Junggar basin[J].Petroleum Exploration andDevelopment,2007,34(4):413-418.
[22]刘顺,刘树根,李智武,等.南大巴山褶断带西段中新生代构造应力场的节理研究[J].成都理工大学学报:自然科学版,2005,32(4):345-350.LIU Shun,LIU Shu-gen,LI Zhi-wu,et al.Analysisof joints from the Meso-Cenozoic tectonic stress fieldin the west section of south Dabashan fault-fold beltin China[J].Journal of Chengdu University of Tech-nology:Science&Technology Edition,2005,32(4):345-350.
[23]何登发,贾承造,童晓光,等.含油气区构造学研究进展[J].石油勘探与开发,2004,31(5):1-7.HE Deng-fa,JIA Cheng-zao,TONG Xiao-guang,etal.Advances in studies of petroliferous structures andtectonics[J].Petroleum Exploration and Develop-ment,2004,31(5):1-7.
[24]周玉琦,周荔青,郭念发.中国东部新生代盆地油气地质[M].北京:石油工业出版社,2004:130-141.ZHOU Yu-qi,ZHOU Li-qing,GUO Nian-fa.Petro-leum geology of Cenozoic basins in East China[M].Beijing:Petroleum Industry Press,2004:130-141.
[25]XU J W.The Tangcheng-Lujiang wrench fault sys-tem[M].London:John Wiley&Sons,1993:1-74.
[26]朱光,刘国生,牛漫兰,等.郯庐断裂带晚第三纪以来的浅部挤压活动与深部过程[J].地震地质,2002,24(2):265-277.ZHU Guang,LIU Guo-sheng,NIU Man-lan,et al.Post-Eogene compressive activities on the Tan-Lufault zone and their deep processes[J].Seismologyand Geology,2002,24(2):265-277.
[27]陈全茂,李忠飞.辽河盆地东部凹陷构造及含油气性分析[M].北京:地质出版社,1998:141-148.CHEN Quan-mao,LI Zhong-fei.Structures of eastdepression in Liaohe basin and petroliferous analysis[M].Beijing:Geological Publishing House,1998:141-148.
[28]程有义,李晓清,汪泽成,等.潍北拉分盆地形成演化及其对成油气条件的控制[J].石油勘探与开发,2004,31(6):32-35.CHENG You-yi,LI Xiao-qing,WANG Ze-cheng,etal.Tectonic evolution and its controlling on petrole-um generation in Weibei basin[J].Petroleum Explo-ration and Development,2004,31(6):32-35.
[29]陈义贤.辽河裂谷盆地断裂演化序次和油气藏形成模式[J].石油学报,1985,6(2):1-11.CHEN Yi-xian.The evolution of faults and formationof oil and gas reservoirs in the Liaohe rift valley[J].Acta Petrolei Sinica,1985,6(2):1-11.
[30]刘祥.中国东北地区新生代火山活动构造控制及火山灾害[J].世界地质,1999(2):23-29.LIU Xiang.Tectonic control of Cenozoic volcanism inNortheastern China[J].World Geology,1999(2):23-29.
[31]马宗晋,张进,任金卫,等.全球GPS矢量场的分区描述及规律性分析[J].地质学报,2006,80(8):1089-1100.MA Zong-jin,ZHANG Jin,REN Jin-wei,et al.Sub-regional descriptions of global GPS vector fieldand its geodynamic significance[J].Acta GeologicaSinica,2006,80(8):1089-1100.
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