吉林东部盆地群早白垩世原型盆地恢复
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摘要
通过区域地质、电法和地震资料等对吉林东部盆地群早白垩世地层、沉积和构造特征进行研究,从而恢复沉积古地理及原型盆地面貌,结合现今勘探成果与原型盆地控制烃源岩展布,残留盆地改造情况,预测有利勘探区。研究结果表明:该区早白垩世原型盆地为一大型陆相湖盆的一部分,果松组—鹰嘴砬子组沉积期为初始裂陷孤立盆地发展阶段,林子头组沉积期为断坳转换期,沙河子组—营城组沉积期为统一的坳陷盆地,至登娄库组沉积期原型盆地完全遭到破坏,泉头组沉积期各盆地进入独立发展阶段。靠近原型盆地湖盆中心的(扇)三角洲相、河流相及湖沼相沉积区且位于现今盆地的凹陷区是吉林东部盆地群的有利油气勘探区。
Based on the regional geological data,electrical and seismic data,we research the stratigraphic,sedimentary,tectonic features of Early Cretaceous basin group in eastern Jilin,restoring the sedimentary paleogeography and the visage of prototype basin.Combined with the distribution of hydrocarbon source rocks controlled by the prototype basin and the residual basins transformation in the modern exploration,favorable exploration areas can be predicted.We concluded that prototype basin in this region was a part of a large terrigenous lake basin in Early Cretaceous.Guosong-Yingzuilazi formations sedimentary stage was the initial rifting isolated basin development stage,Linzitou Formation sedimentary stage was a fault-depressed diversionary stage,Shahezi-Yingcheng formations sedimentary stage was the time for unified depression basin,and the prototype basin was totally destroyed in Denglouku Formation sedimentary stage.Since Quantou Formation sedimentary stage,every basin was into an independent development stage.The(fan) delta facies,fluvial facies and paludal facies deposition areas which near the lake center of prototype basin,and in the depression of present basins are the advantageous areas for oil and gas exploration of the basin group in eastern Jilin.
Based on the regional geological data,electrical and seismic data,we research the stratigraphic,sedimentary,tectonic features of Early Cretaceous basin group in eastern Jilin,restoring the sedimentary paleogeography and the visage of prototype basin.Combined with the distribution of hydrocarbon source rocks controlled by the prototype basin and the residual basins transformation in the modern exploration,favorable exploration areas can be predicted.We concluded that prototype basin in this region was a part of a large terrigenous lake basin in Early Cretaceous.Guosong-Yingzuilazi formations sedimentary stage was the initial rifting isolated basin development stage,Linzitou Formation sedimentary stage was a fault-depressed diversionary stage,Shahezi-Yingcheng formations sedimentary stage was the time for unified depression basin,and the prototype basin was totally destroyed in Denglouku Formation sedimentary stage.Since Quantou Formation sedimentary stage,every basin was into an independent development stage.The(fan) delta facies,fluvial facies and paludal facies deposition areas which near the lake center of prototype basin,and in the depression of present basins are the advantageous areas for oil and gas exploration of the basin group in eastern Jilin.
引文
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[9]和钟铧,刘招君,陈秀艳,等.黑龙江省东部残留盆地群早白垩世沉积相特征及演化[J].古地理学报.2008,10(2):151-158.HE Zhong-hua,LIU Zhao-jun,CHEN Xiu-yan,et al.Sedimentary facies characteristics and their evolution ofthe Early Cretaceous relict basins in eastern HeilongjiangProvince[J].Journal of Palaeogeography.2008,10(2):151-158.
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[11]曹洁.黑龙江东部盆地群早白垩世岩相古地理研究与油气远景分析:博士学位论文[D].北京:中国地质科学院,2010.CAO Jie.Lithofacies palaeogeographical study and oil-Gas prospect analysis of Early Cretaceous in easten Hei-longjiang basins:Ph’D dissertation[D].Beijing:Chinese Academy of Geological Sciences,2010.
[12]温泉波,刘永江,韩国卿,等.黑龙江东部盆地群中、新生代构造演化[J].世界地质,2008,27(4):370-377.WEN Quan-bo,LIU Yong-jiang,HAN Guo-qing,et al.Mesozoic and Cenozoic tectonic evolution of the basingroup in eastern Heilongjiang,China[J].Global Geol-ogy,2008,27(4):370-377.
[13]郝诒纯,苏德英,余静贤,等.中国地层典-白垩系[M].北京:地质出版社,2000:26-99.HAO Yi-chun,SU De-ying,YU Jing-xian,et al.Stra-tigraphy dictionary of China-Cretaceous[M].Beijing:Geologic Publishing House,2000:26-99.
[14]吉林省地质矿产局.吉林省岩石地层[M].北京:中国地质大学出版社,1997:178-264.The Bureau of Geology and Mineral Resources,JilinProvince.The lithostratigraphic of Jilin Province[M].Beijing:China University of Geosciences Press,1997:178-264.
[15]杜旭东,漆家福,陆克政,等.大港探区中生代原型盆地恢复及成盆模式[J].应用基础与工程科学学报,1999,7(3):230-239.DU Xu-dong,QI Jia-fu,LU Ke-zheng,et al.Modeland recovery of primary basin of the Mesozoic basin inDagang explortation area[J].Journal of Basic Scienceand Engineering,1999,7(3):230-239.
[16]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘.2003,10(3):51-59.WU Fu-yuan,GE Wen-chun,SUN De-you,et al.Dis-cussions on the lithospheric thinning in eastern China[J].Earth Science Frontiers,2003,10(3):51-59.
[17]罗群.中国东北地区断裂系统及其控藏特征[J].石油实验地质,2010,32(3):205-210.LUO Qun.Fault systems and characteristics of theircontrolling reservoir formation in the northeast China[J].Petroleum Geology&Experiment,2010,32(3):205-210.
[18]孙晓猛,王书琴,王英德,等.郯庐断裂带北段构造特征及构造演化序列[J].岩石学报,2010,26(1):165-176.SUN Xiao-meng,WANG Shu-qin,WANG Ying-de,etal.The structural feature and evolutionary series in thenorthern segment of Tancheng--Lujiang fault zone[J].Acta Petrologica Sinica,2010,26(1):165-176.
①吉林省东部中新生代沉积盆地评价[R].松原:中国石油吉林油田分公司勘探开发研究院,1999.
②1∶20万通化市幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1977.
③1∶20万靖宇幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1979.
①1∶20万海龙县幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1978.
[2]刘池洋,杨兴科.改造盆地研究和油气评价的思路[J].石油与天然气地质,2000,21(1):11-14.LIU Chi-yang,YANG Xing-ke.Thinking for researchesand oil-gas assessment of reformed basins[J].Oil&GasGeology,2000,21(1):11-14.
[3]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(1):126-135.HE Deng-fa,ZHOU Xin-yuan,ZHANG Chao-jun,et al.The evolution and types of Ordovician prototype basins inTarim area[J].Chinese Science Bulletin,2007,52(I):126-135.
[4]赵文智,靳久强,薛良清,等.中国西北地区侏罗纪原型盆地形成与演化[M].北京:地质出版社,2000:5-93.ZHAO Wen-zhi,JIN Jiu-qiang,XUE Liang-qing,et al.Proto-types and evolution of Jurassic basins in NW China[M].Beijing:Geological Publishing House,2000:5-93.
[5]陈启林,周洪瑞,李相博,等.蒙甘青地区早白垩世原型盆地特征及其对烃源岩分布的控制[J].地球科学进展,2005,20(6):656-663.CHEN Qi-lin,ZHOU Hong-rui,LI Xiang-bo,et al.Characteristics of Early Cretaceous prototype basin and itscontrol on source rock in Mongolia-Gansu-Qinghai area[J].Advances in Earth Science,2005,20(6):656-663.
[6]徐旭辉.塔里木古生代原型盆地分析的油气勘探意义[J].石油与天然气地质,2002,23(3):224-228.XU Xu-hui.The significance of the analysis of Tarim Pa-leozoic prototype basins in oil and gas exploration[J].Oil&Gas Geology,2002,23(3):224-228.
[7]马金苹.大庆探区外围东部盆地群油气远景评价:硕士学位论文[D].长春:吉林大学地球科学学院,2008.MA Jin-ping.Petroleum prospect evaluation in the easternperipheral pasins of the Daqing exploration area:master’s degree thesis[D].Changchun:College of Earth Sci-ences,Jilin University,2008.
[8]曹成润,郑庆道.黑龙江省东部残留盆地群构造演化特征及其油气勘探意义[J].吉林大学学报:地球科学版,2003,33(2):167-172.CAO Cheng-run,ZHENG Qing-dao.Structural evolutionfeatures and its significance of hydrocarbon exploration inrelict basin group,eastern Heilongjiang Province[J].Journal of Jilin University:Earth Science Edition,2003,33(2):167-172.
[9]和钟铧,刘招君,陈秀艳,等.黑龙江省东部残留盆地群早白垩世沉积相特征及演化[J].古地理学报.2008,10(2):151-158.HE Zhong-hua,LIU Zhao-jun,CHEN Xiu-yan,et al.Sedimentary facies characteristics and their evolution ofthe Early Cretaceous relict basins in eastern HeilongjiangProvince[J].Journal of Palaeogeography.2008,10(2):151-158.
[10]何玉平.黑龙江省东部早白垩世沉积特征与原型盆地恢复:博士学位论文[D].长春:吉林大学地球科学学院,2006.HE Yu-ping.The Early Cretaceous sedimentary charac-teristics and prototype basin restoration in eastern Hei-longjiang Province:Ph’D dissertation[D].Chang-chun:College of Earth Sciences,Jilin University,2006.
[11]曹洁.黑龙江东部盆地群早白垩世岩相古地理研究与油气远景分析:博士学位论文[D].北京:中国地质科学院,2010.CAO Jie.Lithofacies palaeogeographical study and oil-Gas prospect analysis of Early Cretaceous in easten Hei-longjiang basins:Ph’D dissertation[D].Beijing:Chinese Academy of Geological Sciences,2010.
[12]温泉波,刘永江,韩国卿,等.黑龙江东部盆地群中、新生代构造演化[J].世界地质,2008,27(4):370-377.WEN Quan-bo,LIU Yong-jiang,HAN Guo-qing,et al.Mesozoic and Cenozoic tectonic evolution of the basingroup in eastern Heilongjiang,China[J].Global Geol-ogy,2008,27(4):370-377.
[13]郝诒纯,苏德英,余静贤,等.中国地层典-白垩系[M].北京:地质出版社,2000:26-99.HAO Yi-chun,SU De-ying,YU Jing-xian,et al.Stra-tigraphy dictionary of China-Cretaceous[M].Beijing:Geologic Publishing House,2000:26-99.
[14]吉林省地质矿产局.吉林省岩石地层[M].北京:中国地质大学出版社,1997:178-264.The Bureau of Geology and Mineral Resources,JilinProvince.The lithostratigraphic of Jilin Province[M].Beijing:China University of Geosciences Press,1997:178-264.
[15]杜旭东,漆家福,陆克政,等.大港探区中生代原型盆地恢复及成盆模式[J].应用基础与工程科学学报,1999,7(3):230-239.DU Xu-dong,QI Jia-fu,LU Ke-zheng,et al.Modeland recovery of primary basin of the Mesozoic basin inDagang explortation area[J].Journal of Basic Scienceand Engineering,1999,7(3):230-239.
[16]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘.2003,10(3):51-59.WU Fu-yuan,GE Wen-chun,SUN De-you,et al.Dis-cussions on the lithospheric thinning in eastern China[J].Earth Science Frontiers,2003,10(3):51-59.
[17]罗群.中国东北地区断裂系统及其控藏特征[J].石油实验地质,2010,32(3):205-210.LUO Qun.Fault systems and characteristics of theircontrolling reservoir formation in the northeast China[J].Petroleum Geology&Experiment,2010,32(3):205-210.
[18]孙晓猛,王书琴,王英德,等.郯庐断裂带北段构造特征及构造演化序列[J].岩石学报,2010,26(1):165-176.SUN Xiao-meng,WANG Shu-qin,WANG Ying-de,etal.The structural feature and evolutionary series in thenorthern segment of Tancheng--Lujiang fault zone[J].Acta Petrologica Sinica,2010,26(1):165-176.
①吉林省东部中新生代沉积盆地评价[R].松原:中国石油吉林油田分公司勘探开发研究院,1999.
②1∶20万通化市幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1977.
③1∶20万靖宇幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1979.
①1∶20万海龙县幅区域地质调查报告[S].长春:吉林省地质局区域地质调查大队,1978.
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