东北大三江地区早白垩世岩相古地理研究
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摘要
通过大量野外观察,结合岩芯、测井及地震剖面资料,研究东北大三江地区早白垩世穆棱组、城子河组的沉积相;并在对各个沉积相带的沉积特征和时空展布归纳和总结的基础上,编制了一套早白垩世穆棱组、城子河组岩相古地理图。结果表明:城子河组和穆棱组沉积相类型丰富,以滨浅湖、三角洲平原等浅水沉积为主,夹数层沼泽相煤和海相夹层;在古隆起的边缘有扇三角洲、辫状河相存在,向盆内过渡为滨浅湖和半深湖。城子河组沉积时期,汤原断陷周边发育扇三角洲沉积,绥滨坳陷和前进坳陷以三角洲和滨浅湖沉积为主,局部发育半深湖,并发育海相夹层和沼泽沉积;鸡西盆地和勃利盆地以三角洲和滨浅湖沉积为主,虎林盆地以滨浅湖沉积为主,局部发育半深湖,并发育海相夹层和沼泽沉积;穆棱组沉积时期,汤原断陷周边发育扇三角洲沉积,绥滨坳陷和前进坳陷地层不太发育,鸡西盆地和勃利盆地以三角洲和滨浅湖沉积为主,局部发育半深湖,并发育海相夹层和沼泽沉积,虎林盆地南部凹陷以滨浅湖沉积为主。早白垩世穆棱组、城子河组时期,张广才岭和桦南隆起是盆地主要物源供给区。
According to field observation,analysis of cores,logging and seismic data,sedimentary facies of Early Cretaceous Muling Formation and Chengzihe Formation in Dasanjiang area of Northeast China was conducted;sedimentary feature and temporal-spatial distribution of each sedimentary facies belt were summarized,and then lithofacies paleogeography maps of Muling Formation and Chengzihe Formation were drawn up.The results showed that types of sedimentary facies in Muling Formation and Chengzihe Formation were rich,shallow-water sedimentary including shore shallow lacustrine and delta plain was predominant with a little coal beds,with swamp facies and marine interlayers;fan delta and braided river existed in the margin of palaeohigh,and changed to shore shallow lacustrine and semi-deep lake from the margin to the depocenter of the basin.Fan delta deposit developed around Tangyuan rift during the sedimentary period of Chengzihe Formation,delta and shore shallow lacustrine were the main sedimentary facies in Suibin rift and Qianjin rift,and semi-deep lake,marine interlayer and swamp deposit developed partially;delta and shore shallow lacustrine were the main sedimentary facies in JixiBasin and Boli Basin,and shore shallow lacustrine deposit developed in Hulin Basin,and semi-deep lake,marine interlayer and swamp deposit developed partially;fan delta deposit developed around Tangyuan rift during the sedimentary period of Muling Formation,the strata in Suibin rift and Qianjin rift developed insignificantly,delta and shore shallow lacustrine were the main sedimentary facies in Jixi Basin and Boli Basin,and semi-deep lake,marine interlayer and swamp deposit developed partially,while shore shallow lacustrine was the main sedimentary facies in the southern sag of Hulin Basin.Zhangguangcai Mountain and Huanan uplift were the major material source of the basin during the sedimentary period of Early Cretaceous Chengzihe Formation and Muling Formation.
According to field observation,analysis of cores,logging and seismic data,sedimentary facies of Early Cretaceous Muling Formation and Chengzihe Formation in Dasanjiang area of Northeast China was conducted;sedimentary feature and temporal-spatial distribution of each sedimentary facies belt were summarized,and then lithofacies paleogeography maps of Muling Formation and Chengzihe Formation were drawn up.The results showed that types of sedimentary facies in Muling Formation and Chengzihe Formation were rich,shallow-water sedimentary including shore shallow lacustrine and delta plain was predominant with a little coal beds,with swamp facies and marine interlayers;fan delta and braided river existed in the margin of palaeohigh,and changed to shore shallow lacustrine and semi-deep lake from the margin to the depocenter of the basin.Fan delta deposit developed around Tangyuan rift during the sedimentary period of Chengzihe Formation,delta and shore shallow lacustrine were the main sedimentary facies in Suibin rift and Qianjin rift,and semi-deep lake,marine interlayer and swamp deposit developed partially;delta and shore shallow lacustrine were the main sedimentary facies in JixiBasin and Boli Basin,and shore shallow lacustrine deposit developed in Hulin Basin,and semi-deep lake,marine interlayer and swamp deposit developed partially;fan delta deposit developed around Tangyuan rift during the sedimentary period of Muling Formation,the strata in Suibin rift and Qianjin rift developed insignificantly,delta and shore shallow lacustrine were the main sedimentary facies in Jixi Basin and Boli Basin,and semi-deep lake,marine interlayer and swamp deposit developed partially,while shore shallow lacustrine was the main sedimentary facies in the southern sag of Hulin Basin.Zhangguangcai Mountain and Huanan uplift were the major material source of the basin during the sedimentary period of Early Cretaceous Chengzihe Formation and Muling Formation.
引文
[1]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 Evolu-tion of the Early Cretaceous Relict Basins in EasternHeilongjiang Province[J].Journal of Palaeogeogra-phy,2008,10(2):151-158.
[2]和钟铧,刘招君,张晓冬,等.黑龙江东部晚中生代盆地群构造层划分及构造沉积演化[J].世界地质,2009,28(1):20-27.HE Zhong-hua,LIU Zhao-jun,ZHANG Xiao-dong,et al.Subdivisions of Structural Layers and Tectonic-sedimentary Evolution of Eastern Basins in Hei-longjiang in Late Mesozoic[J].Global Geology,2009,28(1):20-27.
[3]杨晓平,李仰春,柳震,等.黑龙江东部鸡西盆地构造层序划分与盆地动力学演化[J].吉林大学学报:地球科学版,2005,35(5):616-621.YANG Xiao-ping,LI Yang-chun,LIU Zhen,et al.Classification of Tectonic Sequence and Dynamic Evo-lution of Jixi Basin,Eastern Heilongjiang Province[J].Journal of Jilin University:Earth Science Edi-tion,2005,35(5):616-621.
[4]孙革,刘风香.黑龙江鸡西含煤盆地早白垩世城子河组特尔姆叶(Tyrmia)的发现[J].煤田地质与勘探,2007,35(2):1-4.SUN Ge,LIU Feng-xiang.Discovery of TyrmiafromLower Cretaceous Chengzihe Formation in Jixi Coal-bearing Basin of Heilongjiang,China[J].Coal Geologyand Exploration,2007,35(2):1-4.
[5]于恩君.黑龙江省鸡西—勃利含煤盆地层序地层学讨论[J].吉林地质,2008,27(2):8-13.YU En-jun.Jixi-Boli Coal-bearing Basin StratigraphicSequence,Heilongjiang Province[J].Jilin Geology,2008,27(2):8-13.
[6]王金山.黑龙江省鸡西盆地南、北两带城子河组精细对比[J].中国煤炭地质,2008,20(8):5-9,25.WANG Jin-shan.Meticulous Correlation BetweenSouthern and Northern Belts of Chengzihe Formationin Jixi Basin,Heilongjiang Province[J].Coal Geologyof China,2008,20(8):5-9,25.
[7]杨绍芳.泛三江盆地成藏系统分析[J].石油天然气学报,2005,27(4):413-415.YANG Shao-fang.Analysis of Oil-gas Reservoir-forming System in Generic Sanjiang Basin,NortheastChina[J].Journal of Oil and Gas Technology,2005,27(4):413-415.
[8]刘云武,唐振国,刘文龙.三江盆地演化特征与油气勘探方向[J].石油天然气学报,2006,28(2):1-5.LIU Yun-wu,TANG Zhen-guo,LIU Wen-long.Evo-lutional Characteristics of Sanjiang Basin and Direc-tion of Hydrocarbon Exploration[J].Journal of Oiland Gas Technology,2006,28(2):1-5.
[9]胡志方,马义忠,乔桂林,等.三江盆地石油地质条件与勘探前景[J].河南石油,2006,20(1):1-4.HU Zhi-fang,MA Yi-zhong,QIAO Gui-lin,et al.Petroleum Geologic Conditions and Exploration Pros-pect of Sanjiang Basin[J].Henan Petroleum,2006,20(1):1-4.
[10]韩春花,曹成润,曹宪双,等.勃利盆地中生界地质特征与油气资源量计算[J].世界地质,2004,23(4):365-370.HAN Chun-hua,CAO Cheng-run,CAO Xian-shuang,et al.Mesozoic Geological Features and Calculation ofOil-gas Resources in Boli Basin[J].Global Geology,2004,23(4):365-370.
[11]杨建国,吴河勇,刘俊来.大庆探区外围盆地中、新生代地层对比及四大勘探层系[J].地质通报,2006,25(9/10):1088-1093.YANG Jian-guo,WU He-yong,LIU Jun-lai.Strati-graphic Correlation of the Mesozoic and Cenozoic inthe Outer Basins of the Daqing Exploration Area[J].Geological Bulletin of China,2006,25(9/10):1088-1093.
[12]成都理工大学地球科学学院.大庆探区外围盆地含油气性评价与优选[R].成都:成都理工大学,2003.School of Earth Sciences,Chengdu University ofTechnology.Evaluation and Optimum of PeripheralBasins in Daqing Exploration Area[R].Chengdu:Chengdu University of Technology,2003.
[13]李仰春,娄本军,杨晓平,等.黑龙江鸡西盆地北部穆棱组高分辨率层序地层[J].地球科学与环境学报,2007,29(3):263-268.LI Yang-chun,LOU Ben-jun,YANG Xiao-ping,et al.High-resolution Sequence Stratigraphy of MulingFormation in Jixi Basin of Northern HeilongjiangProvince[J].Journal of Earth Sciences and Environ-ment,2007,29(3):263-268.
[14]王伟涛,刘招君,陈秀艳.虎林盆地北部坳陷中、新生代碎屑岩源区构造背景与物源区分析[J].世界地质,2007,26(1):14-19.WANG Wei-tao,LIU Zhao-jun,CHEN Xiu-yan.Tec-tonic Setting and Provenance Analysis of Mesozoic-Cenozoic Clastic Rocks in Northern Depression ofHulin Basin[J].Global Geology,2007,26(1):14-19.
[15]王孔伟,张帆,林东成.汤原断陷构造活动对沉积的控制[J].石油地质与工程,2007,21(6):7-10.WANG Kong-wei,ZHANG Fan,LIN Dong-cheng.The Control of Tectonic Activities on Sedimentationin Tangyuan Fault Depression Basin[J].PetroleumGeology and Engineering,2007,21(6):7-10.
[16]温泉波,刘永江,李俊杰,等.鸡西、勃利盆地白垩纪砂岩的物源分析及构造意义[J].沉积与特提斯地质,2008,28(3):52-59.WEN Quan-bo,LIU Yong-jiang,LI Jun-jie,et al.Provenance Analysis and Tectonic Implications forthe Cretaceous Sandstones in the Jixi and Boli Basins,Heilongjiang[J].Sedimentary Geology and TethyanGeology,2008,28(3):52-59.
[17]陈秀艳.三江地区晚中生代层序地层格架及古地理演化[D].长春:吉林大学,2007.CHEN Xiu-yan.The Late Mesozoic Sequence Strati-graphic Framework and Palaeogeographic Evolutionin Sanjiang Area[D].Changchun:Jilin University,2007.
[18]何玉平.黑龙江省东部早白垩世沉积特征与原型盆地恢复[D].长春:吉林大学,2006.HE Yu-ping.The Early Cretaceous SedimentaryCharacteristics and Prototype Basin Restoration inEastern Heilongjiang Province[D].Changchun:JilinUniversity,2006.
[19]杨小菊.黑龙江省东部鸡西盆地早白垩世穆棱组植物化石新材料[J].古生物学报,2003,42(4):561-584.YANG Xiao-ju.New Material of Fossil Plants fromthe Early Cretaceous Muling Formation of the JixiBasin,Eastern Heilongjiang Province,China[J].ActaPalaeontologica Sinica,2003,42(4):561-584.
[20]杨小菊,何承全,黎文本,等.鸡西盆地早白垩世穆棱组海相沟鞭藻的发现及其古环境意义[J].科学通报,2003,48(14):1553-1556.YANG Xiao-ju,HE Cheng-quan,LI Wen-ben,et al.Marine Dinoflagellates from the Lower CrataceousMuling Formation of the Jixi Basin,China and TheirPalaeoenvironmental Significance[J].Chinese ScienceBulletin,2003,48(14):1553-1556.
[21]何承全,孙学坤.黑龙江省东部鸡西盆地城子河组下部早白垩世欧特里夫晚期海相沟鞭藻类[J].古生物学报,2000,39(1):46-62.HE Cheng-quan,SUN Xue-kun.Late Hauterivian Di-noflagellates from the Lower Part of the ChengziheFormation in Jixi Basin,Eastern Heilongjiang,NEChina[J].Acta Palaeontologica Sinica,2000,39(1):46-62.
[22]SHA J G,MATSUKAWA M,CAI H W,et al.TheUpper Jurassic-Lower Cretaceous of Eastern Hei-Longjiang,Northeast China:Stratigraphy and Region-al Basin History[J].Cretaceous Research,2003,24(6):715-728.
[23]贾承造,郑民.东北白垩纪大三江盆地沉积构造演化及其残留盆地群的油气勘探意义[J].大庆石油学院学报,2010,34(6):1-12.JIA Cheng-zao,ZHENG Min.Sedimentary History,Tectonic Evolution of Cretaceous Dasanjiang Basin inNortheast China and the Significance of Oil and GasExploration of Its Residual Basins[J].Journal ofDaqing Petroleum Institute,2010,34(6):1-12.
[24]陈秀艳,刘招君,何玉平,等.三江盆地群城子河组—穆棱组层序地层对比[J].科技导报,2010,28(22):55-59.CHEN Xiu-yan,LIU Zhao-jun,HE Yu-ping,et al.Se-quence Stratigraphy Correlation of Chengzihe-MulingFormation in Sanjiang Basins[J].Science and Tech-nology Review,2010,28(22):55-59.
[25]张云鹏,任建业,侯艳平,等.黑龙江东部大三江盆地群城子河组和穆棱组时期重矿物特征及物源分析[J].岩石矿物学杂志,2011,30(4):674-682.ZHANG Yun-peng,REN Jian-ye,HOU Yan-ping,et al.Heavy Mineral Characteristics and Provenance Analysisof Chengzihe and Muling Formations in DasanjiangBasin Group,East Heilongjiang Province[J].ActaPetrologica et Mineralogica,2011,30(4):674-682.
[26]王杰.鸡西盆地早白垩世沉积特征及物源分析[D].长春:吉林大学,2007.WANG Jie.The Early Cretaceous Sedimentary Char-acteristics and Analysis of the Provenances in JixiBasin[D].Changchun:Jilin University,2007.
[27]方石,张培震,刘招君,等.东三江盆地南部白垩纪以来的沉积特征及其演化[J].吉林大学学报:地球科学版,2012,42(1):66-76.FANG Shi,ZHANG Pei-zhen,LIU Zhao-jun,et al.Sedimentation Features and Its Evolution Since Creta-ceous in the South of Eastern Sanjiang Basin[J].Journal of Jilin University:Earth Science Edition,2012,42(1):66-76.
[28]曹洁,张永生,宋天锐,等.黑龙江东部盆地群白垩纪海侵存在的矿物学证据及其意义[J].地质通报,2010,29(7):1024-1030.CAO Jie,ZHANG Yong-sheng,SONG Tian-rui,et al.Mineralogical Evidences and Significance of Trans-gression Event in the Cretaceous Basins of EasternHeilongjiang Province,China[J].Geological Bulletinof China,2010,29(7):1024-1030.
[29]吉林大学地球科学学院.大庆探区外围中新生代断陷盆地群沉积充填特征及成盆规律[R].长春:吉林大学,2007.School of Earth Sciences,Jilin University.Sedimenta-tion-filing Characteristics and Basin-forming Rules inDown-faulted Basins Group of Mesozoic and CenozoicEra,Daqing Exploration Area[R].Changchun:JilinUniversity,2007.
[2]和钟铧,刘招君,张晓冬,等.黑龙江东部晚中生代盆地群构造层划分及构造沉积演化[J].世界地质,2009,28(1):20-27.HE Zhong-hua,LIU Zhao-jun,ZHANG Xiao-dong,et al.Subdivisions of Structural Layers and Tectonic-sedimentary Evolution of Eastern Basins in Hei-longjiang in Late Mesozoic[J].Global Geology,2009,28(1):20-27.
[3]杨晓平,李仰春,柳震,等.黑龙江东部鸡西盆地构造层序划分与盆地动力学演化[J].吉林大学学报:地球科学版,2005,35(5):616-621.YANG Xiao-ping,LI Yang-chun,LIU Zhen,et al.Classification of Tectonic Sequence and Dynamic Evo-lution of Jixi Basin,Eastern Heilongjiang Province[J].Journal of Jilin University:Earth Science Edi-tion,2005,35(5):616-621.
[4]孙革,刘风香.黑龙江鸡西含煤盆地早白垩世城子河组特尔姆叶(Tyrmia)的发现[J].煤田地质与勘探,2007,35(2):1-4.SUN Ge,LIU Feng-xiang.Discovery of TyrmiafromLower Cretaceous Chengzihe Formation in Jixi Coal-bearing Basin of Heilongjiang,China[J].Coal Geologyand Exploration,2007,35(2):1-4.
[5]于恩君.黑龙江省鸡西—勃利含煤盆地层序地层学讨论[J].吉林地质,2008,27(2):8-13.YU En-jun.Jixi-Boli Coal-bearing Basin StratigraphicSequence,Heilongjiang Province[J].Jilin Geology,2008,27(2):8-13.
[6]王金山.黑龙江省鸡西盆地南、北两带城子河组精细对比[J].中国煤炭地质,2008,20(8):5-9,25.WANG Jin-shan.Meticulous Correlation BetweenSouthern and Northern Belts of Chengzihe Formationin Jixi Basin,Heilongjiang Province[J].Coal Geologyof China,2008,20(8):5-9,25.
[7]杨绍芳.泛三江盆地成藏系统分析[J].石油天然气学报,2005,27(4):413-415.YANG Shao-fang.Analysis of Oil-gas Reservoir-forming System in Generic Sanjiang Basin,NortheastChina[J].Journal of Oil and Gas Technology,2005,27(4):413-415.
[8]刘云武,唐振国,刘文龙.三江盆地演化特征与油气勘探方向[J].石油天然气学报,2006,28(2):1-5.LIU Yun-wu,TANG Zhen-guo,LIU Wen-long.Evo-lutional Characteristics of Sanjiang Basin and Direc-tion of Hydrocarbon Exploration[J].Journal of Oiland Gas Technology,2006,28(2):1-5.
[9]胡志方,马义忠,乔桂林,等.三江盆地石油地质条件与勘探前景[J].河南石油,2006,20(1):1-4.HU Zhi-fang,MA Yi-zhong,QIAO Gui-lin,et al.Petroleum Geologic Conditions and Exploration Pros-pect of Sanjiang Basin[J].Henan Petroleum,2006,20(1):1-4.
[10]韩春花,曹成润,曹宪双,等.勃利盆地中生界地质特征与油气资源量计算[J].世界地质,2004,23(4):365-370.HAN Chun-hua,CAO Cheng-run,CAO Xian-shuang,et al.Mesozoic Geological Features and Calculation ofOil-gas Resources in Boli Basin[J].Global Geology,2004,23(4):365-370.
[11]杨建国,吴河勇,刘俊来.大庆探区外围盆地中、新生代地层对比及四大勘探层系[J].地质通报,2006,25(9/10):1088-1093.YANG Jian-guo,WU He-yong,LIU Jun-lai.Strati-graphic Correlation of the Mesozoic and Cenozoic inthe Outer Basins of the Daqing Exploration Area[J].Geological Bulletin of China,2006,25(9/10):1088-1093.
[12]成都理工大学地球科学学院.大庆探区外围盆地含油气性评价与优选[R].成都:成都理工大学,2003.School of Earth Sciences,Chengdu University ofTechnology.Evaluation and Optimum of PeripheralBasins in Daqing Exploration Area[R].Chengdu:Chengdu University of Technology,2003.
[13]李仰春,娄本军,杨晓平,等.黑龙江鸡西盆地北部穆棱组高分辨率层序地层[J].地球科学与环境学报,2007,29(3):263-268.LI Yang-chun,LOU Ben-jun,YANG Xiao-ping,et al.High-resolution Sequence Stratigraphy of MulingFormation in Jixi Basin of Northern HeilongjiangProvince[J].Journal of Earth Sciences and Environ-ment,2007,29(3):263-268.
[14]王伟涛,刘招君,陈秀艳.虎林盆地北部坳陷中、新生代碎屑岩源区构造背景与物源区分析[J].世界地质,2007,26(1):14-19.WANG Wei-tao,LIU Zhao-jun,CHEN Xiu-yan.Tec-tonic Setting and Provenance Analysis of Mesozoic-Cenozoic Clastic Rocks in Northern Depression ofHulin Basin[J].Global Geology,2007,26(1):14-19.
[15]王孔伟,张帆,林东成.汤原断陷构造活动对沉积的控制[J].石油地质与工程,2007,21(6):7-10.WANG Kong-wei,ZHANG Fan,LIN Dong-cheng.The Control of Tectonic Activities on Sedimentationin Tangyuan Fault Depression Basin[J].PetroleumGeology and Engineering,2007,21(6):7-10.
[16]温泉波,刘永江,李俊杰,等.鸡西、勃利盆地白垩纪砂岩的物源分析及构造意义[J].沉积与特提斯地质,2008,28(3):52-59.WEN Quan-bo,LIU Yong-jiang,LI Jun-jie,et al.Provenance Analysis and Tectonic Implications forthe Cretaceous Sandstones in the Jixi and Boli Basins,Heilongjiang[J].Sedimentary Geology and TethyanGeology,2008,28(3):52-59.
[17]陈秀艳.三江地区晚中生代层序地层格架及古地理演化[D].长春:吉林大学,2007.CHEN Xiu-yan.The Late Mesozoic Sequence Strati-graphic Framework and Palaeogeographic Evolutionin Sanjiang Area[D].Changchun:Jilin University,2007.
[18]何玉平.黑龙江省东部早白垩世沉积特征与原型盆地恢复[D].长春:吉林大学,2006.HE Yu-ping.The Early Cretaceous SedimentaryCharacteristics and Prototype Basin Restoration inEastern Heilongjiang Province[D].Changchun:JilinUniversity,2006.
[19]杨小菊.黑龙江省东部鸡西盆地早白垩世穆棱组植物化石新材料[J].古生物学报,2003,42(4):561-584.YANG Xiao-ju.New Material of Fossil Plants fromthe Early Cretaceous Muling Formation of the JixiBasin,Eastern Heilongjiang Province,China[J].ActaPalaeontologica Sinica,2003,42(4):561-584.
[20]杨小菊,何承全,黎文本,等.鸡西盆地早白垩世穆棱组海相沟鞭藻的发现及其古环境意义[J].科学通报,2003,48(14):1553-1556.YANG Xiao-ju,HE Cheng-quan,LI Wen-ben,et al.Marine Dinoflagellates from the Lower CrataceousMuling Formation of the Jixi Basin,China and TheirPalaeoenvironmental Significance[J].Chinese ScienceBulletin,2003,48(14):1553-1556.
[21]何承全,孙学坤.黑龙江省东部鸡西盆地城子河组下部早白垩世欧特里夫晚期海相沟鞭藻类[J].古生物学报,2000,39(1):46-62.HE Cheng-quan,SUN Xue-kun.Late Hauterivian Di-noflagellates from the Lower Part of the ChengziheFormation in Jixi Basin,Eastern Heilongjiang,NEChina[J].Acta Palaeontologica Sinica,2000,39(1):46-62.
[22]SHA J G,MATSUKAWA M,CAI H W,et al.TheUpper Jurassic-Lower Cretaceous of Eastern Hei-Longjiang,Northeast China:Stratigraphy and Region-al Basin History[J].Cretaceous Research,2003,24(6):715-728.
[23]贾承造,郑民.东北白垩纪大三江盆地沉积构造演化及其残留盆地群的油气勘探意义[J].大庆石油学院学报,2010,34(6):1-12.JIA Cheng-zao,ZHENG Min.Sedimentary History,Tectonic Evolution of Cretaceous Dasanjiang Basin inNortheast China and the Significance of Oil and GasExploration of Its Residual Basins[J].Journal ofDaqing Petroleum Institute,2010,34(6):1-12.
[24]陈秀艳,刘招君,何玉平,等.三江盆地群城子河组—穆棱组层序地层对比[J].科技导报,2010,28(22):55-59.CHEN Xiu-yan,LIU Zhao-jun,HE Yu-ping,et al.Se-quence Stratigraphy Correlation of Chengzihe-MulingFormation in Sanjiang Basins[J].Science and Tech-nology Review,2010,28(22):55-59.
[25]张云鹏,任建业,侯艳平,等.黑龙江东部大三江盆地群城子河组和穆棱组时期重矿物特征及物源分析[J].岩石矿物学杂志,2011,30(4):674-682.ZHANG Yun-peng,REN Jian-ye,HOU Yan-ping,et al.Heavy Mineral Characteristics and Provenance Analysisof Chengzihe and Muling Formations in DasanjiangBasin Group,East Heilongjiang Province[J].ActaPetrologica et Mineralogica,2011,30(4):674-682.
[26]王杰.鸡西盆地早白垩世沉积特征及物源分析[D].长春:吉林大学,2007.WANG Jie.The Early Cretaceous Sedimentary Char-acteristics and Analysis of the Provenances in JixiBasin[D].Changchun:Jilin University,2007.
[27]方石,张培震,刘招君,等.东三江盆地南部白垩纪以来的沉积特征及其演化[J].吉林大学学报:地球科学版,2012,42(1):66-76.FANG Shi,ZHANG Pei-zhen,LIU Zhao-jun,et al.Sedimentation Features and Its Evolution Since Creta-ceous in the South of Eastern Sanjiang Basin[J].Journal of Jilin University:Earth Science Edition,2012,42(1):66-76.
[28]曹洁,张永生,宋天锐,等.黑龙江东部盆地群白垩纪海侵存在的矿物学证据及其意义[J].地质通报,2010,29(7):1024-1030.CAO Jie,ZHANG Yong-sheng,SONG Tian-rui,et al.Mineralogical Evidences and Significance of Trans-gression Event in the Cretaceous Basins of EasternHeilongjiang Province,China[J].Geological Bulletinof China,2010,29(7):1024-1030.
[29]吉林大学地球科学学院.大庆探区外围中新生代断陷盆地群沉积充填特征及成盆规律[R].长春:吉林大学,2007.School of Earth Sciences,Jilin University.Sedimenta-tion-filing Characteristics and Basin-forming Rules inDown-faulted Basins Group of Mesozoic and CenozoicEra,Daqing Exploration Area[R].Changchun:JilinUniversity,2007.
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