松辽盆地北部白垩纪超层序特征
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摘要
松辽盆地北部白垩系由3个超层序组、8个超层序、28个沉积层序组成。断陷湖盆期发育3个超层序和6个沉积层序,以火山岩与粗碎屑岩组合为特征。断拗转化期形成1个超层序和4个沉积层序,以中粗碎屑岩为特征。典型的大型拗陷湖盆期,可识别出3个超层序和15个沉积层序,以湖泊、三角洲相中细碎屑岩沉积为主,水进体系域和高水位体系域沉积时期半深湖—深湖相暗色泥岩广为发育。湖盆萎缩期,可识别出1个超层序和3个沉积层序,以湖泊、三角洲相中粗碎屑岩沉积为主。超层序组界面包括白垩系基岩顶面、营城组顶界面和嫩江组顶界面,与燕山运动各主要幕次形成的区域不整合面相对应,区域构造运动对其起着重要的控制作用。超层序界面可以是上述超层序组界面,也可由平行不整合面和剥蚀界面构成。超层序界面处沉积间断的时间较长,河道下切、地层缺失、暴露等沉积现象发育,与岩石地层单位界面一致。沉积层序界面处沉积间断的时间相对超层序界面要短,与岩石地层单位界面往往不一致。超层序界面在地震剖面上最明显的特征是出现削截、上超和顶超等反射终止现象,岩性、测井曲线也发生剧烈变化。
The Cretaceous in northern Songliao Basin can be divided into three supersequence sets,eight supersequences and twenty-eight sequences. Volcanic and coarse clastic successions formed during faulting stage contain three supersequences and six sequences. Medium-coarse grained clastics formed in the interim stage from faulting stage to depression stage contain one supersequence and four sequences. During the depression stage the lithology is dominated by lacustrine and deltaic medium-fine grained clasuics and can be divided into three supersequences and fifteen sequences. During uhe deposition of transgressive systems tract(TST)and highstand systems tract(HST)semi-deep and deep lacustrine dark mudstone were widely deposited. One supersequence and three sequences were identified during the shrinkage phase of lake basin when the lacustrine and deltaic medium-coarse grained clastics were dominant.Supersequence set boundaries that were controlled by tectogenesis, include the top boundaries of Cretaceous bedrock, Yingcheng Formation and Nenjiang Formation, which correspond to regional unconformities formed by major tectonic phases of Yanshan Movement. Supersequence boundaries can be either supersequence set boundaries disconformities or erosional surfaces levels. At the supersequence boundaries, the depositional hiatus is quite long, so that channel downcutting, stratigraphic gap and exposure etc. widely exist. Supersequence boundaries are in accord with lithostratigraphic unit boundaries. Compared to supersequence boundaries, the depositional hiatus at sequence boundaries is shorter and sequence boundaries are not compatible with lithostratigraphic unit boundaries. Supersequence boundaries are characterized by truncation, onlap and toplap etc. on the seismic sections and sudden change of lithology and logging curve.
The Cretaceous in northern Songliao Basin can be divided into three supersequence sets,eight supersequences and twenty-eight sequences. Volcanic and coarse clastic successions formed during faulting stage contain three supersequences and six sequences. Medium-coarse grained clastics formed in the interim stage from faulting stage to depression stage contain one supersequence and four sequences. During the depression stage the lithology is dominated by lacustrine and deltaic medium-fine grained clasuics and can be divided into three supersequences and fifteen sequences. During uhe deposition of transgressive systems tract(TST)and highstand systems tract(HST)semi-deep and deep lacustrine dark mudstone were widely deposited. One supersequence and three sequences were identified during the shrinkage phase of lake basin when the lacustrine and deltaic medium-coarse grained clastics were dominant.Supersequence set boundaries that were controlled by tectogenesis, include the top boundaries of Cretaceous bedrock, Yingcheng Formation and Nenjiang Formation, which correspond to regional unconformities formed by major tectonic phases of Yanshan Movement. Supersequence boundaries can be either supersequence set boundaries disconformities or erosional surfaces levels. At the supersequence boundaries, the depositional hiatus is quite long, so that channel downcutting, stratigraphic gap and exposure etc. widely exist. Supersequence boundaries are in accord with lithostratigraphic unit boundaries. Compared to supersequence boundaries, the depositional hiatus at sequence boundaries is shorter and sequence boundaries are not compatible with lithostratigraphic unit boundaries. Supersequence boundaries are characterized by truncation, onlap and toplap etc. on the seismic sections and sudden change of lithology and logging curve.
引文
[1]王建功.2006.松辽盆地北部青山口组层序地层、沉积相与成藏条件研究.大庆油田有限责任公司勘探开发研究院内部报告
[2]王雅峰.2006.松辽盆地北部葡萄花油层高分辨率层序地层学及隐蔽油气藏分布规律研究.大庆油田有限责任公司勘探开发研究院内部报告
陈丕基.2000.中国陆相侏罗—白垩系划分对比述评[J].地层学杂志,24(2):114-119.
陈烨菲,彭仕宓,钟显彪,等.2003.松辽盆地四五家子油田下白垩统泉头组沉积相[J].古地理学报,5(3):316-327.
高瑞祺,赵传本,乔秀云,等.1999.松辽盆地白垩纪石油地层孢粉学[M].北京:地质出版社,1-373.
黄清华,谭伟,杨会臣.1999.松辽盆地白垩纪地层序列与年代地层[J].大庆石油地质与开发,18(6):15-28.
林春明,冯志强,张顺,等.2006.松辽盆地北部晚白垩世青山口-姚家组层序地层界面特征[J].西北大学学报(自然科学版),36(增刊):174-178.
林春明,凌洪飞,王淑君,等.2002a.苏皖地区石炭纪海相碳酸盐岩碳、氧同位素演化规律[J].地球化学,31(5):415-423.
林春明,王淑君,张顺,等.2002b.苏皖地区石炭系露头层序地层研究[J].沉积学报,20(4):537-544.
林春明,杨湘宁,卓弘春,等.2005.贵州宗地剖面晚石炭世-二叠纪早期层序地层特征[J].地质论评,51(6):698-707.
刘招君,董清水,王嗣敏,等.2002.陆相层序地层学导论与应用[M].北京:石油工业出版社,1-178.
刘招君,王东坡,刘立,等.1992.松辽盆地白垩纪沉积特征[J].地质学报,66(4):327—338.
蒙启安,王璞君,杨宝俊,等.2005.松辽盆地断陷期超层序界面的地质属性刻画及其油气地质意义[J].地质论评,51(1):46-54.
王东坡,刘招君,刘立.1994.松辽盆地演化与海平面升降[M].北京:地质出版社,1-60.
王鸿祯,史晓颖.1998.沉积层序及海平面旋回的分类级别—旋回周期的成因讨论[J].现代地质,12(1):1-16.
王璞?,杜小弟,王俊,等.1995.松辽盆地白垩纪年代地层研究及地层时代划分[J].地质学报,69(4):372-381.
王志武主编.1993.中国石油地质志(卷2)[M].北京:石油工业出版社,55-305.
魏魁生,徐怀大,雷怀玉,等.1996.非海相层序地层学———以松辽盆地为例[M].北京:地质出版社,1-94.
辛仁臣,蔡希源,王英民.2004.松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,22(3):387-392.
杨万里主编.1985.松辽陆相盆地石油地质[M].北京:石油工业出版社,47-207.
叶得泉,黄清华,张莹,等.2002.松辽盆地白垩纪介形类生物地层学[M].北京:石油工业出版社,1-98.
殷鸿福,童金南.1995.层序地层界面与年代地层界线的关系[J]科学通报,40(6):539-541.
郑玉龙,陈春瑞,任林伟.2005.松辽盆地上白垩统陆相遗迹化石及其沉积环境[J].古地理学报,7(3):337-346.
卓弘春,林春明,李艳丽,等.2007.松辽盆地北部上白垩统青山口-姚家组沉积相及层序地层界面特征[J].沉积学报,25(1):71-79.
Chen Piji.2000.Comments on the classification and correlation of non-marine Jurassic and Cretaceous of China[J].Journal of Stratigra-phy,24(2):114-119(in Chinese with English abstract).
Chen Yefei,Peng Shimi,Zhong Xianbiao,et al.2003.Sedimentary fa-cies of the Quantou Formation of Lower Cretaceous at Siwujiazi Oil-field of Songliao Basin[J].Journal of Palaeogeography,5(3):316-327(in Chinese with English abstract).
Gao Ruiqi,Zhao Chuanben,Qiao Xiuyun,et al.1999.Cretaceous OilStrata Palynology from Songliao Basin[M].Beijing:GeologicalPublishing House,1-373(in Chinese with English abstract).
Haq B U,Hardenbol J,Vail P R.1987.Chronology of fluctuating sealevels since the Triassic[J].Science,235:1,156-1,167.
Huang Qinghua,Tan Wei,Yang Huichen.1999.Cretaceous sequencestratification and chronostratigraphy[J].Petroleum Geology&Oil-field Development of Daqing,18(6):15-28(in Chinese).
Lin Chunming,Feng Zhiqiang,Zhang Shun,et al.2006.Characteristics of sequence boundary in Late Cretaceous Qingshankou-Yaojia For-mation of northern Songliao Basin[J].Journal of Northwest Univer-sity,36(suppl.):174-178(in Chinese with English abstract).
Lin Chunming,Ling Hongfei,Wang Shujun,et al.2002a.The evolu-tion regularities of carbon and oxygen isotopes in Carboniferous ma-rine carbonate rocks from Jiangsu and Anhui provinces,China[J].Geochimica,31(5):415-423(in Chinese with English abstract).
Lin Chunming,Wang Shujun,Zhang Shun,et al.2002b.Study on out-crops sequence stratigraphy on the Carboniferous strata in Anhui andJiangsu provinces,China[J].Acta Sedimentologica Sinica,20(4):537-544(in Chinese with English abstract).
Lin Chunming,Yang Xiangning,Zhuo Hongchun,et al.2005.OutcropsSequence Stratigraphy on the Late Carboniferous-Early Permian Stra-ta at Zongdi in Guizhou Province,China[J].Geological Review,51(6):698-707(in Chinese with English abstract).
Liu Zhaojun,Dong Qingshui,Wang Simin,et al.2002.Introductionand Application of Continental Sequence Stratigraphy[M].Bei-jing:Petroleum Industry Press,1-178(in Chinese with Englishabstract).
Liu Zhaojun,Wang Dongpo,Liu Li,et al.1992.Sedimentary charac-teristics of the Cretaceous in Songliao Basin[J].Acta GeologicaSinica,66(4):327-338(in Chinese with English abstract).
Meng Qi an,Wang Pujun,Yang Baojun,et al.2005.Geological signa-tures of sequence boundary of the Songliao Basin:Newinterpretationand their relation to gas accumulation[J].Geological Review,51(1):46-54(in Chinese with English abstract).
Shanley K W,McCabe P J.1994.Perspectives on the sequence stratig-raphy of continental strata[J].AAPG Bulletin,78(4):544-568.
Vail P R,Audemard F,Bowman S A,et al.1991.The stratigraphic sig-natures of tectonics,eustasy and sedimentology:An overview[C].In:Einsele G,et al(eds).Cycles and Event in Stratigraphy.BelinHeidberg:Springer-Verlag,617-659.
Van Wagoner J C,Posamentier HW,Mitchum R M,et al.1988.An o-verview of the fundamentals of sequence stratigraphy and key defini-tions[M].In:Wilgus C K,et al(eds).Sea-level Changes:AnIntegrated Approach.SEPMSpecial Publication,42:39-45.
Wang Dongpo,Liu Zhaojun,Liu Li.1994.Evolution and Sea LevelChanges of Songliao Basin[M].Beijing:Geological PublishingHouse,1-60(in Chinese with English abstract).
Wang Hongzhen,Shi Xiaoying.1998.Hierarchy of depositional se-quences and eustatic cycles:Adiscussion on the mechanism of sedi-mentary cycles[J].Geoscience,12(1):1-16(in Chinese withEnglish abstract).
Wang Pujun,Du Xiaodi,Wang Jun,et al.1995.The chronostratigraphyand stratigraphic classification of the Cretaceous of the Songliao Ba-sin[J].Acta Geologica Sinica,69(4):372-381(in Chinesewith English abstract).
Wang Zhiwu.1993.Petroleum Geology of China(Vol.2)[M].Bei-jing:Petroleum Industry Press,55-305(in Chinese with English abstract).
Wei Kuisheng,Xu Huaida,Lei Huaiyu,et al.1996.Nonmarine se-quence stratigraphy:Example of Songliao Basin[M].Beijing:Ge-ological Publishing House,1-94(in Chinese).
Xin Renchen,Cai Xiyuan,Wang Yingmin.2004.Depositional model oflowstand system tract and characteristics of sequence boundary indeep-water lake,Songliao Depression Basin[J].Acta Sedimento-logica Sinica,22(3):387-392(in Chinese with English ab-stract).
Xue L Q,Galloway W E.1993.Genetic sequence stratigraphic frame-work,depositional style and hydrocarbon occurrence of the UpperCretaceous QYN Formations in the Songliao lacustrine Basin,north-eastern China[J].AAPG Bulletin,77(10):1,792-1,808.
Yang Wanli.1985.Monograph on Continental Petroleum Geology inSongliao Basin[M].Beijing:Petroleum Industry Press,47-207(in Chinese with English abstract).
Ye Dequan,Huang Qinghua,Zhang Ying,et al.2002.Biostratigraphyof Cretaceous Ostracoda from the Songliao Basin[M].Beijing:Pe-troleum Industry Press,1-98(in Chinese with English abstract).
Yin Hongfu,Tong Jinnan.1995.Relationship between sequence stratig-raphical boundary and chronostratigraphical boundary[J].ChineseScience Bulletin,40(6):539-541(in Chinese with English ab-stract).
Zheng Yulong,Chen Chunrui,Ren Linwei.2005.Continental trace fos-sils and their sedimentary environments of the Upper Cretaceous inSongliao Basin[J].Journal of Palaeogeography,7(3):337-346(in Chinese with English abstract).
Zhuo Hongchun,Lin Chunming,Li Yanli,et al.2007.Characteristicsof sedimentary facies and sequence boundary in Upper CretaceousQingshankou-Yaojia Formation of Northern Songliao Basin[J].Ac-ta Sedimentologica Sinica,25(1):71-79(in Chinese with Englishabstract).
[2]王雅峰.2006.松辽盆地北部葡萄花油层高分辨率层序地层学及隐蔽油气藏分布规律研究.大庆油田有限责任公司勘探开发研究院内部报告
陈丕基.2000.中国陆相侏罗—白垩系划分对比述评[J].地层学杂志,24(2):114-119.
陈烨菲,彭仕宓,钟显彪,等.2003.松辽盆地四五家子油田下白垩统泉头组沉积相[J].古地理学报,5(3):316-327.
高瑞祺,赵传本,乔秀云,等.1999.松辽盆地白垩纪石油地层孢粉学[M].北京:地质出版社,1-373.
黄清华,谭伟,杨会臣.1999.松辽盆地白垩纪地层序列与年代地层[J].大庆石油地质与开发,18(6):15-28.
林春明,冯志强,张顺,等.2006.松辽盆地北部晚白垩世青山口-姚家组层序地层界面特征[J].西北大学学报(自然科学版),36(增刊):174-178.
林春明,凌洪飞,王淑君,等.2002a.苏皖地区石炭纪海相碳酸盐岩碳、氧同位素演化规律[J].地球化学,31(5):415-423.
林春明,王淑君,张顺,等.2002b.苏皖地区石炭系露头层序地层研究[J].沉积学报,20(4):537-544.
林春明,杨湘宁,卓弘春,等.2005.贵州宗地剖面晚石炭世-二叠纪早期层序地层特征[J].地质论评,51(6):698-707.
刘招君,董清水,王嗣敏,等.2002.陆相层序地层学导论与应用[M].北京:石油工业出版社,1-178.
刘招君,王东坡,刘立,等.1992.松辽盆地白垩纪沉积特征[J].地质学报,66(4):327—338.
蒙启安,王璞君,杨宝俊,等.2005.松辽盆地断陷期超层序界面的地质属性刻画及其油气地质意义[J].地质论评,51(1):46-54.
王东坡,刘招君,刘立.1994.松辽盆地演化与海平面升降[M].北京:地质出版社,1-60.
王鸿祯,史晓颖.1998.沉积层序及海平面旋回的分类级别—旋回周期的成因讨论[J].现代地质,12(1):1-16.
王璞?,杜小弟,王俊,等.1995.松辽盆地白垩纪年代地层研究及地层时代划分[J].地质学报,69(4):372-381.
王志武主编.1993.中国石油地质志(卷2)[M].北京:石油工业出版社,55-305.
魏魁生,徐怀大,雷怀玉,等.1996.非海相层序地层学———以松辽盆地为例[M].北京:地质出版社,1-94.
辛仁臣,蔡希源,王英民.2004.松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,22(3):387-392.
杨万里主编.1985.松辽陆相盆地石油地质[M].北京:石油工业出版社,47-207.
叶得泉,黄清华,张莹,等.2002.松辽盆地白垩纪介形类生物地层学[M].北京:石油工业出版社,1-98.
殷鸿福,童金南.1995.层序地层界面与年代地层界线的关系[J]科学通报,40(6):539-541.
郑玉龙,陈春瑞,任林伟.2005.松辽盆地上白垩统陆相遗迹化石及其沉积环境[J].古地理学报,7(3):337-346.
卓弘春,林春明,李艳丽,等.2007.松辽盆地北部上白垩统青山口-姚家组沉积相及层序地层界面特征[J].沉积学报,25(1):71-79.
Chen Piji.2000.Comments on the classification and correlation of non-marine Jurassic and Cretaceous of China[J].Journal of Stratigra-phy,24(2):114-119(in Chinese with English abstract).
Chen Yefei,Peng Shimi,Zhong Xianbiao,et al.2003.Sedimentary fa-cies of the Quantou Formation of Lower Cretaceous at Siwujiazi Oil-field of Songliao Basin[J].Journal of Palaeogeography,5(3):316-327(in Chinese with English abstract).
Gao Ruiqi,Zhao Chuanben,Qiao Xiuyun,et al.1999.Cretaceous OilStrata Palynology from Songliao Basin[M].Beijing:GeologicalPublishing House,1-373(in Chinese with English abstract).
Haq B U,Hardenbol J,Vail P R.1987.Chronology of fluctuating sealevels since the Triassic[J].Science,235:1,156-1,167.
Huang Qinghua,Tan Wei,Yang Huichen.1999.Cretaceous sequencestratification and chronostratigraphy[J].Petroleum Geology&Oil-field Development of Daqing,18(6):15-28(in Chinese).
Lin Chunming,Feng Zhiqiang,Zhang Shun,et al.2006.Characteristics of sequence boundary in Late Cretaceous Qingshankou-Yaojia For-mation of northern Songliao Basin[J].Journal of Northwest Univer-sity,36(suppl.):174-178(in Chinese with English abstract).
Lin Chunming,Ling Hongfei,Wang Shujun,et al.2002a.The evolu-tion regularities of carbon and oxygen isotopes in Carboniferous ma-rine carbonate rocks from Jiangsu and Anhui provinces,China[J].Geochimica,31(5):415-423(in Chinese with English abstract).
Lin Chunming,Wang Shujun,Zhang Shun,et al.2002b.Study on out-crops sequence stratigraphy on the Carboniferous strata in Anhui andJiangsu provinces,China[J].Acta Sedimentologica Sinica,20(4):537-544(in Chinese with English abstract).
Lin Chunming,Yang Xiangning,Zhuo Hongchun,et al.2005.OutcropsSequence Stratigraphy on the Late Carboniferous-Early Permian Stra-ta at Zongdi in Guizhou Province,China[J].Geological Review,51(6):698-707(in Chinese with English abstract).
Liu Zhaojun,Dong Qingshui,Wang Simin,et al.2002.Introductionand Application of Continental Sequence Stratigraphy[M].Bei-jing:Petroleum Industry Press,1-178(in Chinese with Englishabstract).
Liu Zhaojun,Wang Dongpo,Liu Li,et al.1992.Sedimentary charac-teristics of the Cretaceous in Songliao Basin[J].Acta GeologicaSinica,66(4):327-338(in Chinese with English abstract).
Meng Qi an,Wang Pujun,Yang Baojun,et al.2005.Geological signa-tures of sequence boundary of the Songliao Basin:Newinterpretationand their relation to gas accumulation[J].Geological Review,51(1):46-54(in Chinese with English abstract).
Shanley K W,McCabe P J.1994.Perspectives on the sequence stratig-raphy of continental strata[J].AAPG Bulletin,78(4):544-568.
Vail P R,Audemard F,Bowman S A,et al.1991.The stratigraphic sig-natures of tectonics,eustasy and sedimentology:An overview[C].In:Einsele G,et al(eds).Cycles and Event in Stratigraphy.BelinHeidberg:Springer-Verlag,617-659.
Van Wagoner J C,Posamentier HW,Mitchum R M,et al.1988.An o-verview of the fundamentals of sequence stratigraphy and key defini-tions[M].In:Wilgus C K,et al(eds).Sea-level Changes:AnIntegrated Approach.SEPMSpecial Publication,42:39-45.
Wang Dongpo,Liu Zhaojun,Liu Li.1994.Evolution and Sea LevelChanges of Songliao Basin[M].Beijing:Geological PublishingHouse,1-60(in Chinese with English abstract).
Wang Hongzhen,Shi Xiaoying.1998.Hierarchy of depositional se-quences and eustatic cycles:Adiscussion on the mechanism of sedi-mentary cycles[J].Geoscience,12(1):1-16(in Chinese withEnglish abstract).
Wang Pujun,Du Xiaodi,Wang Jun,et al.1995.The chronostratigraphyand stratigraphic classification of the Cretaceous of the Songliao Ba-sin[J].Acta Geologica Sinica,69(4):372-381(in Chinesewith English abstract).
Wang Zhiwu.1993.Petroleum Geology of China(Vol.2)[M].Bei-jing:Petroleum Industry Press,55-305(in Chinese with English abstract).
Wei Kuisheng,Xu Huaida,Lei Huaiyu,et al.1996.Nonmarine se-quence stratigraphy:Example of Songliao Basin[M].Beijing:Ge-ological Publishing House,1-94(in Chinese).
Xin Renchen,Cai Xiyuan,Wang Yingmin.2004.Depositional model oflowstand system tract and characteristics of sequence boundary indeep-water lake,Songliao Depression Basin[J].Acta Sedimento-logica Sinica,22(3):387-392(in Chinese with English ab-stract).
Xue L Q,Galloway W E.1993.Genetic sequence stratigraphic frame-work,depositional style and hydrocarbon occurrence of the UpperCretaceous QYN Formations in the Songliao lacustrine Basin,north-eastern China[J].AAPG Bulletin,77(10):1,792-1,808.
Yang Wanli.1985.Monograph on Continental Petroleum Geology inSongliao Basin[M].Beijing:Petroleum Industry Press,47-207(in Chinese with English abstract).
Ye Dequan,Huang Qinghua,Zhang Ying,et al.2002.Biostratigraphyof Cretaceous Ostracoda from the Songliao Basin[M].Beijing:Pe-troleum Industry Press,1-98(in Chinese with English abstract).
Yin Hongfu,Tong Jinnan.1995.Relationship between sequence stratig-raphical boundary and chronostratigraphical boundary[J].ChineseScience Bulletin,40(6):539-541(in Chinese with English ab-stract).
Zheng Yulong,Chen Chunrui,Ren Linwei.2005.Continental trace fos-sils and their sedimentary environments of the Upper Cretaceous inSongliao Basin[J].Journal of Palaeogeography,7(3):337-346(in Chinese with English abstract).
Zhuo Hongchun,Lin Chunming,Li Yanli,et al.2007.Characteristicsof sedimentary facies and sequence boundary in Upper CretaceousQingshankou-Yaojia Formation of Northern Songliao Basin[J].Ac-ta Sedimentologica Sinica,25(1):71-79(in Chinese with Englishabstract).
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