苏北盆地白驹凹陷古近系层序地层特征及充填演化模式
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摘要
根据陆相断陷盆地层序界面在电测曲线和地震剖面上的识别标志、岩石类型组合特点以及古生物资料等方面的特征,在苏北盆地白驹凹陷古近系共识别出6个层序界面,划分出1个超层序组、2个超层序、5个三级层序,其中SQ1、SQ2~SQ4分别为断陷Ⅰ幕初始断陷、断陷-坳陷转化阶段的湖泊层序,SQ5为断陷Ⅲ幕断陷收敛阶段的河流层序。根据盆地幕式构造演化、气候条件以及物源供给的条件不同,建立了初始断陷阶段、断陷-坳陷转换阶段和断陷收敛阶段3种层序地层充填模式,认为不同构造演化阶段的充填序列、体系域构成和砂体发育存在显著的差异。初步分析了不同层序充填演化模式与油气的关系,认为断陷Ⅰ幕的断陷-坳陷转换阶段的充填层序低位体系域和高位体系域砂体与湖侵体系域优质烃源岩配置关系最好,成藏条件最优越。
Based on the identification features of stratigraphic sequences of the continental faulted basin along electric logging curves and seismic profiles as well as the characteristics of lithologic combination and palaeontological data,the authors identified six Paleogene sequence boundaries in Baiju sag of Subei basin and divided the Paleogene into one super sequence group,two super sequences,and five sequences.SQ1 and SQ2~SQ4 are lacustrine sequences developed in the initial faulting phase and faulting-depression stage of faulting episode I,while SQ5 is the fluvial sequence developed in the faulting convergence stage of faulting episode Ⅲ.Based on the episodic tectonic evolution,different climate conditions and suppy of sediments for the basin in each evolution phase,the authors established three kinds of sequence stratigraphy filling evolution models composed of initial faulting phase,faulting-depression stage and faulting convergence stage.It is thought that differenttectono-evolutionary stages have significantly different filling sequences,system tract constituents and sand body developments.A preliminary analysis was made on the relationship between sequence stratigraphic filling evolution models and oil-gas exploration potentials,which reveals that the configuration relationship between sand bodies in lowstand and highstand systems tracts and hydrocarbon source rock in lacustrine transgressive system tract of faulting-depression stage of the faulting episodeⅠ is the best in that it has the most advantageous hydrocarbon accumulation condition.
Based on the identification features of stratigraphic sequences of the continental faulted basin along electric logging curves and seismic profiles as well as the characteristics of lithologic combination and palaeontological data,the authors identified six Paleogene sequence boundaries in Baiju sag of Subei basin and divided the Paleogene into one super sequence group,two super sequences,and five sequences.SQ1 and SQ2~SQ4 are lacustrine sequences developed in the initial faulting phase and faulting-depression stage of faulting episode I,while SQ5 is the fluvial sequence developed in the faulting convergence stage of faulting episode Ⅲ.Based on the episodic tectonic evolution,different climate conditions and suppy of sediments for the basin in each evolution phase,the authors established three kinds of sequence stratigraphy filling evolution models composed of initial faulting phase,faulting-depression stage and faulting convergence stage.It is thought that differenttectono-evolutionary stages have significantly different filling sequences,system tract constituents and sand body developments.A preliminary analysis was made on the relationship between sequence stratigraphic filling evolution models and oil-gas exploration potentials,which reveals that the configuration relationship between sand bodies in lowstand and highstand systems tracts and hydrocarbon source rock in lacustrine transgressive system tract of faulting-depression stage of the faulting episodeⅠ is the best in that it has the most advantageous hydrocarbon accumulation condition.
引文
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陶丽,张廷山,戴传瑞,李秋菊,李斌.2010.苏北盆地白驹凹陷泰州组一段沉积物源分析[J].中国地质,37(2):414-420.
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严德天,王华,王清晨.2008.中国东部第三系典型断陷盆地幕式构造旋回及层序地层特征[J].石油学报,29(2):185-190.
张喜林,朱筱敏,钟大康,梁兵,曹冰,贺向阳.2004.苏北盆地高邮凹陷第三系—上白垩统层序地层格架特征[J].沉积学报,22(3):393-399.
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顾家裕,范土芝.2001.层序地层学回顾与展望[J].海相油气地质,6(4):15-25.
顾家裕.1995.陆相盆地层序地层学格架概念及模式[J].石油勘探与开发,22(4):6-10.
纪友亮,张世奇,张宏,张立强.1998.层序地层学原理及层序成因机制模式[M].北京:地质出版社.
纪友亮,张世奇.1996.陆相断陷湖盆层序地层学[M].北京:石油工业出版社.
姜在兴.2003.沉积学[M].北京:石油工业出版社:7-498.
柯光明,郑荣才,石和.2006.苏北盆地古近纪构造-层序岩相古地理特征与演化[J].中国地质,33(6):1305-1311.
李思田,林畅松,解习农,杨士恭,焦养泉.1995.大型陆相盆地层序地层学研究——以鄂尔多斯中生代盆地为例[J].地学前缘,2(3-4):133-148.
李思田,杨士恭,林畅松.1992.论沉积盆地等时地层格架和基本建造单元[J].沉积学报,10(4):11-22.
廖远涛,王振升,肖敦清,韦阿娟,王家豪,严德天.2008.黄骅坳陷中区古近系层序构成样式分析[J].地球学报,29(2):221-227.
林畅松,张燕梅,李思田,任建业,张英志.2004.中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型[J].地球科学——中国地质大学学报,29(5):583-588.
刘宝珺,曾允孚.1985.岩相古地理基础和工作方法[M].北京:地质出版社.
刘长利,朱筱敏,王兴明,任红民,李树静.2010.苏北盆地海安凹陷泰州组层序地层及沉积特征[J].吉林大学学报(地球科学版),40(3):519-526.
刘成林,朱筱敏,费安玮,朱玉新,张英.2003.苏北盆地白驹凹陷深层油气成藏研究[J].西南石油学院学报,25(5):23-25.
罗怀忠,梁兴,张介辉,周松源.2010.苏北盆地白驹凹陷油气富集规律与成藏模式[J].天然气工业,30(9):22-24.
邱海峻,许志琴,乔德武.2006.苏北盆地构造演化研究进展[J].地质通报,25(9-10):1117-1120.
邱旭明,刘玉瑞,傅强.2006.苏北盆地上白垩统-第三系层序地层与沉积演化[M].北京:地质出版社:7-37.
沈玉林,郭英海,李壮福,魏新善,贾志刚.2009.鄂尔多斯盆地东缘本溪组—太原组层序地层特征[J].地球学报,30(2):187-193.
汤永梅,梁兴,周松源,陈方鸿.2009.薄层测井评价技术在白驹凹陷的应用[J].油气地球物理,7(1):43-47.
陶丽,张廷山,戴传瑞,李秋菊,李斌.2010.苏北盆地白驹凹陷泰州组一段沉积物源分析[J].中国地质,37(2):414-420.
吴因业,张天舒,张志杰,崔化娟.2010.沉积体系域类型、特征及石油地质意义[J].古地理学报,12(1):70-81.
徐怀大.1993.层序地层学原理[M].北京:石油工业出版社.
徐怀大.1997.陆相层序地层学研究中的某些问题[J].石油与天然气地质,18(2):83-89.
严德天,王华,王清晨.2008.中国东部第三系典型断陷盆地幕式构造旋回及层序地层特征[J].石油学报,29(2):185-190.
张喜林,朱筱敏,钟大康,梁兵,曹冰,贺向阳.2004.苏北盆地高邮凹陷第三系—上白垩统层序地层格架特征[J].沉积学报,22(3):393-399.
赵澄林,朱莜敏.2001.沉积岩石学[M].北京:石油工业出版社:6-24.
BOYD R,DIESSEL C,WADSWORTH J,CHALMERS G,LITTLEM,LECKIE D,ZAITLIN B.1999.Development of a non-marine sequence stratigraphic model[C].American Associa-tion of Petroleum Geologists:A15.
CHI Qiu-e,GONG Fu-hua.2001.The basis and the application of sequence stratigraphy[M].Beijing:Petroleum Industry Press(in Chinese).
CURRIE B S.1997.Sequence stratigraphy of nonmarine Juras-sic-Cretaceous rocks,central Cordillenan foreland basin system[J].Geological Society of America Bulletin,109(6):1206-1222.
DENG Hong-wen,WANG Hong-liang,LI Xi-zhe.1996.Identification and correlation techniques of sequence stratigraphic base-levels and their application[J].Oil&Gas Geology,17(3):177-184(in Chinese with English abstract).
GU Jia-yu,FAN Tu-zhi.2001.Looking back and ahead on Sequence Stratigraphy[J].Marine Origin Petroleun Geology,6(4):15-25(in Chinese).
GU Jia-yu.1995.Framework concepts and models of sequence stratigraphy in nonmarine petroliferous basin[J].Petroleum Exploration and Development,22(4):6-10(in Chinese with English abstract).
JI You-liang,ZHANG Shi-qi,ZHANG Hong,ZHANG Li-qiang.1998.The Theory of Sequence Stratigraphy and Mechanic Patterns of Formation Cause of Sequence[M].Beijing:Geo-logical Publishing House(in Chinese).
JI You-liang,ZHANG Shi-qi.1996.The sequence stratigraphy of the fault-depression lake basin[M].Beijing:Petroleum Indus-try Press(in Chinese).
JIANG Zai-xing.2003.Sedimentary[M].Beijing:Petroleum Industry Press:7-498(in Chinese).
KE Guang-ming,ZHENG Rong-cai,SHI He.2006.Lithofacies and paleogeography of Paleogene tectonic sequences in the Subei basin and their evolution[J].Geology in China,33(6):1305-1311(in Chinese with English abstract).
LI Si-tian,LIN Chang-song,XIE Xi-nong,YANG Shi-gong,JIAO Yang-quan.1995.Approaches of nonmarine sequence strati-graphy—a case study on the Mesozoic Ordos basin[J].Earth Science Frontiers,2(3-4):133-148(in Chinese with English abstract).
LI Si-tian,YANG Shi-gong,LIN Chang-song.1992.On the Chronostratigraphic Framwork and Basic Building Blocks of Sedimentary Basin[J].Acta Sedimentologica Sinica,10(4):11-22(in Chinese with English abstract).
LIAO Yuan-tao,WANG Zhen-sheng,XIAO Dun-qing,WEI A-juan,WANG Jia-hao,YAN De-tian.2008.Styles of Sequence Components in the Central Area of the Huanghua Depres-sion[J].Acta Geoscientica Sinica,29(2):221-227(in Chinese with English abstract).
LIN Chang-song,ZHANG Yan-mei,LI Si-tian,REN Jian-ye,ZHANG Ying-zhi.2004.Episodie Rifting Dynamic Proeess and Quantitative Model of Mesozoie-Cenozoie Faulted Basins in Eastern China[J].Earth Science—Journal of China Univer-sity of Geosciences,29(5):583-588(in Chinese with English abstract).
LIU Bao-jun,ZENG Yun-fu.1985.Elements in lithopa-laeo-geolography and its working methods[M].Beijing:Geo-logical Publishing House(in Chinese).
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