松辽盆地北部西部斜坡姚家组四级层序格架沉积微相分布
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摘要
根据测井、录井、地震、岩心和古生物资料,运用层序地层学、沉积岩石学理论,建立松辽盆地北部西斜坡姚家组层序格架,分析四级层序格架沉积微相的分布和沉积体系的组合类型.结果表明:松辽盆地北部西斜坡姚家组划分为2个四级层序(Cp1-s3、Cs2),其中四级层序Cp1-s3划分为四级湖泊扩张体系域(Ep1)和四级湖泊萎缩体系域(Ss3);四级层序Cs2只发育四级湖泊扩张体系域(Es2).自下而上,Ep1地层分布范围最小,尖灭线位于西斜坡的东部;Ss3地层分布范围增大,尖灭线位于西斜坡的中部;Es2尖灭线继续向西推进,地层分布范围达到最大.剖面上,三级和各四级层序界面附近以富砂的下切谷充填、三角洲前缘和滨浅湖砂质滩坝为主;富泥的滨浅湖混合滩微相在四级层序最大湖泛面附近最为发育.平面上,姚家组沉积初期,湖岸线在西部斜坡区东部波动,物源供给充足,沉积相以三角洲相为主;至姚家组沉积末期,湖岸线向斜坡西侧大规模推移,发育下切谷充填—三角洲—湖泊沉积分布格局.不同的四级层序体系域的沉积微相分布有明显的差异性和一定的继承性.
According to the data of logging,seismic,core data and paleontology,the forth-order sequence framework of No.3sections of Yaojia formation in west clinoform region of north Songliao basin has been constructed and the forth-grade sequence within the framework of sendimentary facies spatial distribution has been discovered.The Yaojia formation in the west clinoform of the Songliao basin was divided into 2forth-order sequences:Cp1-s3 and Cs2,the former can be divided into fourth lake expanding system tract(Ep1)and fourth lake contracting system tract(Ss3);the latter only developed fourth lake expanding system tract(Es2).From bottom to top,Ep1,the pinch-out line which was located in the east of the west clinoform region has the smallest area;Ss3,the pinch-out line which was located in the middle of the west clinoform has a larger area than Ep1.While Es2,with the largest area,has a pinch-out line migrating further toward the west.In the profile section,the main sendimentary microfacies was the sand-rich incised valley filling,delta front and shore-shallow lacustrine sandy beach-bars,and these microfacies are developed near the 3rd or 4th-order sequence boundary,while the mud-rich shore-shallow lacustrine mixed beach is well developed near the maximum flooding surfaces of the 4thorder sequence.In the plane,in the early time of the Yaojia formation depositing,because shoreline fluctuated in the eastern of the western slope and the supply of sediment was strong,the delta facies dominated the sedimentary facies.However,in the late period,the shoreline migrated strongly toward the west and it leaded to the form of a very special distribution pattern:delta-Incised valley fills-shallow lake deposits.The characteristics of microfacies distribution of different 4th sequences system tracts have obvious difference,and has the certain inheritance as well.
引文
[1]舒良树,慕玉福,王伯长.松辽盆地含油气地层及其构造特征[J].地层学杂志,2003,27(4):340-347.Shu Liangshu,Mu Yufu,Wang Bochang.The oil-gas-bearing strata and the structural features in the Songliao basin,NE China[J].Journal of Stratigraphy,2003,27(4):340-347.
    [2]刘鸿友,苗洪波,陈文龙,等.松辽盆地南部中浅层资源潜力[J].中国石油勘探,2003,8(3):21-25.Liu Hongyou,Miao Hongbo,Chen Wenlong,et al.Resources potential of medium-shallow formation in the south of Songliao basin[J].China Petroleum Exploration,2003,8(3):21-25.
    [3]侯启军,魏兆胜,赵占银,等.松辽盆地的深盆油藏[J].石油勘探与开发,2006,33(4):406-411.Hou Qijun,Wei Zhaosheng,Zhao Zhanyin,et al.Deep basin reservoir in Songliao basin[J].Petroleum Exploration and Development,2006,33(4):406-411.
    [4]王树恒,吴河勇,辛仁臣,等.松辽盆地北部西部斜坡高台子油层三砂组沉积微相研究[J].大庆石油地质与开发,2006,25(3):10-12.Wang Shuheng,Wu Heyong,Xin Renchen,et al.Study on sedimentary microfacies of No.3sand group of Gaotaizi reservoir in west slope in northern Songliao basin[J].Petroleum Geology and Oilfield Development in Daqing,2006,25(3):10-12.
    [5]杜江峰,刘招君,董清水,等.松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究[J].吉林大学学报:地球科学版,2005,35(2):171-176.Du Jiangfeng,Liu Zhaojun,Dong Qingshu,et al.Study on slope breaks of the late Cretaceous depression basin around the western slope in the southern Songliao basin[J].Journal of Jilin University:Earth Science Edition,2005,35(2):171-176.
    [6]大庆油田石油地质志编写组.中国石油地质志卷二——大庆油田:上册[M].北京:石油工业出版社,1993:155-160.Edit committee of Daqing oilfield petroleum geology.Petroleum geology of China II—Daqing oilfield[M].Beijing:Petroleum Industry Press,1993:155-160.
    [7]付晓飞,王朋岩,申家年,等.简单斜坡油气富集规律——以松辽盆地西部斜坡北段为例[J].地质论评,2006,52(4):522-531.Fu Xiaofei,Wang Pengyan,Shen Jianian,et al.Migration and accumulation of oil and gas in a simple slope area:A case study on the western slope of the northern Songliao basin[J].Geoligical Review,2006,52(4):522-531.
    [8]傅广,张云峰,杜春国.松辽盆地北部岩性油藏形成机制及主控因素[J].石油勘探与开发,2002,29(5):22-24.Fu Guang,Zhang Yunfeng,Du Chunguo.Formation mechanism and main controlling factors for lithologic reservoirs in northern Songliao basin[J].Petroleum Exploration and Development,2002,29(5):22-24.
    [9]蒙启安,黄薇,林铁峰,等.松辽盆地北部岩性油藏形成条件与分布规律[J].中国石油勘探,2004,9(4):6-11.Meng Qi'an,Huang Wei,Lin Tiefen,et al.Formation conditions and distribution law of lithologic oil reservoirs in northern part of Songliao basin[J].China Petroleum Exploration,2004,9(4):6-11.
    [10]单玄龙,俎云浩,罗洪浩,等.松辽盆地西部斜坡大岗地区白垩系油砂储层成因类型及其影响因素[J].科技导报,2012,30(27):24-29.Shan Xuanlong,Zu Yunhao,Luo Honghao,et al.Originand influencing factors of Cretaceous oil sand reservoir in Dagang area,western slope of Songliao basin[J].Articles,2012,30(27):24-29.
    [11]杨万里.松辽陆相盆地石油地质特征[M].北京:石油工业出版社,1985.Yang Wanli.Petroleum geology characteristics of Songliao continental basin[M].Beijing:Petroleum Industry Press,1985.
    [12]冯志强,张顺,付秀丽.松辽盆地姚家组—嫩江组沉积演化与成藏响应[J].地学前缘,2012,19(1):78-87.Feng Zhiqiang,Zhang Shun,Fu Xiuli.Depositional evolution and accumulation respomse of Yaojia-Nenjiang formation in Songliao basin[J].Earth Science Frontiers,2012,19(1):78-87.
    [13]高瑞祺,萧德铭.松辽及其外围盆地油气勘探新进展[M].北京:石油工业出版社,1995:19-24.Gao Ruiqi,Xiao Deming.The advancement of oil and gas exploration in Songliao basin and its periphery basins[M].Beijing:Petroleum Industry Press,1995:19-24.
    [14]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].北京:石油工业出版社,1997:47-103.Gao Ruiqi,Cai Xiyuan.The formation conditions and distribution of oil and gas pools of Songliao basin[M].Beijing:Petroleum Industry Press,1997:47-103.
    [15]王建功,王天奇,卫平生,等.松辽盆地青山口组三段底界不整合面的发现及石油地质学意义[J].地质学报,2009,83(1):78-88.Wang Jiangong,Wang Tianqi,Wei Pingsheng,et al.Identification of uncomformity plane at the bottom(K2qn3)of Qingsan member(Qingshankou formation)in the Songliao basin and its implication for petroleum geology[J].Acta Geologica Sinica,2009,83(1):78-88.
    [16]黄清华,吴怀春,万晓樵,等.松辽盆地白垩系综合年代地层学研究新进展[J].地层学杂志,2011,35(3):250-257.Huang Huaqing,Wu Huaichun,Wan Xiaoqiao,et al.New progress of integrated chronostratigraphy of the Cretaceous in Songliao basin[J].Journal of Stratigraphy,2011,35(3):250-257.
    [17]孙佳珺,辛仁臣,梁江平.松辽盆地西斜坡上白垩统青山口组二段及三段底部四级层序格架下沉积微相分布[J].古地理学报,2014,16(4):461-471.Sun Jiajun,Xin Renchen,Liang Jiangping.Sedimentary microfacies distribution under the 4th-order sequence stratigraphic framework of the 2and lower member 3of upper Cretaceous Qingshankou formation in west slope of Songliao basin[J].Journal of Palaeogeography,2014,16(4):461-471.
    [18]杨勉,陈艳丽,李培海.松辽盆地北部西斜坡油气藏类型与分布预测[J].科学技术与工程,2012,22(8):5588-5592.Yang Mian,Chen Yanli,Li Peihai.Reservoir types and distribution prediction in the western slope of the northern Songliao basin[J].Science Technology and Engineering,2012,22(8):5588-5592.
    [19]叶淑芬,魏魁生.松辽盆地白垩系的密集段及海水进侵的新证[J].地球科学——中国地质大学学报,1996,21(3):267-271.Ye Shufen,Wei Kuisheng,Condensen section and new evidence of marine inundation in Cretaceous,Songliao basin[J].Earth Science:Journal of China Universiry of Geosciences,1996,21(3):267-271.
    [20]辛仁臣,蔡希源,王英民.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,2004,22(3):387-392.Xin Renchen,Cai Xiyuan,Wang Yingmin.Depositional model of lowstand and characteristics of sequence boundary in deep-water lake,Songliao depression basin[J].Acta Sedimentologica Sinica,2004,22(3):387-392.
    [21]辛仁臣,王英民.松辽盆地北部青山口—姚家组西部坡折带成因及演化[J].地球科学—中国地质大学学报,2004,29(5):621-624.Xin Renchen,Wang Yingmin.Origin and evolution of west slope breaks of Qingshankou-Yaojia formation in northern Songliao basin[J].Earth Science:Journal of China University of Geoscienes,2004,29(5):621-624.
    [22]Vail P R.Seismie stratigraphy interpretation using stratigraphy.Partl:Seismie stratigraphy inter-pretation proeedure:Ameriean assoeiation of Petroleum Geologists[J].Studiesin Geology,1987,27(l):1-10.
    [23]朱筱敏.沉积岩石学[M].北京:石油工业出版社,2008:9.Zhu Xiaomin.Sedimentary Petrology[M].Beijing:Petroleum Industry Press,2008:9.
    [24]付志方,王焕弟,邢卫新,等.层序地层学研究现状及进展[J].勘探地球物理进展,2005,28(5):26-30.Fu Zhifang,Wang Huandi,Xing Weixin,et al.Review of sequence stratigraphy[J].Progress in Exploration Geophysics,2005,28(5):26-30.
    [25]徐怀大.陆相层序地层学研究中的某些问题[J].石油与天然气地质,1997,18(2):3-9.Xu Huaida.Some problems in study of continental sequence stratigraphy[J].Oil and Gas Geology,1997,18(2):3-9.
    [26]姜在兴.沉积体系及层序地层学研究现状及发展趋势[J].石油与天然气地质,2010,31(5):535-541.Jiang Zaixing.Studies of depositional systems and sequence stratigraphy the present and the future[J].Oil and Gas Geology,2010,31(5):535-541.
    [27]Van Wagoner J C,Mitchum R M,Campion K M,et al.Siliciclastic sequence stratigraphy in well,cores and outcrops—concept for high-resolution correlation of times and facies[J].AAPG,Methods in Exploration Series,1990,7:1-55.
    [28]林畅松,刘景彦,刘丽军,等.高精度层序地层分析:建立沉积相和储层规模的等时地层格架[J].现代地质,2002,16(3):276-281.Lin Changsong,Liu Jingyan,Liu Lijun,et al.High resolution sequence stratigraphy analysis:Construcyion of chronostratigraphic sequence framework on facies and reservoir scale[J].Geoscience,2002,16(3):276-281.
    [29]刘爱武,王英民,王明培,等.高频层序划分在隐蔽油气藏勘探中的作用[J].江汉石油科技,2009,19(1):1-9.Liu Aiwu,Wang Yingmin,Wang Mingpei,et al.The effect of high resolution sequence division in the subtle reservoir exploration[J].Jianghan Petroleum Science and Technology,2009,19(1):1-9.
    [30]邓宏文,王红亮,祝勇军,等.高分辨层序地层学——原理及应用[M].北京:地质出版社,2002:80-120.Deng Hongwen,Wang Hongliang,Zhu Yongjun,et al.High resolution sequence stratigraphy:Principle and application[J].Beijing:Geological Publishing Press,2002:80-120.
    [31]王红亮,夏志远,李世臻,等.松辽盆地南部大布苏地区青山口组高频层序沉积微相分析与岩性圈闭预测[J].现代地质,2009,23(5):776-782.Wang Hongliang,Xia Zhiyuan,Li Shizhen,et al.Sedimentary facies analysis and lithologic trap prediction in high-resolution sequence framework of Qingshankou formation,Dabusu area,southern Songliao basin[J].Geoscience,2009,23(5):776-782.
    [32]梅冥相.浅海相碎屑岩米级旋回层序的成因类型及其在长周期旋回层序中的有序叠加形式[J].岩相古地理,1998,18(5):64-70.Mei Mingxiang.The genetic type for meter-scale cyclic sequences and order sequences formation for long term cyclic sequences of clastic rook in shallow sea facies[J].Sedimentary Facies and Palaeogeography,1998,18(5):64-70.
    [33]郭少斌.辽河凹陷东部桃园——大平房地区东营组层序地层及沉积特征[J].现代地质,2006,20(3):473-479.Guo Shaobin.Study on the sequence stratigraphy and sedimentary characteristics of Dongying formation in Taoyuan:Dapingfang area in the east of Liaohe depression[J].Geoscience,2006,20(3):473-479.
    [34]辛仁臣,王树恒,梁江平,等.松辽盆地北部西斜坡青山口组三段四级层序格架内沉积微相分布[J].现代地质,2014,28(4):782-790+798.Xin Renchen,Wang Shuheng,Liang Jiangping,et al.Sedimentary microfacies distribution under the 4th-order sequence stratigraphic framework of the third member of Qingshankou formation in west slope of the northern part of Songliao basin[J].Geoscience,2014,28(4):782-790+798.
    [35]辛仁臣,张雪辉,张翼,等.湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J].沉积学报,2008,26(1):77-85.Xin Renchen,Zhang Xuehui,Zhang Yi,et al.Characteristics and genesis of sequence boundaries on subaqueous gentle slope of lacustrine basin:A case study on upper Cretaceous in Talaha region of Songliao basin[J].Acta Sedimentologica Sinica,2008,26(1):77-85.
    [36]威尔格斯.层序地层学原理(海平面变化综合分析)[M].徐怀大,魏魁生,洪卫东,等译.北京:石油工业出版社,1993:47-254.Weilgus C K.The principle of sequence stratigraphy(Comprehensive analysis of sea-level change)[M].translator:Xu Huaida,Wei Kuisheng,Hong Weidong,et al.Beijing:Petroleum Industry Press,1993:47-254.
    [37]辛仁臣,李桂范,向淑敏.松辽盆地盆西斜坡白垩系姚家组下切谷充填结构[J].地球科学,2008,33(6):834-842.Xin Renchen,Li Guifan,Xiang Shumin.The incised valley filling architecture of Cretaceous Yaojia formation in the western clinoform of Songliao basin[J].Earth Science,2008,33(6):834-842.

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