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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2012  >  34(1): 40-46
Mo Wuling, Wu Chaodong, Zhang Shun, Peng Guoliang. Provenance and palaeocurrent direction of Upper Cretaceous Nenjiang Formation in northern Songliao Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(1): 40-46. doi: 10.11781/sysydz201201040
Citation: Mo Wuling, Wu Chaodong, Zhang Shun, Peng Guoliang. Provenance and palaeocurrent direction of Upper Cretaceous Nenjiang Formation in northern Songliao Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(1): 40-46. doi: 10.11781/sysydz201201040
shu

Provenance and palaeocurrent direction of Upper Cretaceous Nenjiang Formation in northern Songliao Basin

doi: 10.11781/sysydz201201040
  • 1.

    Institute of Oil & Gas, Peking University, Beijing 100871, China

  • 2. Langfang Branch, Petro China Exploration and Development Research Institute, Langfang, Hebei 065007, China

  • 3. Key Laboratory of Gas Reservoir Formation and Development, CNPC, Langfang, Hebei 065007, China

  • 4. Exploration and Development Research Institute of Daqing Oil Field, Petro China, Daqing, Heilongjiang 163712, China

  • Received Date: 2011-04-02
  • Rev Recd Date: 2011-12-31
  • Publish Date: 2012-01-28
    Abstract
  • The provenance and palaeocurrent direction of the Upper Cretaceous Nenjiang Formation in the northern Songliao Basin were analyzed by means of strata slicing in seismic-sedimentologic studies and combined with detrital and heavy mineral components tests.A sedimentary distribution model of meandering river-delta-ake sedimentary systems in the Nenjiang Formation was established based on the studies of palaeocurrent direction.It was concluded that the deposition of the Nenjiang Formation was controlled by the eastern and northeastern deltas.The northeastern sources played important roles during the deposition of the 1st member of the Nenjiang Formation and the palaeocurrents were SN oriented along down-slop.After the maximum lake flooding during the 2nd and 3rd members of the Nenjing Formation,the northeastern sources were taken place by the eastern ones and the palaeocurrents changed to be EW oriented along down-slope.The sedimentary model provides geologic support for petroleum exploration in Heidimiao reservoir in the north of the Songliao Basin.

     

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    • References(28)
  • [1]
    高瑞祺,蔡希源.大庆油气勘探的新进展及勘探经验的初步总结[M].北京:石油工业出版社,2004:1-12.
    [2]
    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.
    [3]
    陈涛.大型非海相三角洲体系储层精细构成研究:以松辽盆地北部嫩江组为例[D].北京:中国地质大学,2005:5-21.
    [4]
    郭迎春,苏明,何云龙,等.松辽盆地黑鱼泡凹陷姚家组层序地层与体系[J].油气地质与采收率,2010,17(1):29-32.
    [5]
    赵波,冯子辉,梁江平.松辽盆地安达地区泉头组四段沉积特征与油气分布关系[J].石油实验地质,2010,32(1):35-40.
    [6]
    谢忱,胡纯心.松辽盆地长岭断陷南部天然气成藏与富集特征[J].石油与天然气地质,2010,31(3):381-385.
    [7]
    萧德铭,迟元林,蒙启安,等.松辽盆地北部向斜区岩性油藏勘探认识与实践[M].北京:石油工业出版社,2005:1-65.
    [8]
    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,1997:3-21.
    [9]
    任延广,杨玉峰.松辽盆地中浅层地层层序及沉积相研究[R].大庆:大庆油田有限责任公司勘探开发研究院,1999:8-21.
    [10]
    解习农,陆永潮,任建业.松辽盆地层序地层格架和中浅层沉积体系研究[R].大庆:大庆油田有限责任公司勘探开发研究院,2007:2-65.
    [11]
    张琴,张满郎,朱筱敏,等.准噶尔盆地阜东斜坡区侏罗系物源分析[J].新疆石油地质,1999,20(6):501-504.
    [12]
    陈纯芳,郑浚茂,王德发.板桥凹陷沙三段沉积体系与物源分析[J].古地理学报,2001,3(1):53-62.
    [13]
    李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998,25(6):5-7.
    [14]
    彭国亮,吴朝东,张顺,等.松辽盆地北部上白垩统嫩江组二、三段物源分析[J].北京大学学报(自然科学版),2010,46(4):555-562.
    [15]
    莫午零,吴朝东,张顺.松辽盆地齐家—古龙凹陷上白垩统嫩江组沉积体系及沉积相的地震成像[J].古地理学报,2010,12(4):399-408.
    [16]
    陆永潮,杜学斌,陈平,等.油气精细勘探的主要方法体系:地震沉积学研究[J].石油实验地质,2008,30(1):1-5.
    [17]
    董春梅,张宪国,林承焰.地震沉积学的概念、方法和技术[J].沉积学报,2006,24(5):698-704.
    [18]
    范代读,邱桂强,李从先,等.东营三角洲的古流向研究[J].石油学报,2000,21(1):29-33.
    [19]
    和钟铧,刘招君,张峰,等.重矿物在盆地分析中的应用研究进展[J].地质科技情报,2001,20(4):29-32.
    [20]
    Brown A R,Dahm C G,Graebner R J.A stratigraphic case history using three-dimensional seismic data in the Gulf of Thailand[J].Geophysical Prospecting,1981,29(3):327-349.
    [21]
    Zeng Hongliu.Facies-guided 3-D seismic modeling and reservoir characterization[D].Austin,Texas:University of Texas at Austin,1994:164-168.
    [22]
    Zeng Hongliu,Loucks R G.Mapping sediment dispersal patterns and associated systems tracts in fourth-and fifth-order sequences using seismic sedimentology:Example from Corpus Christi Bay,Texas[J].AAPG Bulletin,2007,91(7):981-1003.
    [23]
    Hentz T F,Zeng Hongliu.High-frequency sequence stratigraphy from seismic sedimentology:Applied to Miocene,Vermilion Block 50,Tiger Shoal area,offshore Louisiana[J].AAPG Bulletin,2004,88(2):153-174.
    [24]
    冯志强,张顺,解习农,等.松辽盆地嫩江组大型陆相坳陷湖盆湖底水道的发现及其石油地质意义[J].地质学报,2006,80(8):1226-1233.
    [25]
    Prins M A,Postma G.Effects of climate,sea level,and tectonics unraveled for last deglaciation turbidite records of the Arabian Sea[J].Geology,2000,28(4):375-378.
    [26]
    Normark W R,Piper D J W,Posamentier H.Variability in form and growth of Sediment waves on turbidite channel levees[J].Marine Geology,2002,192(1-3):23-58.
    [27]
    Mutti E,Tinterri R,Benevelli G,et al.Deltaic,mixed and turbidite sedimentation of ancient foreland basins[J].Marine and Petroleum Geology,2003,20(6-8):733-755.
    [28]
    Zhang Shanwen.The application of an integrated approach in exploration of lacustrine turbidites in Jiyang Sub-basin,Bohai Bay Basin,China[J].Journal of Petroleum Science and Engineering,2004,41(1-3),67-77.
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