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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2003  >  25(2): 143-148
ZHU Guang-you, JIN Qiang, ZHOU Jian-lin, ZHANG Lin-ye. STUDY ON THE INFILLING PATTERNS OF LACUSTRINE BASINS IN THE DONGYING DEPRESSION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(2): 143-148. doi: 10.11781/sysydz200302143
Citation: ZHU Guang-you, JIN Qiang, ZHOU Jian-lin, ZHANG Lin-ye. STUDY ON THE INFILLING PATTERNS OF LACUSTRINE BASINS IN THE DONGYING DEPRESSION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(2): 143-148. doi: 10.11781/sysydz200302143
shu

STUDY ON THE INFILLING PATTERNS OF LACUSTRINE BASINS IN THE DONGYING DEPRESSION

doi: 10.11781/sysydz200302143
  • 1.

    The Earth Resources and Information College, Petroleum University, Dongying, Shandong 257061, China

  • 2. Shengli Oil Production Factory, Shengli oil field, Dongying, Shandong 257051, China

  • 3. Research Institute of Geological Sciences, Shengli oil field, Dongying, Shandong 257015, China

  • Received Date: 2002-09-24
  • Rev Recd Date: 2003-01-24
  • Publish Date: 2003-03-25
    Abstract
  • The infilling patterns of lacustrine basins are the important means to evaluate the sedimentary characteristics of hydrocarbon source rocks.Combined with the geochemical characteristics of source rocks in this paper,the sedimentary succession of source rocks,the developing features of strata and the infilling and evolutionary process of basins in the Lower Triassic Shahejie Formation of the Dongying Depression were analysed.The source rocks of the Shahejie Formation can be divided into three evolutionary stages from lower to upper.The evaporite facies(the Upper Shasi Subformation),the oscillatory deep lake facies(the Lower Shasan Subformation)and the delta lacustrine facies(the Middle and Upper Shasan Subformation)assemblage patterns were established,which corresponding to underinfilling,equilibrium infilling and overinfilling lacustrine types respectively.They reflected the generation,spreading and consumption process of lakes.

     

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    • References(25)
  • [1]
    邓宏文,钱凯.深湖相泥岩的成因类型和组合演化[J].沉积学报,1990,8(3):1-20.
    [2]
    王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315-319.
    [3]
    Soreghan M J,Cohen A S.Textural and compositional variability across littoral segments of lake Tanganyika:the effect of asymmetric basin structure on sedimentation in large rift lakes[J].AAPG Bull,1996,80(3):382-409.
    [4]
    朱筱敏.层序地层学[M].山东东营:石油大学出版社,2000.108-146.
    [5]
    Lambias J J.A model of tectonic control of lacustrine stratigraphic sequences in continental rift basins[A].Barry J K.Lacustrine Basin Exploration:Case Study and Model Analysis[J].AAPG Memoir,1991,50:137-149.
    [6]
    林畅松,李思田,任建业.断陷湖盆层序地层学研究和计算机模拟[J].地学前缘,1995,2(3):124-132.
    [7]
    Ravans R,Steel R J.Architecture of marine rift-basin successions[J].AAPG Bull,1998,82(2):197-226.
    [8]
    汤良杰,金之钧,贾承造,等.叠合盆地构造解析几点思考[J].石油实验地质,2001,23(3):251-255.
    [9]
    Carroll A R,Bohacs K M.Stratigraphic classification of ancient lakes:balancing tectonic and climatic controls[J].Geo-logy,1999,27(2):99-102.
    [10]
    邓宏文,王红亮,宁宁.沉积物体积分配原理--高分辨率层序地层学的理论基础[J].地学前缘,2000,7(4):305-313.
    [11]
    刘文汇.试论成烃的地球化学场[J].石油实验地质,2000,22(1):1-8.
    [12]
    Bertrand P,Lallier-Verges E,Boussafir M.Enhancement of accumulation and anoxic degradation of organic matter controlled by cyclic productivity:a model[J].Organic Geochemi-stry,1993,22:511-520.
    [13]
    Derenne S,Largeau C,Brukner-Wein A.Origin of variations in organic mater abundance and composition in a lithologically homogeneous maar-type oil shale deposit[J].Organic Geochemistry,2000,31:787-798.
    [14]
    Carroll A R,Bohacs K M.Lake-type controls on petroleum source rock potential in nonmarine basin[J].AAPG Bull,2001,85(6):1033-1053.
    [15]
    张水昌,张保民,王飞宇,等.塔里木盆地两套海相有效烃源岩层--(Ⅰ)有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261-268.
    [16]
    朱光有,金强.烃源岩的非均质性及其研究--以东营凹陷牛38井为例[J].石油学报,2002,23(5).20-26.
    [17]
    郭元岭,赵乐强,石红霞,等.济阳坳陷探明石油地质储量特点分析[J].石油勘探与开发,2001,28(3):33-37.
    [18]
    金强,查明.柴达木盆地西部第三系蒸发岩与生油岩共生沉积作用研究[J].地质科学,2000,35(4):465-473.
    [19]
    何斌.渤海湾复式盆地动力学探讨[J].石油实验地质,2001,23(1):27-31.
    [20]
    王苏民,张振克.中国湖泊沉积与环境演变研究的新进展[J].科学通报,1999,44(6):579-587.
    [21]
    晋慧娟,李育慈.深海沉积物中的特征原生沉积构造[J].中国科学,1995,25(8):890-896.
    [22]
    杨明慧,夏文臣,张兵山,等.非海相盆地准层序级别的有机相变化及其地质意义[J].沉积学报,2000,18(2):297-301.
    [23]
    蔡进功,姜秀芳,范存堂.东营凹陷中、晚始新世湖泊沉积体系及盆地演化[J].复式油气田,1994,5(3):1-7.
    [24]
    王德坪.湖相内成碎屑流的沉积及形成机理[J].地质学报,1991,65(4):299-316.
    [25]
    冯有良,李思田.东营凹陷沙河街组三段层序低位域砂体沉积特征[J].地质论评,2001,47(3):278-286.
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