大庆油田北一区断东水平井区曲流河道砂体内部建筑结构研究
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摘要
目前国内大部分油田已进入开发中后期,随着开发的不断深入,用合理有效的方法寻找并挖潜剩余油显得尤为重要。开展储层精细描述、单砂体内部建筑结构及内部流动单元研究,加深油田地质情况认识,为寻找剩余油提供依据。
大庆油田北一区断东葡Ⅰ2曲流河沉积储层,发育有大型复合河道砂体,通过可分性研究,可将葡Ⅰ2小层进一步划分成葡Ⅰ21、葡Ⅰ22两个河流期沉积时间单元,葡Ⅰ21沉积时间单元发育的是曲流河砂体及大型高弯曲分流河道砂体,葡Ⅰ2：沉积时间单元发育泛滥平原相的高弯曲的大型复合曲流带砂体。曲流河道在侧向加积的过程中形成薄夹层,对单砂体内部4级界面侧积薄夹层的建筑结构研究,包括4级侧积界面倾向、倾角、结构体规模和夹层空间分布模式。为进入高含水期油田的开发揭示出了更为复杂的储层内部结构,反映出非常强的储层非均质性,结合目的层剩余油的研究,为总结出储层内剩余油的分布特征,为持续、高效开发油田,提高采收率具有重要的现实意义。
At present the domestic majority of oil fields entered the developed part, with de velopment unceasing thoroughly, seeks for and taps latent potentialities the remaining oil with the reasonable effective method appears especially important.The fine descripti on of reservoir,the internal construction structure of the single sand and the internal m obile unit research, the deepening oil field geology situation knew provide the basis to seek for the remaining oil.
The PⅠ2 of beiyi area of daqing oil field is meandering river reservoir,developin g with large scale complex channel sand.Through thoroughly investigate, PⅠ2 of Beiy i area was subdivided into two sedimentary units(PⅠ21, PⅠ22).The sedimentary unit of PⅠ21 develop meandering river sand and large scale and high bending distributary channel. The sedimentary unit of PⅠ22 develop high bending with large compound meandering sand body of flood plain facies.Monosandstone is formed with the lateral deposit of meandering river. The research of the architecture of point bar including te ndency and dip and scale and distribution space.Entered the high watery time, the mul tiple well pattern encryption three extraction stage after the oil field to promulgate the more complex reservoir internal structure, reflected very strong reservoir anisotropism, the union goal level remaining oil's research, to summarize in the reservoir. The outc ome of this text provided full geological references for exploration of remaining oil in the point bar of meandering stream channel and had geological direction to selection of producing methods.
大庆油田北一区断东葡Ⅰ2曲流河沉积储层,发育有大型复合河道砂体,通过可分性研究,可将葡Ⅰ2小层进一步划分成葡Ⅰ21、葡Ⅰ22两个河流期沉积时间单元,葡Ⅰ21沉积时间单元发育的是曲流河砂体及大型高弯曲分流河道砂体,葡Ⅰ2：沉积时间单元发育泛滥平原相的高弯曲的大型复合曲流带砂体。曲流河道在侧向加积的过程中形成薄夹层,对单砂体内部4级界面侧积薄夹层的建筑结构研究,包括4级侧积界面倾向、倾角、结构体规模和夹层空间分布模式。为进入高含水期油田的开发揭示出了更为复杂的储层内部结构,反映出非常强的储层非均质性,结合目的层剩余油的研究,为总结出储层内剩余油的分布特征,为持续、高效开发油田,提高采收率具有重要的现实意义。
At present the domestic majority of oil fields entered the developed part, with de velopment unceasing thoroughly, seeks for and taps latent potentialities the remaining oil with the reasonable effective method appears especially important.The fine descripti on of reservoir,the internal construction structure of the single sand and the internal m obile unit research, the deepening oil field geology situation knew provide the basis to seek for the remaining oil.
The PⅠ2 of beiyi area of daqing oil field is meandering river reservoir,developin g with large scale complex channel sand.Through thoroughly investigate, PⅠ2 of Beiy i area was subdivided into two sedimentary units(PⅠ21, PⅠ22).The sedimentary unit of PⅠ21 develop meandering river sand and large scale and high bending distributary channel. The sedimentary unit of PⅠ22 develop high bending with large compound meandering sand body of flood plain facies.Monosandstone is formed with the lateral deposit of meandering river. The research of the architecture of point bar including te ndency and dip and scale and distribution space.Entered the high watery time, the mul tiple well pattern encryption three extraction stage after the oil field to promulgate the more complex reservoir internal structure, reflected very strong reservoir anisotropism, the union goal level remaining oil's research, to summarize in the reservoir. The outc ome of this text provided full geological references for exploration of remaining oil in the point bar of meandering stream channel and had geological direction to selection of producing methods.
引文
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[13]贾爱林,肖敬修著.油藏评价阶段建立地质模型的技术与方法[J].北京：石油工业出版社,2002年.
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[15]倪晋仁等.现代冲积河流的河型空间转换模式探讨[J].沉积学报,2000,18(1)：1-6.
[16]张欧阳等.游荡河型造床实验过程中河型的时空演替和复杂响应现象[J].地理研究,2000,19(2)：180-188.
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[18]许炯心.我国游荡河型的地域分布特征[J].泥沙研究,1990,(2)：47-53.
[19]许炯心.中国江心洲河型的地域分布特征[M],云南地理环境研究,1992,4(2)：46-55.
[20]许炯心.高含沙型曲流河床的形成机理[M].科学通报,1989,34(21)：1649-1651.
[21]许炯心.南运河弯曲河型的成因[M].地理学与国土研究,1989,5(2)：54-59.
[22]王继贿等.根据河道形态和沉积物特征的河流新分类[J].沉积学报,1999,17(2)：240-246.
[23]高健等.滦河中游现代河流沉积构造与水动力关系[J].沉积学报,1983,1(1)：27-41.
[24]何鲤等.长江上游的心滩-重庆珊瑚坝现代沉积考察[J].沉积学报,1986,4(1)：116-125.
[25]赖志云.荆江太平口边滩现代沉积研究[J].沉积学报,1986,4(4)：109-118.
[26]李从先等.滦河废弃三角洲和沙坝-泻湖沉积体系[J].沉积学报,1983,1(2)：60-71.
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[29]顾家裕,范土芝.层序地层学回顾与展望[J].海相油气地质,2001,6(4)：15-25.
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