石油与天然气地质 ›› 2002, Vol. 23 ›› Issue (3): 218-223.doi: 10.11743/ogg20020304

• 前沿探索 • 上一篇    下一篇

濮阳凹陷白庙气田沙河街组三段下亚段扇三角洲沉积模拟研究

夏长淮1, 张春生2, 周海彬3, 施斌全4, 刘忠保2, 李力3   

  1. 1. 中国科学院广州地球化学研究所, 广东广州, 750000;
    2. 江汉石油学院地球科学系, 湖北荆州, 434102;
    3. 中原石油勘探局钻井综合工程处, 河南兰考, 475300;
    4. 胜利油田测井公司, 山东河口, 257200
  • 收稿日期:2002-05-13 出版日期:2002-09-25 发布日期:2012-01-16
  • 基金项目:

    国家“973”项目子课题“储集层原型地质规律研究”;CNPC石油中青年创新基金“盆地陡坡带沉积模拟研究”;Petro-China重点实验室课题“扇三角洲及辫状河储层沉积过程物理模拟与数值模拟”资助

STUDY ON SEDIMENTARY SIMULATION OF FAN DELTA IN LOWERSUB-MEMBER ES3 OF BAIMIAO GAS FIELD IN PUYANG DEPRESSION

Xia Changhuai1, Zhang Chunsheng2, Zhou Haibin3, Shi Bingquan4, Liu Zhongbao2, Li Li3   

  1. 1. Guangzhou Geochemical Research Institute of the Chinese Academy of Sciences, Guangzhou;
    2. Earth Science Department, Jianghan Petroleum Institute, Jingzhou, Hubei;
    3. Multi-Well Drilling Engineering Section of Oil Exploration Bureau of Zhongyuan Oilfield;
    4. Shen Li Oilfidd well-logging corporation, Hekou, Shandong
  • Received:2002-05-13 Online:2002-09-25 Published:2012-01-16

PDF (PC)

725

被引次数

16

摘要：

根据白庙地区砂体沉积特征设计的沙三下砂体形成过程模拟实验表明,沙三下扇三角洲主要是碎屑流和牵引流交替作用的结果,洪水期以碎屑流作用为主,平水期以牵引流作用为主,扇三角洲存在叠置与展开两种结合形式,前者厚度大而面积小,后者厚度小而面积大。它的发育和演变主要受上游水流强度、泥砂搬运、水流分汊变迁、湖水位升降及活动底板下降速率等因素的影响。模拟认为,沙三下扇三角洲在形成过程中,在白5井、白3井和白28井之间及白 7井一带主要发育3条主辫状河道,最宽达 750m,最窄为 300m;辫状河道在杜寨断层处,砂岩质纯、厚度大、物性好,在兰聊断层与杜寨断层之间,砂岩厚度大且分布普遍,而在靠近兰聊断层处则砂岩厚度减薄,物性变差。

关键词: 扇三角洲, 模拟, 发育过程, 控制因素, 分布, 白庙地区

Abstract:

Simulation of genetic process of sand body in sub-member Es3 which is designed on the basis of sedimentation characteristics of the sandbody in Baimiao region indicates that the development of delta in sub-member E s3 fan is the result and caused chiefly by the intersected process of clastic current and traction current. The clastic current played a main rule in the flooding period while the traction current played a chief rule in the period of normal water level year; Two types of combinations(stack and spread)exist in the fan delta, the former with small size but in great thickness, and the later in small thickness but with big size. The development and evolution of sub-member E s3 fan delta is largely effected by several factors of upper reaches current intensity, migration of muddy sand, braiding and migration of water current, uplift and subsidence of lake water level as well as subsidence rate of the mobile bottom bed etc.. It is believed by simulating that the width of three braided channels between Bai No.5,and No.3 and No.28, and No.7 well which mainly developed in the process of the development of the delta in sub-member Es3 fan are 750m at maximum and 300m at minimum; In Duzai fault where purified sandstones are found in the braided channels with great thickness and good physical property, between Lanqing fault and Duzai fault sandstones are with great thickness and widely spread while sandstones near Lanqing fault become thinner and thinner and with poor property.

Key words: fan delta, simulation, develop process, controlling factor, distribution, Baimiao region

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