古地理学报 ›› 2012, Vol. 14 ›› Issue (4): 487-498. doi: 10.7605/gdlxb.2012.04.007

• 岩相古地理学及沉积学 • 上一篇    下一篇

黄骅坳陷歧口凹陷古近系沙三2亚段辫状河三角洲沉积模拟实验研究

文沾1 刘忠保1 何幼斌1 苑伯超1 罗进雄1 蒲秀刚2 陈长伟2 林常梅2   

  1. 1 长江大学地球科学学院,湖北荆州 434023
    2 中国石油大港油田分公司勘探开发研究院,天津 300280
  • 收稿日期:2011-09-06 修回日期:2011-12-05 出版日期:2012-08-01 发布日期:2012-08-01
  • 通讯作者: 通讯作者简介 刘忠保,男,1965年生,副教授,硕士生导师,主要从事湖盆沉积模拟及水动力学的研究及教学工作 E-mail:wenzhan915@126.com
  • 作者简介:文沾,女,1986年生,长江大学地球科学学院硕士生,研究方向为储集层地质学。通讯地址:湖北省荆州市南环路1号长江大学地球科学学院;邮政编码:434023。E-mail:wenzhan915@126.com。
    通讯作者简介 刘忠保,男,1965年生,副教授,硕士生导师,主要从事湖盆沉积模拟及水动力学的研究及教学工作。E-mail:lzb623@163.com。

Sedimentation simulation experiment of braided fluvial delta of the second submember of Member 3 of Paleogene Shahejie Formation in Qikou Sag of Huanghua Depression

Wen Zhan1, Liu Zhongbao1, He Youbin1, Yuan Bochao1, Luo Jinxiong1, Pu Xiugang2, Chen Changwei2, Lin Changmei2   

  1. 1 School of Geosciences,Yangtze University,Jingzhou 434023,Hubei
    2 Research Institute of Exploration and Development,PetroChina Dagang Oilfield Company,Tianjin 300280
  • Received:2011-09-06 Revised:2011-12-05 Online:2012-08-01 Published:2012-08-01
  • About author:Wen Zhan,born in 1986,is a master candidate in School of Geosciences,Yangtze University,and is engaged in reservoir geology.E-mail: wenzhan915@126.com.
    About the corresponding author Liu Zhongbao,born in 1965,is an associate professor and master degree supervisor in School of Geosciences,Yangtze University.He is engaged in lake sedimentation simulation and hydrodynamic.E-mail:lzb623@163.com.

摘要: 黄骅坳陷歧口凹陷古近系沙河街组是大港油田油气勘探的主要目的层,该组主要发育辫状河三角洲和扇三角洲沉积砂体,其中辫状河三角洲砂体是有利的油气储集体。在区域构造、古地貌和沉积体系等研究基础上,应用沉积模拟技术,再现了研究区孔店物源辫状河三角洲的形成过程和沉积微相特征,在实验条件下,孔店物源辫状河三角洲可划分为3个亚相、7个微相。实验研究表明,基底沉降、相对湖平面升降、流量及流量变幅、加砂量(物源供给)等是影响辫状河三角洲的形成及其演化的控制因素。通过实际砂体和实验砂体厚度展布对比分析,预测了有利储集层分布区域。综合歧口凹陷原始地质模型和实验模拟成果,建立了模拟实验条件下歧口凹陷古近系沙三2亚段辫状河三角洲沉积模式。

关键词: 黄骅坳陷, 歧口凹陷, 沉积模拟, 辫状河三角洲, 控制因素, 沉积模式

Abstract: The Shahejie Formation of Paleogene in Qikou Sag of Huanghua Depression is the main target strata of Dagang Oilfield,which is dominated by braided fluvial delta and fan delta sandbodies. The braided fluvial delta is the favorable reservoir. Based on the study of regional tectonic,palaeogeomorphology feature,sedimentary system of the study area,the formation process of the braided fluvial delta is reconstructed and the sedimentary microfacies feature are observed through using the technology of simulation experiment.The experiment shows that the braided fluvial delta from the Kongdian provenance can be divided into 3 subfacies and 7 microfacies.The systematic study on the main controlling factors of the formation and evolution of the braided fluvial delta is completed.It is proved that basement subsidence,relative lake level changes,flow and flow fluctuation,amount of adding sand and mud(sediment supply)and so on are the main controlling factors.By comparing the actual and the experimental thickness of sand body,the distribution of the favorable reservoir in the study area has been predicted. Based on the initial geological pattern and combining with the phenomena and results of the simulation experiment,the sedimentary model of the braided fluvial delta of the second submember of member 3 of Paleogene Shahejie Formation (Es32) in Qikou Sag of Huanghua Depression is set up under the experimental condition.

Key words: Huanghua Depression, Qikou Sag, sedimentation simulation, braided fluvial delta, controlling factors, sedimentary model

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