石油学报 ›› 2014, Vol. 35 ›› Issue (4): 715-724.DOI: 10.7623/syxb201404012

• 油田开发 • 上一篇    下一篇

砂质辫状河储层构型表征方法——以苏丹穆格莱特盆地Hegli油田为例

孙天建1, 穆龙新1, 吴向红1, 赵国良1, 徐锋1, 王振军2, 覃志2, 方子奇3   

  1. 1. 中国石油勘探开发研究院 北京 100083;
    2. 中国石油吉林油田公司勘探开发研究院 吉林松原 138000;
    3. 石油工业出版社有限公司 北京 100011
  • 收稿日期:2014-02-21 修回日期:2014-05-12 出版日期:2014-07-25 发布日期:2014-08-05
  • 通讯作者: 孙天建,男,1978年4月生,2003年获江汉石油学院学士学位,2012年获中国地质大学(北京)博士学位,现为中国石油勘探开发研究院博士后,主要从事油气田开发地质方面的研究。Email:suntianjian@petrochina.com.cn
  • 作者简介:孙天建,男,1978年4月生,2003年获江汉石油学院学士学位,2012年获中国地质大学(北京)博士学位,现为中国石油勘探开发研究院博士后,主要从事油气田开发地质方面的研究。Email:suntianjian@petrochina.com.cn
  • 基金资助:

    中国石油天然气集团公司重大科技专项(2011E-2507)资助。

A quantitative method for architectural characterization of sandy braided-river reservoirs:taking Hegli oilfield of Muglad Basin in Sudan as an example

Sun Tianjian1, Mu Longxin1, Wu Xianghong1, Zhao Guoliang1, Xu Feng1, Wang Zhenjun2, Qin Zhi2, Fang Ziqi3   

  1. 1. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;
    2. Institute of Petroleum Exploration & Development, PetroChina Jilin Oilfield Company, Jilin Songyuan 138000, China;
    3. Petroleum Industry Press co., LTD, Beijing 100011, China
  • Received:2014-02-21 Revised:2014-05-12 Online:2014-07-25 Published:2014-08-05

摘要:

分析了苏丹穆格莱特盆地Hegli油田S1A单层砂质辫状河沉积微相特征,识别了砂质辫状河储层不同层次的构型界面,将其划分为辫流带、单砂体和心滩内增生体3个层次,明确了目的层辫状河道具有泥质充填、半泥质充填和砂质充填3种模式。依据砂质辫状河储层不同层次构型单元规模的计算公式,实现了砂质辫状河储层的辫流带、单砂体和心滩内增生体规模的定量表征,形成了一套砂质辫状河储层不同层次构型单元定量表征的方法。定量表征的结果表明,研究区辫流带宽度约3 200 m,心滩宽度350~900 m,心滩长度1 200~3 200 m,单河道宽度100~300 m,增生体的宽度和长度分别为100~400 m和700~2 000 m。以不同构型单元定量表征的规模为约束条件,采用相控与人机交互的方法,建立了能够反映辫状河储层构型空间分布特征的三维地质模型。

关键词: 苏丹, 砂质辫状河, 层次分析, 储层构型, 构型建模

Abstract:

The characteristics of microfaces in single-layer sandy braided-river deposits of the S1A of the Hegli oilfield, Muglad Basin, Sundan are analyzed, and three hierarchical levels of architecture interfaces in sandy braided-river reservoirs are identified, including single braided channel belt, single sand body, and single accretion of channel bar. The target braided channels are filled in three models with mudstone, semi-mudstone, and sand bodies, respectively. The scales of architectural units at different hierarchical levels in sandy braided-river reservoirs are quantitatively characterized using specific calculation formulas, and a set of methods for quantitative characterization of architectural units in sandy braided-river reservoirs is developed. The results of sing-level quantitative characterization show that single belts are approximately 3 200 m wide; single channel bars are 350-900 m wide and 1 200-3 200 m long; single channels are 100-300 m wide; and single accretions are 100-400 m wide and 700-2 000 m long in S1A of the study area. With the constraint of the scale for quantitative characterization of different architectural units, a three-dimensional geological model is built using facies-control and man-computer interaction method to accurately delineate spatial distribution pattern of architectural units in sandy braided-river reservoirs.

Key words: Sudan, sandy braided river, analytical hierarchy process, reservoir architecture, architecture model

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