J4 ›› 2011, Vol. 41 ›› Issue (4): 999-1005.

• 地质与资源 • 上一篇    下一篇

杏南开发区葡Ⅰ31小层废弃河道类型及其研究意义

翟志伟1|施尚明1|朱焕来1|师江波2   

  1. 1.东北石油大学地球科学学院|黑龙江 大庆163318;
    2.大庆油田有限责任公司勘探开发研究院|黑龙江 |大庆163712
  • 收稿日期:2010-10-09 出版日期:2011-07-26 发布日期:2011-07-26
  • 作者简介:翟志伟(1982-)|男|山西晋中人|博士研究生|主要从事油气田开发地质及地热资源综合评价研究|E-mail:dqpizzw@126.com
  • 基金资助:

    黑龙江省自然科学基金项目(ZJG0606-02)

Types and Study Significance of Abandoned Channel for PⅠ31 Layer in Xingnan Development Area

ZHAI Zhi-wei1|SHI Shang-ming1|ZHU Huan-lai1|SHI Jiang-bo2   

  1. 1.College of Earth Sciences, Northeast Petroleum University, Daqing163318, Heilongjiang, China;
    2.Exploration &|Development Institute, Daqing Oil Field Company Ltd., Daqing163712|Heilongjiang, China
  • Received:2010-10-09 Online:2011-07-26 Published:2011-07-26

摘要:

油田开采进入高含水期后,储层构型的精细描述对改善油田开采效果具有重大意义。废弃河道作为单一河道的边界以及识别点坝砂体的重要依据,其顶部的泥质沉积或者砂泥岩互层沉积对储层内部流体具有遮挡作用,因此正确识别废弃河道是进一步分析储层构型及挖潜油田剩余油的重要科学依据。以杏南开发区葡Ⅰ31小层为例,通过分析废弃河道在平面及剖面的沉积特征,利用砂顶相对等深图法,综合废弃河道的砂体平面分布形态和测井曲线响应特征,在葡Ⅰ31小层内识别出26处规模不等的废弃河道,宽度一般在100 m左右,其中3处突弃型废弃河道与渐弃型相比,弯曲程度更大,砂体延伸更短,沉积厚度为2~8 m不等。由于砂泥互层或泥质沉积的侧向遮挡作用,废弃河道砂体与正常河道砂体组成的半连通体导致有注无采或有采无注的注采不平衡现象,使得河道砂体顶部成为剩余油聚集的有利场所,成为进一步挖潜的重点对象。

关键词: 储层构型, 单一河道, 点坝, 废弃河道, 沉积作用, 大庆

Abstract:

When the oil fields exploration enters the period of high water-cut, fine description of reservoir structure is of great significance to improve the effect of oil exploration. As abandoned channels are important basis for identification of point-bar sand bodies and single channels boundary, the mud or sand and shale inter bedded sedimentary on the top of abandoned channels keeps off fluids in reservoir, so it is essential scientific basis for analyzing reservoir structure deeply and tapping remaining oil to identify the abandoned channels correctly. We take PⅠ31 layer in Xingnan development area for example, by analyzing the plane and section sedimentary characters of abandoned channels, utilizing method of relative depth contour of sand top, combining plane patterns of sand distribution and log curves response characteristics of abandoned channels, 26 abandoned channels of different size are identified in PⅠ31 layer of the area, and the width is generally around 100 m. Compared with gradually disposable abandoned channels, three sudden disposable abandoned channels sand bending degree is even bigger and extension range is shorter, and the sedimentary thickness is between 2 and 8 meters. As the lateral block action of inter bedded sandstone and mudstone or mud stone, the semi-communicated sand body combined with abandoned channels and general channels brings about unbalanced injection and production system for having injection no production or having production no injection. Top of channels sand becomes favorable zone for collection of residual oil, which is the focal points for further excavation.

Key words: reservoir structure, single channel, point bar, abandoned channel, sedimentation, Daqing

中图分类号: 

  • P618.13
[1] 刘海, 林承焰, 张宪国, 王宏伟, 付晓亮, 李佳. 孔店油田馆陶组辫状河储层构型及剩余油分布规律[J]. 吉林大学学报(地球科学版), 2018, 48(3): 665-677.
[2] 高翔, 刘志宏, 聂志阳, 姚勇, 贾卧, 王超, 宋健. 松辽盆地大庆长垣形成时间的厘定及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 74-83.
[3] 康健, 韦庆海, 周琳, 高研, 张永刚, 高峰. 利用地震台阵观测资料研究大庆地区深部构造[J]. 吉林大学学报(地球科学版), 2016, 46(3): 900-910.
[4] 陈欢庆, 梁淑贤, 舒治睿, 邓晓娟, 彭寿昌. 冲积扇砾岩储层构型特征及其对储层开发的控制作用——以准噶尔盆地西北缘某区克下组冲积扇储层为例[J]. 吉林大学学报(地球科学版), 2015, 45(1): 13-24.
[5] 刘志宏, 梅梅, 柳行军, 吴相梅, 万传彪, 林东成, 高军义. 海拉尔盆地贝尔凹陷伸展断层转折褶皱作用及其对沉积作用的制约[J]. J4, 2012, 42(5): 1330-1337.
[6] 汤洁, 李娜, 李海毅, 卞建民, 李昭阳, 崔玉军. 大庆市大气干湿沉降重金属元素通量及来源[J]. J4, 2012, 42(2): 507-513.
[7] 白云风, 冯志强, 程日辉, 任延广, 唐华风. 大庆长垣扶余油层沉积层序构成及充填响应[J]. J4, 2012, 42(2): 312-320.
[8] 王长明. 内蒙古大井矿床碳氧同位素组成及其成因意义[J]. J4, 2010, 40(4): 810-820.
[9] 张志斌, 李建华, 黄超义, 刘虹, 赵岩辉. 东升庙矿床成因和找矿研究[J]. J4, 2010, 40(4): 791-800.
[10] 伊振林, 吴胜和, 杜庆龙, 张保国, 岳大力, 李艳平. 冲积扇储层构型精细解剖方法--以克拉玛依油田六中区下克拉玛依组为例[J]. J4, 2010, 40(4): 939-946.
[11] 李飞, 程日辉, 王璞珺, 侯景涛. 松辽盆地东缘下白垩统营城组二段火山碎屑岩的发育特征[J]. J4, 2009, 39(5): 803-810.
[12] 马志红, 王连生, 郭占谦, 刘立,李福来. 大庆长垣喇、萨、杏油田天然气动态机制及深部气源[J]. J4, 2008, 38(5): 726-0730.
[13] 高淑琴,苏小四,杜新强,谢轶,齐素文. 大庆西部地下水位降落漏斗区水资源人工调蓄方案[J]. J4, 2008, 38(2): 261-0267.
[14] 王璞珺,吴河勇,庞颜明,门广田,任延广,刘万洙, 边伟华. 松辽盆地火山岩相:相序、相模式与储层物性的定量关系[J]. J4, 2006, 36(05): 805-812.
[15] 付 广,康德江,段海凤. 泥质岩盖层对水溶相天然气封闭能力的综合评价方法及其应用[J]. J4, 2006, 36(01): 60-0065.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!