首页 | 官方网站   微博 | 高级检索  
     

珠江口盆地西江30-2油田新近系中新统沉积微相及层序地层分析
引用本文:李胜利,于兴河,张志杰,朱庆荣,王庆如,梁卫,周锦.珠江口盆地西江30-2油田新近系中新统沉积微相及层序地层分析[J].古地理学报,2004,6(1):30-40.
作者姓名:李胜利  于兴河  张志杰  朱庆荣  王庆如  梁卫  周锦
作者单位:1.中国地质大学能源系北京1000832 ;2.中国海洋石油南海东部公司研究院广州510240
基金项目:国家自然科学基金资助 ,编号 :40 2 42 0 15,珠江口盆地 (东部 )砂岩油田典型油藏沉积微相、储量复算和剩余油分布研究,横向合作项目资助,编号 :2 0 0 1-SW -0 02
摘    要:西江30-2油田位于珠江口盆地惠州凹陷南部的次级构造带上,油田主要分布在新近系中新统的珠江组及韩江组下部。研究区目的层段主要为三角洲沉积,其沉积微相类型丰富,既包括三角洲平原的分流河道、分流间湾、天然堤、决口扇沉积,又包括三角洲前缘的水下分流河道、河口坝、远砂坝及席状砂沉积等,其中分流河道、水下分流河道及河口坝等主要砂体的单层厚度大、连续性好。目的层段可划分为4个长期基准面旋回和15个中期旋回。根据区内的4种测井旋回划分模式,其短期旋回(五级层序)对应油藏级别;而超短期旋回(六级层序)与砂体级别一致,且基本与砂体微相的划分一致。本文中采用高分辨率层序地层学的方法进行油田开发过程中的砂体对比,充分考虑了区块大小、构造位置、沉积微相变化及井距大小,其结果表明油藏顶部以上升半旋回(正旋回)为主的分流河道或水下分流河道易产生水淹;而以下降半旋回(反旋回)为主的河口坝砂体和间湾不易水淹,这有利于剩余油的分布。

关 键 词:沉积微相  高分辨率层序地层  砂体对比  水淹  剩余油分布
文章编号:1671-1505(2004)01-0030-11
修稿时间:2003年8月2日

Sedimentary microfacies and sequence stratigraphy of the Miocene of Neogene in Xijiang 30-2 Oil Field,Pearl River Mouth basin
Li Shengli Yu Xinghe Zhang Zhijie Zhu Qingrong Wang Qingru Liang Wei Zhou Jin China University of Geosciences,Beijing ,Nan Hai East Institute of CNOOC,Guangzhou ,Guangdong.Sedimentary microfacies and sequence stratigraphy of the Miocene of Neogene in Xijiang 30-2 Oil Field,Pearl River Mouth basin[J].Journal of Palaeogeography,2004,6(1):30-40.
Authors:Li Shengli Yu Xinghe Zhang Zhijie Zhu Qingrong Wang Qingru Liang Wei Zhou Jin China University of Geosciences  Beijing  Nan Hai East Institute of CNOOC  Guangzhou  Guangdong
Affiliation:1.China University of Geosciences, Beijing100083,;2.Nan Hai East Institute of CNOOC, Guangzhou510240,Guangdong
Abstract:Xijiang30-2 Oil Field is located at the sub-structural belt in southern Huizhou Depression in the Pearl River Mouth basin.This oilfield is mainly distributed in the Zhujiang Formation and the lower part of the Hanjiang Formation of Miocene of Neogene. The sedimentary facies of the studied formation is a delta in Xijiang 30-2 Oil Field. In this area, the types of sedimentary microfacies include distributary channel, inter-distributary, natural levee and crevasse splay in the delta plain and underwater distributary channel, mouth bar,distributary bar and sand sheet in the delta front. The major sandbodies, such as distributary channel, underwater distributary channel and mouth bar, relatively, are thick and continuous. Meanwhile, the studied formation consists of 4 long-term base level cycles and 15 mid-term base level cycles in Xijiang 30-2 oilfield. On the basis of these, 4 types of logging models about short-term and supper short-term base level cycles are summarized in this area.As for this area, approximately, short-term base level cycle, which is equal to the fifth order sequence, can be correlated with reservoir strata,while supper short-term cycle, which corresponds to the sixth order sequence,corresponds to sand body and sedimentary micro-facies. When correlating the sand bodies based on high resolution sequence stratigraphy, it is very important to take into account the scale of the work area, the tectonic position,the diversities of the sedimentary microfacies and the well spacing.In Xijiang 30-2 Oil Field, at the reservoir top, the distributary channel or underwater distributary channel mostly with base level rising half cycle is apt to flood,however, the sand bar(distributary mouth bar or distal bar) or distributary bay mainly with base level falling half cycle is not prone to flood ,among which it is propitious to remaining oil distribution.
Keywords:sedimentary microfacies  high resolution sequence stratigraphy  sandbody correlation  waterflooding  remaining oil distribution
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《古地理学报》浏览原始摘要信息
点击此处可从《古地理学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号