首页 | 本学科首页   官方微博 | 高级检索  
     检索      

金湖凹陷铜城断裂带低渗透储层特征研究
引用本文:高德群,陈佳梁,李学英,汤武.金湖凹陷铜城断裂带低渗透储层特征研究[J].地质学刊,2005,29(3):147-151.
作者姓名:高德群  陈佳梁  李学英  汤武
作者单位:[1]中石化江苏油田分公司物探技术研究院,江苏南京210046 [2]中国地质大学,北京100083
摘    要:研究了金湖凹陷铜城断裂带阜宁组低渗透储层,该区阜宁组具有沉积物偏细、孔喉半径小、储层物性差的特点。对影响砂岩储层物性的主要因素进行了分析,认为成岩作用、泥岩欠压实、沉积环境、流体活动、裂缝是主要的控制因素,并对储层改造效果进行了分析。

关 键 词:铜城断裂带  低渗透储层  成岩作用  泥岩欠压实  流体活动  裂缝  江苏金湖
文章编号:1003-6474(2005)03-0147-05
收稿时间:2005-04-01
修稿时间:2005-04-07

Characteristics of low permeability reservoirs of Tongcheng fault zone in Jinhu depression of Jiangsu Province
GAO De-qun,CHEN Jia-liang,LI Xue-ying,TANG Wu.Characteristics of low permeability reservoirs of Tongcheng fault zone in Jinhu depression of Jiangsu Province[J].Jiangsu Geology,2005,29(3):147-151.
Authors:GAO De-qun  CHEN Jia-liang  LI Xue-ying  TANG Wu
Institution:1. Geophysical Technology Research Institute, Jiangsu Oilfield Branch Company, SINOPEC, Nanjing 210046, China; 2. China Geological University, Beijing 100083, China
Abstract:The characteristics of low permeability reservoirs of Funing Formation in Tongcheng fault zone of Jinhu depression are stated: they are thin sediment, small pore throat size, low porosity and permeability. In view of those characteristics, the authors analyze the mechanism of low permeability reservoirs and think that the main causes are diagenesis, mudstone lesscompaction, sedimentary environment, fluid flow, fracture.
Keywords:Tongcheng fault zone  Low permeability reservoirs  Diagenesis  Mudstone ill-compaction  Fluid flow  Fractures  Jinhu  Jiangsu
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地质学刊》浏览原始摘要信息
点击此处可从《地质学刊》下载免费的PDF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