海拉尔盆地乌东地区裂缝储层综合分析
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摘要
本文基于海拉尔盆地乌东地区三维地震资料,通过构造应力场分析、叠前地震属性方位各向异性分析和叠后地震衰减属性分析等方法,对该地区的裂缝储层进行了预测。利用叠后裂缝属性和构造应力场分析对宏观裂缝发育带进行了定性预测,总结出乌东地区裂缝方向以北北西向和北东东向为主,并利用叠前地震属性方位各向异性定量预测了该区裂缝密度。
Based on the 3D seismic data in Wudong Area of Hailar Basin,the fracture reservoir was predicted in this area by using several methods,such as tectonic stress field analysis,pre-stack seismic attribute azimuth anisotropy analysis,post-stack seismic attenuation attribute analysis and so on.The qualitative prediction for the macroscopic fracture development zone was conducted by using post-stack fracture attribute method and the tectonic stress field analysis method,it was found out in the study that the fracture orientation is mainly in NNW and NEE direction,the fracture density was quantitatively predicted by using pre-stack seismic attribute azimuth anisotropy analysis method.
引文
[1]张亚中,周晶,李建华.青西凹陷南次凹裂缝性储层地震综合预测.石油地球物理勘探,2009,44(2):225~230
    [2]童亨茂.储层裂缝描述与预测研究进展.新疆石油学院学报,2004,25(5):9~14
    [3]陈守田,刘招君.海拉尔盆地含油气系统.吉林大学学报(地球科学版),2002,32(2):151~154
    [4]王建民,刘杰烈,陈守田.海拉尔盆地岩性—地层油气藏勘探前景.石油地球物理勘探,2006,41(4):439~441

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