济阳坳陷馆上段河道砂体地震识别方法——以孤南洼陷为例
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
济阳坳陷馆上段岩性油气藏隐蔽性强,直接的地震识别有因难。本文在研究孤南洼陷馆上段基本地质特征的基础上,总结了曲流河砂体的地震识别方法:运用地震相分析初步确定砂体发育区域;根据地震相干分析显值低、累计振幅值强的特点划分砂体有利区带和分布范围;在地震反演剖面上落实砂体位置;综合解释确定砂体几何形态。该方法已付诸实践,识别效果好。
A lithological reservoir of the upper of Ng2 in Jiyang depression is extremely subtle, the direct seismic identification is difficult. A seismic method for identifying meander river has been summed based on analyzing Guna sag upper Ng2 geology character. Sand body growth area has been determined by using seismic facies, benefit sand body belt and distribution range have been divided according to the low seismic facies analysis and strong added amplitude. Sand body position has been carried out in seismic inversion section and sand body geometry has been determined by synthesis interpretation. The method has been put into practice and identification effect is better.
引文
[1]张善文,王永诗,石砥石等.网毯式油气成藏体系——以济阳坳陷新近系为例.石油勘探与开发,2003.30(1):1 ̄9
    [2]孙义梅,陈程等.相干技术的参数选取及其效果.石油地球物理勘探,2001,36(5):640 ̄645
    [3]王永刚,乐友喜.综合地球物理信息孔隙率预测方法及应用效果.石油地球物理勘探,2001,36(6):707 ̄715
    [4]张善文,杨凤丽,李文涛等.几种类型油气藏的描述方法及应用.石油地球物理勘探,2000,35(4):419 ̄427
    [5]于建国,路慎强等.测井约束反演技术在史南浊积砂体描述中的应用.石油物探,2002,40(2):104 ̄107

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心