作者:范宇婷; 时间:2015-01-01 点击数:
范宇婷;
1:中国科学院地质与地球物理研究所
2:中国海洋石油总公司信息化部
摘要(Abstract):
地下介质并不是理想的弹性介质,地层存在黏性吸收作用,对地震子波的频带及峰值频率等参数产生影响.基于波场延拓理论,采用波动方程正演模拟方法,对3种不同黏性吸收程度及厚度的薄砂层进行正演模拟;采用广义S变换,分析反射复合波的瞬时频谱.结果表明:薄砂层瞬时频谱的峰值频率与无黏性吸收作用下相比大幅度变化,导致由峰值频率预测薄砂层厚度出现较大误差.陷频频率受地层黏性吸收作用比较小,相对比较稳定.利用陷频频率出现的周期性与薄砂层厚度之间的关系预测薄砂层厚度,可以为复杂地质环境下有利薄储层的定性识别和厚度定量预测提供支持.
关键词(KeyWords):黏性吸收;薄砂层;正演模拟;瞬时频谱;广义S变换
Abstract:
Keywords:
基金项目(Foundation):国家自然科学基金创新研究群体项目(41021063)
作者(Author):范宇婷;
Email:
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