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低频阴影的分析和应用基于多孔介质的非对称理论
Shoucheng Xu1, Xiuquan Hu2,3,4, Duo Xu5
1College of Energy (College of Modern Shale Gas Industry), Chengdu University of Technology, Chengdu, 610059, Sichuan, China.
Scientific reports
|October 29, 2024
概括
气体储库下面的低频阴影是由缓慢的P波在多孔介质中从快速的P波转换而产生的. 这项研究证实,缓慢的P波是分散和减弱的关键,解释了这些地震异常.
科学领域:
- 地质物理学 地质物理学
- 地震勘探 - 地震勘探
- 孔隙介质物理 孔隙介质物理
背景情况:
- 气体储下面的低频阴影并不能完全由传统的P波衰减或分散来解释.
- 现有的理论无法解释观察到的时间延迟和能量损失.
研究的目的:
- 为了研究低频阴影的原因,使用一个新的透介质的无对称理论.
- 分析地震P波在层层的透气水库中的分散和衰减特征.
- 验证一种用于计算和分析3D地震数据中的低频阴影的方法.
主要方法:
- 基于多孔介质的非对称理论,对快速和缓慢的P波分散和衰减进行前分析.
- 分析计算低频阴影发生频率的方法.
- 应用S变换时间频率分析到四川工作区的3D地震数据的应用M.
主要成果:
- 快P波在地震频段内没有显著的分散或衰减.
- 慢P波被确定为分散和衰减的主要原因,导致低频阴影.
- 对地震数据的S转换分析揭示了与井数据一致的低频阴影异常.
结论:
- 新的非对称理论有效地解释了在多孔介质中通过P波模式转换的低频阴影.
- 缓慢的P波对于理解天然气储库中的地震波行为至关重要.
- 在实际的地震勘探中,S-转换方法在识别低频阴影方面具有很强的适用性.
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