近地表强各向异性介质对纵波-横波转换的影响

Rina Yoneki, H. Mikada
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引用次数: 0

摘要

地层,如近地表和储层岩石,估计具有强各向异性的弹性波传播。为了从地震勘探资料中提取各向异性信息,许多研究开展了弹性各向异性研究。然而,这些研究大多是基于弱各向异性介质的假设。前人的研究表明,地下强各向异性介质对地震波特别是PS转换波的波形影响显著。在本研究中,我们对PS转换波进行逆时偏移(RTM)来确定各向异性层的深度。并对其进行归一化处理,取差值比较成像结果。为了从观测数据中提取PS转换波,我们还开发了一种新的波分离方法。通过数值实验验证了该方法的有效性。数值结果表明,该方法可以成像各向同性层和各向异性层之间的层边界,从而产生PS转换波。
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Influence of near-surface strongly anisotropic medium on P-to-S wave conversion
Formations, like near surface and reservoir rock, are estimated to be strongly anisotropic for elastic wave propagation. To extract anisotropic information from seismic exploration data, many researches have conducted elastic anisotropy studies. However, most of these studies are based on the assumption of weakly anisotropic media. Our previous studies showed that strong anisotropic media in the subsurface significantly influence the seismic waveforms especially on the PS converted waves. In the present study, we apply the reverse time migration (RTM) to the PS converted waves to determine the depth of anisotropic layer. In addition, we normalized them and take difference for comparing imaging results. To extract PS converted waves from observed data, we also develop a novel wave separation method. We demonstrate the effectiveness of our method using a numerical experiment. Our numerical result shows that our method can image layer boundary between isotropic and anisotropic layers which generates PS converted waves.
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