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摘要
利用最小相位逆小波计算地震Q值介绍1 M.T. TANER 1 S. TREITEL 2 Rock Solid Images 2600 South Gessner Ste 650 Houston TX 77063 USA 2 TriDekon压力波和横波衰减的估计与层间速度的估计同样重要。衰减为岩性和储层特征提供了额外的视角。另一方面，由于吸收引起的高频损耗降低了地震波的带宽，从而降低了地震图像的分辨率。在一种情况下，我们需要确定衰减，而在另一种情况下，我们必须这样做
Computing Seismic Q Using Minimum Phase Inverse Wavelet
P002 COMPUTING SEISMIC Q USING MINIMUM PHASE INVERSE WAVELETS INTRODUCTION 1 M.T. TANER 1 S. TREITEL 2 1 Rock Solid Images 2600 South Gessner Ste 650 Houston TX 77063 USA 2 TriDekon Estimation of attenuation of pressure and shear waves is as important as the estimation of interval velocities. Attenuation provides an additional perspective of the lithology and reservoir characteristics. On the other hand high frequency losses due to absorption reduce the bandwidth of the seismic waves and consequently the resolution of the seismic images. In one case we need to determine attenuation while in the other we have to
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