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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Source wavelet and local wave propagation effects on the amplitude-variation-with-offset response of thin-layer models: A physical modeling study
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Source wavelet and local wave propagation effects on the amplitude-variation-with-offset response of thin-layer models: A physical modeling study

机译:源小波和局部波传播对薄层模型的幅度变化 - 偏移响应的影响:物理建模研究

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In target layers with thicknesses below the vertical seismic resolution as thin layers, the tuning effect/interference between the wave propagation modes may increase the challenge of doing amplitude-variation-with-offset (AVO) analysis because it is difficult to recover the primary PP amplitudes embedded in the data by further seismic data processing. Thus, we have investigated the importance of the primary PP reflections, locally P-SV converted waves, and internal multiple reflections in the amplitude response of two thin-layer seismic physical models. One model consists of a thin water layer embedded between two nylon plates, and another model with a thin acrylic layer surrounded by water. Numerical modeling using the reflectivity method was applied to analyze each wave propagation mode and the source waveform role in the experimental data. Before the experimental reflection data acquisition, we characterized two source and receiver piezoelectric transducer (PET) pairs: one with a circular plane face and the other with a semispherical face. We measured the source wavelet, its dominant frequency, and the PETs' directivity pattern. Semispherical PETs were chosen to acquire common midpoint reflection data. Thereafter, a processing workflow was applied to remove linear events interfering with the target reflections and to correct amplitudes due to transmission losses, source/receiver directivity, and geometric spreading effects. Finally, we investigated the thin-layer targets near incidence angle amplitude and the AVO response. The results showed that the interference between the primary PP reflections and the locally converted shear waves may considerably affect the observed amplitude response. The source wavelet bandwidth appeared as a second-order effect, and the internal multiple reflections were practically negligible. These results suggested that in real data sets, it is important to investigate the wave propagation modes and source wavelet role in the amplitud
机译:在垂直地震分辨率以下厚度的靶层中,波传播模式之间的调谐效果/干扰可能增加进行幅度变化 - 偏移(AVO)分析的挑战,因为难以恢复主PP通过进一步的地震数据处理嵌入数据中的幅度。因此,我们研究了主PP反射,局部P-SV转换波的重要性,以及两个薄层地震物理模型的幅度响应中的内部多反射。一种模型由嵌入两个尼龙板之间的薄水层和另一种模型组成,以及由水包围的薄丙烯酸层的另一模型。应用了使用反射率方法的数值建模来分析实验数据中的每个波传播模式和源波形作用。在实验反射数据采集之前,我们表征了两个源和接收器压电换能器(PET)对:一个具有圆形平面面,另一个具有半球形面。我们测量了源小波,其主频率和宠物的方向性模式。选择半球形宠物获取共同的中点反射数据。此后,应用处理工作流以消除干扰目标反射的线性事件,并通过传输损耗,源/接收器方向性和几何扩展效果来校正幅度。最后,我们研究了近摄接触角幅度和AVO响应的薄层目标。结果表明,主PP反射和局部转换的剪切波之间的干扰可以显着影响观察到的幅度响应。源小波带宽出现为二阶效果,内部多个反射实际上是可忽略不计的。这些结果表明,在实际数据集中,重要的是要研究众所周知的波传播模式和源小波角色

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