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Traveltimes and conversion-point positions for P-SV converted wave propagation in a transversely medium: numerical calculations and physical model studies

机译:P-SV转换波在横向介质中传播的传播时间和转换点位置:数值计算和物理模型研究

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This study uses ultrasonic physical modelling to test the accuracies of numerical calculations of traveltimes and conversion-point (CP) positions for P-SV wave propagation in a horizontal transversely isotropic (TI) medium. Study results show that the traveltimes and CP positions for P-SV wave propagation on the isotropic plane of a TI medium computed using Fermat's minimum-time principle are the same as those of using the isotropic non-hyperbolic moveout equation and the isotropic CP equation. However, for P-SV wave propagation on the symmetry-axis plane of a TI medium, the arrival times and CP positions of SV-waves are difficult to determine by any ray methods when the propagation directions of SV-waves are within the cuspoidal SV-wave group velocities zone. But the first arrival times and the propagation of the dominant energy of P-SV waves can still be analysed by ray methods. Based on the calculation of Fermat's minimum-time principle, if the source-receiver offset is greater than a critical distance, the reflection angles of the converted SV-waves are fixed at a specific angle with a local maximum SV-wave group velocity of the neighbourhood area. This is because the converted SV-waves prefer to propagate along the cuspoidal directions with larger amplitude and higher velocity. Verified by the physical modelling, the Fermat's minimum-time principle used to calculate traveltimes of P-SV waves is better than the anisotropic non-hyperbolic moveout equation. The physical modelling for the CP position experiment can give a clearer visualisation of the variations of CP positions in the profile, and the feasibility of using Fermat's minimum-time principle to determine CP positions is also better than that of the anisotropic CP equations. Therefore, in the seismic data processing, Fermat's minimum-time method is recommended to accurately determine the arrival times and CP positions of P-SV wave propagation in TI media.
机译:这项研究使用超声物理建模来测试在水平横观各向同性(TI)介质中P-SV波传播的传播时间和转换点(CP)位置的数值计算的准确性。研究结果表明,使用费马最小时间原理计算的TI介质各向同性平面上P-SV波传播的传播时间和CP位置与使用各向同性非双曲时差方程和各向同性CP方程的传播时间和CP位置相同。然而,对于P-SV波在TI介质的对称轴平面上的传播,当SV波的传播方向在棘突状SV内时,很难通过任何射线方法确定SV波的到达时间和CP位置。波群速度带。但是,仍然可以通过射线方法分析P-SV波的初次到达时间和主要能量的传播。根据Fermat最小时间原理的计算,如果源-接收器偏移量大于临界距离,则转换后的SV波的反射角将固定为特定角度,且该波的局部最大SV波组速度为邻里区域。这是因为转换后的SV波更喜欢以较大的振幅和较高的速度沿针状方向传播。通过物理建模验证,用于计算P-SV波传播时间的费马最小时间原理优于各向异性非双曲时差方程。 CP位置实验的物理模型可以更清晰地显示轮廓中CP位置的变化,并且使用Fermat的最小时间原理确定CP位置的可行性也比各向异性CP方程更好。因此,在地震数据处理中,建议使用Fermat的最小时间方法来准确确定TI介质中P-SV波传播的到达时间和CP位置。

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