【摘要】 地层存在各向异性时,将使地震波速度和时距曲线变得很复杂。在现有理论基础上,较系统地分析了地层各向异性系数与速度及时距曲线之间的关系,并进一步研究了各向异性介质纵波,特别是P-SV转换波的速度分析方法。该方法不仅可求得各向异性介质的地震波速度,而且可求得地层各向异性参数。经理论模型试处理证明了该方法的正确性。更多还原

【Abstract】 When the layers have the anisotropic properties, seismic wave’s velocity and moveout will (become) complex. On the basis of literatures appeared, this paper analyses the relations between anisotropic parameters and velocity as well as moveout by the numbers. It studies the method of anisotropic velocity analysis about pressure wave, especially converted-wave. This method can derive not only seismic wave’s velocity but also the anisotropic parameters. And it is proved to be valid by processing theoretical models.更多还原