VTI介质中的地层弹性参数反演
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摘要
在VTI介质中,用非双曲线可以很好地近似P—P波中长排列情况下的旅行时;而对于P-SV波来说,应用非双曲线却不能很好地近似P-SV波的旅行时。对P-P波、P-SV波的旅行时进行三项泰勒展开时,它们的系数却包含了地震波的各向异性信息及其垂直速度信息,这为地震波的弹性参数反演提供了基础。实验分析表明,在中等排列长度下可以精确地得到P—P波、P—SV波旅行时的三项泰勒展式系数,从而可以精确地进行地层弹性参数反演。
In VTI media, P - P wave traveltime curve can be approximated by a nonhyperbola for a long or middle spread, as for P - SV wave, nonhyperbola is not accurate enough to fit traveltime curve. Three - term Taylor series for t2 - x2 curves of P - P and P - SV waves over layered vertically transverse isotropic media are related to dimensionless parameters and vertical velocities of P - and S - wave, which provide a basis for seismic elastic parameter inversion. Only in middle spread, three- term Taylor series for t2 - x2 curves of P - P and P - SV waves can precisely be obtained in modeling analysis, meanwhile seismic elastic parameter inversion can'be implemented precisely too.
引文
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