小波多尺度井间地震衰减层析成像

 本文提出了一种井间地震衰减层析成像方法，首先采用小波多尺度分解；然后采用程函方程有限差分法进行井间地震走时计算，反演出井间速度结构；最后采用相邻道比值法消除震源对成像结果的影响，完成共炮集记录的振幅衰减成像。通过对含洞层状模型用黏滞声波方程交错网格高阶有限差分法合成的井间数据的计算表明：本方法与程函方程有限差分法计算的初至走时精度吻合较好，波场快照不但精确描述了正传方向和反传方向上地震波前面的特征，而且定量描述了地震波传播过程中的能量转换；振幅衰减值层析成像剖面准确刻画出了模型中洞的大小和位置。

Multi-scaled seismic-attenuated cross-hole tomographic imaging of wavelet

The paper presented a method of seismic-attenuated cross-hole tomographic imaging. Firstly, Using multi-scaled wavelet decomposition; then, using finite-difference algorithm of eikonal equation to compute the cross-hole seismic travel times and make inversion of cross-hole velocity structure; finally, using adjacent traces ratio method to eliminate the influence of source on imaging results, finishing the amplitude-attenuated imaging of common-shot gather records. The computation of cross-hole data, synthesized by high-order staggering finite-difference algorithm of viscous-acoustic equation of cavern-bearing layered model, showed that the precision of first breaks travel-time computed by the method is coincident with that by finite-difference of eikonal equation; the wavefield snapshots not only precisely describe the feature of seismic wavefronts in both forward and backward travel directions, but also quantitatively describe the energy transformation in a process of seismic wave propagation; the amplitude-attenuated tomographic imaging sections can accurately describe the size and position of caverns in model.