Abstract

This paper presents an approach to estimation of frequency-dependent attenuation of seismic waves that propagate in the earth’s subsurface. This approach is based on the waveform inversion of vertical seismic profiling data acquired in a borehole. The use of well log data (in particular, sonic and density logs) in the forward modeling routine makes it possible to separate two factors that cause frequency-dependent seismic attenuation. In particular, the inversion facilitates separation of 1D scattering versus inelastic absorption in the horizontally layered subsurface.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call