The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

From the analysis of local earthquake coda waves recorded by the Benioff short‐period
vertical seismograph at Riverside, California, we found a surprisingly large and systematic …

During the 1999 Athens earthquake, the town of Adàmes, located on the eastern side of the
Kifissos river canyon, experienced unexpectedly heavy damage. Despite the particular …

In order to separate the scattering effect from intrinsic attenuation, we need a multiple
scattering model for seismic wave propagation in random heterogeneous media. In paper I …

This is the first study to present simultaneously both deconvolution and inversion, two
powerful tools of data analysis. Featured within this volume are various geophysical …

Analyzing horizontal component seismograms of small earthquakes with intermediate
hypocentral distances in southeastern Honshu, Japan, we found that time widths of …

In geophysics, the correlation functions of random media are of principal importance for
understanding and inverting the properties of seismic waves propagating in geological …

The De Wolf approximation has been introduced to overcome the limitation of the Born and
Rytov approximations in long range forward propagation and backscattering calculations …

Crustal heterogeneities and their statistical characteristics bear important information about
the dynamic processes and evolution of the crust. The velocity well‐log data from the …

The heterogeneous nature of Earth's crust is manifested in the scattering of propagating
seismic waves. In recent years, different techniques have been developed to include such …