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Seismological observations, including envelope broadening with increasing distance from an earthquake source and the excitation of long-lasting coda waves, provide a means of investigating velocity ..

The eikonal equation (Section 3.3.2.5) establishes that these two methods of treating seismic wave propagation are equivalent. The passage of a wave through a medium and across interfaces between ...

Ministers Piantedosi and Musumeci at the Memory Park in Sant’Angelo dei Lombardi for the laying of a wreath at the Plaque in ...

Shear waves split into fast and slow waves when they travel through elastically anisotropic media, and the anisotropy of the seismic velocity is recorded by seismic stations. In the Earth's deep ...