Page 293 - Numerical Analysis and Modelling in Geomechanics

274 THE 2-D CHEBYSHEV SPECTRAL ELEMENT METHOD

Figure 9.6 Transect t03. (a) Detail of the uppermost part of the model. See Table 9.1 for
the model parameters. Surface distribution of (b) response spectra (5% damping) and (c)
displacement difference (horizontal component) computed for a receiver distance ≥ x=50
m. (d) Seismograms (three components) and (e) response spectra (radial and vertical
components) predicted at two near receivers (see panel (a)) located on sediments (A) and
lava (B), respectively (from Priolo (2000)).