docchapter 3 - Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi
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the time domain boundary element method for scalar wave problems
boundary B; the fundamental solutions and the
actual states of the differential equation (1) can be
combined through the use of the dynamical
reciprocity theorem (Banerjee, 1994), to give the
follo...
Nevzat Gencer
The seismograms correspond to the physical
geometries of Figures 1 and 4 have time (in seconds)
on the horizontal axis. All displacement values
received at the selected receiver points are
position...