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The dynamics of the earthquake rupture process are closely related
to fault zone properties which the authors have intensively
investigated by various observations in the field as well as by
laboratory experiments. These include geological investigation of
the active and fossil faults, physical and chemical features
obtained by the laboratory experiments, as well as the
seismological estimation from seismic waveforms. Earthquake dynamic
rupture can now be modeled using numerical simulations on the basis
of field and laboratory observations, which should be very useful
for understanding earthquake rupture dynamics.
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