Abstract
We report that during the two devastating 1999 earthquakes in Turkey,
rupture propagated over a large part of the nearly 200 km long fault
zone at supershear speed approaching 5 km/s. We present observations
and modeling which confirm the original inference of supershear rupture
during the Izmit earthquake and we show that supershear rupture also
occurred during the Düzce earthquake. We show that the rupture
velocity measured - about 2 times the shear wave velocity - is the
value predicted by theoretical studies in fracture dynamics. We look
for clues to explain these observations.
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