Seismological asperities from the point of view of dynamic rupture modeling: the 2007 Mw6.6 Chuetsu-Oki, Japan, earthquake
Abstract
We study the ground motion simulations
based on three finite-source models for the 2007
Mw6.6 Niigata Chuetsu-oki, Japan, earthquake in order
to discuss the performance of the input ground motion
estimations for the near-field seismic hazard analysis.
The three models include a kinematic source inverted
from the regional accelerations, a dynamic source on a
planar fault with three asperities inferred from the very-
near-field ground motion particle motions, and another
dynamic source model with conjugate fault segments.
The ground motions are calculated for an available 3D
geological model using a finite-difference method. For
the comparison, we apply a goodness-of-fit score to the
ground motion parameters at different stations, includ-
ing the nearest one that is almost directly above the
ruptured fault segments. The dynamic rupture models
show good performance. We find that seismologically
inferred earthquake asperities on a single fault plane can
be expressed with two conjugate segments. The rupture
transfer from one segment to another can generate a
significant radiation; this could be interpreted as an
asperity projected onto a single fault plane. This
example illustrates the importance of the fault geometry
that has to be taken into account when estimating the
very-near-field ground motion
Domains
Earth Sciences
Origin : Publication funded by an institution
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