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S eismic wave P ropagation and I maging in C omplex media: a E uropean network. Preliminary results of earthquake ground-motion modeling in the Valley of Grenoble, French Alps FRANTISEK GALLOVIC PETER FRANEK Charles University, Prague Comenius University, Bratislava
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Seismic wave Propagation and Imaging in Complex media: a European network Preliminary results of earthquake ground-motion modeling in the Valley of Grenoble, French Alps FRANTISEK GALLOVIC PETER FRANEK Charles University, Prague Comenius University, Bratislava Task Groups: Local Scale, Numerical Methods
Grenoble prediction experiment Input: Structural modelandbasic properties of the point (finite-extent) sourceTask: ground motions inside and outside of the Grenoble Valley Its extention (finite-extent source) • Two rupture scenarios (more in near future) • Applicability of “synthetic transfer functions” in scenario studies to account for the basin effects
3D finite-difference (FD) method • staggered-grid displacement-velocity-stress scheme • 4th-order in space, 2nd-order in time • Adjusted FD Approximation technique (Kristek et al. 2002) • Rheology of Generalized Maxwell Body (Kristek and Mozco 2003) • Parallelized by Kristek (on 4CPU approximately 10x faster than on 1CPU)
N Computational FD model BEDROCK SOIL Q: 50 m Q: : 2730 kg/m3
grid spacing in finer grid: 30.0 m grid spacing in coarser grid: 90.0 m time step: 0.002 s frequency range: 0.2 – 2.0 Hz Computational FD model
Homogeneous Source model • Kinematic model • Strike 120°, Dip 90°, Rake 180° • Fault plane: 9 x 4.5 km2 • Hypocentral depth: 3 km • Boxcar slip velocity function • Constant • Rise time (1.1 sec) • Rupture velocity (2.8 km/s) • Final slip (1.1 m)
Heterogeneous Source model • Kinematic model • Strike 120°, Dip 90°, Rake 180° • Fault plane: 9 x 4.5 km2 • Hypocentral depth: 3 km • Brune’s pulse slip velocity function • Constant • Rise time (1.1 sec) • Rupture velocity (2.8 km/s) • Final slip (1.1 m)
Heterogeneous Source model • Slip distribution is randomly distributed subsources over the fault plane (Gallovic & Brokesova, submitted to PEPI) • Considered scaling impliesthatresultingslip distributionisk-2 (Andrews, 1980)
NS 1 sec 5 sec 9 sec EW Z
“synthetic transfer function” Models’ nomenclature Basin model included Basin model excluded Heterogeneous source model G1 G2 Homogeneous source model G3 G4 Point source model G5 G6 rG34 = G3 / G4 * G2 … uses finite-source rG56 = G5 / G6 * G2 … uses point-source
R 34EW comp. Rock site - additional arrivals of waves reflected from the basin
R 34EW comp. Rock site - additional arrivals of waves reflected from the basin
R 5NS comp. Great improvement of synthetics when the transfer functions is applied
R 5EW comp. Great improvement of synthetics when the transfer functions is applied
EW comp. R 6 NS comp. Same fit for rG34 and rG56 at NS comp., while better fit for rG34 at NS comp.
EW comp. R 6 NS comp. Same fit for rG34 and rG56 at EW comp., while better fit for rG34 at NS comp.
Preliminary conclusion Outlook • Use of “synthetic transfer functions”taking into account finite extent of the fault (model rG34) results generally in better agreement with exact calculation (with respect to rG56) • The method seems promising for quick scenario studies • To recompute G3 and G4 models with smooth slip function • To perform the same procedure with different scenarios (varying slip and nucleation point position) • To utilize a method for quantitative comparisons • To consider, in addition, topography in the Grenoble area