Spice training network EU & ANR cattel Earthquake Energy Balance Raúl Madariaga Laboratoire de...
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![Page 1: Spice training network EU & ANR cattel Earthquake Energy Balance Raúl Madariaga Laboratoire de Géologie Ecole Normale Supérieure de Paris.](https://reader036.fdocuments.in/reader036/viewer/2022062714/56649d595503460f94a3a067/html5/thumbnails/1.jpg)
Spice training network EU & ANR cattel
Earthquake Energy Balance
Raúl MadariagaLaboratoire de Géologie
Ecole Normale Supérieure de Paris
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Modern test of earthquake scaling law
Test by Prieto et al JGR, 2004
collapsed
fs
fp
6.1/ sp ff
Circular crack model
7.1/ sp ff
)/1()(
20
20
M
Universal Spectral Shape
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Consequence of the scaling law
2300
0
CCMM
Esa
App
Apparent stress is a fraction of stress drop
Where C2 = 0.23 for Brune’s spectrum
C2= 0.33 for Boatwright’s
a
Ide et al 2004
(Savage and Wood,1971, Madariaga, 1976, Boatwright, 1980-84)
and a are almost scale independent
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vr
A simple shear crack (earthquake) moving at fast speed
Local energy balance
Gc w
Dc
slip
friction
ini
es = w - Gc
peak
external
residual
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Energy balance
sc EWSG
Self-energy change
Seismic energy
Fracture energy
S
MG ac
022
1
More than 1/3 of the stress drop is used to move the rupture!!
(used by Abercombrie and Rice, 2005)
slip
Gc scales with slip !
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= w/Gc
1
1.4
-1 = es/G
c
0
0.2
Tsunami EQ
Kunlun EQ
How to reduce speed? increase Gc
vr= 0
vr > v
s
What controls rupture propagation?
acG
w
2
a=0.33
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Far field radiation from circular crack
SpectrumDisplacement pulse
4s
0.25 Hz
decay is controled by the stopping phases not by the duration
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Elliptical crack dynamics
Stopping phase (S wave)
Slip rate Slip Stress change
Fully spontaneousrupture propagation
underslip weakening friction
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Far field radiation from an elliptical fault
Radiated signals are very variable
Spectra are not
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Isochrones and stopping phases
1st Stopping phase
2nd Stopping phase
1
2
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Stopping phases in the near field
Antiplane (SH) sectionIn plane (P-SV) section
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Conclusions
1. Current spectral models contain information about fracture and friction
2. Naive interpretation is that rupture speed is related to apparent stress
3. Gc scales with slip
4. Rough energy release rate estimates Gc can be done directly fromapparent stress (Abercombrie et Rice, 2005)
5. Actually spectral model only sees energy release rate changes!
6. Modern numerical methods simulate stopping phases very well
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P st.phase Rayleigh
S
Slip rate Slip
Rupture process for a circular crack
The rupture process is controlled by wave propagation!
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Global Energy Balance
Seismologists mesure Es directly (still difficult)
Estimate Wc from seismic moment (easily measured)
L = length scaleS = surfaceE
s = radiated energy
W
s = strain energy change
Gc
= surface energy
Kt
= Kostrov's term
L
W
s
KostrovSGWE css
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Energy flow and rupture speed
Radiated energy density es
Static energy density
From Kostrov, Eshelby, Husseini, Freund
v)(1 v
w
es
(v)
v0
Husseini et al, 1978
ass w
e 2
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Radiation from an antiplane crack with a kink
S
kink S wave(-2 )
Starting asperity
Velocity z
Stress zy
Stresszx
Rupture front
vr < v
s
Corner stresses
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Scaling of energy
Landers Gc ~ Es ~ DW ~ 106 J/m2
Sumatra Gc ~ Es ~ DW ~ 107 J/m2 W~150 km
W~15 km