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Insights into earthquake source physics from high-frequency ... - IRIS

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Order of magnitude estimates of contributions<br />

T<br />

m 0 c*<br />

/ V 1<br />

0 ).<br />

/ V 1<br />

d 0 ) c*<br />

/ V2 0 ) c / c /.<br />

/ V 2<br />

m # *<br />

i<br />

ij<br />

c ijkl<br />

ij<br />

c ijkl<br />

T<br />

kl<br />

d # ) *<br />

kl<br />

c ).<br />

m / d 0 V1 / V<br />

) c .<br />

2<br />

Lab and seismic data suggests that C/)C during brittle failure may be ~0.5 or more<br />

(can be ~1 in explosions).<br />

Seismic data suggest that )./. during <strong>earthquake</strong>s is ~0.1-0.2.<br />

Unless V 1<br />

>> V 2<br />

, u damage > u trad !!!<br />

The DC component of u damage<br />

can be zero, so much of the radiation is<br />

expected to be in <strong>high</strong> <strong>frequency</strong> waves!

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