The radiation-pattern section showed that the far-field P amplitude of a double…
PHYSICS · Multi-part · Fermi University Physics · Mathematical Methods for Physics · Earth, Climate & Energy Physics · Seismology, tectonics and geodynamics
The Solid Earth, Ch The earthquake source: moment tensor, radiation and spectra
Problem
The radiation-pattern section showed that the far-field P amplitude of a double couple is proportional to r^⋅Mr^=M0sin2θcosϕ, with r^ the unit vector from the source to a station, θ the angle from the fault normal n^ and ϕ the azimuth about n^ measured from the slip direction d^. Finding θ and ϕ afresh for every station is awkward. This problem works with the vector form instead, on a fault that is pure dip-slip rather than the vertical strike-slip case worked in the text.
((a)) Show that r^⋅Mr^=2M0(r^⋅n^)(r^⋅d^) for the double couple Mij=M0(n^id^j+n^jd^i), and that this expression is unchanged when n^ and d^ are exchanged. Say what that exchange does to the fault plane, and hence what first motions alone can and cannot decide.
((b)) A thrust fault has strike ϕf=350∘, dip δ=12∘ and rake λr=90∘ (pure reverse slip). Find n^ and d^ in the frame x north, y east, z down.
((c)) A ray leaving the source with take-off angle ih (from the downward vertical) and azimuth Az (clockwise from north) points in the direction r^=(sinihcosAz,sinihsinAz,cosih). Two stations report (Az,ih)=(080∘,30∘) and (260∘,30∘). Using the result of part (a), say whether the first P motion at each station is a push (compression) or a pull (dilatation).