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- W2056881026 abstract "Average S-wave coda-Q (Qc) at 6 Hz and to about 10 sec after the S-wave arrival shows: (1) temporal variation positively correlated with the magnitude distribution parameter b for foreshocks and aftershocks of the 1979 Petatlan, Mexico earthquake; (2) spatial variation through the aftershock area, positively correlated with b, high Qc -b values at the two activity centers, intermediate values in between and landward, and low values toward the Middle America Trench, which remain low for two weeks after the main shock; and (3) five-foreshock average Qc = 135±1.6% and eleven-aftershock average Qc= 175±1.3% for the eastern asperity. The b values—and possibly Qc values—seem to correlate with the level of aftershock activity." @default.
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- W2056881026 date "1985-11-01" @default.
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- W2056881026 title "Time-space variation of seismic S-wave coda attenuation (Q<sub>c</sub><sup>−1</sup>) and magnitude distribution (b-values) for the Petatlan Earthquake" @default.
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- W2056881026 doi "https://doi.org/10.1029/gl012i011p00789" @default.
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