Elastic relaxation model for seismic wave attenuation in the earth

Details Elastic relaxation model for seismic wave attenuation in the earth Elastic relaxation model for seismic wave attenuation in the earth

Apr 1969

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1969pepi....2...30j&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 2, Issue 1, p. 30-34.

Physics

6

Scientific paper

Love wave amplitude data are satisfied by an Earth model in which the intrinsic internal friction (Q-1) at each depth is taken to be due to a single thermally activated relaxation mechanism. In this model the intrinsic Q-1 is completely specified by a simple function of frequency, temperature, and pressure. This model is in better agreement with observed behavior of solids than previous models and requires fewer arbitrary parameters to satisfy seismic data.

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