Spherically symmetric attenuation within the Earth from natural mode data.

Physics

Scientific paper

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Earth Interior: Structure

Scientific paper

Observations of the attenuation of free oscillations after large
earthquakes are used to determine the spherically symmetric dissipative
structure within the Earth. The authors model intrinsic attenuation of
seismic energy between 0.3 and 10 mHz with a frequency-independent Q
model.

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