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A two‐layer attenuation model for the upper mantle at short periods
Author(s) -
Sharrock D. S.,
Main I. G.,
Douglas A.
Publication year - 1995
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/95gl02658
Subject(s) - attenuation , geology , extrapolation , seismology , mantle (geology) , anelastic attenuation factor , geodesy , seismic wave , geophysics , optics , physics , mathematics , mathematical analysis
Estimates of maximum mean P ‐wave attenuation (described by the quality factor Q α ) are used to make a two‐layer model of Q α in the period range 0.125–1 s for the northwest Pacific subducting region. A shallow highly attenuating layer ( Q α ≈ 150) of only 85 km thickness overlays a less attenuating layer to a depth of 450 km ( Q α > 1000). The added bandwidth made available by the use of array data yields key information for testing the validity of textbook models predominantly based on extrapolation from longer period data. We find that seismic attenuation at short periods appears to behave differently to long‐period attenuation. This reversal is represented by a modification to the absorption band model obtained from longer period data.