Open AccessFrequency‐Dependent Attenuation of P and S Waves In the Kanto Area, Japan, Based On the Coda‐Normalization Method
Author(s) -
Yoshimoto Kazuo,
Sato Haruo,
Ohtake Masakazu
Publication year - 1993
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1993.tb01476.x
Subject(s) - coda , seismogram , attenuation , amplitude , seismology , geology , frequency dependence , lithosphere , s wave , seismic wave , normalization (sociology) , scattering , microseism , geodesy , physics , optics , tectonics , nuclear magnetic resonance , sociology , anthropology
Summary We propose a new method for the simultaneous measurement of P ‐ and S ‐wave attentuation by extending the conventional coda‐normalization method which had been limited to the estimation of S ‐wave attenuation. Using this method, we measured frequency‐dependent attenuation of both P and S waves in the lithosphere beneath the Kanto area, Japan, from seismograms of 174 local earthquakes for the frequency range 1.5 ≤ f ≤ 24 Hz. the values of Q s −1 and Q p −1 corresponding to peak amplitude decays show strong frequency dependence, and are expressed by using power laws Q S −1 =0.012 f −0.73 and Q P −1 = 0.031 f −0.95 , respectively. the ratio Q P −1 /Q S −1 is found to be larger than unity for the whole frequency range. the apparent attenuations of P and S waves with travel distance are almost the same for frequencies higher than 1Hz. Our results differ from the characteristics of low‐frequency wave attenuation reported by other studies for frequencies lower than 1 Hz. This frequency dependence and the ratio may suggest that scattering loss due to random heterogeneities in the earth medium plays an important role in seismic‐wave attenuation in the lithosphere.