Abstract
Coda waves from local earthquakes are interpreted as single isotropic scattered waves by numerous heterogeneities distributed homogeneously and randomly in the earth. A mean free path characterizes the distribution of the scatterers in the earth. Seismograms obtained at the Iwatsuki observatory during the period between April and September, 1976 are studied. The S-wave codas of 96 local earthquakes with magnitude 3.0–5.5 are analyzed, where only the S-wave to S-wave scattering is assumed. The total seismic energy of the S-waves (1–30 Hz) is estimated from the earthquake magnitude by the Gutenberg-Richter formula. The mean free path of S-waves (1–30 Hz) under the Kanto district of Japan is estimated to be 106,92±0–50cm. © 1978, The Seismological Society of Japan, The Volcanological Society of Japan, The Geodetic Society of Japan. All rights reserved.
Cite
CITATION STYLE
Sato, H. (1978). Mean free path of S-waves under the Kanto district of Japan. Journal of Physics of the Earth, 26(2), 185–198. https://doi.org/10.4294/jpe1952.26.185
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.