Short-wavelength crustal heterogeneities in the Nikko area, Central Japan, revealed from the three-component seismogram envelope analysis

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Scientific paper

The short-wavelength crustal heterogeneity is investigated in the Nikko area (Central Japan), using a three-component seismogram envelope analysis applied to small local earthquakes. We stochastically model fluctuations in crustal density and seismic wave velocities by using an exponential auto-correlation function. The model parameters are correlation length a and root mean square (rms) fractional fluctuation strength ɛ. Free surface and non-spherical source radiation effects are incorporated in the synthesis of three-component seismogram envelopes. We use 149 short-period seismograms recorded by array stations from 10 local earthquakes with magnitudes 1 ~ 2 and epicentral distances less than 15 km. A best fit minimum residual between observed and synthetic envelopes in the frequency band of 8 ~ 16 Hz gives ɛ2/a ~= 8 × 10-6 m-1. With the additional information on the strength of direct wave attenuation and the excitation of coda waves at low frequencies, we estimate that a = 300 ~ 800 m and ɛ = 5 ~ 8%. This strong heterogeneity and short correlation length probably reflect the geological condition of the Nikko area which is located in the vicinity of the volcanic front.

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