2011
DOI: 10.5047/eps.2011.07.018
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Fault extent of the largest aftershock of the 1968 Tokachi-Oki, Japan, earthquake and an interpretation of the normal faulting focal mechanism

Abstract: The focal mechanism of the 1968 Tokachi-Oki earthquake (M J = 7.9) was thrust faulting but that of the largest aftershock (M J = 7.5) was normal faulting. The tectonic implication of the reversal of the focal mechanisms of the two events has not been clarified yet. In order to investigate this, we ought to take into account the relative location of the two fault planes. In the present study, the length and the direction of rupture propagation for the largest aftershock is derived from the azimuth dependence of… Show more

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Cited by 2 publications
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“…The system is simulated with parameters m = 1, c = 1, α = 0.7, k c = 4π 2 , x y = 0.025, γ = 0.5, β = 0.5, n = 2, and A = 6 under the Hachinohe earthquake time history [64] with a sampling rate of 500 Hz. Then, noise is added to the synthetic data with SNR = 30, and only the noisy acceleration is used as input during the estimation process.…”
Section: Competing Interestsmentioning
confidence: 99%
“…The system is simulated with parameters m = 1, c = 1, α = 0.7, k c = 4π 2 , x y = 0.025, γ = 0.5, β = 0.5, n = 2, and A = 6 under the Hachinohe earthquake time history [64] with a sampling rate of 500 Hz. Then, noise is added to the synthetic data with SNR = 30, and only the noisy acceleration is used as input during the estimation process.…”
Section: Competing Interestsmentioning
confidence: 99%