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For the megathrust fault model, a rupture along a 440-km × 120-km fault is calculated to have almost 3.5 m of slip and will generate a Mw8.5 earthquake.
The amount of shift necessary to correct the fault is calculated from β ( i ) = 1 2 N t ∑ t B ( i, t ) - B ( i - k 1, t ) + ∑ t B ( i, t ) - B ( i + k 2, t ), (9).
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The pore pressure ratio for each earthquake fault was calculated under the assumption that reduced frictional strength was caused by pore fluid pressure.
The static displacements and strains due to the slip on the fault are calculated using the source code developed by Okada (1992) for a half-space medium.
The static displacements and strains due to slip on fault was calculated using the source code developed by Okada (1992), assuming a half-space medium with a Poisson ratio equal to 0.25.
Given the values for the dynamic frictional coefficient (μd), a pore fluid factor (λv), and a constant c, the stress drop Δσ ξ, η; c, μd, λ V ) at on the fault was calculated as follows: Δσ ξ, η ; c, μ d, λ V = c τ s ξ, η - μ d c σ n ξ, η + 1 - λ V σ V ξ, η (7).
Using the residual generation technique, residual vibrations are generated from experimental results for the rotor bearing system subject to misalignment and unbalance, and then the residual forces due to presence of faults are calculated.
The activity rate of the main secondary oil source faults was calculated using the fault activity rate method (Table 3).
The R values between TEE and the median of the N222 values for the seven faults were calculated for each time period.
Based on our assumption that the lower limit of the fault occurs at 10-km depth, the fault width is calculated to be 19 km.
The fault distance is calculated assuming a 10 km × 10 km rectangular fault having a strike angle of 211° and a dip angle of 87°.
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