Exact(1)
In general, environmental parameters can be estimated using inversion methods [23, 24].
Similar(59)
The slip vector on the plate interface was estimated using the inversion technique of Yabuki and Matsu'ura (1992), with some modifications (Naito and Yoshikawa 1999; Yamamoto 2005), based on the point source formulation of Okada (1992).
The rake angle of the reference focal mechanism was assumed to be parallel to the resolved shear stress direction on the best-fit plane under the stress field reported by Yukutake et al. (2007), in which the stress field around the mainshock fault was estimated using a stress inversion method and focal mechanism data of the aftershocks.
The depth of the upper boundary of the aseismic slab in the inland areas was estimated using the receiver function inversion results.
The rupture area of the earthquake was estimated using the trimming criterion of Somerville et al. (1999) with the slip model from the waveform inversion.
Sequence diversity was estimated using three criteria calculated as: (1) [(number of substitutions*2)+(number of indels)+(number of inversions)]/amplicon length, (2) number of substitutions+indels+inversions, and (3) sequence diversity (number of substitutions/sequence length).
1/S' was estimated using BlastPhen.
Statistical power was estimated using 1000 simulations.
Protein concentration was estimated using the Micro BCA Protein Assay Kit Thermoo).
Confidence intervals were estimated using normal approximation.
RNA concentration was estimated using nanodrop spectrophotometer.
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