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We calculated the static displacements in an elastic half space (Okada 1992) from the total slip distribution of our second source model (Fig. 9a).
We also calculated the static displacements from our previous model with northwest-dipping F1 segment (Irikura et al. 2017, in which segment 4 corresponds the F1 segment in the present paper).
Once stress-strain curves were obtained and AE data are processed, we calculated the static elastic moduli for each specimen utilizing Equations 6 and 7 with the tangent deformation modulus at 50%% of the maximum peak stress (Ulusay and Hudson [2007]).
In a previous study, Hikima (2012) calculated the static ΔCFF using his final slip model on the Itozawa fault plane and found an area with a positive ΔCFF that included his rupture starting point when he assumed the apparent friction coefficient to be 0.8.
Toda et al. (2011) calculated the static ΔCFF on known major faults and megathrusts using the source model of the 2011 Tohoku earthquake and the MW 7.9 aftershock, and the results showed that the static ΔCFF on the fault near the Yunodake fault has a positive value of approximately 0.1 MPa when an apparent friction coefficient of 0.4 is adopted.
Similarly, we calculated the static scores of the MI-dysregulated miRNAs (Figure 2A).
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We have developed a method for calculating the static field in arbitrary 3D magnetic susceptibility distributions and performed calculations in a complete model of the human head and shoulders.
We first calculate the static then dynamic safety factors.
For each step, the plateau pressure was recorded in order to calculate the static compliance.
Then we applied our results to calculate the static properties and form factors of deuteron system.
Utilize pressure gauges to measure the static pressure and static temperature at different points; calculate the static pressure and static temperature of the middle reservoir.
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