It is important to discuss whether the asperity estimated from waveform inversion using long-period strong motion is the same as those using the tsunami, and to discuss the relationship between large slip area (asperities) expected to excite tsunami, and strong-motion generating areas (SMGAs).
The strong motion-generating area derived by EGF modeling (Kurahashi and Irikura, 2011) agrees well with the peak moment-rate distribution, rather than the slip distribution.
Here, we assume that each of the wave packets S1 S4 are generated from individual strong motion generation areas, SMGA1 SMGA4.
THE Fidelity contract attached to the complaint also hints at the money each motion generates.
The motion generated by a UP chain has three DOF.
The smoothed camera motion generates a correction motion for each frame.
In addition, a scenario ground motion generated by the Izmir Fault with a magnitude of 6.5, having an average distance of 10 km to the study area, is also considered.
Their approach tries to detect and distinguish between the 'static motion' generated by the motion of the camera, usually known as ego-motion, and the 'dynamic objects motion'.
The plate spin motion generates a shear motion at the plate boundary and is associated with toroidal motion, whereas straight plate motion results in poloidal motion at both subduction zones and ridges, and toroidal motion along transform faults.
This increased molecular motion generates frictional heat and consequently increases tissue temperature.
It is costly, time consuming, has blood flow and motion generated artifacts, and has limited availability.
