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The amplification effect on the water level in Changping well, driven by the pressure fluctuation induced by the surface wave, was relatively small, but a low-to-high characteristic is apparent during the coseismic period, related to the gradual enhancement of aquifer permeability due to the action of seismic waves.
We calculated dynamic stress changes induced by the surface wave following the method of Hill et al. (1993).
Figure 14a shows the relationship between the R and τ error medians for the vertical component, which can be evaluated directly by the surface wave comparisons.
The shallow subsurface S-wave velocities of the observation sites were investigated by the surface wave method during installation of accelerometers (Takai et al. 2015).
The predominant signal visible in the T T component was outstanding among the nine components for most station pairs, which was likely caused by the surface wave excitation and propagation characteristics of the Osaka basin.
However, they were not triggered by the surface wave arrivals shown in this study and were located far from the tremors, and therefore, it is assumed that these events were not related to the tremors.
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For the vibration of container itself Flügge's exact theory is used and the radial dynamic pressure generated by the surface waves is obtained in terms of the liquid velocity potential function φ.
Non-volcanic tremors were induced by the surface waves of the 2012 Sumatra earthquake around the Hinagu fault zone in Kyushu, Japan.
Because the long-period ground motions are caused by the surface waves developed in the sedimentary basin, the study of the basin structure is necessary for gaining a better understanding of the observed phenomena.
Therefore, the rCMT requires a longer time window, but can also determine CMTs for large aftershocks, when the body wave signal (and thus the W-phase) may still be buried by the surface waves from a previous large event, such as some of the large aftershocks in the first day after the Tohoku mainshock.
The rCMT method uses data with a similar period range as the W-phase moment tensor (Hayes et al., 2009), also in use at the NEIC, but its input signal is dominated by the surface waves, which arrive later and are of higher amplitude.
More suggestions(17)
by the surface state
by the surface functionalization
by the surface friction
by the surface layer
by the surface accelerogram
by the surface team
by the surface wettability
by the surface frivolity
by the pressure wave
by the surface contact
by the surface potential
by the surface mobility
by the surface interaction
by the blast wave
by the surface area
by the surface displacement
by the surface flatness
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