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First, in long periods, ground motions normal to the fault line have greater spectrum values as compared with parallel motion to the fault line.
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That grace period ground to a close when negotiations stalled with both the Palestinians and the Syrians this year.
This study reports the seismic performance of a seismically-isolated nuclear reactor containment building (NRCB) under strong short-period ground motions (SPGMs) and long-period ground motions (LPGMs).
It has been reported that long-period ground motions were induced in Tokyo, Nagoya and Osaka.
It was reported that long-period ground motions were induced extensively in Tokyo, Nagoya and Osaka.
These subfaults with long-duration moment release are expected to cause weak short-period ground motions.
During this time period, ground motion on the seabed was dominated by source effects.
People in Taipei experienced strong long-period ground shaking for more than 40 s.
However, our target is the simulation of long-period ground motion.
These long-duration subfaults are expected to cause weak short-period ground motions.
Figure 10 Snapshot of the propagation of simulated long-period ground motions (period of 4 to 8 s).
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