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NTIS 바로가기Pure and applied geophysics, v.167 no.11, 2010년, pp.1343 - 1363
Gusev, Alexander A.
AbstractA wavetrain of high-frequency (HF) P waves from a large earthquake, when recorded at a distant station, looks like a segment of modulated noise, with its duration close to the duration of rupture. These wavetrains, with their bursts and fadings, look much more intermittent than a segment of ...
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