積分波形です。
５月２５日
静岡県西部で発生した中規模地震
最大震度３
気象庁による震源要素
009 5 25 20:26 22.1 34゜43.3'N 137゜48.0'E 26 4.7 静岡県西部
犬山での観測記録
典型的な波形を示しています。
静岡県西部で発生した中規模地震
最大震度３
気象庁による震源要素
009 5 25 20:26 22.1 34゜43.3'N 137゜48.0'E 26 4.7 静岡県西部
犬山での観測記録
典型的な波形を示しています。
PALU, Palau station seismic record
originated from experiment source
Applied band-pass filter with 0.02-0.05 Hz
In vertical component, surface wave is detected.
In horizontal components, the signal was covered by large
seismic noise.
originated from experiment source
Applied band-pass filter with 0.02-0.05 Hz
In vertical component, surface wave is detected.
In horizontal components, the signal was covered by large
seismic noise.
MDJ/ IC network VBB seismic data:
reteived by BUD, IRIS
N.Korea Nuclear experiment's signal
1: P and refraction P phase
2: S wave also observed
3: surface wave with dominant period of 5 sec
reteived by BUD, IRIS
N.Korea Nuclear experiment's signal
1: P and refraction P phase
2: S wave also observed
3: surface wave with dominant period of 5 sec
