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Fig. 7 | Earth, Planets and Space

Fig. 7

From: Real-time crustal monitoring system of Japanese Islands based on spatio-temporal seismic velocity variation

Fig. 7

Spatio-temporal velocity maps determined by using ae the ARM and fj the SRM. The ARM and SRM have different temporal resolutions because the current trace was made with stacking periods of 17 and 11 days, respectively. Both methods identified spatio-temporal velocity changes caused by the Kumamoto earthquake. But, the velocity changes derived from both methods are largely different

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