RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES2001, doi:10.2205/2018ES000649, 2019
Figure 6. Examples of the signal duration block performance for different detected seismic events: a) high-amplitude noisy microquakes; b) local microearthquakes, c) regional earthquakes. Automated estimates of the duration for each detected seismic event are shown to the right of the event records.
Citation: Krylov A. A., L. I. Lobkovsky, A. I. Ivashchenko (2019), Automated detection of microearthquakes in continuous noisy records produced by local ocean bottom seismographs or coastal networks, Russ. J. Earth Sci., 19, ES2001, doi:10.2205/2018ES000649.
Copyright 2019 by the Geophysical Center RAS.
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