RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES2001, doi:10.2205/2018ES000649, 2019
Figure 3. Examples of the STA/LTA algorithm performance with different parameter values for different seismic events: a) local microearthquake and a series of noisy microquakes; b) regional earthquake with clearly seen P and S phases; c) noisy signals produced by engineering works. Three plots for each example show: upper – raw record; middle – events are detected by the algorithm; lower – events are missed by the algorithm.
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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