Seismicity rate immediately before and after main shock rupture from high-frequency waveforms in Japan

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Connecting near-field and far-field earthquake triggering to dynamic strain (2010, background): “early aftershocks are usually missing from earthquake catalogs [Kagan, 2004; Peng et al., 2007].”
Rate‐Dependent Incompleteness of Earthquake Catalogs (2016, background): “…(1) estimations solely based on catalog information (see Mignan and Woessner, 2012, and references therein) and (2) methods based also on additional information, whether measurements of noise levels (Peng et al., 2007) or picking information of seismic waves (Schorlemmer and Woessner, 2008).”
Afterslip and aftershocks in the rate‐and‐state friction law (2007, background): “Is it however likely that many events triggered by the coseismic stress change occur at very short times after the main shock and are not detected [Kagan, 2004; Peng et al., 2007].”