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It is also desirable to recover information on missing aftershocks using modeling of detection rates, particularly in the early stage of aftershocks (Omi et al. 2013, 2014a, b).
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From the plot of magnitude versus transformed time in Fig. 4d, there are a substantial number of missing aftershocks of M ≥ 4.2 immediately after the M7.3 event.
It is difficult to omit such normal-fault aftershocks and identify interplate aftershocks using only the Kagan's angle and depth information.
Since the aftershock period continues to the present, we decided to calculate the b-value of aftershocks using the data from the mainshock until April 2017 (Fig. 4).
Thus, no missing values were used.
Many efforts have been made to fix the problem of missing small aftershocks in the early stage of an earthquake sequence.
Four days after the mainshock, we started an aftershock observation using pop-up type OBSs in order to obtain the detailed aftershock activity of the 2011 Tohoku Earthquake.
We carried out aftershock observations using pop-up-type OBSs in order to obtain a detailed aftershock distribution of the 2011 Tohoku earthquake.
Missing values were estimated using mLOCF.
The missing residues were modeled using MODELLER [65].
The spatial extent of aftershocks is used to estimate the source fault location.
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