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A few low-angle normal fault earthquakes at approximately the depth of the plate interface, with a strike nearly parallel to the trench axis, were detected immediately after the 2011 Tohoku-oki earthquake. After that, however, no such normal fault events have been observed until the occurrence of the 2014 MW 6.6 Fukushima-oki earthquake. Here we analyze the teleseismic body waveforms of the 2014...
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