Fig. 8
From: Discriminating non-seismic long-period pulses and noise to improve earthquake source inversion
![Fig. 8](http://media.springernature.com/full/springer-static/image/art%3A10.1186%2Fs40623-016-0426-0/MediaObjects/40623_2016_426_Fig8_HTML.gif)
Locations of a F-net stations and b earthquakes used in our analysis of source amplitudes. Focal mechanisms are CMT solutions in the F-net catalog (http://www.fnet.bosai.go.jp/event/joho.php?LANG=en). Star in (a) is the source location used in our synthetic tests