Fig. 5
From: Discriminating non-seismic long-period pulses and noise to improve earthquake source inversion
![Fig. 5](http://media.springernature.com/full/springer-static/image/art%3A10.1186%2Fs40623-016-0426-0/MediaObjects/40623_2016_426_Fig5_HTML.gif)
Comparisons of source locations for a automatic and manual CMT solutions and b reprocessed automatic and manual CMT solutions. Reprocessed automatic CMT solutions were obtained using a threshold source amplitude ratio (R) of 11