“…The waveform data acquired by the CRL and collaborating networks in the western Corinth Rift have provided working material for several recent earthquake studies. This includes seismotectonics, relocation, multiplet, spatio-temporal analyses Lambotte et al, 2014;Godano et al, 2014;Kapetanidis et al, 2015;Bourouis & Cornet, 2009) but also earthquake tomography (Gautier et al, 2008;Karakonstantis & Papadimitriou, 2016), measurements of relative velocity changes (Cociani et al, 2010) and others. In the present study the The seismicity is mainly distributed at focal depths between 5 and 12 km, with the majority of events being concentrated in a thin seismic layer between 7.0 and 8.5 km.…”