“…Later, the SeisComP Hypo71 (Lee and Lahr, 1975) was used to relocate our events, weighting the arrivals using the assigned time uncertainties. The velocity/depth structure beneath the eastern Pyrenees was investigated by Antonio-Vigil et al, 2019 andDiaz et al, 2018 using wideangle refraction and reflection profiles constructed using natural seismicity as source. Although poorly constrained, the obtained models, including sediments and distinct upper, middle and lower crust, are consistent with controlled source profiles acquired in the late 1970s (Gallart et al, 1981) and with estimated of the crustal depth derived from RFs studies (Diaz et al, 2018).…”