HIGHLIGHTS
- who: Diego Rincon-Yanez et al. from the For the Campi Flegrei caldera, we selected data recorded in, when a relevant low-frequency hydrothermal component in the background seismic signal was evidenced by [36] and interpreted as related to fluid injections from a deeper geothermal reservoir toward system of of theOnIschia, Ischia, considered towardthe theshallower shallower hydrothermal hydrothermal system wewe considered samples earthquake, which whichoccurred occurredonon August, when samplesrecorded recordedafter after the the Mw, ., earthquake, August, when the thehydrothermal hydrothermalsource sourcewas wasparticularly particularlyactive activeand andits itspersistent persistent signature signature was was identified identiinfied background noise noise [9 . . .

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