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E. De Lauro, S. De Martino, M. Falanga and S. Petrosino Synchronization between tides and sustained oscillations of the hydrothermal system of Campi Flegrei (Italy) Geochemistry, Geophysics, Geosystems 14

Version of Record online: 2 AUG 2013 | DOI: 10.1002/ggge.20149

Key Points

  • Background seismic noise is a sustained polarized oscillations
  • Persistent oscillations are induced by the upper hydrothermal system
  • Lunar tidal modulation as marker of increased amount of fluids

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