Frontiers in Earth Science (Jul 2021)

One Year of Seismicity Recorded Through Ocean Bottom Seismometers Illuminates Active Tectonic Structures in the Ionian Sea (Central Mediterranean)

  • Tiziana Sgroi,
  • Alina Polonia,
  • Laura Beranzoli,
  • Andrea Billi,
  • Alessandro Bosman,
  • Antonio Costanza,
  • Marco Cuffaro,
  • Giuseppe D’Anna,
  • Mariagrazia De Caro,
  • Maria Di Nezza,
  • Gioacchino Fertitta,
  • Francesco Frugoni,
  • Luca Gasperini,
  • Stephen Monna,
  • Caterina Montuori,
  • Lorenzo Petracchini,
  • Patrizio Petricca,
  • Stefania Pinzi,
  • Andrea Ursino,
  • Carlo Doglioni,
  • Carlo Doglioni

DOI
https://doi.org/10.3389/feart.2021.661311
Journal volume & issue
Vol. 9

Abstract

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Seismological data recorded in the Ionian Sea by a network of seven Ocean Bottom Seismometers (OBSs) during the 2017–2018 SEISMOFAULTS experiment provides a close-up view of seismogenic structures that are potential sources of medium-high magnitude earthquakes. The high-quality signal-to-noise ratio waveforms are observed for earthquakes at different scales: teleseismic, regional, and local earthquakes as well as single station earthquakes and small crack events. In this work, we focus on two different types of recording: 1) local earthquakes and 2) Short Duration Events (SDE) associated to micro-fracturing processes. During the SEISMOFAULTS experiment, 133 local earthquakes were recorded by both OBSs and land stations (local magnitude ranging between 0.9 and 3.8), while a group of local earthquakes (76), due to their low magnitude, were recorded only by the OBS network. We relocated 133 earthquakes by integrating onshore and offshore travel times and obtaining a significant improvement in accuracy, particularly for the offshore events. Moreover, the higher signal-to-noise ratio of the OBS network revealed a significant seismicity not detected onshore, which shed new light on the location and kinematics of seismogenic structures in the Calabrian Arc accretionary prism and associated to the subduction of the Ionian lithosphere beneath the Apennines. Other signals recorded only by the OBS network include a high number of Short Duration Events (SDE). The different waveforms of SDEs at two groups of OBSs and the close correlation between the occurrence of events recorded at single stations and SDEs suggest an endogenous fluid venting from mud volcanoes and active fault traces. Results from the analysis of seismological data collected during the SEISMOFAULTS experiment confirm the necessity and potential of marine studies with OBSs, particularly in those geologically active areas of the Mediterranean Sea prone to high seismic risk.

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