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1000 Titel
  • One Year of Seismicity Recorded Through Ocean Bottom Seismometers Illuminates Active Tectonic Structures in the Ionian Sea (Central Mediterranean)
1000 Autor/in
  1. Sgroi, Tiziana |
  2. Polonia, Alina |
  3. Beranzoli, Laura |
  4. Billi, Andrea |
  5. Bosman, Alessandro |
  6. Costanza, Antonio |
  7. Cuffaro, Marco |
  8. D’Anna, Giuseppe |
  9. De Caro, Mariagrazia |
  10. Di Nezza, Maria |
  11. Fertitta, Gioacchino |
  12. Frugoni, Francesco |
  13. Gasperini, Luca |
  14. Monna, Stephen |
  15. Montuori, Caterina |
  16. Petracchini, Lorenzo |
  17. Petricca, Patrizio |
  18. Pinzi, Stefania |
  19. Ursino, Andrea |
  20. Doglioni, Carlo |
1000 Verlag
  • Frontiers Media S.A.
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-07-29
1000 Erschienen in
1000 Quellenangabe
  • 9:661311
1000 Copyrightjahr
  • 2021
1000 Embargo
  • 2022-01-31
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.3389/feart.2021.661311 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Abstract/Summary
  • <jats:p>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.</jats:p>
1000 Sacherschließung
lokal active faults
lokal marine network
lokal short duration events (SDE)
lokal Calabrian Arc
lokal SEISMOFAULTS
lokal local earthquakes
lokal Earth Science
lokal Ionian Sea (Italy)
lokal ocean bottom seismometer (OBS)
1000 Liste der Beteiligten
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1000 Erstellt am 2024-05-21T14:38:24.390+0200
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