EGU2020-19205
https://doi.org/10.5194/egusphere-egu2020-19205
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Seismicity cluster below the Moho indicates thrust faulting in the central Ligurian Basin

Martin Thorwart1, Anke Dannowski2, Heidrun Kopp2, Dietrich Lange2, Wayne Crawford3, Anne Paul4, and Felix Noah Wolf2
Martin Thorwart et al.
  • 1University of Kiel, Institute of Geosciences, Kiel, Germany (martin.thorwart@ifg.uni-kiel.de)
  • 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany
  • 3Institut de Physique du Globe de Paris, France
  • 4Institut des Sciences de la Terre (ISTerre) CNRS & Université Grenoble Alpes, France

The Alpine orogen and the Apennines system are part of the complex tectonic settings in the Mediterranean Sea caused by the convergence between Africa and Eurasia. Between 30 Ma and 15 Ma, the Calabrian Subduction retreated in southeast direction pulling Corsica and Sardinia away from the Eurasian continent. In this extensional setting, the Ligurian Sea was formed as a back-arc basin. The rifting jumped 15 MA ago to the Tyrrhenian Sea leaving Corsica and Sardinia in a stable position relative to Eurasia as observed by GPS measurements.

Within the framework of the AlpArray research initiative and its German component “4D Mountain building” (SPP2017 4D-MB) a long-term experiment was conducted in the Ligurian sea to investigate the lithosphere structure and the seismicity in the Ligurian basin. The passive seismic network was operated by France and Germany and consisted of 29 broad-band ocean bottom stations. It was in operation between June 2017 and February 2018. At the end of the experiment two active seismic profiles were conducted additionally.

A cluster of 15 events with magnitudes lower than 2.5 occurred in the centre of the Ligurian Basin. The earthquakes are located at a depth of 20 km to 35 km, i.e. 10 - 25 km below the Moho. The cluster was not continuously active but had several active periods which lasted between 2 and 5 days.

A fault plane solution could be determined of the larger events in the cluster. The mechanism is a thrust faulting. Smaller events should have a similar mechanism due to the highly coherent waveforms. A similar mechanism was observed for the Mw=4.9 earthquake on 07.07.2011 which occurred 50 km east of the cluster. Both solutions show a SW-NE striking, northwest dipping fault plane. This indicates a convergence in NW-SE direction between Corsica and Eurasia.

How to cite: Thorwart, M., Dannowski, A., Kopp, H., Lange, D., Crawford, W., Paul, A., and Wolf, F. N.: Seismicity cluster below the Moho indicates thrust faulting in the central Ligurian Basin, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19205, https://doi.org/10.5194/egusphere-egu2020-19205, 2020

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