Untangling the complex origin of turbidite activity on the Calabrian Arc (Ionian Sea) over the last 60 ka
文摘

Various origins and processes for turbidites are distinguished on the Calabrian Arc.

A palaeoearthquake calendar has been defined on the last 60 ka.

Co-seismic turbidites have a return time of 240 years in the abyssal plain and 450 to 1000 years in slope basins.

A co-tsunami turbidite has been linked with the Cape-Riva Santorini caldera collapse.

Volcaniclastic turbidites are linked to Etna flank collapses.

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