Untangling the complex origin of turbidite activity on the Calabrian Arc (Ionian Sea) over the last 60 ka
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- 作者：Elé ; onore Kö ; nga ; eleonore.kong@u-bordeaux.fr" class="auth_mail" title="E-mail the corresponding author ; Sé ; bastien Zaragosia ; Jean-Luc Schneidera ; Thierry Garlanb ; Patrick Bachè ; leryc ; Laurine San Pedrod ; Chloé ; Seiberta ; Calypso Racinea
- 关键词：Ionian Sea ; Accretionary prism ; Palaeoearthquakes ; Palaeotsunamis ; Co-seismic turbidites ; Volcaniclastic turbidites ; Natural hazard
- 刊名：Marine Geology
- 出版年：2016
- 出版时间：1 March 2016
- 年：2016
- 卷：373
- 期：Complete
- 页码：11-25
- 全文大小：3843 K
文摘
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Various origins and processes for turbidites are distinguished on the Calabrian Arc.
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A palaeoearthquake calendar has been defined on the last 60 ka.
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Co-seismic turbidites have a return time of 240 years in the abyssal plain and 450 to 1000 years in slope basins.
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A co-tsunami turbidite has been linked with the Cape-Riva Santorini caldera collapse.
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Volcaniclastic turbidites are linked to Etna flank collapses.