Published January 1, 2015
| Version v1
Journal article
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Are repetitive slumpings during sapropel S1 related to paleo-earthquakes?
Creators
- 1. CNR, ISMAR, Inst Marine Sci, I-40126 Bologna, Italy
- 2. Istanbul Tech Univ, Dept Geol Engn, TR-80626 Istanbul, Turkey
- 3. Univ Bologna, Dipartimento Sci Biol Geol & Ambientali, I-40126 Bologna, Italy
- 4. Univ Parma, Dipartimento Fis & Sci Terra Macedonio Melloni, I-43100 Parma, Italy
Description
The recurrence of mass-flow units within sapropel S1, an organic carbon-rich lower Holocene marker bed in the Eastern Mediterranean Sea, was used to study the interplay between earthquakes and sedimentation along the seismically active Calabrian Arc (Ionian Sea).
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