A recent study investigated turbidites that preserved in a 457-m deep ICDP drilling from the Dead Sea depocenter. This is the first work to show detailed information on turbidites in the region.
1. Key Points:
- Seismic origin for prehistoric turbidites is established by analyzing the underlying in situ deformation structures for each turbidite
- Data validate a previous hypothesis that soft-sediment deformation formed at the sediment-water interface in the Dead Sea
- The new approach permits a more confident geohazard assessment by improving the completeness of a paleoseismic archive