Transparent layers in seismic reflection records from the central Ionian Sea (Mediterranean) - evidence for repeated catastrophic turbidite sedimentation during the Quaternary

Sedimentary Geology

Volumn 135, Issue 1-4, 2000, Pages 89-98

  Hieke, W ^a  

^a TECHNICAL UNIVERSITY OF MUNICH   (Germany)

Author keywords

Mediterranean Sea; Megaturbidite; Quaternary; Transparent seismic layer

Indexed keywords

PALEOCEANOGRAPHY; QUATERNARY; SEISMIC REFLECTION; SEISMIC SURVEY; TURBIDITE;

MEDITERRANEAN SEA;

EID: 0033781443     PISSN: 00370738     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0037-0738(00)00065-8     Document Type: Conference Paper

References (15)

1. Sedimentation rates in Neogene deep-sea sediments from the Mediterranean and geodynamic implications of their changes
2. New findings of Bronze Age homogenites in the Ionian Sea: Geodynamic implications for the Mediterranean
3. A thick Holocene homogenite from the Ionian Abyssal Plain (Eastern Mediterranean)
4. The Victor Hensen structure in the central Ionian Sea and its relation to the Medina Ridge (Eastern Mediterranean)
5. The Victor Hensen Seahill (Central Ionian Sea)-morphology and structural aspects
6. The Augias megaturbidite in the central Ionian Sea (Central Mediterranean) and its relation to the Holocene Santorini event
7. The Ionian Abyssal Plain (Mediterranean Sea)-morphology
8. Results of seismic refraction and seismic reflection measurements in the Ionian Sea
9. Site 374: Messina Abyssal Plain
10. Tsunami-induced sediment transport in the abyssal Mediterranean Sea
11. Turbidites at site 374: Their composition, provenance and paleobathymetric significance
12. Seismoturbidites: A new group of resedimented deposits
13. Acoustic facies of Holocene megaturbidities in the eastern Mediterranean