1980
DOI: 10.2307/529518
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Late Quaternary History of the Coastal Zone near Franchthi Cave, Southern Argolid, Greece

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“…Almost everywhere the seismic profiler achieved penetration to bedrock or to a strong, smooth reflector representing the late Quaternary emerged coastal plain Lianos, 1983, 1984). Seaward, this strong alluvial reflector terminates against thinbedded marine slope deposits marking the late glacial shore at about -120 m. The Holocene transgressive sediments above the alluvial and bedrock surfaces are generally less than 2 m thick except in Koiladha Bay where they reach 5 m ( van Andel et al, 1980).…”
Section: Reconstruction Of Past Shore Environmentsmentioning
confidence: 99%
“…Almost everywhere the seismic profiler achieved penetration to bedrock or to a strong, smooth reflector representing the late Quaternary emerged coastal plain Lianos, 1983, 1984). Seaward, this strong alluvial reflector terminates against thinbedded marine slope deposits marking the late glacial shore at about -120 m. The Holocene transgressive sediments above the alluvial and bedrock surfaces are generally less than 2 m thick except in Koiladha Bay where they reach 5 m ( van Andel et al, 1980).…”
Section: Reconstruction Of Past Shore Environmentsmentioning
confidence: 99%