The terraces of Corinth (Gerrce) — A detailed record of eustatic sea-level variations during the last 500,000 years

1987/07/01 by Bertrand Keraudren, Bertrand Kéraudren, Denis Sorel · 14 citations
Arts and Humanities · Earth and Planetary Sciences · #Maritime and Coastal Archaeology #Geology and Paleoclimatology Research #Marine and environmental studies

paper · doi:10.1016/0025-3227(87)90085-5

Cited by

• Holocene and Quaternary uplift in the central part of the southern coast of the Corinth Gulf (Greece)
• Stratigraphic architecture of the Plio-Pleistocene infill of the Corinth Rift: Implications for its structural evolution
• Late Quaternary basin evolution of the Gulf of Corinth: Sequence stratigraphy, sedimentation, fault–slip and subsidence rates
• Along strike changes in the structural evolution over a brittle detachment fault: Example of the Pleistocene Corinth–Patras rift (Greece)
• Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean
• Sedimentation and tectonic geomorphology adjacent to major active and inactive normal faults, southern Greece
• Patterns of Quaternary uplift of the Corinth rift southern border (N Peloponnese, Greece) revealed by fluvial landscape morphometry
• Geomorphic and biological indicators of paleoseismicity and Holocene uplift rate at a coastal normal fault footwall (western Corinth Gulf, Greece)
• Drainage evolution in a rifted basin, Corinth graben, Greece
• Uplift and slip rates of the eastern Eliki fault segment, Gulf of Corinth, Greece, inferred from Holocene and Pleistocene terraces
• Eustatic and tectonic controls upon Quaternary coastal sedimentation in the Corinth Basin, Greece
• Age and environmental evolution of the syn-rift fill of the southern coast of the gulf of Corinth (Akrata-Derveni region, Greece)
• Rift migration and lateral propagation: evolution of normal faults and sediment-routing systems of the western Corinth rift (Greece)
• Lateral propagation of the surface trace of the South Alkyonides normal fault segment, central Greece: its impact on models of fault growth and displacement–length relationships