Holocene and Quaternary uplift in the central part of the southern coast of the Corinth Gulf (Greece)

2004/11/01 by P.A. Pirazzoli, Paolo A. Pirazzoli, Stathis C. Stiros +5 · 7 citations
Arts and Humanities · Earth and Planetary Sciences · #Maritime and Coastal Archaeology #Archaeology and ancient environmental studies #Marine and environmental studies

paper · doi:10.1016/j.margeo.2004.09.006

Citations

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

Cited by

• Tectono-climatic controls of the early rift alluvial succession: Plio-Pleistocene Corinth Rift (Greece)
• Stratigraphic architecture of the Plio-Pleistocene infill of the Corinth Rift: Implications for its structural evolution
• 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)
• 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)
• High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift. [europepmc]