Uplift and slip rates of the eastern Eliki fault segment, Gulf of Corinth, Greece, inferred from Holocene and Pleistocene terraces
Author:
Publisher
Geological Society of London
Subject
Geology
Reference68 articles.
1. The generation and degradation of marine terraces
2. Quaternary evolution of the Corinth Rift and its implications for the Late Cenozoic evolution of the Aegean
3. Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge
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1. Increasing fault slip rates within the Corinth Rift, Greece: A rapidly localising active rift fault network;Earth and Planetary Science Letters;2024-06
2. Uplifted Pleistocene Marine Terraces at Active Margins: Modeling Reveals the Effects of Sea Reoccupation and Coseismic Uplift on Uplift Rate Calculation;Geochemistry, Geophysics, Geosystems;2024-03-30
3. Clustering of earthquakes along the Pidima-Anthia normal fault: New data from palaeoseismology and tectonic geomorphology and their significance on the earthquake's regularity and recurrence across southern Greece;Journal of Structural Geology;2023-11
4. Late Quaternary Relative Sea-Level Changes and Vertical GNSS Motions in the Gulf of Corinth: The Asymmetric Localization of Deformation Inside an Active Half-Graben;Geosciences;2023-10-28
5. Long-term glacial and fluvial system coupling in southern Greece and evidence for glaciation during Marine Isotope Stage 16;Quaternary Science Reviews;2023-10
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