Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3040
AuthorsPalyvos, N.* 
Sorel, D.* 
Lemeille, F.* 
Mancini, M.* 
Pantosti, D.* 
Julia, R.* 
Triantaphylou, M.* 
De Martini, P. M.* 
TitleReview and new data on uplift rates at the W termination of the Corinth Rift and the NE Rion Graben area (Achaia, NW Peloponnesos)
Issue DateMay-2007
Series/Report no./ 40 (2007)
URIhttp://hdl.handle.net/2122/3040
KeywordsTectonic geomorphology
Differential coastal uplift
deformation rates
active normal faults
Corinth Gulf
Greece
Subject Classification04. Solid Earth::04.04. Geology::04.04.03. Geomorphology 
AbstractWe review and present new geochronological data on the uplifted Middle-Late Pleistocene marine deposits at the western termination of the Corinth Rift and the Rion area. Geomorphological and geological observations define the general morphotectonic context of these deposits, which predicts a pattern of differential uplift. Uplift rate estimates based on previous geochronological data (ranging from 0.4 to 6 mm/yr) are discussed in the proposed morphotectonic context of differential uplift, together with estimates from new geochronological data. Based on the data available for post-MIS11 marine deposits, we conclude that time-averaged uplift rates in the last 300-200 ka have been higher than ca. 1.8 mm/yr at the areas of faster uplift (e.g. Profitis Elias, Ano Kastritsi). To define just how higher than 1.8 mm/yr they have been, and to cross-check the validity of very high uplift rate estimates (≥ 4 mm/yr) existing in the bibliography, more datings than those available are required.
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