REVIEW AND NEW DATA ON UPLIFT RATES AT THE W TERMINATION OF THE CORINTH RIFT AND THE NE RION GRABEN AREA (ACHAIA, NW PELOPONNESOS)

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Publiée : Ιουν 8, 2007
DOI : https://doi.org/10.12681/bgsg.16631
N. Palyvos
Istituto Nazionale di Geofìsica e Vulcanologia, Sez. Sismologia e Tettonofìsica, Active Tectonics Group; Harokopio University, Geography Department
D. Sorel
Université Paris-Sud, Centre d'Orsay, Faculty of Geology
F. Lemeille
Institut de Radioprotection et de Surete Nucléaire, Seismic Hazard Division, Fontenay-aux-roses Cedex
M. Mancini
CNR -Istituto di Geologia Ambientale e Geo ingegneria
D. Pantosti
Istituto Nazionale di Geofìsica e Vulcanologia, Sez. Sismologia e Tettonofìsica, Active Tectonics Group
R. Julia
Institute of Earth Sciences Jaume Aimera
M. Triantaphyllou
National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Hist. Geology - Paleontology
P. M. De Martini
Istituto Nazionale di Geofìsica e Vulcanologia, Sez. Sismologia e Tettonofìsica, Active Tectonics Group
Résumé

We 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-MISl 1 marine deposits, we conclude that time-averaged uplift rates in the last 300-200 lea have been higher than ca. 1.8 mm/yr at the areas of faster uplift (e.g. Profus 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.

Article Details
  • Rubrique
  • Tectonic- Dynamic- Applied Geology
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Références
Bischoff, J.L., Fitzpatrick, J.Α., 1991. U-series dating of impure carbonates: an isochron technique using total-sample dissolution, Geochimica et Cosmochimica Acta, 55, 543-554.
Chappell, J., and Shackleton, N.J., 1986. Oxygen isotopes and sea-level, Nature, 324, 137-140.
Doutsos, T., Kontopoulos, N., and Ferentinos, G., 1985. Das westliche ende des Korinth-Grabens, Ν. Jb. Geol. Palaont. Mh., Hl 1, 652-666.
Doutsos, T., Kontopoulos, N, and Poulimenos, G., 1988, The Corinth-Patras Rift as the initial stage of Continental fragmentation behind an active island arc (Greece), Basin Research, 1, 177-190.
Doutsos, T., and Poulimenos, G., 1992. Geometry and kinematics of active faults and their seismotectonic significance in the western Corinth-Patras rift (Greece), Journal of Structural Geology, 14 (6), 689-699.
Flotté, Ν. 2003. Caracterisation structurale et cinématique d'un rift sur détachement: Le rift de Corinthe-Patras, Grece, These doct., 196pp., Univ. de Paris-Sud.
Flotte, N., Sorel, D., Müller, C, and Tensi, J., 2005. Along strike changes in the structural evolution over a brittle detachment faultç example of the Pleistocene Corinth-Patras Rift (Greece), Tectonophysics, 403, 77-94.
Frydas, D., 1991. Palaookologische und stratigraphische untersuchugen der diatomeen des pleistozans der N. Peloponnes, Griechenland, Bull. Geol. Soc. Greece, XXV/2, 499-513.
Frydas, D., Kontopoulos, N., Stamatopoulos, L., Guernet, C, and Voltaggio, M., 1995. Middle-Late Pleistocene sediments in the northwestern Peloponnesus, Greece. A combined study of biostratigraphical, radiochronological and sedimentological results, Berliner Gowiss, E16, 589-605.
Hillaire-Marcel,C, Gariepy, C, Ghaleb, B., Goy, J.-L., Zazo, C, and Barcelos, J.C., 1996. USeries measurements in Thyrrhenian deposits from Mallorca - further evidence for two last-interglacial high sea levels in the Balearic Islands, Quaternary Science Reviews, 15, 53-62.
Houghton, S.L., Roberts, G.P., Papanikolaou, I.D., and McArthur, J.M., 2003. New 234U-230Th coral dates from the western Gulf of Corinth: implications for extensional tectonics, Geophysical Research Letters, 30(19), 2013. doi: 10.1029/2003GL018112
Jedoui, Y., Reyss, J.-L., Kallel, N., Montacer, M., and Davaud, E., 2003, U-series evidence for two high Last Interglacial sea levels in southeastern Tunisia, Quat. Sci. Rev., 22, 343-351.
Keraudren, B., and Sorel, D., 1987. The terraces of Corinth (Greece) - A detailed record of eustatic sea-level variations during the last 500,000 years, Marine Geology, 11, 99-107.
Kontopoulos, N., and Zelilidis, Α., 1992. Upper Pliocene lacustrine environments in the intramontane Rio graben basin, NW Peloponnesus, Greece, N. Jb. Geol. Palaont. Mh., H2, 102-114.
Kontopoulos, N., and Zelilidis, Α., 1997. Depositional environments of the coarse-grained lower Pleistocene deposits in the Rio-Antirio basin, Greece. In G. Marinos, et al. (eds), Engineering Geology and the Environment, A. A. Balkema, Rotterdam, 199-204.
Koukouvelas, I., and Doutsos, T., 1997. The effects of active faults on the generation of landslides in NW Péloponnèse. In G. Marinos, et al. (eds), Engineering Geology and the Environment, A. A. Balkema, Rotterdam, 799-804.
Ku, T.-L., 2000. Uranium series methods, In Noller et al. (eds), Quaternary Geochronology -methods and applications, AGU reference shelf 4, 101-114.
Lajoie, K.R., Ponti, D.J., Powell, C.L., Mathieson, S.A., and Sarna-Wojcicki, A.M., 1991. Emergent marine Strandlines and associated sediments, coastal California: a record of Quaternary sea-level fluctuations, vertical tectonic movements, climatic changes and coastal processes, In R.B. Morrison (ed.), Quaternary Non-Glacial Geology: Conterminous United States: Geological Society of America Decade of North America Geology, K-2, 190-214pp.
McLaren, S.J., and Rowe, P.J., 1996. The reliability of Uranium-series mollusc dates from the western Mediterranean basin, Quaternary Science Reviews, 15, 709-717.
Palyvos, N., Pantosti, D., Stamatopoulos, L., and De Martini, P.M., 2007a. A geomorphological reconnaissance of the Psathopyrgos and Rion-Patras fault systems (Achaia, NW Peloponnesus), Bull. Geol. Soc. Gr., XXXVII. (submitted)
Palyvos, N., Lemeille, F., Sorel, D., Pantosti, D., Pavlopoulos, K., and Philippon, J., 2006. Undocumented uplifted Holocene shorelines at the western termination of the Corinth Gulf Rift: a record of coseismic uplift episodes? Geophysical Research Abstracts, vol. 8, 04754.
Palyvos, N., Pantosti, D., DeMartini, P. M., Lemeille, F., Sorel, D., and Pavlopoulos, K, 2005. The Aigion-Neos Erineos normal fault system (Western Corinth Gulf Rift, Greece): Geomorphological signature, recent earthquake history and evolution, Journal of Geophysical Research, Vol. 110, No. B9, B09302, 15 pp.
Pantosti, D., and Palyvos, N, (eds), 2007. "3HAZ Corinth" Project Deliverable 30, Maps of active faults, marine terraces and landslides, Unpubl. Report, INGV.
Perissoratis, C, Piper, D.J.W., and Lykousis, V., 2000. Alternating marine and lacustrine sedimentation during the late Quaternary in the Gulf of Corinth rift basin, central Greece, Marine Geology, 167, 391-411.
Piper, D.J.W., Doutsos, T., and Stamatopoulos, L., 1990. Quaternary history of the Gulfs of Patras and Corinth, Greece, Z. Geomorphol, 34, 4, 451-461.
Rozos, D., 1991. Engineering geological conditions in Achaia Province – geomechanical characteristics of the Plio-Pleistocene Sediments, PhD Thesis, Department of Geology, University of Patras. (in Greek)
Siddall, M., Rohling, E.J., Almogi-Labin, Α., Hemleben, C, Meischner, D., Schmelzer, I., and Smeed, D.A., 2003, Sea-level fluctuations during the last glacial cycle, Nature, 423, 853-858.
Sorel, D., Pantosti, D., Lemeille, F., Palyvos, N., and De-Martini, P.M., 2005, The step-over between the Eliki and Aigion fault systems: slip transfer and present rates of activity. Unpubl. report for CNRS project GDR Corinthe n° 234, 13pp.
Stamatopoulos, L., Voltaggio, M., and Kontopoulos, N., 1994. 230Th / 2 3 8U dating of corals from Tyrrhenian marine deposits and the Palaeogeographic evolution of the Western Peloponnesus (Greece), Munster. Forsch. Geol. Palaont., 76, 345-352.
Stamatopoulos, L., Kontopoulos, N., Voltaggio, M., and Branca, M., 2004. Radiochronological data with U/Th method in lagoonal/marine deposits of the NW Péloponnèse, Greece. Bull. Geol Soc. Greece, XXXVI, 1064-1067. (in Greek)
Stournaras, G, Tsimpidis, G, Tsoumanis, P., Yannatos, G., and Guillande, 1998. Instability phenomena in the Neogene deposits of Northern Peloponnesus, Greece, Bull. Eng. Geol. Env., 57, 65-68.
Symeonidis, N., Theodorou, G., Schutt, H., and Velitzelos, E., 1987. Paleontological and stratigraphical observations in the area of Achaia and Etoloakarnania (W Greece), Ann. Geol. Pays. Hellen., 38, 317-353.
Thompson, W.G., and Goldstein, S.L., 2005. Open-system coral ages reveal persistent suborbital sea-level cycles, Science, 308, 401-404.
Tsoflias, P., and Loftus, D.L., 1971. Geological map of Greece in 1:50,000- Nafpaktos sheet, IGME, Athens.
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