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A. Pallikarakis, I. Papanikolaou, M. Triantaphyllou, C. Grützner, G. Migiros, K. Reicherter, J. Mason, S. Schneiderwind
A. Pallikarakis, I. Papanikolaou, M. Triantaphyllou, C. Grützner, G. Migiros, K. Reicherter, J. Mason, S. Schneiderwind


Τhe most important active fault that intersects the eastern tip of Corinth Canal,the Kalamaki-Isthmia fault, is studied in detail, involving data analysis from nine boreholes, magnetic susceptibility measurements within boreholes and paleoenvironmental interpretations. Samples taken from boreholes were analysed and paleoenvironmental changes in the sequence are described. We correlate magnetic susceptibility (MS) measurements with paleoenvironmental and lithological alternations within the boreholes. We have ascribed low MS values to marine highstand deposits and high MS values to lowstand terrestrial deposits. Glacioeustatic sea level changes and tectonic movements have led to a very complicated lithosedimentary pattern that involves subaerial exposure, fluvialterrestrial, lagoonal, shallow marine environments and possibly even some lake sediments. Our results indicate that the Kalamaki fault is active and has a low slip rate of 0.05±0.02 mm/yr.


Benthic foraminifera; active faulting; Corinth gulf; Saronic Gulf

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Armijo, R., Meyer, B., King, G.C.P., Rigo. A. and Papanastassiou, D., 1996. Quaternary evolution

of the Corinth Rift and its implications for the Late Cenozoic evolution of the Aegean,

Geophys. J. Int., 126, 11-53.

Bornovas, J., Lalechos, N. and Filipakis, N., 1972. 1:50.000-scale geological map, Sheet -Korinthos.

Institute of Geology and Mineral Exploration.

Bornovas, J., Gaitanakis, P. and Spiridopoulos, A., 1984. 1:50.000-scale geological map, Sheet -

Perachora, Institute of Geology and Mineral Exploration, Athens.

Collier, R.E.L., 1990. Eustatic and tectonic controls upon Quaternary coastal sedimentation in the

Corinth Basin, Greece, J. Geol. Soc. London, 147, 301-314.

Collier, R.E.L. and Dart, C.J., 1991. Neogene to Quaternary rifting, sedimentation and uplift in the

Corinth Basin, Greece, Journal of the Geological Society, London, 148, 1049-563 1065, doi:


Collier, R.E.L. and Thompson, J., 1991. Transverse and linear dunes in an upper Pleistocene marine

sequence, Corinth Basin, Greece, Sedimentology, 38, 1021-1040.

Collier, R.E.L., Leeder, R.M., Rowe, P. and Atkinson, T., 1992. Rates of tectonic uplift in the

Corinth and Megara basins, Central Greece, Tectonics, 1159-1167.

Da Silva, A.C., Potma, K., Weissenberger, J.A.W., Whalen, M.T., Humblet, M., Mabille, C. and

Boulvain, F., 2009: Magnetic susceptibility evolution and sedimentary environments on

carbonate platform sediments and atolls, comparison of the Frasnian from Belgium and

Alberta, Canada, Sed. Geol., 214, 3-18.

Freyberg, V., 1973. Geologie des Isthmus von Korinth, Erlanger Geologische Abhandlungen, Heft

, Junge und Sohn, Universitätsbuchdruckerei Erlangen, 183 pp. (in German).

Gawthorpe, R.L., Fraser, A.Jj. and Collier, R., 1994. Sequence stratigraphy in active extensional

basins: implications for the interpretation of ancient basin fills, Marine and Petroleum

Geology, 11, 642-658.

Gaitanakis, P., Mettos, A. and Fytikas, M., 1984. 1:50.000 scale geological map, Sheet “Sofikon”,

Institute of Geology and Mineral Exploration.

Mullins, C.E., 1977. Magnetic susceptibility of the soil and its significance in soil science-a review,

Journal of soil science, 28(2), 223-246.

Oldfield, F., 1991. Environmental magnetism-a personal perspective, Quaternary Science Reviews,

(1), 73-85.

Pallikarakis, A., Papanikolaou, I., Triantaphyllou, M., Reicherter, K. and Migiros, G., 2015. Study

of an active fault at the eastern tip of the Corinth Canal, through surface and borehole data,

Proceedings of the 6th International INQUA Meeting on Paleoseismology, Active Tectonics

and Archaeoseismology, 19-24 April 2015, Pescina, Fucino Basin, Italy, 04/2015, 336-341.

Papanikolaou, D., Chronis, G., Lykousis, V., Pavlakis, P., Roussakis, G. and Syskakis, D., 1989.

:100.000 scale, Offshore Neotectonic Map the Saronic Gulf. Earthquake Planning and

Protection Organization, National Centre for Marine Research, University of Athens.

Papanikolaou, D., Logos, E., Lozios, S. and Sideris, Ch., 1996. 1:100.000 scale Neotectonic Map of

Korinthos Sheet, Earthquake Planning and Protection Organization, Athens.

Papanikolaou, I.D., Triantaphyllou, M., Pallikarakis, A. and Migiros, G., 2015. Active faulting at

the Corinth Canal based on surface observations, borehole data and paleoenvironmental

interpretations, Passive rupture during the 1981 earthquake sequence? Geomorphology, 237,


Reicherter, K., Vonberg, D., Koster B., Fernández-Steeger, T., Grützner, C. and Mathes-Schmidt,

M., 2010. The sedimentary inventory of tsunamis along the southern Gulf of Cádiz

(southwestern Spain), Zeitschrift für Geomorphologie, 54(3), 147-173.

Roberts, G.P., Houghton, S.L., Underwood, C., Papanikolaou, I., Cowie, P.A., van Calsteren, P.,

Wigley, T., Cooper, F.J. and McArthur, J.M., 2009. Localization of Quaternary slip rates in

an active rift in 105 years: An example from central Greece constrained by 234U-230Th coral

dates from uplifted paleoshorelines, Journal of Geophysical Research, 114, B10406, doi:


Siddall, M., Rohling, E.J., Almogi-Labin, A., Hemleben, Ch., Meischner, D., Schmelzer, I. and

Smeed, D.A., 2003. Sea-level fluctuations during the last glacial cycle, Nature, 423, 853-

Triantaphyllou, M.V., Pavlopoulos, K., Tsourou, Th. and Dermitzakis, M.D., 2003. Brackish marsh

benthic microfauna and paleoenvironmental changes during the last 6.000 years on the

coastal plain of Marathon (SE Greece), Rivista Italiana Paleontologia et Stratigafia, 109(3),



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