Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4095
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dc.contributor.authorallPantosti, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallDe Martini, P. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallKoukouvelas, I.; University of Patras, Greeceen
dc.contributor.authorallStamatopoulos, L.; University of Patras, Greeceen
dc.contributor.authorallPalyvos, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallPucci, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallLemeille, F.; IRSN, CEA, 60–68, av. du Général-Leclerc, BP 6, 92265 Fontenay-aux-Roses cedex, Franceen
dc.contributor.authorallPavlides, S.; Aristotle University of Thessaloniki, Greeceen
dc.date.accessioned2008-10-01T13:34:12Zen
dc.date.available2008-10-01T13:34:12Zen
dc.date.issued2004-03en
dc.identifier.urihttp://hdl.handle.net/2122/4095en
dc.description.abstractWe performed palaeoseismological investigations along the Aigion Fault, one of the main faults that bound the southern side of the Corinth Gulf. The mapped trace of the Aigion Fault onland is about 8 km long and may extend as much as 14 km if one includes its offshore trace. We made detailed studies at two sites adjacent to the Meganitas River. Although dating of faulted sediments was a bit problematic, we present a preliminary estimate of the faults short-term slip rate and recurrence interval. Slip rates range from 1.6 to 4.3 mmyr−1, with a maximum up to 6.3 mmyr−1. Three surface faulting events occurred in the seven centuries prior to 1888 AD, yielding an average (maximum) recurrence interval of 360 yr.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofComptes Rendus Geoscienceen
dc.relation.ispartofseries4-5 / 336 (2004)en
dc.subjectpalaeoseismologyen
dc.subjectAigion Faulten
dc.subjectCorinth Gulfen
dc.subjectGreeceen
dc.titlePalaeoseismological investigations of the Aigion Fault (Gulf of Corinth, Greece)en
dc.title.alternativeTectonicsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber335-342en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismologyen
dc.identifier.doi10.1016/j.crte.2003.12.005en
dc.relation.references[1] N.N. Ambraseys, J.A. Jackson, Seismicity and associated strain of central Greece between 1890 and 1988, Geophys. J. Int. 101 (1990) 663–708. [2] P. Bernard, et al., The Ms = 6.2, June 15, 1995 Aigion earthquake (Greece): evidence for low angle normal faulting in the Corinth rift, J. Seismol. 1 (1997) 131–150. [3] P. Bernard (Ed.), CORSEIS project final report, Workpackage 8, European Commission, 2002. [4] P. Briole, A. Rigo, H. Lyon-Caen, J.C. Ruegg, K. Papazissi, C. Mitsakaki, A. Balodimou, G. Veis, D. Hatzfield, A. Deschamps, Active deformation of the Corinth rift, Greece: results from repeated Global Positioning System surveys between 1990 and 1995, J. Geolphys. Res. 105 (2000) 25605– 25625. [5] P.J. Clarke, R.R. Davies, P.C. England, B.E. Parsons, H. Billiris, D. Paradissis, G. Veis, P.H. Denys, P.A. Cross, V. Ashkenazi, R. Bingley, Geodetic estimate of seismic hazard in the Gulf of Korinthos, Geophys. Res. Lett. 24 (1997) 1303–1306. [6] R.E.L. Collier, R.L. Gawthorpe, Neotectonics, drainage and sedimentation in central Greece: insights into coastal reservoir geometries in syn-rift sequences, in: J.J. Lambiase (Ed.), Hydrocarbon Habitat in Rift Basins, Geol. Soc. Spec. Publ. 80 (1995) 165–181. [7] R.E.L. Collier, D. Pantosti, G. D’Addezio, P.M. De Martini, E. Masana, D. Sakellariou, Paleoseismicity of the 1981 Corinth earthquake fault: seismic contribution to extensional strain in central Greece and implications for seismic hazard, J. Geophys. Res. 103 (B12) (1998) 30001–30020. [8] P.M. De Martini, D. Pantosti, N. Palyvos, F. Lemeille, L. Mc- Neill, R. Collier, Slip rates of the Aigion and Eliki Faults from uplifted marine terraces, Corinth Gulf, Greece, C. R. Geoscience 336 (2004) 325–334, this volume. [9] J.A. Jackson, J. Gagnepain, G. Houseman, G.C.P. King, P. Papadimitriou, C. Soufleris, J. Virieux, Seismicity, normal faulting, and the geomorphological development of the Gulf of Corinth (Greece): the Corinth earthquakes of February and March 1981, Earth Planet. Sci. Lett. 57 (1982) 377–397. [10] I.K. Koukouvelas, The Egion fault, earthquake-related and long-term deformation, Gulf of Corinth, Greece, J. Geodynam. 26 (1998) 501–513. [11] I.K. Koukouvelas, L. Stamatopoulos, D. Katsonopoulou, S. Pavlides, A paleoseismological and geoarchaeological investigation of the Eliki Fault, Gulf of Corinth, Greece, J. Struct. Geol. 23 (2001) 531–543. [12] B.C. Papazachos, C.B. Papazachou, The Earthquakes of Greece, Ziti Publications, Greece, 1997. [13] C.B. Ramsey, Radiocarbon Calibration program Oxcal 3.5, http://www.rlaha.ox.ac.uk/oxcal, 2000. [14] G.P. Roberts, I.K. Koukouvelas, Structural and seismological segmentation of the Gulf of Corinth fault system: implications for models of fault growth, Ann. Geofis. 23 (1996) 619–646. [15] J. Schmidt, in: C. Schottze (Ed.), Studien uber Erdbeben, Leipzig, Germany, 1879, pp. 68–83. [16] S. Soter, D. Katsonopoulou, The search for Ancient Elike: geological, sonar and bore hole studies, Geoarchaeology 14 (1999) 531–563. [17] D.L. Wells, K.J. Coppersmith, New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement, Bull. Seismol. Soc. Am. 84 (1994) 974–1002.en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPantosti, D.en
dc.contributor.authorDe Martini, P. M.en
dc.contributor.authorKoukouvelas, I.en
dc.contributor.authorStamatopoulos, L.en
dc.contributor.authorPalyvos, N.en
dc.contributor.authorPucci, S.en
dc.contributor.authorLemeille, F.en
dc.contributor.authorPavlides, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversity of Patras, Greeceen
dc.contributor.departmentUniversity of Patras, Greeceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIRSN, CEA, 60–68, av. du Général-Leclerc, BP 6, 92265 Fontenay-aux-Roses cedex, Franceen
dc.contributor.departmentAristotle University of Thessaloniki, Greeceen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDepartment of Geology, University of Patras, Greece-
crisitem.author.deptUniversity of Patras, Greece-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptInstitut de Radioprotection et de Surete Nucléaire, Seismic Hazard Division-
crisitem.author.deptAristotle University of Thessaloniki, Department of Geology, Thessaloniki, Greece-
crisitem.author.orcid0000-0001-7308-9104-
crisitem.author.orcid0000-0002-3598-5191-
crisitem.author.orcid0000-0002-3557-2936-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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