Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3040
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dc.contributor.authorallPalyvos, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallSorel, D.; Université Paris-Sud, Faculty of Geologyen
dc.contributor.authorallLemeille, F.; Institut de Radioprotection et de Surete Nucléaire, Seismic Hazard Divisionen
dc.contributor.authorallMancini, M.; CNR- Istituto di Geologia Ambientale e Geoingenieriaen
dc.contributor.authorallPantosti, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallJulia, R.; Institute of Earth Sciences Jaume Almera, Barcelonaen
dc.contributor.authorallTriantaphylou, M.; national and Capodistrian Univesrity of Athens, Faculty of Geology and Geoenvironmenten
dc.contributor.authorallDe Martini, P. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2007-12-10T15:42:16Zen
dc.date.available2007-12-10T15:42:16Zen
dc.date.issued2007-05en
dc.identifier.urihttp://hdl.handle.net/2122/3040en
dc.description.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.en
dc.description.sponsorship"3HAZ Corinth" EU project; CNRS project GDR Corinthe n. 234; Istituto Nazionale di Geofisica e Vulcanologiaen
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Greeceen
dc.relation.ispartofBulletin of the Geological Society of Greeceen
dc.relation.ispartofseries/ 40 (2007)en
dc.subjectTectonic geomorphologyen
dc.subjectDifferential coastal upliften
dc.subjectdeformation ratesen
dc.subjectactive normal faultsen
dc.subjectCorinth Gulfen
dc.subjectGreeceen
dc.titleReview and new data on uplift rates at the W termination of the Corinth Rift and the NE Rion Graben area (Achaia, NW Peloponnesos)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber412-424en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.03. Geomorphologyen
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextreserveden
dc.contributor.authorPalyvos, N.en
dc.contributor.authorSorel, D.en
dc.contributor.authorLemeille, F.en
dc.contributor.authorMancini, M.en
dc.contributor.authorPantosti, D.en
dc.contributor.authorJulia, R.en
dc.contributor.authorTriantaphylou, M.en
dc.contributor.authorDe Martini, P. M.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversité Paris-Sud, Faculty of Geologyen
dc.contributor.departmentInstitut de Radioprotection et de Surete Nucléaire, Seismic Hazard Divisionen
dc.contributor.departmentCNR- Istituto di Geologia Ambientale e Geoingenieriaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentInstitute of Earth Sciences Jaume Almera, Barcelonaen
dc.contributor.departmentnational and Capodistrian Univesrity of Athens, Faculty of Geology and Geoenvironmenten
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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.deptUniversité Paris-Sud, Centre d'Orsay, Faculty of Geology-
crisitem.author.deptInstitut de Radioprotection et de Surete Nucléaire, Seismic Hazard Division-
crisitem.author.deptCNR, Istituto di Geologia Ambientale e Geoingegneria-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptInstitute of Earth Sciences Jaume Almera, Barcelona-
crisitem.author.deptnational and Capodistrian Univesrity of Athens, Faculty of Geology and Geoenvironment-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0001-7308-9104-
crisitem.author.orcid0000-0002-3598-5191-
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-
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