Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/4093| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | De Martini, P. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.authorall | Pantosti, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.authorall | Palyvos, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.authorall | Lemeille, F.; IRSN, Fontenay-aux-Roses, France | en |
| dc.contributor.authorall | McNeill, L.; Southampton Oceanography Centre, University of Southampton, UK | en |
| dc.contributor.authorall | Collier, R.; School of Earth Sciences, University of Leeds, UK | en |
| dc.date.accessioned | 2008-10-01T13:31:58Z | en |
| dc.date.available | 2008-10-01T13:31:58Z | en |
| dc.date.issued | 2004-03 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/4093 | en |
| dc.description.abstract | Along the southern coast of the Gulf of Corinth, important coastal uplift is illustrated by raised Late-Pleistocene marine platforms. Terrace remnants preserved on the footwall of the Aigion and Eliki Faults were mapped in detail. To derive cumulative uplift rates, the individual terraces were tentatively correlated with the eustatic sea-level curve, constrained by some direct dating of the deposits blanketing the terraces. We obtain uplift rates of 1.05–1.2 mmyr−1 for the Aigion Fault footwall and of 1.0 and 1.25 mmyr−1 for the East and West Eliki Fault footwalls respectively. A forward modelling procedure was adopted to fit the best-preserved terrace transects, using a code based on standard dislocation theory and assuming reasonable scenarios of regional uplift. We obtained maximum slip rates consistently in the range of 7–11 mmyr−1 for the West and East Eliki Faults and of 9–11 mmyr−1 for the Aigion Fault. | en |
| dc.language.iso | English | en |
| dc.publisher.name | Elsevier | en |
| dc.relation.ispartof | Comptes Rendus Geoscience | en |
| dc.relation.ispartofseries | 4-5 / 336 (2004) | en |
| dc.subject | slip rate | en |
| dc.subject | marine terraces | en |
| dc.subject | modeling | en |
| dc.subject | Corinth Gulf, Greece | en |
| dc.title | Slip rates of the Aigion and Eliki Faults from uplifted marine terraces, Corinth Gulf, Greece | en |
| dc.title.alternative | Tectonics | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 325-334 | en |
| dc.subject.INGV | 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations | en |
| dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.03. Geomorphology | en |
| dc.identifier.doi | 10.1016/j.crte.2003.12.006 | en |
| 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] N.N. Ambraseys, J.A. Jackson, Seismicity and strain in the Gulf of Corinth (Greece) since 1694, J. Earthquake Eng. 1 (1997) 433–474. [3] R. Armijo, B.Meyer, G.C.P. King, A. Rigo, D. Papanastassiou, Quaternary evolution of the Corinth Rift and its implications for the Late Cenozoic evolution of the Aegean, Geophys. J. Int. 126 (1996) 11–53. [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. Geophys. Res. 105 (2000) 25605– 25625. [5] P.J. Clarke, R.R. Davies, P.C. England, B. Parson, H. Billiris, D. Paradissis, G. Veis, P.A. Cross, P.H. Denys, V. Ashkenazi, R. Bingley, H.-G. Kahle, M.-V.Muller, P. Briole, Crustal strain in central Greece from repeated GPS measurements in the interval 1989–1997, Geophys. J. Int. 135 (1998) 195–214. [6] R.E.L. Collier, M.R. Leeder, R.J. Rowe, T.C. Atkinson, Rates of tectonic uplift in the Corinth and Megara basins, central Greece, Tectonics 11 (1992) 1159–1167. [7] D. Hatzfeld, V. Karakostas, M. Ziazia, I. Kassaras, E. Papadimitriou, K. Makropoulos, N. Voulgaris, C. Papaioannou, Microseismicity and faulting geometry in the Gulf of Corinth (Greece), Geophys. J. Int. 141 (2000) 438–456. [8] B. Keraudren, D. Sorel, The terraces of Corinth (Greece) – a detailed record of eustatic sea-level variations during the last 500 000 years, Mar. Geol. 77 (1987) 99–107. [9] K.R. Lajoie, D.J. Ponti, C.L. Powell, S.A. Mathieson, A.M. Sarna-Wojcicki, 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, 1991, pp. 190–214. [10] F. Lemeille, F. Chatoupis, M. Foumelis, D. Rettenmaier, I. Unkeld, L. Micarelli, I. Moretti, C. Bourdillon, C. Guernet, C. Müller, Recent syn-rift deposits in the hangingwall of the Aigion Fault, C. R. Geoscience 336 (2004) 425–434, this issue. [11] L.C. McNeill, R.E.L. Collier, Footwall uplift rates of the Eastern Eliki Fault segment, Gulf of Corinth, Greece, inferred from Holocene and Pleistocene terraces, J. Geol. Soc. London 161 (2004) 81–92. [12] D. Pantosti, P.M. De Martini, I. Koukouvelas, L. Stamatopoulos, N. Palyvos, S. Pucci, F. Lemeille, S. Pavlides, Paleoseismological investigations across the Aigion Fault (Gulf of Corinth, Greece), C. R. Geoscience 336 (2004) 335–342, this issue. [13] A. Rigo, H. Lyon-Caen, R. Armijo, A. Deschamps, D. Hatzfeld, K. Makropoulos, P. Papadimitriou, I. Kassaras, A microseismic study in the western part of the Gulf of Corinth (Greece): implications for large-scale normal faulting mechanisms, Geophys. J. Int. 126 (1996) 663–688. [14] J. Schmidt, in: C. Schottze (Ed.), Studien über Erdbeben, Leipzig, 1879, pp. 68–83. [15] I. Stewart, Holocene uplift and palaeoseismicity on the Eliki Fault,Western Gulf of Corinth, Greece, Ann. Geofis. 39 (1996) 575–588. [16] C. Tiberi, H. Lyon-Caen, D. Hatzfeld, H. Achauer, E. Karagianni, A. Kiratzi, E. Louvari, D. Panagiotopoulos, I. Kassaras, G. Kaviris, K. Makropoulos, P. Papadimitriou, Crustal and upper mantle structure beneath the Corinth rift (Greece) from teleseismic tomography study, J. Geophys. Res. 105 (2000) 28159–28171. [17] S.N.Ward, G. Valensise, Fault parameters and slip distribution of the 1915, Avezzano, Italy earthquake derived from geodetic observations, Bull. Seismol. Soc. Amer. 79 (1989) 690–710. | en |
| dc.description.obiettivoSpecifico | 3.2. Tettonica attiva | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | De Martini, P. M. | en |
| dc.contributor.author | Pantosti, D. | en |
| dc.contributor.author | Palyvos, N. | en |
| dc.contributor.author | Lemeille, F. | en |
| dc.contributor.author | McNeill, L. | en |
| dc.contributor.author | Collier, R. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
| dc.contributor.department | IRSN, Fontenay-aux-Roses, France | en |
| dc.contributor.department | Southampton Oceanography Centre, University of Southampton, UK | en |
| dc.contributor.department | School of Earth Sciences, University of Leeds, UK | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
| crisitem.author.dept | Institut de Radioprotection et de Surete Nucléaire, Seismic Hazard Division | - |
| crisitem.author.dept | Southampton Oceanography Centre, School of Ocean and Earth Science, University of Southampton, Southampton SO14 3ZH, UK | - |
| crisitem.author.dept | Department of Earth Sciences, University of Leeds, Leeds, England, United Kingdom | - |
| crisitem.author.orcid | 0000-0002-3598-5191 | - |
| crisitem.author.orcid | 0000-0001-7308-9104 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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| File | Description | Size | Format | Existing users please Login |
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| CRGeo_DeMartini_2004.pdf | main article | 554.42 kB | Adobe PDF |
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