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Tephrostratigraphy of the last 160 ka in Western Limagne (France)

hal.structure.identifierLaboratoire de Géographie Physique et Environnementale [GEOLAB]
dc.contributor.authorVERNET, Gérard
hal.structure.identifierDe la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
dc.contributor.authorRAYNAL, Jean-Paul
hal.structure.identifierLaboratoire de Physique Corpusculaire - Clermont-Ferrand [LPC]
dc.contributor.authorFAIN, Jean
hal.structure.identifierLaboratoire de Physique Corpusculaire - Clermont-Ferrand [LPC]
dc.contributor.authorMIALLIER, Didier
hal.structure.identifierLaboratoire de Physique Corpusculaire - Clermont-Ferrand [LPC]
dc.contributor.authorMONTRET, Michèle
hal.structure.identifierLaboratoire de Physique Corpusculaire - Clermont-Ferrand [LPC]
dc.contributor.authorPILLEYRE, Thierry
hal.structure.identifierLaboratoire de Physique Corpusculaire - Clermont-Ferrand [LPC]
dc.contributor.authorSANZELLE, Serge
dc.date.accessioned2023-06-28T08:38:36Z
dc.date.available2023-06-28T08:38:36Z
dc.date.issued1998
dc.identifier.issn1040-6182
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/182951
dc.description.abstractEnThe GEOCLER 1 core extracted from the Clermont crater lake sediments and surface studies made at several localities north of Clermont provided numerous stratigraphic, environmental and chronological data (TL and radiocarbon) which allow us to present a chronostratigraphy of the Limagne for the past 160 ka. 118 ash-falls have been recorded in the crater-lake sediments of the Clermont maar. They demonstrate that a basaltic phreatic activity developed along the western fault-scarp of the Limagne between 160 and 70 ka, after which began the Chaîne des Puys activity. Moreover, several acid eruptions occured between 160 and 40 ka. From Older Dryas to Atlantic, between 15 and 7 ka, fourteen ash-falls occured and in some cases the source volcanoes have been identified. These include Puy de La Nugère, Puy de Dôme, Puy Chopine, Kilian Crater and Puy de Pariou which contribute mainly to the local tephra succession. Prospects for further prehistoric research in volcanic areas are outlined.
dc.language.isoen
dc.publisherElsevier
dc.source.titleQuaternary International
dc.subject.enFrance
dc.subject.enMassif Central
dc.subject.enMiddle Moutain
dc.subject.enVolcanism
dc.subject.enAsh-Falls
dc.subject.enTL-Dating
dc.subject.enPrehistory
dc.title.enTephrostratigraphy of the last 160 ka in Western Limagne (France)
dc.typeArticle de revue
dc.subject.halSciences de l'Homme et Société/Archéologie et Préhistoire
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Volcanologie
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Stratigraphie
bordeaux.journalQuaternary International
bordeaux.page139-146
bordeaux.volume47/48
bordeaux.hal.laboratoriesPACEA - UMR 5199*
bordeaux.countryGB
bordeaux.peerReviewedoui
hal.identifierhalshs-00004450
hal.version1
hal.origin.linkhttps://hal.archives-ouvertes.fr//halshs-00004450v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.btitle=Quaternary%20International&rft.jtitle=Quaternary%20International&rft.date=1998&rft.volume=47/48&rft.spage=139-146&rft.epage=139-146&rft.eissn=1040-6182&rft.issn=1040-6182&rft.au=VERNET,%20G%C3%A9rard&RAYNAL,%20Jean-Paul&FAIN,%20Jean&MIALLIER,%20Didier&MONTRET,%20Mich%C3%A8le&rft.genre=article


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