Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/46243
DC FieldValueLanguage
dc.contributor.authorGuillou, Hervéen_US
dc.contributor.authorNomade, Sébastienen_US
dc.contributor.authorCarracedo, Juan Carlosen_US
dc.contributor.authorKissel, Catherineen_US
dc.contributor.authorLaj, Carloen_US
dc.contributor.authorPerez Torrado, Francisco Joséen_US
dc.contributor.authorWandres, Camilleen_US
dc.contributor.otherPerez-Torrado, Francisco Jose-
dc.contributor.otherCarracedo, Juan-Carlos-
dc.date.accessioned2018-11-23T02:41:44Z-
dc.date.available2018-11-23T02:41:44Z-
dc.date.issued2011en_US
dc.identifier.issn1871-1014en_US
dc.identifier.urihttp://hdl.handle.net/10553/46243-
dc.description.abstractIn this study, the effectiveness of combined unspiked K–Ar and 40Ar/39Ar dating methods as currently applied now at LSCE in the 14C age range was evaluated by studying two 30,000 years old phonolites from Tenerife (Canary Islands). New 40Ar/39Ar ages obtained in this work are comparable with the K–Ar ages, and of similar precision. This remarkable agreement obtained between the two dating methods in this young age range, validates the new LSCE 40Ar/39Ar facility and provides a very promising approach to calibrate the Quaternary timescale and to date key events such as geomagnetic field instabilities and climatic changes. The approach combining the 40Ar/39Ar and the unspiked K–Ar methods has the advantage that all the basic assumptions, which rule the K–Ar clock, are checked via the isochron approach. In the event of positive check, the 40Ar/39Ar and unspiked K–Ar ages can be pooled to produce very precise ages.en_US
dc.languageengen_US
dc.relation.ispartofQuaternary Geochronologyen_US
dc.sourceQuaternary Geochronology [ISSN 1871-1014], v. 6 (6), p. 530-538en_US
dc.subject250621 Vulcanologíaen_US
dc.subject.otherGeochronologyen_US
dc.subject.otherCanary islandsen_US
dc.subject.otherVolcanismen_US
dc.titleEffectiveness of combined unspiked K–Ar and 40Ar/39Ar dating methods in the 14C age rangeen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.quageo.2011.03.011
dc.identifier.scopus80053178367-
dc.identifier.isi000297092300002-
dcterms.isPartOfQuaternary Geochronology-
dcterms.sourceQuaternary Geochronology[ISSN 1871-1014],v. 6 (6), p. 530-538-
dc.contributor.authorscopusid36950485500-
dc.contributor.authorscopusid6601976794-
dc.contributor.authorscopusid55663151400-
dc.contributor.authorscopusid7005416537-
dc.contributor.authorscopusid7006827313-
dc.contributor.authorscopusid6602207526-
dc.contributor.authorscopusid35119645800-
dc.description.lastpage538-
dc.identifier.issue6-
dc.description.firstpage530-
dc.relation.volume6-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid28049990-
dc.contributor.daisngid34857662
dc.contributor.daisngid382175-
dc.contributor.daisngid551723-
dc.contributor.daisngid192681-
dc.contributor.daisngid190158-
dc.contributor.daisngid1111499-
dc.contributor.daisngid4425783-
dc.identifier.investigatorRIDN-9727-2018-
dc.identifier.investigatorRIDN-9641-2018-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Guillou, H
dc.contributor.wosstandardWOS:Nomade, S
dc.contributor.wosstandardWOS:Carracedo, JC
dc.contributor.wosstandardWOS:Kissel, C
dc.contributor.wosstandardWOS:Laj, C
dc.contributor.wosstandardWOS:Torrado, FJP
dc.contributor.wosstandardWOS:Wandres, C
dc.date.coverdateDiciembre 2011
dc.identifier.ulpgces
dc.description.sjr2,493
dc.description.jcr3,083
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGeología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptFísica-
crisitem.author.orcid0000-0002-4282-2796-
crisitem.author.orcid0000-0002-4644-0875-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameCarracedo Gomez, Juan Carlos-
crisitem.author.fullNamePérez Torrado, Francisco José-
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