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dc.contributor.authorHasözbek, Altuğ-
dc.contributor.authorPourmand, A.-
dc.contributor.authorSharifi, A.-
dc.contributor.authorOrtega Martínez, Ana Isabel-
dc.contributor.authorParés, Josep María-
dc.contributor.authorVallverdú Poch, J.-
dc.contributor.authorConstantin, Silviu-
dc.date.accessioned2025-03-
dc.date.accessioned2025-03-28T09:55:27Z-
dc.date.issued2025-04-
dc.identifier.citationEGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Onlinees_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3450-
dc.descriptionPonencia presentada en: EGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Onlinees_ES
dc.description.abstractU-Th geochronology is a key tool in Quaternary geology, widely applied to carbonate matrices with significant advancements achieved through MC-ICP-MS technology. However, 230Th dating remains challenging for samples with low-uranium concentrations and high-detrital thorium content which often reflecting open-system behavior. These factors increase uncertainties in age calculations. This study introduces an optimized U-Th dating methodology that integrates refined wet chemistry protocols and 10¹³-ohm amplifiers, significantly reducing expanded uncertaintieses_ES
dc.language.isoenes_ES
dc.publisherEuropean Geosciences Union (EGU)es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución 4.0 International*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectU-Th Chronometryes_ES
dc.subjectQuaternary geologyes_ES
dc.subjectCueva Fantasmaes_ES
dc.subjectAtapuercaes_ES
dc.subjectMC-ICP-MSes_ES
dc.subjectU-Th geochronologyes_ES
dc.titleOptimized U-Th Chronometry for Carbonates Using MC-ICP-MS: Advancements in Precision and Applicationses_ES
dc.typePresentationes_ES
dc.typeOtheres_ES
dc.identifier.doi10.5194/egusphere-egu25-6277-
dc.relation.publisherversionhttps://doi.org/10.5194/egusphere-egu25-6277es_ES
dc.date.available2025-03-28T09:55:27Z-
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