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Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3449
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dc.contributor.authorErturaç, Mehmet Korhan-
dc.contributor.authorŞahiner, Eren-
dc.contributor.authorKandemir, R.-
dc.contributor.authorOkur, Hilal-
dc.contributor.authorSalman, İrem-
dc.contributor.authorHasözbek, Altuğ-
dc.contributor.authorÖncel, M. S.-
dc.contributor.authorQin, J.-
dc.contributor.authorAkçar, N.-
dc.date.accessioned2025-03-
dc.date.accessioned2025-03-28T09:45:57Z-
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/20.500.12136/3449-
dc.descriptionPoster presentado en: EGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Onlinees_ES
dc.description.abstractThe Antarctic Peninsula is uplifting rapidly due to the isostatic response to ice sheet unloading since the Holocene. Understanding the timing and rate of this process is crucial for addressing several key research questions: (1) exploring the elastic interactions between the mantle and lithosphere to improve Glacial Isostatic Adjustment (GIA) models, (2) assessing the contribution of the Antarctic ice sheet to Holocene global sea level rise, and (3) investigating the modern response of Antarctic ice sheets to climate change, helping to identify high-impact research areas for polar sciencees_ES
dc.language.isoenes_ES
dc.publisherEuropean Geosciences Union (EGU)es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución 4.0 International (CC BY 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectAntarctic Peninsulaes_ES
dc.subjectGlacial evolutiones_ES
dc.subjectHolocenees_ES
dc.titleTiming of glacier retreat and spatio-temporal variations in the vertical deformation rate of the Horseshoe Island, Marguarite Bay, west Antarctic Peninsulaes_ES
dc.typePresentationes_ES
dc.typeOtheres_ES
dc.identifier.doi10.5194/egusphere-egu25-6751-
dc.relation.publisherversionhttps://doi.org/10.5194/egusphere-egu25-6751es_ES
dc.date.available2025-03-28T09:45:57Z-
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Geocronología y Geología

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