Late local glacial maximum in the Central Altiplano triggered by cold and locally-wet conditions during the paleolake Tauca episode (17–15ka, Heinrich 1)

dc.contributor.authorPierre‐Henri Blard
dc.contributor.authorJérôme Lavé
dc.contributor.authorKenneth A. Farley
dc.contributor.authorMichel Fornari
dc.contributor.authorNéstor Jiménez
dc.contributor.authorV. Ramirez
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T13:55:13Z
dc.date.available2026-03-22T13:55:13Z
dc.date.issued2009
dc.descriptionCitaciones: 80
dc.identifier.doi10.1016/j.quascirev.2009.09.025
dc.identifier.urihttps://doi.org/10.1016/j.quascirev.2009.09.025
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/43491
dc.language.isoen
dc.publisherElsevier BV
dc.relation.ispartofQuaternary Science Reviews
dc.sourceCentre de Recherches Pétrographiques et Géochimiques
dc.subjectDeglaciation
dc.subjectGlacier
dc.subjectMoraine
dc.subjectGeology
dc.subjectGlacial period
dc.subjectChronology
dc.subjectPhysical geography
dc.subjectSurface exposure dating
dc.subjectLast Glacial Maximum
dc.subjectClimatology
dc.titleLate local glacial maximum in the Central Altiplano triggered by cold and locally-wet conditions during the paleolake Tauca episode (17–15ka, Heinrich 1)
dc.typearticle

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