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<dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:invenio="http://invenio-software.org/elements/1.0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><dc:identifier>doi:10.1130/G52152Y.1</dc:identifier><dc:language>eng</dc:language><dc:creator>Rodríguez-López, Juan Pedro</dc:creator><dc:creator>Liesa, Carlos L.</dc:creator><dc:creator>Luzón, Aránzazu</dc:creator><dc:creator>Muñoz, Arsenio</dc:creator><dc:creator>Mayayo, María J.</dc:creator><dc:creator>Murton, Julian B.</dc:creator><dc:creator>Soria, Ana R.</dc:creator><dc:title>Ice-rafted dropstones at midlatitudes in the Cretaceous of continental, Iberia: REPLY</dc:title><dc:identifier>ART-2024-138176</dc:identifier><dc:description>We recently reported glacial dropstones in a glacial–deglacial succession in the Cretaceous of continental Iberia (Rodríguez-López et al., 2024), and here we reply to the Comment by Benito et al. (2024)...</dc:description><dc:date>2024</dc:date><dc:source>http://zaguan.unizar.es/record/134532</dc:source><dc:doi>10.1130/G52152Y.1</dc:doi><dc:identifier>http://zaguan.unizar.es/record/134532</dc:identifier><dc:identifier>oai:zaguan.unizar.es:134532</dc:identifier><dc:identifier.citation>Geology 52, 4 (2024), e575</dc:identifier.citation><dc:rights>All rights reserved</dc:rights><dc:rights>http://www.europeana.eu/rights/rr-f/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

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