<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-919BIXZL</identifier><date>2022</date><creator>Diercks, Manuel</creator><creator>Grützner, Christoph</creator><creator>Ustaszewski, Kamil</creator><creator>Vrabec, Marko</creator><relation>documents/doc/9/URN_NBN_SI_doc-919BIXZL_001.pdf</relation><relation>documents/doc/9/URN_NBN_SI_doc-919BIXZL_001.txt</relation><format format_type="issue">1</format><format format_type="volume">65</format><format format_type="type">article</format><format format_type="extent">str. 73-92</format><identifier identifier_type="ISSN">0016-7789</identifier><identifier identifier_type="DOI">10.5474/geologija.2022.006</identifier><identifier identifier_type="COBISSID_HOST">116558339</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-919BIXZL</identifier><language>eng</language><publisher publisher_location="Ljubljana">Geološki zavod Slovenije</publisher><source>Geologija</source><rights>BY</rights><subject language_type_id="slv">erozija</subject><subject language_type_id="slv">geomorfologija</subject><subject language_type_id="slv">Pradol</subject><subject language_type_id="slv">suha dolina</subject><subject language_type_id="slv">vrezovanje</subject><subject language_type_id="slv">zadnji glacialni maksimum</subject><title>Addendum to Diercks et al., 2021: A model for the formation of the Pradol (Pradolino) dry valley in W Slovenia and NE Italy</title></Record>