<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-J8X620LX</identifier><date>2017</date><creator>Stojilković, Borut</creator><relation>documents/doc/J/URN_NBN_SI_doc-J8X620LX_001.pdf</relation><relation>documents/doc/J/URN_NBN_SI_doc-J8X620LX_001.txt</relation><format format_type="issue">47</format><format format_type="type">article</format><format format_type="extent">str. 127-141</format><identifier identifier_type="ISSN">0354-0596</identifier><identifier identifier_type="COBISSID_HOST">66465122</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-J8X620LX</identifier><language>eng</language><publisher>Znanstvena založba Filozofske fakultete</publisher><source>Dela - Oddelek za geografijo Filozofske fakultete v Ljubljani</source><rights>BY-SA</rights><subject language_type_id="slv">geomorfologija</subject><subject language_type_id="eng">geomorphology</subject><subject language_type_id="eng">Kamnik–Savinja Alps</subject><subject language_type_id="slv">Kamniško-Savinjske Alpe</subject><subject language_type_id="slv">ledena doba</subject><subject language_type_id="slv">pleistocen</subject><subject language_type_id="eng">Slovenia</subject><subject language_type_id="slv">Slovenija</subject><title>The traces of the last Pleistocene glacial maximum in the eastern Kamnik-Savinja Alps</title></Record>