<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-59XEO141</identifier><date>2016</date><creator>Serianz, Luka</creator><relation>documents/doc/5/URN_NBN_SI_doc-59XEO141_001.pdf</relation><relation>documents/doc/5/URN_NBN_SI_doc-59XEO141_001.txt</relation><format format_type="issue">2</format><format format_type="volume">59</format><format format_type="type">article</format><format format_type="extent">str. 193-204</format><identifier identifier_type="ISSN">0016-7789</identifier><identifier identifier_type="COBISSID">2579029</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-59XEO141</identifier><language>eng</language><publisher>Geološki zavod Slovenije</publisher><source>Geologija</source><rights>BY</rights><subject language_type_id="slv">doline</subject><subject language_type_id="slv">geomorfologija</subject><subject language_type_id="eng">geomorphology</subject><subject language_type_id="slv">kvartar</subject><subject language_type_id="slv">ledena doba</subject><subject language_type_id="slv">ledeniki</subject><subject language_type_id="slv">Radovna (reka)</subject><subject language_type_id="eng">Slovenia</subject><subject language_type_id="slv">Slovenija</subject><title>Tri-dimensional model of the Radovna glacier from the last glacial period</title><title>Tridimenzionalni model Radovniškega ledenika iz zadnje poledenitve</title></Record>