<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-2Y8T8P26</identifier><date>2021</date><creator>Kunaver, Jurij</creator><relation>documents/doc/2/URN_NBN_SI_doc-2Y8T8P26_001.pdf</relation><relation>documents/doc/2/URN_NBN_SI_doc-2Y8T8P26_001.txt</relation><format format_type="volume">83</format><format format_type="issue">9/10</format><format format_type="type">article</format><format format_type="extent">str. 409-426</format><identifier identifier_type="ISSN">0033-1805</identifier><identifier identifier_type="COBISSID_HOST">81060355</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-2Y8T8P26</identifier><language>slv</language><publisher publisher_location="Ljubljana">Prirodoslovno društvo Slovenije</publisher><source>Proteus</source><rights>InC</rights><subject language_type_id="slv">geomorfologija</subject><subject language_type_id="slv">Kaninsko pogorje</subject><subject language_type_id="slv">kriosfera</subject><subject language_type_id="slv">ledenica G2</subject><subject language_type_id="slv">permafrost</subject><subject language_type_id="slv">segrevanje ozračja</subject><subject language_type_id="slv">speleologija</subject><subject language_type_id="slv">visokogorski kras</subject><title>Ledenica G2 na Kaninskem pogorju kot indikator segrevanja ozračja</title></Record>