<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:doc-L4A4I3YY</identifier><date>2018</date><creator>Grlj, Aleš</creator><creator>Stepišnik, Uroš</creator><relation>documents/doc/L/URN_NBN_SI_doc-L4A4I3YY_001.pdf</relation><relation>documents/doc/L/URN_NBN_SI_doc-L4A4I3YY_001.txt</relation><format format_type="issue">49</format><format format_type="type">article</format><format format_type="extent">str. 95-111</format><identifier identifier_type="ISSN">0354-0596</identifier><identifier identifier_type="COBISSID">68778850</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-L4A4I3YY</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">Bosna in Hercegovina</subject><subject language_type_id="slv">geomorfologija</subject><subject language_type_id="slv">Grabovica</subject><subject language_type_id="slv">hidrologija</subject><subject language_type_id="slv">krasoslovje</subject><subject language_type_id="slv">kraški pojavi</subject><title>Caves, denuded caves and collapse dolines as past hydrological pattern indicators of the Grabovica Plateau, the Dinaric Karst (Bosnia and Herzegovina)</title></Record>