<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:DOC-5VFOBPR3</identifier><date>2005</date><creator>Dolenec, Matej</creator><relation>documents/doc/5/URN_NBN_SI_doc-5VFOBPR3_001.pdf</relation><relation>documents/doc/5/URN_NBN_SI_doc-5VFOBPR3_001.txt</relation><format format_type="issue">2</format><format format_type="volume">52</format><format format_type="type">article</format><format format_type="extent">str. 437-445</format><identifier identifier_type="ISSN">1408-7073</identifier><identifier identifier_type="COBISSID">531038</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-5VFOBPR3</identifier><language>eng</language><publisher>Inštitut za rudarstvo, geotehnologijo in okolje</publisher><publisher>Naravoslovnotehniška fakulteta</publisher><source>RMZ-materials and geoenvironment</source><rights>InC</rights><subject language_type_id="slv">Karavanke</subject><subject language_type_id="eng">Karawanks</subject><subject language_type_id="slv">stratigrafija</subject><subject language_type_id="eng">stratigraphy</subject><subject language_type_id="slv">torij</subject><subject language_type_id="slv">uran</subject><title>RMZ - Materiali in geookolje</title><title>The Permian Triassic boundary in the Karavanke mountains (Brsnina section, Slovenia): the ratio of Th/U as a possible indicator of changing redox conditions at the P/T transition</title></Record>