Now showing 1 - 2 of 2
  • 2018Journal Article Research Paper
    [["dc.bibliographiccitation.firstpage","1359"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Journal of Petrology"],["dc.bibliographiccitation.lastpage","1382"],["dc.bibliographiccitation.volume","59"],["dc.contributor.author","Sorger, Dominik"],["dc.contributor.author","Hauzenberger, Christoph A"],["dc.contributor.author","Linner, Manfred"],["dc.contributor.author","Iglseder, Christoph"],["dc.contributor.author","Finger, Friedrich"],["dc.date.accessioned","2021-12-14T16:42:42Z"],["dc.date.available","2021-12-14T16:42:42Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1093/petrology/egy063"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/96809"],["dc.language.iso","en"],["dc.relation.issn","0022-3530"],["dc.relation.issn","1460-2415"],["dc.title","Carboniferous Polymetamorphism Recorded in Paragneiss-Migmatites from the Bavarian Unit (Moldanubian Superunit, Upper Austria): Implications for the Tectonothermal Evolution at the End of the Variscan Orogeny"],["dc.type","journal_article"],["dc.type.internalPublication","no"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]
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  • 2020Journal Article Research Paper
    [["dc.bibliographiccitation.firstpage","124"],["dc.bibliographiccitation.journal","Gondwana Research"],["dc.bibliographiccitation.lastpage","148"],["dc.bibliographiccitation.volume","85"],["dc.contributor.author","Sorger, Dominik"],["dc.contributor.author","Hauzenberger, Christoph A."],["dc.contributor.author","Finger, Fritz"],["dc.contributor.author","Linner, Manfred"],["dc.date.accessioned","2021-12-14T16:37:18Z"],["dc.date.available","2021-12-14T16:37:18Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1016/j.gr.2020.04.004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/96806"],["dc.language.iso","en"],["dc.relation.issn","1342-937X"],["dc.title","Two generations of Variscan garnet: Implications from a petrochronological study of a high-grade Avalonia-derived paragneiss from the Drosendorf unit, Bohemian Massif"],["dc.type","journal_article"],["dc.type.internalPublication","no"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]
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