Miller, ChristineKonzett, JurgenTiepolo, M.Armstrong, RichardMartin, Thoni2015-12-080024-4937http://hdl.handle.net/1885/34339In the Eclogite Zone of the Tauern Window, a layer of strongly retrogressed leucocratic jadeite-bearing gneiss is intercalated between mafic kyanite-eclogites. The jadeite-gneiss consists of garnet + quartz + paragonite ± phengite ± zoisite + zircon + rKeywords: geochemistry; gneiss; isotopic composition; jadeite; metamorphism; morphology; protolith; recrystallization; sedimentary rock; trace element; uranium-lead dating; zircon; Alps; Eastern Alps; Eurasia; Europe; Tauern Window Eastern Alps; High-pressure metasediment; Tauern window; U-Pb dating; ZirconJadeite-gneiss from the Eclogite Zone, Tauern Window, Eastern Alps, Austria: Metamorphic, geochemical and zircon record of a sedimentary protolith200710.1016/j.lithos.2006.03.0452015-12-08