Neufeld, Kai2007-12-172007-12-172007https://openscience.ub.uni-mainz.de/handle/20.500.12030/1693engInC-1.0https://rightsstatements.org/vocab/InC/1.0/550 Geowissenschaften550 Earth sciencesLattice preferred orientation in omphacite: Examples from the Tauern Window, Austria and the Western Gneiss Region, NorwayDissertationurn:nbn:de:hebis:77-14662