EPR has beenused to study yttrium-stabilised electron-hole centres of natural anhydrites. Geometrical models have been constructed by measuring the main directions of the tensors of the spectroscopic constants accurately and by correlating them with the crystal structure. Hyperfine splitting constant and thermal stability of the centres have been shown to vary as the localization of the unpaired electron density at the yttrium ions which replace calcium of the initial lattice.Mittels EPR wurden Yttrium-stabilisierte Elektron-Loch-Zentren in natiirlichem Anhydrit untersucht. Geometrische Modelle werden durch genaue Messung der Hauptwerte der Tensoren der spektroskopischen Konstanten und durch Korrelation mit der Kristallstruktur konstruiert. Es wird gezeigt, daB die Hyperfeinaufspaltungskonshnte und die thermische Stabilitiit der Zentren wie die Lokalisierung des ungepaarten Elektrons am Yttriumatom variiert, das das Kalziumatom des urspriinglichen Gitters ersetzt.
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