Abstract
Ces mesures indiquent la presence de 2 sites VO 2+ physiquement equivalents dans la maille unitaire. Chacun est constitue de 3 ions VO 2+ inequivalents, l'un d'eux etant present avec une probabilite beaucoup plus petite. On explique l'origine des decompositions superhyperfines des quintets, anisotropes et independantes de la temperature
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