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VOLUME 31 (1980) | ISSUE 6 | PAGE 338
Peculiarities of the metamagnetic transition of a garnet single crystal Ca3Mn2Ge3O12
The existence of a magnetic phase transition, which does not correspond to the conventional model of a metamagnet with a high anisotropy, was determined from measurements of the magnetization of a Ca3Mn2Ge3012 single crystal below tn = 13.85 K.