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VOLUME 22 (1975) | ISSUE 3 | PAGE 140
Direct measurement of the magnetic and deformation contribution to birefringence in the weakly-ferromagnetic phase of hematite (α-Fe2O3)
It is shown experimentally that 98% of the entire birefringence in a-Fe203, with the Hght propagating along the C3 axis, is due to the polarizability anisotropy connected with the magnetizations of the sublattices and their orientation relative to the crystallographic axes.