Ferrimagnetism

A property of material where there is an antiparallel alignment of magnetic moments but these alignments are unbalanced either because one direction has stronger moments or a larger number of moments. Inverse spinel structures (“ferrites”) are often ferrimagnetic, where magnetic moments of ferric iron cations in the tetrahedral sites and one-half the cations in the octahedral sites (also ferric iron) are opposed and cancel, whereas the remaining occupied octahedral sites can have either balanced (e.g., Mg, Cd, Zn, zero unpaired electrons) or unbalanced (e.g., Mn, Fe2+, Co, Ni, Cu) magnetic moments, approximately proportional to the number of unpaired electrons.

Ferrimuscovite

An invalid name for a hypothetical end member.

Ferriphlogopite

An obsolete varietal term for ferrian phlogopite, tetra-ferriphlogopite.

Ferripyrophyllite

The ferric iron analogue of pyrophyllite.

Ferrisepiolite

A member of the palygorskite-sepiolite group with a composition of approximately (Fe3+,Fe2+,Mg)4 (Si,Fe3+)6O15(O,OH)2.6H2O.
See palygorskite-sepiolite group

Ferristilpnomelane
Ferrites
Ferrititanbiotite

An obsolete varietal term for biotite.

Ferriwodanite

An obsolete varietal term for biotite.

Ferriwotanite

An obsolete varietal term for biotite.