A trioctahedral member of the true mica group. The end-member formula is KFe2+3Fe3+Si3O10(OH)2 and the known polytype is 1M. The ferri-iron component is found in the tetrahedral site. Tetra-ferri-annite is commonly associated with stilpnomelane. Stilpnomelane, when coexisting with tetra-ferri-annite, often appears to be replaced by tetra-ferri-annite. Therefore, tetra-ferri-annite occurs in very low-grade metamorphosed iron formations.