Golyshevite is a rare mineral of the eudialyte group, with the formula Na<sub>10</sub>Ca<sub>3</sub>Ca<sub>6</sub>Zr<sub>3</sub>Fe<sub>2</sub>SiNb(Si<sub>3</sub>O<sub>9</sub>)<sub>2</sub>(Si<sub>9</sub>O<sub>27</sub>)<sub>2</sub>CO<sub>3</sub>(OH)<sub>3</sub>â¢H<sub>2</sub>O. The original formula was extended to show both the presence of cyclic silicate groups and silicon at the M4 site, according to the nomenclature of the eudialyte group. The characteristic feature of golyshevite is calcium-rich composition, with calcium at two main sites instead of one site. Together with feklichevite, fengchengite, ikranite and mogovidite it is a ferric-iron-dominant representative of the group. It is chemically similar to mogovidite. Golyshevite was named after Russian crystallographer Vladimir Mikhailovich Golyshev.
Golyshevite and mogovidite were found in calcium-bearing peralkaline pegmatites of the Kovdor massif, Kola Peninsula, Russia. Minerals associated with golyshevite are aegirine-augite, calcite, cancrinite, hedenbergite, orthoclase, pectolite, tacharanite, and thomsonite-Ca.
Impurities in golyshevite include chlorine, potassium, manganese, aluminium, cerium and lanthanum.
Calcium in golyshevite is present at M(1) and N(4) sites.