There are known two alkaline syenite pegmatite outcrops within shists of Imandra-Varzuga formation in the vicinity of Khibiny Station.
Refs.:
- Shlyukova Z.V., Burova T.A. (1963) Chevkinite from Khibina, - ZVMO, v92, N5, pp.597-599 (in Russ.)
- Shlyukova Z.V., Vlasova E.V., Kazakova M.E. (1973) New data on tundrite, - DAN SSSR, v211, N2, pp. 426-429 (in Russ.)
- Shlyukova Z.V. (1976) Lavenite - typomorphic mineral of contact zone of Khibina massif, - Studies on genetical mineralogy, Moscow, Nauka, pp. 28-35 (in Russ.)
- Shlyukova Z.V. (1986) Mineralogy of contact formations of Khibina massif, - Moscow, Nauka, p. 96 (in Russ.)
