A skarn porphyry copper deposit.
Located 5 "versts" west of Chernaya River. Wrongly considered as the type locality of Planerite.
Refs.:
- Rastsvetaeva, R.K., Bolotina, N.B., Zadov, A.E., Chukanov, N.V. (2005): "Crystal structure of fukalite dimorph Ca4[Si2O6](CO3)(OH)2
from the Gumeshevsk Deposit, the Urals", Transactions (Doklady) of the Russian Academy of Sciences/Earth Science Section 405A, 1347-1351
- Zadov, A. E.; Grabezhev, A. I.; Pertsev, N. N.; Chukanov, N. V.; Pribavkin, S. V. (2006): Tobermorite-plombierite metasomatites of the Gumeshevsk skarn-porphyry copper deposit, Middle Urals. Doklady Earth Sciences 407A, 495-497.
