Elinovskii is a long, narrow granitic body of some 400x50 m lying within terrigenous lower Devonian sandstones and limestones and lower Silurian limestones. In the southeastern part of the contact they are intensively altered to skarns. The main intrusive phase is a medium-grained riebeckite granite that gradually merges into medium- to coarse-grained peralkaline alaskites. In the country rocks there are rare dykes of granosyenite and alaskite as well as aplitic granites.
ERMOLOV, P.V., VLADIMIROV, A.G. and TIKHOMIROVA, N.I. 1988. The petrology of silica oversaturated agpaitic alkaline rocks. Nauka, Novosibirsk. 86 pp.