Physicochemical conditions of the formation of the Larino granite-gneiss dome (South Ural)

Physicochemical conditions of the formation of the Larino granite-gneiss dome (South Ural)

The Larino granite-gneiss dome is located on the border of the Aramil-Sukhtelya and Magnitogorsk megazones and is a two-headed anticlinal structure, the nuclear parts of which are composed of granitoids of the Pervomai and Larino massifs, and their framing – apovolcanic amphibolites, garnet-mica-tin...

Full description

Bibliographic Details
Main Authors: Vladimir I. Snachev, Aleksandr V. Snachev, Vsevolod Yu. Prokofiev
Format: Article
Language:English
Published: Georesursy Ltd. 2022-03-01
Series:Georesursy
Subjects:
south ural
larino dome
geodynamics
petrogeochemistry
granite-gneisses
migmatites
granites
melt inclusions
garnet-amphibole thermobarometer
Online Access:https://geors.ru/archive/article/1143/

Internet

https://geors.ru/archive/article/1143/

Similar Items