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, garnetmica-tins...

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Principais autores:	V. I. Snachev, A. V. Snachev, V. Yu. Prokofiev
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Georesursy Ltd. 2024-04-01
Colecção:	Georesursy
Assuntos:	south ural larino dome geodynamics petrogeochemistry granite-gneisses migmatites granites melt inclusions garnet-amphibole thermobarometer
Acesso em linha:	https://www.geors.ru/jour/article/view/156
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