THE WATER AND CARBON DIOXIDE REGIME DURING THE CHARNOCKITIZATION OF GRANULITE COMPLEXES

dc.contributor.author	Perchuk L.L.
dc.contributor.author	Gerya T.V.
dc.date.accessioned	2020-12-01T08:37:40Z
dc.date.available	2020-12-01T08:37:40Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=20957078
dc.identifier.citation	Vestnik Moskovskogo universiteta. Seriâ 4: Geologiâ, 1996, , 4, 36-48
dc.identifier.issn	0579-9406
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20017
dc.description.abstract	Research was carried out into the water and carbon dioxide regime during the charnockitization of gneissic complexes. It was shown that CO2 plays a considerable role in the dehydration of metapelites and biotite-bearing gneisses with the formation of parageneses typical of enderbites and charnockites. The activity of H2O during the charnockitization of metapelites and gneisses does not always decrease, but even increases in a number of cases. Besides the H2O and CO2 regimes, the chemical potentials of fully mobile alkalis also play a significant role in the charnockitization of gneissic complexes.
dc.title	THE WATER AND CARBON DIOXIDE REGIME DURING THE CHARNOCKITIZATION OF GRANULITE COMPLEXES
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.