THE INTERACTION BETWEEN WATER AND ALUMINOSILICATE MAGMAS

dc.contributor.author	Kohn S.C.
dc.contributor.author	Dupree R.
dc.contributor.author	Mortuza M.G.
dc.date.accessioned	2020-11-09T02:14:15Z
dc.date.available	2020-11-09T02:14:15Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=31562328
dc.identifier.citation	Chemical Geology, 1992, , 3, 399-409
dc.identifier.issn	0009-2541
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18695
dc.description.abstract	29Si, 27Al and 23Na NMR data are presented for a variety of dry and dydrous aluminosilicate glasses. For 29Si and 27Al spectra only minor differences were observed between dry and hydrous glasses, but significant changes were observed in 23Na spectra. As found in our earlier study of hydrous albite glasses, the data are consistent with a model for the mechanism of water dissolution which involves no breakage of T-O-T linkages. Viscosity, phase equilibrium and vibrational spectroscopic data from other studies are discussed and shown to be consistent with such a model.
dc.title	THE INTERACTION BETWEEN WATER AND ALUMINOSILICATE MAGMAS
dc.type	Статья

Files in this item

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