SOME ASPECTS OF THE PROBLEM OF GRANITIZATION

dc.contributor.authorZharikov V.A.
dc.date.accessioned2020-12-01T08:48:30Z
dc.date.available2020-12-01T08:48:30Z
dc.date.issued1996
dc.description.abstractThe article summarizes some of the author's conclusions and results obtained during experimental and mathematical studies of granitization. The following main points are discussed: the possibility that granitization may be caused by mantle fluids; the characteristics of fusion in the presence of a fluid; the possibility that granitoid magmas may be formed in subduction zones; the absence of a particular dehydration-melting mechanism; and the association of the europium minimum with the effect of acidified solutions.
dc.identifierhttps://elibrary.ru/item.asp?id=20957473
dc.identifier.citationVestnik Moskovskogo universiteta. Seriâ 4: Geologiâ, 1996, , 4, 3-12
dc.identifier.issn0579-9406
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/20040
dc.titleSOME ASPECTS OF THE PROBLEM OF GRANITIZATION
dc.typeСтатья

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