USE OF TRITIUM TO INVESTIGATE THE DYNAMICS OF MELTING OF WATER-SATURATED BASALT

dc.contributor.author	Mironov A.G.
dc.contributor.author	Konnikov E.G.
dc.contributor.author	Epel'baum M.B.
dc.date.accessioned	2020-10-11T11:10:11Z
dc.date.available	2020-10-11T11:10:11Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31155908
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 6, 140-143
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17935
dc.description.abstract	In order to understand the role of volatiles in the phase transition from crystal to melt, it is very important to know not only the total concentration of fluid in the system, but also its distribution. The authors performed a series of experiments involving the partial melting of water-containing basalt, in which radioactive tritium had been added to the fluid as a tracer. Autoradiographic study of the products provided a revealing distribution of the fluid phase within the molten basalt and revealed interesting, previously unknown properties of that distribution.
dc.title	USE OF TRITIUM TO INVESTIGATE THE DYNAMICS OF MELTING OF WATER-SATURATED BASALT
dc.type	Статья

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