THERMODYNAMICS AROUND A MAGMA CONDUIT

dc.contributor.author	Efimov A.B.
dc.contributor.author	Ershova T.Y.
dc.date.accessioned	2021-01-14T07:54:06Z
dc.date.available	2021-01-14T07:54:06Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=20939921
dc.identifier.citation	Volcanology & Seismology, 1999, 20, 4, 479-495
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22940
dc.description.abstract	This paper deals with the process of the development of a viscoplastic envelope around a magma conduit and an accompanying hydrothermal system. It is estimated that the discharge of hot water at the surface (possibly as steam) may be as high as hundreds of cubic meters per day. According to the model presented here, the formation of the viscoplastic envelope is related to periodic magma injections facilitated by a significantly nonstationary thermal regime.
dc.title	THERMODYNAMICS AROUND A MAGMA CONDUIT
dc.type	Статья

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