FORMATION OF DIKES AND SILLS UNDER KLYUCHEVSKOI VOLCANO BY MAGMA INTRUSION THROUGH THE CONDUIT

dc.contributor.author	Efimov A.B.
dc.contributor.author	Ershova T.Ya.
dc.contributor.author	Fedotov S.A.
dc.date.accessioned	2020-12-01T08:48:30Z
dc.date.available	2020-12-01T08:48:30Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=20957482
dc.identifier.citation	Volcanology & Seismology, 1996, , 1, 1-23
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20044
dc.description.abstract	The problem of magma intrusion through conduit walls is examined using the example of Klyuchevskoi Volcano. Magma intrusion takes place at all depths; the initial break through the wallrocks occurs mainly as a vertical dike. The properties and behavior of the dike-invaded viscoelastic wallrocks are discussed.
dc.title	FORMATION OF DIKES AND SILLS UNDER KLYUCHEVSKOI VOLCANO BY MAGMA INTRUSION THROUGH THE CONDUIT
dc.type	Статья

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