The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts

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dc.contributor.author Gavrilenko M.
dc.contributor.author Ozerov A.
dc.date.accessioned 2019-09-03T12:51:24Z
dc.date.available 2019-09-03T12:51:24Z
dc.date.issued 2014
dc.identifier http://repo.kscnet.ru/3541/
dc.identifier http://repo.kscnet.ru/3541/1/Gavrilenko-2014-AGU.pdf
dc.identifier.citation Gavrilenko M., Ozerov A. (2014) The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts // Abstract V51A-4726 presented at 2014 Fall Meeting, AGU, San Francisco, Calif., 15-19 Dec..
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/6251
dc.language.iso en
dc.subject 38.37.25 Вулканология
dc.subject Ключевской
dc.title The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts
dc.type Конференционный материал


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