The chemical composition of the accessory minerals inclusions in the olivine and pyroxene phenocrysts, as an indicator of the calc-alkaline magmas evolution conditions at the Gorely volcano (Kamchatka)

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dc.contributor.author Gavrilenko M.G.
dc.contributor.author Ozerov A.Yu.
dc.date.accessioned 2019-09-03T12:51:22Z
dc.date.available 2019-09-03T12:51:22Z
dc.date.issued 2010
dc.identifier http://repo.kscnet.ru/3526/
dc.identifier http://repo.kscnet.ru/3526/1/Gavrilenko_GSA_2010.pdf
dc.identifier.citation Gavrilenko M.G, Ozerov A.Yu. (2010) The chemical composition of the accessory minerals inclusions in the olivine and pyroxene phenocrysts, as an indicator of the calc-alkaline magmas evolution conditions at the Gorely volcano (Kamchatka) // 2010 GSA Denver Annual Meeting (31 October – 3 November 2010). Geological Society of America Abstracts with Programs. Denver: GSA. No. 5. Vol. 42. pp. 626.
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/6235
dc.language.iso en
dc.publisher GSA
dc.subject 38.37.25 Вулканология
dc.subject Горелый
dc.title The chemical composition of the accessory minerals inclusions in the olivine and pyroxene phenocrysts, as an indicator of the calc-alkaline magmas evolution conditions at the Gorely volcano (Kamchatka)
dc.type Статья


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