Composition Heterogeneity of Xenoliths of Mantle Peridotites from Alkaline Basalts of the Sverre Volcano, the Svalbard Archipelago

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dc.contributor.author Ashikhmin Dmitriy S.
dc.contributor.author Skublov Sergey G.
dc.date.accessioned 2020-01-24T08:27:06Z
dc.date.available 2020-01-24T08:27:06Z
dc.date.issued 2019
dc.identifier https://cyberleninka.ru/article/n/composition-heterogeneity-of-xenoliths-of-mantle-peridotites-from-alkaline-basalts-of-the-sverre-volcano-the-svalbard-archipelago
dc.identifier Федеральное государственное бюджетное образовательное учреждение высшего образования «Санкт-Петербургский горный университет»
dc.identifier.citation Записки Горного института, 2019, 239 (англ.),
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/14858
dc.description.abstract The article presents the results of a study of the composition of xenoliths of mantle peridotites (seven samples), collected from the Quaternary basalts of the Sverre volcano, the Svalbard archipelago. The presence of two big (more than 15 cm in diameter) xenoliths of spinel lherzolite allowed us to consider a change in their composition in the central, intermediate, and marginal parts of the samples. It is proposed to distinguish three types of xenoliths by the distribution of trace and rare earth elements. Enrichment of mantle peridotites with light rare earth elements, as well as high field strength (HFS) and large-ion lithophile (LIL) elements, is presumably associated with mantle metasomatism.
dc.publisher Федеральное государственное бюджетное образовательное учреждение высшего образования «Санкт-Петербургский горный университет»
dc.subject mantle xenoliths
dc.subject mantle metasomatism
dc.subject peridotite
dc.subject trace elements
dc.subject rare earth elements
dc.subject Svalbard
dc.title Composition Heterogeneity of Xenoliths of Mantle Peridotites from Alkaline Basalts of the Sverre Volcano, the Svalbard Archipelago
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dc.type Article


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