Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)

Yu R. Vasil’ev; M. P. Gora; D. V. Kuzmin

doi:10.1134/S1028334X18010282

Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)

Yu R. Vasil’ev, M. P. Gora, D. V. Kuzmin

Лаборатория корреляции геологических процессов ГГФ

Результат исследования: Научные публикации в периодических изданиях › статья

Аннотация

For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.

Язык оригинала	английский
Страницы (с-по)	103-107
Число страниц	5
Журнал	Doklady Earth Sciences
Том	478
Номер выпуска	1
DOI	https://doi.org/10.1134/S1028334X18010282
Состояние	Опубликовано - 1 янв 2018

Доступ к документу

10.1134/S1028334X18010282

Link to publication in Scopus

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Цитировать

Vasil’ev, Y. R., Gora, M. P., & Kuzmin, D. V. (2018). Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). Doklady Earth Sciences, 478(1), 103-107. https://doi.org/10.1134/S1028334X18010282

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