Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt

A. A. Tomilenko; D. V. Kuzmin; T. A. Bul’bak; N. V. Sobolev

doi:10.1134/S1028334X17080281

Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt

A. A. Tomilenko, D. V. Kuzmin, T. A. Bul’bak, N. V. Sobolev

Результат исследования: Научные публикации в периодических изданиях › статья

3 Цитирования (Scopus)

Аннотация

The primary melt and fluid inclusions in regenerated zonal crystals of olivine and homogeneous phenocrysts of olivine from kimberlites of the Udachnaya-East pipe, were first studied by means of microthermometry, optic and scanning electron microscopy, electron and ion microprobe analysis (SIMS), inductively coupled plasma mass-spectrometry (ICP MSC), and Raman spectroscopy. It was established that olivine crystals were regenerated from silicate–carbonate melts at a temperature of ~1100°C.

Язык оригинала	английский
Страницы (с-по)	949-952
Число страниц	4
Журнал	Doklady Earth Sciences
Том	475
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X17080281
Состояние	Опубликовано - 1 авг 2017

Доступ к документу

10.1134/S1028334X17080281

Link to publication in Scopus

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Цитировать

Tomilenko, A. A., Kuzmin, D. V., Bul’bak, T. A., & Sobolev, N. V. (2017). Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt. Doklady Earth Sciences, 475(2), 949-952. https://doi.org/10.1134/S1028334X17080281

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title = "Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt",

abstract = "The primary melt and fluid inclusions in regenerated zonal crystals of olivine and homogeneous phenocrysts of olivine from kimberlites of the Udachnaya-East pipe, were first studied by means of microthermometry, optic and scanning electron microscopy, electron and ion microprobe analysis (SIMS), inductively coupled plasma mass-spectrometry (ICP MSC), and Raman spectroscopy. It was established that olivine crystals were regenerated from silicate–carbonate melts at a temperature of ~1100°C.",

keywords = "CHROMATOGRAPHY-MASS SPECTROMETRY, HYPABYSSAL KIMBERLITES, VOLATILE COMPONENTS, RUSSIA, AGES",

author = "Tomilenko, {A. A.} and Kuzmin, {D. V.} and Bul{\textquoteright}bak, {T. A.} and Sobolev, {N. V.}",

year = "2017",

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doi = "10.1134/S1028334X17080281",

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Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia : The problem of the kimberlite melt. / Tomilenko, A. A.; Kuzmin, D. V.; Bul’bak, T. A.; Sobolev, N. V.

В: Doklady Earth Sciences, Том 475, № 2, 01.08.2017, стр. 949-952.

Результат исследования: Научные публикации в периодических изданиях › статья

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T2 - The problem of the kimberlite melt

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KW - HYPABYSSAL KIMBERLITES

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