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 изданияхстатья

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 оригиналаанглийский
Страницы (с-по)949-952
Число страниц4
ЖурналDoklady Earth Sciences
Том475
Номер выпуска2
DOI
СостояниеОпубликовано - 1 авг 2017

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