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 | |
Состояние | Опубликовано - 1 авг 2017 |