Инд. авторы: Tomilenko A.A., Kuzmin D.V., Bul’bak T.A, Sobolev N.V.
Заглавие: 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
Библ. ссылка: Tomilenko A.A., Kuzmin D.V., Bul’bak T.A, Sobolev N.V. 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. - 2017. - Vol.475. - Iss. 2. - P.949-952. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы: РИНЦ: 31065570; DOI: 10.1134/S1028334X17080281; SCOPUS: 2-s2.0-85028747236; WoS: 000408900300025;
Реферат: eng: 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. © 2017, Pleiades Publishing, Ltd.
Ключевые слова: Olivine; Minerals; Mineralogy; Mass spectrometry; Udachnaya Pipe; Sakha; Russian Federation; silicate melt; phenocryst; olivine; Silicate minerals; fluid inclusion; carbonate rock; Crystals; Yakutia; Olivine crystals; Microthermometry; Ion microprobe analysis; Fluid inclusion; Carbonate melts; Volcanic rocks; Silicates; kimberlite; Scanning electron microscopy;
Издано: 2017
Физ. характеристика: с.949-952