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: DOI: 10.1134/S1028334X17080281; РИНЦ: 31065570; 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: Volcanic rocks; Carbonate melts; Fluid inclusion; Ion microprobe analysis; Microthermometry; Olivine crystals; Yakutia; Crystals; carbonate rock; fluid inclusion; kimberlite; olivine; phenocryst; silicate melt; Russian Federation; Sakha; Udachnaya Pipe; Silicate minerals; Scanning electron microscopy; Olivine; Minerals; Mineralogy; Mass spectrometry; Silicates;
Издано: 2017
Физ. характеристика: с.949-952