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

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

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.

Original languageEnglish
Pages (from-to)949-952
Number of pages4
JournalDoklady Earth Sciences
Volume475
Issue number2
DOIs
Publication statusPublished - 1 Aug 2017

Keywords

  • CHROMATOGRAPHY-MASS SPECTROMETRY
  • HYPABYSSAL KIMBERLITES
  • VOLATILE COMPONENTS
  • RUSSIA
  • AGES

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