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.
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Original Russian Text © A.A. Tomilenko, D.V. Kuzmin, T.A. Bul’bak, N.V. Sobolev, 2017, published in Doklady Akademii Nauk, 2017, Vol. 475, No. 6, pp. 680–684.
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Tomilenko, A.A., Kuzmin, D.V., Bul’bak, T.A. et al. 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. Dokl. Earth Sc. 475, 949–952 (2017). https://doi.org/10.1134/S1028334X17080281
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DOI: https://doi.org/10.1134/S1028334X17080281