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


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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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A. Tomilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

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Email: tomilen@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

D. Kuzmin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: tomilen@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

T. Bul’bak

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

N. Sobolev

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: tomilen@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

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