Enviar artigo por via de e-mail 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
- Autores: Tomilenko A.1, Kuzmin D.1,2, Bul’bak T.1, Sobolev N.1,2
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Afiliações:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- Novosibirsk State University
- Edição: Volume 475, Nº 2 (2017)
- Páginas: 949-952
- Seção: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/190592
- DOI: https://doi.org/10.1134/S1028334X17080281
- ID: 190592
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Resumo
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.
Sobre autores
A. Tomilenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Autor responsável pela correspondência
Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090
D. Kuzmin
Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University
Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090; Novosibirsk
T. Bul’bak
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090
N. Sobolev
Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University
Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090; Novosibirsk
