Email this article Some Structural and Mineralogical Peculiarities of Quenching Liquids Obtained by Melting of Mantle Ultrabasite Xenoliths and Mafic Volcanics by an Electron Beam
- Authors: Logachev P.V.1,2, Semenov Y.I.1,2, Sharapov V.N.2,3, Boguslavskii A.E.3, Podgornykh N.M.3
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Affiliations:
- Budker Institute of Nuclear Physics, Siberian Branch
- Novosibirsk State University
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- Issue: Vol 481, No 2 (2018)
- Pages: 1095-1098
- Section: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/193924
- DOI: https://doi.org/10.1134/S1028334X18080317
- ID: 193924
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Abstract
The experimental results presented below shine a light upon the physics of phase transition processes during melting, intensive evaporation, and subsequent explosive destruction of stony meteorites entering the Earth’s atmosphere.
About the authors
P. V. Logachev
Budker Institute of Nuclear Physics, Siberian Branch; Novosibirsk State University
Email: vik@igm.nsc.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090
Yu. I. Semenov
Budker Institute of Nuclear Physics, Siberian Branch; Novosibirsk State University
Email: vik@igm.nsc.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090
V. N. Sharapov
Novosibirsk State University; Sobolev Institute of Geology and Mineralogy, Siberian Branch
Author for correspondence.
Email: vik@igm.nsc.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090
A. E. Boguslavskii
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: vik@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
N. M. Podgornykh
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: vik@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
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