Some Structural and Mineralogical Peculiarities of Quenching Liquids Obtained by Melting of Mantle Ultrabasite Xenoliths and Mafic Volcanics by an Electron Beam

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.

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Veröffentlicht in:Doklady earth sciences 2018-08, Vol.481 (2), p.1095-1098
Hauptverfasser: Logachev, P. V., Semenov, Yu. I., Sharapov, V. N., Boguslavskii, A. E., Podgornykh, N. M.
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container_end_page 1098
container_issue 2
container_start_page 1095
container_title Doklady earth sciences
container_volume 481
creator Logachev, P. V.
Semenov, Yu. I.
Sharapov, V. N.
Boguslavskii, A. E.
Podgornykh, N. M.
description 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.
doi_str_mv 10.1134/S1028334X18080317
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1531-8354
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source SpringerNature Journals
subjects Earth
Earth and Environmental Science
Earth Sciences
Electron beams
Evaporation
Geochemistry
Liquids
Melting
Meteorites
Phase transitions
Physics
Stony meteorites
Xenoliths
title Some Structural and Mineralogical Peculiarities of Quenching Liquids Obtained by Melting of Mantle Ultrabasite Xenoliths and Mafic Volcanics by an Electron Beam
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