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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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.

作者简介

P. Logachev

Budker Institute of Nuclear Physics, Siberian Branch; Novosibirsk State University

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

Yu. Semenov

Budker Institute of Nuclear Physics, Siberian Branch; Novosibirsk State University

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

V. Sharapov

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

编辑信件的主要联系方式.
Email: vik@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090

A. Boguslavskii

Sobolev Institute of Geology and Mineralogy, Siberian Branch

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

N. Podgornykh

Sobolev Institute of Geology and Mineralogy, Siberian Branch

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

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