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

Logachev P. V.; Semenov Yu. I.; Sharapov V. N.; Boguslavskii A. E.; Podgornykh N. M.

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

机译：电子束熔化地幔超Basite异种岩和铁镁质火山岩获得的淬火液的一些结构和矿物学特性

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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.

机译：下面给出的实验结果阐明了熔融，强烈蒸发以及随后进入地球大气层的石陨石的爆炸性破坏期间的相变过程的物理原理。

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《Doklady Earth Sciences》 |2018年第2期|1095-1098|共4页
作者
Logachev P. V.; Semenov Yu. I.; Sharapov V. N.; Boguslavskii A. E.; Podgornykh N. M.;
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Russian Acad Sci, Siberian Branch, Budker Inst Nucl Phys, Novosibirsk 630090, Russia;

Russian Acad Sci, Siberian Branch, Budker Inst Nucl Phys, Novosibirsk 630090, Russia;

Novosibirsk State Univ, Novosibirsk 630090, Russia;

Russian Acad Sci, Siberian Branch, Sobolev Inst Geol & Mineral, Novosibirsk 630090, Russia;

Russian Acad Sci, Siberian Branch, Sobolev Inst Geol & Mineral, Novosibirsk 630090, Russia;

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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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