Condensate glasses from the Zhamanshin crater. I. Irghizites


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The presence of condensate glass was established for the first time in natural terrestrial impact glasses. Its existence was previously predicted on the basis of shock evaporation experiments. Condensate glass was found in the irghizites of the Zhamanshin crater. Its characteristic features were described, including a combination of high silica content with the presence of nanoscale crystalline nuclei and typical globular morphology under TEM.

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T. Gornostaeva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)

Email: avm8okhov@gmail.com
俄罗斯联邦, Staromonetnyi per. 35, Moscow, 119017

A. Mokhov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)

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Email: avm8okhov@gmail.com
俄罗斯联邦, Staromonetnyi per. 35, Moscow, 119017

P. Kartashov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)

Email: avm8okhov@gmail.com
俄罗斯联邦, Staromonetnyi per. 35, Moscow, 119017

O. Bogatikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)

Email: avm8okhov@gmail.com
俄罗斯联邦, Staromonetnyi per. 35, Moscow, 119017

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