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Analysis of shock metamorphic processes in the Zagami meteorite

Central European Geology
Volume/Issue:
Volume 62: Issue 1
DOI:
https://doi.org/10.1556/24.61.2018.12
Authors:
Ildikó Gyollai
,
Ákos Kereszturi
, and
Elias Chatzitheodoridis

-related alteration, that is, whether pseudotachylite-like impact melting occurred along earlier fractures [supported by the coexistence of maskelynite (a diaplectic feldspar glass) and the silica glass], or fractional melting of the Martian crust (supported by the

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