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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

by chemical inhomogeneity (inherited schlieren features with poorer and richer regions in Ca and Fe) within a μm spatial scale, because of the lack of time for mechanical mixing and homogenization ( Langenhorst and Poiriere 2000 ). Dingwell and Webb

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