The formation of impact coesite

Abstract Coesite in impact rocks is traditionally considered a retrograde product formed during pressure release by the crystallisation of an amorphous phase (either silica melt or diaplectic glass). Recently, the detailed microscopic and crystallographic study of impact ejecta from Kamil crater and...

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Autores principales: F. Campanale, E. Mugnaioli, M. Gemmi, L. Folco
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/cdf0e856fae14f29bc69ebf991c0722a
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