To be or not to be oxidized: A case study of olivine behavior in the fusion crust of ureilite A 09368 and H chondrites A 09004 and A 09502

Meteorite fusion crusts are quenched melt layers formed during meteoroid atmospheric entry, mostly preserved as coating on the meteorite surface. Antarctic ureilite Asuka (A) 09368 and H chondrites A 09004 and A 09502 exhibit well preserved thick fusion crusts, characterized by extensive olivine cry...

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Detalles Bibliográficos
Autores principales: Pittarello, Lidia, Yamaguchi, Akira, Roszjar, Julia, Debaille, Vinciane, Koeberl, Christian, Claeys, Philippe
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6686723/
https://www.ncbi.nlm.nih.gov/pubmed/31423075
http://dx.doi.org/10.1111/maps.13284

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6686723/
https://www.ncbi.nlm.nih.gov/pubmed/31423075
http://dx.doi.org/10.1111/maps.13284

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