Geochronology of an Apollo 16 Clast Provides Evidence for a Basin‐Forming Impact 4.3 Billion Years Ago

We examined lithic breccias from the Apollo sample collection in order to identify ferroan anorthosite samples suitable for geochronology, and better define the age relationships between rocks of the lunar highlands. Clast 3A is a previously unstudied noritic anorthosite from Apollo 16 lithic brecci...

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Detalles Bibliográficos
Autores principales: Marks, N. E., Borg, L. E., Shearer, C. K., Cassata, W. S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919926/
https://www.ncbi.nlm.nih.gov/pubmed/31894195
http://dx.doi.org/10.1029/2019JE005966

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919926/
https://www.ncbi.nlm.nih.gov/pubmed/31894195
http://dx.doi.org/10.1029/2019JE005966

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