A changing thermal regime revealed from shallow to deep basalt source melting in the Moon

Sample return missions have provided the basis for understanding the thermochemical evolution of the Moon. Mare basalt sources are likely to have originated from partial melting of lunar magma ocean cumulates after solidification from an initially molten state. Some of the Apollo mare basalts show e...

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Detalles Bibliográficos
Autores principales: Srivastava, Yash, Basu Sarbadhikari, Amit, Day, James M. D., Yamaguchi, Akira, Takenouchi, Atsushi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9734159/
https://www.ncbi.nlm.nih.gov/pubmed/36494367
http://dx.doi.org/10.1038/s41467-022-35260-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9734159/
https://www.ncbi.nlm.nih.gov/pubmed/36494367
http://dx.doi.org/10.1038/s41467-022-35260-y

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