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Martian magmatism from plume metasomatized mantle
Direct analysis of the composition of Mars is possible through delivery of meteorites to Earth. Martian meteorites include ∼165 to 2400 Ma shergottites, originating from depleted to enriched mantle sources, and ∼1340 Ma nakhlites and chassignites, formed by low degree partial melting of a depleted m...
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| Pubblicato in: | Nat Commun |
|---|---|
| Autori principali: | , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2018
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6237973/ https://ncbi.nlm.nih.gov/pubmed/30442916 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07191-0 |
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