Yüklüyor......
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...
Kaydedildi:
| Yayımlandı: | Nat Commun |
|---|---|
| Asıl Yazarlar: | , , , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Publishing Group UK
2018
|
| Konular: | |
| Online Erişim: | 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 |
| Etiketler: |
Etiketle
Etiket eklenmemiş, İlk siz ekleyin!
|