Kimberlite genesis from a common carbonate-rich primary melt modified by lithospheric mantle assimilation

Quantifying the compositional evolution of mantle-derived melts from source to surface is fundamental for constraining the nature of primary melts and deep Earth composition. Despite abundant evidence for interaction between carbonate-rich melts, including diamondiferous kimberlites, and mantle wall...

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Detalles Bibliográficos
Autores principales: Giuliani, Andrea, Pearson, D. Graham, Soltys, Ashton, Dalton, Hayden, Phillips, David, Foley, Stephen F., Lim, Emilie, Goemann, Karsten, Griffin, William L., Mitchell, Roger H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2020
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7182416/
https://www.ncbi.nlm.nih.gov/pubmed/32494633
http://dx.doi.org/10.1126/sciadv.aaz0424

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7182416/
https://www.ncbi.nlm.nih.gov/pubmed/32494633
http://dx.doi.org/10.1126/sciadv.aaz0424

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