Monomineralic anorthosites in layered intrusions are indicators of the magma chamber replenishment by plagioclase-only-saturated melts

The formation of some Earth’s monomineralic igneous rocks appears to be prohibited by constraints imposed by liquidus phase-equilibria on evolution of mantle-derived magmas. Yet, these rocks exist as stratiform layers in many mafic-ultramafic intrusions. One conspicuous example is monomineralic anor...

Descripción completa

Detalles Bibliográficos
Autores principales: Latypov, Rais, Chistyakova, Sofya, Costin, Gelu, Namur, Olivier, Barnes, Steve, Kruger, Willem
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7052229/
https://www.ncbi.nlm.nih.gov/pubmed/32123247
http://dx.doi.org/10.1038/s41598-020-60778-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7052229/
https://www.ncbi.nlm.nih.gov/pubmed/32123247
http://dx.doi.org/10.1038/s41598-020-60778-w

Ejemplares similares