Microstructural evidence for crystallization regimes in mafic intrusions: a case study from the Little Minch Sill Complex, Scotland

The magma forming the 20 m thick crinanitic/picrodoleritic Dun Raisburgh sill, part of the Little Minch Sill Complex of NW Scotland, comprised a mafic carrier liquid with a crystal cargo of plagioclase and olivine (1 vol%). The olivine component of the cargo settled on the floor of the intrusion whi...

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Detalles Bibliográficos
Autores principales: Nicoli, Gautier, Holness, Marian, Neufeld, Jerome, Farr, Robert
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2018
Materias:
Original Paper
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6404684/
https://www.ncbi.nlm.nih.gov/pubmed/30930465
http://dx.doi.org/10.1007/s00410-018-1525-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6404684/
https://www.ncbi.nlm.nih.gov/pubmed/30930465
http://dx.doi.org/10.1007/s00410-018-1525-7

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