Crystal settling and convection in the Shiant Isles Main Sill

The 168 m-thick Shiant Isles Main Sill is a composite body, dominated by an early, 24 m-thick, picrite sill formed by the intrusion of a highly olivine-phyric magma, and a later 135 m-thick intrusion of olivine-phyric magma that split the earlier picrite into a 22 m-thick lower part and a 2 m-thick...

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Detalles Bibliográficos
Autores principales: Holness, Marian B., Farr, Robert, Neufeld, Jerome A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2017
Materias:
Original Paper
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7115068/
https://www.ncbi.nlm.nih.gov/pubmed/32269384
http://dx.doi.org/10.1007/s00410-016-1325-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7115068/
https://www.ncbi.nlm.nih.gov/pubmed/32269384
http://dx.doi.org/10.1007/s00410-016-1325-x

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