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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...
Autores principales: | Holness, Marian B., Farr, Robert, Neufeld, Jerome A. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Berlin Heidelberg
2017
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Materias: | |
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 |
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