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Henderson, C. M. B., Gibb, F. G. F., Foland, K. A. (2000) Mineral fractionation and pre- and post-emplacement processes in the uppermost part of the Shiant Isles Main Sill. Mineralogical Magazine, 64 (5) 779-790 doi:10.1180/002646100549706

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Reference TypeJournal (article/letter/editorial)
TitleMineral fractionation and pre- and post-emplacement processes in the uppermost part of the Shiant Isles Main Sill
JournalMineralogical Magazine
AuthorsHenderson, C. M. B.Author
Gibb, F. G. F.Author
Foland, K. A.Author
Year2000 (October)Volume64
Issue5
PublisherMineralogical Society
DOIdoi:10.1180/002646100549706Search in ResearchGate
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Mindat Ref. ID243204Long-form Identifiermindat:1:5:243204:9
GUID0
Full ReferenceHenderson, C. M. B., Gibb, F. G. F., Foland, K. A. (2000) Mineral fractionation and pre- and post-emplacement processes in the uppermost part of the Shiant Isles Main Sill. Mineralogical Magazine, 64 (5) 779-790 doi:10.1180/002646100549706
Plain TextHenderson, C. M. B., Gibb, F. G. F., Foland, K. A. (2000) Mineral fractionation and pre- and post-emplacement processes in the uppermost part of the Shiant Isles Main Sill. Mineralogical Magazine, 64 (5) 779-790 doi:10.1180/002646100549706
Abstract/NotesAbstractReinvestigation of the top 25 m of the 165 m thick Shiant Isles Main Sill requires reinterpretation of its internal structure, especially of the last unit emplaced – the granular olivine picro-dolerite. New mineral analyses allow re-assessment of the magmatic processes involved in the intrusion and differentiation of this classic multiple sill. C-shaped vertical mineral composition profiles, which occur in olivine-rich, alkaline basaltic sills, reflect reaction between phenocrysts and variable composition liquids. A case is made for vertical migration of interstitial liquids within and across the boundaries of intrusive units, for the mixing of such liquids from adjacent units, and for their influence on mineral chemistry on both sides of the interface.


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