| Reference Type | Journal (article/letter/editorial) |
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| Title | Low-temperature, hydrothermal garnet associated with zeolites, from basalt lavas near Beith, Ayrshire |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Livingstone, A. | Author |
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| Year | 1989 (March) | Volume | 53 |
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| Issue | 369 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_53/53-369-125.pdf+ |
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| DOI | doi:10.1180/minmag.1989.053.369.17Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 1484 | Long-form Identifier | mindat:1:5:1484:1 |
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| GUID | 0 |
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| Full Reference | Livingstone, A. (1989) Low-temperature, hydrothermal garnet associated with zeolites, from basalt lavas near Beith, Ayrshire. Mineralogical Magazine, 53 (369) 125-129 doi:10.1180/minmag.1989.053.369.17 |
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| Plain Text | Livingstone, A. (1989) Low-temperature, hydrothermal garnet associated with zeolites, from basalt lavas near Beith, Ayrshire. Mineralogical Magazine, 53 (369) 125-129 doi:10.1180/minmag.1989.053.369.17 |
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| In | (1989, March) Mineralogical Magazine Vol. 53 (369) Mineralogical Society |
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| Abstract/Notes | A Working quarry, at Loanhead (NS363557) within the Clyde Plateau Carboniferous lavas, is traversed by a tholeiitic Tertiary dyke some 25-30 m wide. Throughout the quarry the lavas are extensively altered and the most prominent secondary minerals are calcite and prehnite. Adjacent to the dyke is an indefinite alteration zone within which garnet has developed in close association with analcime and thomsonite. Contact metamorphism is not apparent. Secondary minerals in the quarried lavas and from the alteration zone have been described by Meikle (1989). The most salient feature of secondary mineral formation central to this paper is that grossular and andradite occur, in situ, in close proximity to the dyke, and only in the amygdales. |
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