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Appinites, diatremes and granodiorites: the interaction of ‘wet’ basalt with granite

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The Nature and Origin of Granite
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Abstract

Of all the examples of the association of basic rocks with granites, that of the appinite suite is one of the most revealing in respect to the multifactorial processes at work in igneous rock petrogenesis. The essential coherence of this close-knit rock suite was first recognized in 1916 by Bailey and Maufe in the district of Appin, Argyll, where, as elsewhere in the Scottish and Irish Caledonides, such rocks are intimately associated in time and place with the Late Caledonian plutons.

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Selected References

  • Ayrton, S. (1991) Appinites, lamprophyres and mafic magmatic enclaves: Three related products of the interaction between acid and mafic magmas. In: Didier, J. and Barbarin, B. (eds), Enclaves and Granite Petrology. Elsevier, Amsterdam, pp. 465–476.

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  • Hamidullah, S. and Bowes, D.R. (1987) Petrogenesis of the Appinite Suite, Appin District, Western Scotland. Acta Universitatis Carolinae-Geologica, 4, 295–396.

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  • Sabatier, H. (1980) Vaugnérites et granites: une association particuliére de roches grenues acides et basiques. Bulletin de Mineralogie, 103, 507–522.

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© 1997 Springer Science+Business Media Dordrecht

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Pitcher, W.S. (1997). Appinites, diatremes and granodiorites: the interaction of ‘wet’ basalt with granite. In: The Nature and Origin of Granite. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5832-9_10

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  • DOI: https://doi.org/10.1007/978-94-011-5832-9_10

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-6464-4

  • Online ISBN: 978-94-011-5832-9

  • eBook Packages: Springer Book Archive

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