Re–Os geochronology and fluid inclusion microthermometry of molybdenite mineralisation in the late-Caledonian Omey Granite, western Ireland

By Feely M.   Selby D.   Conliffe J.   Judge M.  

Applied Earth Science, Vol. 116, Iss. 3, 2007-09 ,pp. : 143-149

Maney Publishing

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Widespread secondary andradite-grossular-hydrogrossular garnet, epidote, prehnite and titanite occur throughout the Galway Granite and its satellite plutons (Roundstone; Inish; Omey and Letterfrack) and even in some of the country rocks several kilometres from the granites. These minerals are not found in low CaO (<1%) granites. They formed as result of secondary fluid movements which altered the biotite, plagioclase and hornblende and also produced sericite and chlorite.

By Leake Bernard E.  

Mineralogical Magazine, Vol. 62, Iss. 3, 1998-06 ,pp. : 381-386

Mineralogical Society

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Silicate–carbonate liquid immiscibility and crystallization of carbonate and K-rich basaltic magma: insights from melt and fluid inclusions

By Solovova I. P.   Girnis A. V.  

Mineralogical Magazine, Vol. 76, Iss. 2, 2012-04 ,pp. : 411-439

Mineralogical Society

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Disequilibrium textures in the Leinster Granite Complex, SE Ireland: evidence for acid-acid magma mixing

By Grogan S. E.   Reavy R. J.  

Mineralogical Magazine, Vol. 66, Iss. 6, 2002-12 ,pp. : 929-939

Mineralogical Society

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Petrogenesis of plagioclase phenocrysts of Mount Etna, Sicily, with particular reference to the 1983 eruption: contribution from cathodoluminescence petrography

By Stirling D.   Duncan A.M.   Guest J.E.   Finch A.A.  

Mineralogical Magazine, Vol. 63, Iss. 2, 1999-04 ,pp. : 189-189

Mineralogical Society

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