Abstract
The Galway granite in the west of Ireland contains a significant concentration of Mo-Cu at Mace Head in the centre of its westernmost Carna dome. Fluid inclusion studies of the granite, the quartz veins and of a K-feldspar breccia cutting the granite indicate the presence of three aqueous fluid inclusion types. Type 1, the predominant type, are mainly NaCl bearing, type 2 are CO2 bearing and type 3 contain a solid phase. The type 1 inclusions at Mace Head are typical of those found in the peripheral zones of porphyry deposits and in sheeted vein W, Sn and Mo deposits. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1-10 |
| Number of pages | 10 |
| Journal | Irish Journal of Earth Sciences |
| Volume | 11 |
| Issue number | 1 |
| Publication status | Published - 1991 |
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