Fluid Inclusion Trails in Granite Quartz: Evidence for Aqueous Fluid Infiltration in the Oughterard Granite, Eastern Connemara

The results of fluid inclusion petrography and microthermometry of Oughterard Granite quartz reveals the presence of a dominant and ubiquitous population of liquid rich (degree of fill ∼ 0.70-0.95) saline (

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Bibliographic Details
Published in:Irish journal of earth sciences 2006-01, Vol.24 (1), p.1-11
Main Authors: Feely, Martin, Conliffe, James, Faure, Kevin, Power, Siobhain
Format: Article
Language:English
Subjects:
Batholiths
Earth sciences
Fluids
Geology
Granite
Inclusions
Isotopes
Mica
Oxygen isotopes
Quartz
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Description
Summary:The results of fluid inclusion petrography and microthermometry of Oughterard Granite quartz reveals the presence of a dominant and ubiquitous population of liquid rich (degree of fill ∼ 0.70-0.95) saline (
ISSN:0790-1763
2009-0064
DOI:10.3318/ijes.2006.24.1.1