Rayons radiés de plagioclase et olivine aligée à l'intérieur de péridotite feldspathique, Série Centrale, Île de Rum, Écosse: Évidence d'écoulement magmatique

dc.contributor.author	Labonté, Françoise
dc.date.accessioned	2013-11-07T17:25:34Z
dc.date.available	2013-11-07T17:25:34Z
dc.date.created	2004
dc.date.issued	2004
dc.degree.level	Masters
dc.degree.name	M.Sc.
dc.description.abstract	We document the occurrence of the metre-scale stellate plagiolcase and aligned olivine of the Central Serie Peridotite, Isle of Rum, Scotland, characterize them by optical mineralogy, Image analysis, Electron Microprobe (EMP), Crystal Size Distribution (CSD) and Electron Backscatter Diffraction (EBSD). Image analyses combined with crystallographic-preferred orientation (CPO) analyses demonstrate a quasi-tabular habit for olivine, characterised by a short crystallographic b-axis (&sim;a:c:b
dc.format.extent	101 p.
dc.identifier.citation	Source: Masters Abstracts International, Volume: 43-06, page: 2138.
dc.identifier.uri	http://hdl.handle.net/10393/26683
dc.identifier.uri	http://dx.doi.org/10.20381/ruor-18315
dc.language.iso	fr
dc.publisher	University of Ottawa (Canada)
dc.subject.classification	Geology.
dc.title	Rayons radiés de plagioclase et olivine aligée à l'intérieur de péridotite feldspathique, Série Centrale, Île de Rum, Écosse: Évidence d'écoulement magmatique
dc.type	Thesis

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