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Fluid inclusions of quartz-carbonate veins in the Canadian Rocky Mountains

dc.contributor.advisorEnggist, Andreas
dc.contributor.authorLaRiviere, Sarah
dc.date.accessioned2015-06-29
dc.date.accessioned2022-05-27T01:14:14Z
dc.date.available2022-05-27T01:14:14Z
dc.date.issued2015
dc.descriptionPresented on May 1, 2015 at the Undergraduate Research in Science Conference of Alberta (URSCA) held at MacEwan University in Edmonton, Alberta.
dc.description.abstractVein systems in crustal rocks record a variety of processes, including fluid migration and extensive mass transfer, and they preserve information about the composition, temperature, and pressure conditions that mitigate rock-fluid interaction during vein formation. This study will attempt to characterize the formational sequence and origin of fluid inclusions observed in several samples extracted from a quartz-carbonate vein system in the Canadian Rocky Mountains, and explore the role of fluid-rock interaction in the formation of these veins. Preliminary observations of thin sections taken from vein samples are detailed conjointly with petrographic images and a brief review of the formation and significance of fluid inclusions in rock-hosted vein systems.
dc.format.extent339 kb
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/378
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.subjectfluid inclusions
dc.subjectquartz-carbonate veins
dc.subjectCanadian Rocky Mountains
dc.titleFluid inclusions of quartz-carbonate veins in the Canadian Rocky Mountainsen
dc.typeStudent Presentation
dspace.entity.type

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