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dc.contributor.author Cooper, Mark Alan en_US
dc.date.accessioned 2007-05-15T15:15:30Z
dc.date.available 2007-05-15T15:15:30Z
dc.date.issued 1997-05-01T00:00:00Z en_US
dc.identifier.uri http://hdl.handle.net/1993/742
dc.description.abstract Kornerupine is an accessory sorosilicate mineral found in high-grade metamorphic rocks. It has the general formula ($\square,$ Mg, Fe) (Al, Mg, Fe)$\sb9$ (Si, Al, B)$\sb5$ O$\sb{21}$ (OH,F). Previous studies have been unable to arrive at accurate structural formulae and corresponding detailed crystal-chemical relations. Forty seven ferrous-iron kornerupines $\rm(Fe\sp{3+}/Fe\sp{2+}\le0.5)$ from $\sim$35 localities were examined using SREF, EMPA, SIMS and H-extraction line techniques to acquire complete crystallographic and chemical data. EMP data was processed using an anion-normalization scheme whereby cations are scaled to O$\sb{21}$ (OH + F)$\sb1\ pfu,$ which is supported by bond-valence arguments and H values from H-extraction line analysis. B and Fe$\sp{3+}$ quantities were developed via site-occupancy refinement at the T(3) and M(4) sites, respectively. Excellent agreement was attained between B values arrived at by SIMS and SREF methods. Site populations for the three tetrahedra, five octahedra and single eight-coordinate site were developed using standard crystal-chemical criteria. (Abstract shortened by UMI.) en_US
dc.format.extent 19533602 bytes
dc.format.extent 184 bytes
dc.format.mimetype application/pdf
dc.format.mimetype text/plain
dc.language en en_US
dc.language.iso en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title The crystal chemistry of kornerupine en_US
dc.type info:eu-repo/semantics/masterThesis
dc.type master thesis en_US
dc.degree.discipline Geological Sciences en_US
dc.degree.level Master of Science (M.Sc.) en_US


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