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Maharaj, Deepti (2015) Chemical Classifcation of Gem Garnets. MSc, GLY 890 Dissertation, University of Pretoria.

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Reference TypeThesis/Dissertation
TitleChemical Classifcation of Gem Garnets - MSc, GLY 890 Dissertation
AuthorsMaharaj, DeeptiAuthor
Year2015 (November)
PublisherUniversity of Pretoria
URL
Download URLhttps://repository.up.ac.za/bitstream/2263/51329/4/Maharaj_Chemical_2016.pdf
Original EntryDeepti Maharaj, Department of Geology, University of Pretoria, South Africa | Chemical classification of gem garnets | 29183376, GLY 890 Dissertation, November 2015, pp. 40-44
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Mindat Ref. ID16311250Long-form Identifiermindat:1:5:16311250:7
GUIDf5a672f8-de79-487b-b652-14e5b1cadabc
Full ReferenceMaharaj, Deepti (2015) Chemical Classifcation of Gem Garnets. MSc, GLY 890 Dissertation, University of Pretoria.
Plain TextMaharaj, Deepti (2015) Chemical Classifcation of Gem Garnets. MSc, GLY 890 Dissertation, University of Pretoria.
Abstract/NotesGem garnet chemistry is described using the end-members pyrope, almandine, spessartine, andradite, grossular, and uvarovite. The large variation in garnets makes classification difficult. Garnet gemstones are typically classified by means of their refractive indices, together with specific gravity. However, the range of refractive indices for gem garnets can be restrictive and unreliable in gemstone classification. Chemical classification is generally the most accurate means of classification and was used in this thesis by means of a portable XRF for the non-destructive chemical analyses of 1513 garnet gemstones. Colour, refractive index and magnetic susceptibility were also determined. The garnets were divided into two species: ugrandite (uvarovite, grossular and andradite) and pyralspite (pyrope, spessartine and almandine). The chemistry of the pyralspite species was very diverse with a large range in end-member proportions producing extensive solid solutions between end-members. A diverse range in colour, refractive index, and magnetic susceptibility was also observed in the pyralspite species. However, no distinction based on refractive index and magnetic susceptibility could be made in the pyralspite species. Distinctive chemistries were observed in the ugrandite species, which correlates with the magnetic susceptibility and refractive index. Colour was the exception as no relationship between colour and chemistry was observed. The samples with unusual compositions were reported such as pyrope-andradite, spessartine-grossular, and almandine-grossular. This study concluded that refractive index, magnetic susceptibility and colour should not be used in isolation because this can lead to misinterpretation. Rather, analytical techniques, if available, should be used.

Map of Localities

Locality Pages

LocalityCitation Details
Bekily District, Androy, Madagascarpp.40-44
Color-changing garnet occurrence, Tranoroa, Beloha District, Androy, Madagascarpp.39-45

Mineral Pages

MineralCitation Details
Umbalitepp.39-45

Mineral Occurrences

LocalityMineral(s)
Bekily District, Androy, Madagascar Pyrope-Spessartine Series, Umbalite
Color-changing garnet occurrence, Tranoroa, Beloha District, Androy, Madagascar Pyrope-Spessartine Series, Umbalite


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