2014
DOI: 10.1016/j.gca.2014.02.006
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Alkali metal and rare earth element evolution of rock-forming minerals from the Gatumba area pegmatites (Rwanda): Quantitative assessment of crystal-melt fractionation in the regional zonation of pegmatite groups

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Cited by 156 publications
(83 citation statements)
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“…In granitic pegmatite fields reported in the literature, e.g. in Cap de Creus (northeastern Spain, Alfonso and Melgarejo, 2008;Druguet et al, 2014;Van Lichtervelde et al, 2016) or in Gatumba (central Rwanda, Hulsbosch et al, 2014;Melcher et al, 2015), the closest bodies from the sources (usually a granite) (i) are the least evolved, and (ii) contain biotite but no muscovite nor rare-element minerals (i.e. Li, B, Be, Rb, Sn, Nb-Ta… e.g.…”
Section: Potential Sources Of the Lree-rich Pgd From The Lac Okaopéo mentioning
confidence: 99%
See 1 more Smart Citation
“…In granitic pegmatite fields reported in the literature, e.g. in Cap de Creus (northeastern Spain, Alfonso and Melgarejo, 2008;Druguet et al, 2014;Van Lichtervelde et al, 2016) or in Gatumba (central Rwanda, Hulsbosch et al, 2014;Melcher et al, 2015), the closest bodies from the sources (usually a granite) (i) are the least evolved, and (ii) contain biotite but no muscovite nor rare-element minerals (i.e. Li, B, Be, Rb, Sn, Nb-Ta… e.g.…”
Section: Potential Sources Of the Lree-rich Pgd From The Lac Okaopéo mentioning
confidence: 99%
“…Li, B, Be, Rb, Sn, Nb-Ta… e.g. Hulsbosch et al, 2014;London, 2016London, , 2008 or REE mineralization (e.g. Ercit, 2005).…”
Section: Potential Sources Of the Lree-rich Pgd From The Lac Okaopéo mentioning
confidence: 99%
“…The parallel trends followed by the Zr/Hf and Nb/Ta Rayleigh fractionation curves (Fig. 5) are also evidences that CGM and zircon both followed magmatic fractionation trends and therefore crystallized together at the magmatic stage (Hulsbosch et al 2014). …”
Section: Dating Pegmatite Emplacementmentioning
confidence: 63%
“…The most evolved pegmatites belong to the Lithium-Caesium-Tantalum (LCT) family based on the rare element association, and more specifically to the rare element pegmatite class. Based on the rare element mineralogy, they include representatives of the beryl-type (beryl columbite subtype), complex-type (spodumene subtype), and albite-spodumene type [10]. The rare element pegmatite from Gatumba area has attracted different mining companies for exploitation of niobium-tantalum and tin minerals.…”
Section: Geological Settingsmentioning
confidence: 99%
“…Most deposits in Rwanda are not well developed, due to the lack of adequate geologic studies such as in the Gatumba and Gitarama areas. Some information was provided on the geochemistry of pegmatites in the area [10]. The insufficient geologic study and mineralisation relationship have made these areas less attractive to mining investors.…”
Section: Introductionmentioning
confidence: 99%