2012
DOI: 10.1016/j.lithos.2012.04.027
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From granite to highly evolved pegmatite: A case study of the Pinilla de Fermoselle granite–pegmatite system (Zamora, Spain)

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Cited by 84 publications
(36 citation statements)
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“…This type of Li mineralization occurs in the apical or marginal areas of highlyfractionated leucogranites, hosted by metasedimentary rocks of the Schist-Metagreywacke Complex. The associated leucogranites are typically fine grained and enriched in B, Li and F (Martín-Izard et al, 1992, Roda-Robles et al, 2012b. The apical/marginal zones are quite heterogeneous and include a range of mineral associations.…”
Section: Lithium Mineralization Associated With Leucogranitic Cupolasmentioning
confidence: 99%
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“…This type of Li mineralization occurs in the apical or marginal areas of highlyfractionated leucogranites, hosted by metasedimentary rocks of the Schist-Metagreywacke Complex. The associated leucogranites are typically fine grained and enriched in B, Li and F (Martín-Izard et al, 1992, Roda-Robles et al, 2012b. The apical/marginal zones are quite heterogeneous and include a range of mineral associations.…”
Section: Lithium Mineralization Associated With Leucogranitic Cupolasmentioning
confidence: 99%
“…The two facies may occur in the same intrusion (RodaRobles et al, 2015). Usually the contact between the granitic and the pegmatitic rocks is gradual, being difficult to establish the limit between both lithologies (Roda-Robles et al 2012b.…”
Section: Lithium Mineralization Associated With Leucogranitic Cupolasmentioning
confidence: 99%
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