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Article

Barren and Li–Sn–Ta Mineralized Pegmatites from NW Spain (Central Galicia): A Comparative Study of Their Mineralogy, Geochemistry, and Wallrock Metasomatism

Department of geology, University of Oviedo, Arias de Velasco s/n, 33005 Oviedo, Spain
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Author to whom correspondence should be addressed.
Minerals 2019, 9(12), 739; https://doi.org/10.3390/min9120739
Received: 31 October 2019 / Revised: 24 November 2019 / Accepted: 27 November 2019 / Published: 29 November 2019
In Central Galicia, there are occurrences of barren and Li–Sn–Ta-bearing pegmatites hosted by metasedimentary rocks. A number of common and contrasting features between Panceiros pegmatites (barren) and Li–Sn–Ta mineralized Presqueira pegmatite are established in this study. K-feldspar and muscovite have the same trace elements (Rb, Cs, P, Zn, and Ba), but the mineralized one has the highest Rb and Cs and the lowest P contents. The barren bodies show fluorapatite and eosphorite–childrenite replacing early silicates. The mineralized body has primary phosphates (fluorapatite and montebrasite), a metasomatic paragenesis (fluorapatite and goyazite) replacing early silicates, and a late hydrothermal assemblage (vivianite and messelite). Ta–Nb oxides from the Presqueira body show a trend from columbite-(Fe) to tantalite-(Fe) and tapiolite-(Fe). In this body, the Li-aluminosilicate textures support primary crystallization of petalite that was partially transformed into Spodumene + Quartz (SQI) during cooling, and into myrmekite during a Na-metasomatism stage. As a result of both processes, spodumene formed. The geochemical study supports magmatic differentiation increasing from the neighboring granites to the Li–Sn–Ta mineralized pegmatite. In both barren and mineralized bodies, the pegmatite-derived fluids that migrated into the wallrock were enriched in B, F, Li, Rb, and Cs and, moreover, in Sn, Zn, and As. View Full-Text
Keywords: wallrock signature; Li–Sn–Ta pegmatite; spodumene; petalite; myrmekite; columbite–tantalite; tantaliferous cassiterite; NW Spain wallrock signature; Li–Sn–Ta pegmatite; spodumene; petalite; myrmekite; columbite–tantalite; tantaliferous cassiterite; NW Spain
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MDPI and ACS Style

Roza Llera, A.; Fuertes-Fuente, M.; Cepedal, A.; Martin-Izard, A. Barren and Li–Sn–Ta Mineralized Pegmatites from NW Spain (Central Galicia): A Comparative Study of Their Mineralogy, Geochemistry, and Wallrock Metasomatism. Minerals 2019, 9, 739. https://doi.org/10.3390/min9120739

AMA Style

Roza Llera A, Fuertes-Fuente M, Cepedal A, Martin-Izard A. Barren and Li–Sn–Ta Mineralized Pegmatites from NW Spain (Central Galicia): A Comparative Study of Their Mineralogy, Geochemistry, and Wallrock Metasomatism. Minerals. 2019; 9(12):739. https://doi.org/10.3390/min9120739

Chicago/Turabian Style

Roza Llera, Ana, Mercedes Fuertes-Fuente, Antonia Cepedal, and Agustín Martin-Izard. 2019. "Barren and Li–Sn–Ta Mineralized Pegmatites from NW Spain (Central Galicia): A Comparative Study of Their Mineralogy, Geochemistry, and Wallrock Metasomatism" Minerals 9, no. 12: 739. https://doi.org/10.3390/min9120739

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