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Tourmalines in the Namacotche Li-Cs-Ta granitic pegmatite group, Mozambique: cr...

Gomes, C. Leal; Neiva, Ana M. R.

The field work, backscattered electron images and detailed microanalyses of three generations of tourmaline from the Namacotche LCT pegmatites allows de distinction between the compositional magmatic and hydrothermal tourmalines. The generation 1 occurs in the outer intermediate zone of the pegmatite. It consists of zoned crystals with an oscillatory inner core of foitite and schorl, an outer core of schorl and...


The granite‑hosted Variscan gold deposit from Santo António mine in the Iberian...

Neiva, Ana M. R.; Moura, António; Gomes, C. Leal; Pereira, Manuel Francisco; Corfu, Fernando

The study area is located in the Central Iberian Zone, a major tectonic unit of the Iberian Massif (Variscan belt). In this region the basement is composed of Cambrian-Ordovician sedimentary and minor volcanic rocks that underwent deformation and metamorphism during the Carboniferous. These metamorphic rocks host ca. 331–308 Ma granitic plutons emplaced during the D2 extensional and D3–D4 contractional deformat...


Release, Migration, Sorption, and (Re)Precipitation of U during Peraluminous Gr...

Pinto, Marina M. S. Cabral; Silva, Maria M. V. G.; Neiva, Ana M. R.; Guimarães, Fernanda; Silva, Paulo

In this work, in order to study the release, migration, sorption, and (re)precipitation of uranium (U) during alteration under oxidizing conditions, we carried out a systematic study using scanning electron microscopy, X-ray maps, and electron microprobe analyses on uranium minerals—such as uraninite, coffinite, saleeite, meta-saleeite, and thorite—and U-bearing minerals—such as xenotime, monazite, apatite, and...



Portuguese granites associated with Sn-W and Au mineralizations

Neiva, Ana M. R.

In northern and central Portugal, there are different tin-bearing granites. Most of them are of S-type, others have mixed characteristics of I-type and S-type granites and a few are of I-type. Tin-tungsten deposits are commonly associated with Hercynian tin-bearing S-type granites. Some quartz veins with wolframite are associated with an I-type granite, which has a low Sn content. In suites of tin-bearing S-typ...


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