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Combined U–Pb geochronology and Lu–Hf isotope systematics by LAM–ICPMS of zirco...

Geochemical and isotopic constraints on the petrogenesis of Early Ordovician gr...

http://www.sciencedirect.com/science/article/B6V6J-4VGPWSW-1/2/0a38a395dc65fe184f68de82f471c0d5

Geochemical and isotopic constraints on the petrogenesis of Early Ordovician gr...

Geochemistry of Li-bearing aplite-pegmatite veins from Cabeço Queimado and asso...

At Segura area, two-mica granite, muscovite granite, granitic aplite veins and Libearing granitic aplite-pegmatite veins from Cabeco Queimado intruded the Cambrian schist-metagraywacke complex. Aplite veins also intruded both granites. Variation diagrams of major and trace elements of the granitic rocks show fractionation trends for: a) two-mica granite and Li-bearing aplite-pegmatite veins; b) muscovite granit...

Antimony quartz and antimony-gold quartz veins from northern Portugal

Antimony- and Pb-Sb-quartz veins from the Bragança district, Portugal, are mainly hosted by Silurian phyllites. Antimony-Au-quartz veins from the Dúrico-Beirã region are mainly hosted by a Cambrian schist-metagraywacke complex, as well as Ordovician phyllites and quartzites. The deposits were mostly exploited in the late 19th Century. Mineralogical characteristics and chemical compositions of individual ore min...

Geoquímica das rochas granitóides da região de Gouveia, centro de Portugal

Several types of peraluminous Hercynian granites containing generally more primary muscovite than Fe2+-biotite + chlorite, have mainly A/CNK values greater than 1.15, but ranging between 1.01 and 1.41 and δ18O values of 10.34-13.52% and are interpreted of S-type. A Mg-biotite granidorite of I-type having A/CNK of 0.99-1.10 and δ18O of 8.84% also occurs in the Gouveia area. Variation diagrams of major and trace...

Geoquímica de fosfatos de granitos, aplitos, pegmatitos e filões de quartzo no ...

Algumas rochas graníticas do norte e centro de Portugal possuem fosfatos. A triflite altera-se para vivianite maganífera, ludlamite azul, fosfoferrite e mitriadite nos filões aplíticos de Vidago, que também possuem brushite, ludlamite e perlofite verde. A triflite do granito moscovítico de Paredes da Beira altera-se para estrengite. Childrenite e eosforite ocorrem nos granitos de Paredes da Beira e Penamacor-Mo...

Phosphate minerals of some granitic rocks associated quartz veins from northern...

Phosphate minerals are common in northern and central Portuguese granitic rocks. Childrenite, eosphorite and intermediate compositions in this solid-solution séries occur in muscovite granites at Paredes da Beira and Penamacor-Monsanto, muscovite-biotite granites at Penamacor-Monsanto and in aplite veins at Vidago. The composition of childrenite and eosphorite are similar in each of these localities. Germanite...