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Mantle and crustal sources in the genesis of late-hercynian granitoids (NW Port...
Dias, G.; Simões, P. P.; Ferreira, Narciso; Leterrier, J.Large volumes of granitoids were emplaced in the Hercynian Central Iberian Zone during the last ductile deformation phase (D3, 300-320 Ma). The biotite-rich granitoids are the most abundant: (1) syn-D3 granodiorites-monzogranites (313-319 Ma) with calc-alkaline and aluminopotassic affinities; (2) late-D3 granodiorites-monzogranites (306-311 Ma), related to subalkaline and aluminopotassic series. These granitoid...
Sr-Nd isotopic constraints on the genesis of hercynian granitoids from the Cent...
Dias, G.; Simões, P. P.; Mendes, Anabela Carreira; Leterrier, J.Poster apresentado no IV Hutton Symposium, Clermont-Ferrand, França, 20-25 Setembro 1999.
U–Pb zircon and monazite geochronology of post-collisional hercynian granitoids...
Dias, G.; Leterrier, J.; Mendes, Anabela Carreira; Simões, P. P.; Bertrand, J. M.In the Central Iberian Zone (CIZ) of the Iberian Massif large volumes of granitoids were emplaced during the post-collisional stage of the Hercynian orogeny (syn- to post-D3, the last ductile deformation phase). Twelve granitic units and a quartz monzodiorite were selected for a U–Pb zircon and monazite geochronological study. They represent successive stages of the D3 event. The Ucanha-Vilar, Lamego, Sameiro a...
Petrology and U-Pb geochronology of a late-hercynian subalkaline granitic massi...
Mendes, Anabela Carreira; Dias, G.; Leterrier, J.; Bertrand, J. M.
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