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- W2024333691 abstract "Abstract The Fornos de Algodres Complex (FAC) comprises several intrusions of late-post-tectonic Hercynian granitic rocks ranging in composition from hornblende granodiorites and quartz monzodiorites, through coarse porphyritic biotite granites and two-mica granites (coarse-, medium- and fine-grained), to muscovite-rich leucogranites. Field and regional constraints show that the emplacement of this large, composite, batholithic complex post-dates the main Variscan regional deformation phases (D1+D2+D3) and associated metamorphic events. Field, petrographic and geochemical data suggest a strong genetic relationship between most of the members of the FAC. However, their Rb–Sr and Sm–Nd isotopic signatures appear to rule out any genetic process involving a single homogeneous source and/or closed-system fractional crystallization of the same parental magma. A model involving hybridization of mantle-derived basaltic liquids with crustal anatectic melts followed by further contamination and fractional crystallization is proposed to explain the isotopic and geochemical variation trends defined by the FAC granitic rocks." @default.
- W2024333691 created "2016-06-24" @default.
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- W2024333691 date "1998-10-01" @default.
- W2024333691 modified "2023-10-14" @default.
- W2024333691 title "Hercynian late-post-tectonic granitic rocks from the Fornos de Algodres area (Northern Central Portugal)" @default.
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- W2024333691 doi "https://doi.org/10.1016/s0024-4937(98)00019-x" @default.
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