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Iberian late-Variscan granitoids: Some considerations on crustal sources and the significance of mantle extraction ages
A suite of post-tectonic granitoids (mostly peraluminous, broadly I-type granodiorites and monzogranites) and mafic rocks from NW Iberia with crystallization ages between ca. 309 and 290 Ma has been investigated for Sm–Nd isotopes and inherited …
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