Article ID Journal Published Year Pages File Type
4716429 Lithos 2012 12 Pages PDF
Abstract
► Inherited zircon from Gouveia granites is mainly Neoproterozoic. ► The most probable source for the granites is Gondwanan sediments. ► (Re)crystallized monazite is younger than the coexisting igneous zircon. ► Muscovite records either Ar loss or cooling after emplacement at ~ 286 Ma.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
U-Pb and 39Ar/40Ar data constraining the ages of the source, emplacement and recrystallization/cooling events from late- to post-D3 Variscan granites of the Gouveia area, central Portugal
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