REPOSITORIO INSTITUCIONAL DA UFOP
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Rhyacian-Orosirian transitional arc-collisional magmatism in the Archean Piedade Microcontinent, southern São Francisco Paleocontinent, Brazil.
Understanding of ancient accretionary orogenic systems through the correlation between pre-collisional assemblages described in different tectonostratigraphic terranes is not a straightforward task. The investigation of late-to-post collisional rocks, associated with the end-stage of convergent marg
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