Statistics for Field and geochronological evidence for origin of the Contendas-Mirante supracrustal Belt, São Francisco Craton, Brazil, as a Paleoproterozoic foreland basin.

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Field and geochronological evidence for origin of the Contendas-Mirante supracrustal Belt, São Francisco Craton, Brazil, as a Paleoproterozoic foreland basin. 140

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ARTIGO_FieldGeochronologicalEvidence.pdf(legacy) 274
ARTIGO_FieldGeochronologicalEvidence.pdf 119

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