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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May 2024 | 0 |
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ARTIGO_FieldGeochronologicalEvidence.pdf(legacy) | 274 |
ARTIGO_FieldGeochronologicalEvidence.pdf | 119 |
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