Study of the erosion rates in the upper Maracujá Basin (Quadrilátero Ferrífero/MG, Brazil) by the in situ produced cosmogenic 10Be method.

dc.contributor.authorSalgado, André Augusto Rodrigues
dc.contributor.authorVarajão, César Augusto Chicarino
dc.contributor.authorColin, Fabrice
dc.contributor.authorBraucher, Régis
dc.contributor.authorVarajão, Angélica Fortes Drummond Chicarino
dc.contributor.authorNalini Júnior, Hermínio Arias
dc.date.accessioned2017-07-11T16:06:06Z
dc.date.available2017-07-11T16:06:06Z
dc.date.issued2007
dc.description.abstractThe present work quantifies the erosive processes in the two main substrates (schists–phyllites and granites–gneisses) of the upper Maracujá Basin in the Quadrilátero Ferrífero/MG, Brazil, a region of semi-humid tropical climate. Two measuring methods of concentration were used: (i) in situ produced 10Be in quartz veins (surface erosion rates) and (ii) 10Be in fluvial sediments (basin erosion rates). The results confirm that (i) erosion tends to be more aggressive close to the headwaters than in the lower parts of the basin and (ii) the region is now affected by dissection.pt_BR
dc.identifier.citationSALGADO, A. A. R. et al. Study of the erosion rates in the upper Maracujá Basin (Quadrilátero Ferrífero/MG, Brazil) by the in situ produced cosmogenic 10Be method. Earth Surface Processes and Landforms, v. 32, p. 905-911, 2007. Disponível em: <https://onlinelibrary.wiley.com/doi/abs/10.1002/esp.1448>. Acesso em: 20 jun. 2017.pt_BR
dc.identifier.doihttps://doi.org/10.1002/esp.1448
dc.identifier.issn 1096-9837
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/8220
dc.identifier.uri2https://onlinelibrary.wiley.com/doi/abs/10.1002/esp.1448pt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.subjectQuadrilátero Ferríferopt_BR
dc.subjectBrazilpt_BR
dc.subjectErosion ratespt_BR
dc.titleStudy of the erosion rates in the upper Maracujá Basin (Quadrilátero Ferrífero/MG, Brazil) by the in situ produced cosmogenic 10Be method.pt_BR
dc.typeArtigo publicado em periodicopt_BR
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