2010
DOI: 10.1016/j.gr.2010.03.001
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Denudation history of the Bocaina Plateau, Serra do Mar, southeastern Brazil: Relationships to Gondwana breakup and passive margin development

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Cited by 93 publications
(79 citation statements)
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“…As idades TFA refletem esta morfologia de margem passiva, com um aumento das idades de 40-90 Ma na planície costeira para >300 Ma no interior continental, configurando uma maior denudação na planície, como sugerido por diversos autores (p. ex., Gallagher et al, 1994Gallagher et al, , 1995Gallagher & Brown, 1999;Carmo, 2005;Hiruma et al, 2010;Engelmann de Oliveira et al, 2016).…”
Section: Discussão Dos Resultadosunclassified
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“…As idades TFA refletem esta morfologia de margem passiva, com um aumento das idades de 40-90 Ma na planície costeira para >300 Ma no interior continental, configurando uma maior denudação na planície, como sugerido por diversos autores (p. ex., Gallagher et al, 1994Gallagher et al, , 1995Gallagher & Brown, 1999;Carmo, 2005;Hiruma et al, 2010;Engelmann de Oliveira et al, 2016).…”
Section: Discussão Dos Resultadosunclassified
“…Diversos autores (p. ex., Gallagher et al, 1994Gallagher et al, , 1995Hiruma et al, 2010;Jelinek et al, 2014;Engelmann de Oliveira et al, 2016) discutem que as altas taxas de denudação pós-rifte indicadas para a margem, provavelmente refletem a geometria e o momento da reativação tectônica pós-rifte de estruturas intracontinentais maiores, e as taxas de denudação são correlacionáveis às espessuras do registro sedimentar offshore nas bacias de Santos e Espírito Santo. O Arco de Ponta Grossa, na região de Curitiba, apresenta as idades TFA mais jovens de toda a margem continental (Fig.…”
Section: Discussão Dos Resultadosunclassified
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“…According to Soares et al [35], this region is strongly influenced by the topography of the Serra do Mar, with the most intense rainfall occurring on the steep slopes of the escarpment. 2000 1392 1822 2001 1197 1853 2002 1286 2339 2003 1195 2441 2004 1457 2484 2005 1067 2756 2006 1159 2489 2007 1227 1918 2008 1509 2818 2009 1669 2934 2010 1639 2366 The Bocaina Plateau is the highest area (>2000 m of altitude) of the Serra do Mar (1000 km of extension) situated on the eastern flank of the continental rift border of Southeastern Brazil [36]. The main lithologies of Serra da Bocaina are medium to high-grade orthogneisses and paragneisses, dominated by regional NE-SW trending ductile shear zones that dip steeply (~60 • ) to the northwest or southeast [37] (Figure 2).…”
Section: Study Areamentioning
confidence: 99%
“…Lastly, late Pleistocene to Holocene neotectonic reactivation caused significant altitude differences between the Bocaina Plateau and adjacent rift valley, determining the local geomorphologic features with abrupt escarpments, a drainage network pattern controlled by the fault zones, and alluvial fan deposits at the base of mountains [44,45]. The Bocaina Plateau is the highest area (>2000 m of altitude) of the Serra do Mar (1000 km of extension) situated on the eastern flank of the continental rift border of Southeastern Brazil [36]. The main lithologies of Serra da Bocaina are medium to high-grade orthogneisses and paragneisses, dominated by regional NE-SW trending ductile shear zones that dip steeply (~60°) to the northwest or southeast [37] (Figure 2).…”
Section: Year Campos De Cunha Station São Roque Stationmentioning
confidence: 99%