2021
DOI: 10.29396/jgsb.2021.v4.n3.4
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The state of the art of Low-temperature Thermochronology in Brazil

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Cited by 5 publications
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“…In the former, the lithosphere elastic strength/flexural uplift also played a key role in tectonic rejuvenation, as invoked by numerical modelling. Additionally, a Neogene E-W transpression resulted from far-field stress from the opposite plate margin forces (e.g.,.Neogene-Quaternary local rapid denudation in the Doce Catchment near the study area has been justified by interactions between drainage surface processes and differential reactivation of weakness zones of the Araçuaí orogen (e.g.,van Ranst et al, 2021;Novo et al, 2021). Likewise, other studies have shown tectonic reactivation of pre-Cenozoic structures along the São Francisco Craton boundary from the Pliocene to Pleistocene and Pliocene uplift…”
mentioning
confidence: 82%
“…In the former, the lithosphere elastic strength/flexural uplift also played a key role in tectonic rejuvenation, as invoked by numerical modelling. Additionally, a Neogene E-W transpression resulted from far-field stress from the opposite plate margin forces (e.g.,.Neogene-Quaternary local rapid denudation in the Doce Catchment near the study area has been justified by interactions between drainage surface processes and differential reactivation of weakness zones of the Araçuaí orogen (e.g.,van Ranst et al, 2021;Novo et al, 2021). Likewise, other studies have shown tectonic reactivation of pre-Cenozoic structures along the São Francisco Craton boundary from the Pliocene to Pleistocene and Pliocene uplift…”
mentioning
confidence: 82%