DOI: 10.47749/t/unicamp.2019.1088103
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Gênese de horizontes Bt da Formação Marília (Cretáceo Superior)

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Cited by 2 publications
(4 citation statements)
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“…In total, the absolute dating of 114 Optically Stimulated Luminescence (OSL) surface cover samples associated with low river terraces were employed in the present study. In detail, all data collected from 30 rivers were obtained by the Environmental Analysis and Territorial Dynamics of the Laboratory of Geomorphology and Environmental Analysis IG-UNICAMP [27,34,36,37,41,42,44,[66][67][68][69][70][71][72][73].…”
Section: Selection and Spatialization Of Geochronological Datamentioning
confidence: 99%
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“…In total, the absolute dating of 114 Optically Stimulated Luminescence (OSL) surface cover samples associated with low river terraces were employed in the present study. In detail, all data collected from 30 rivers were obtained by the Environmental Analysis and Territorial Dynamics of the Laboratory of Geomorphology and Environmental Analysis IG-UNICAMP [27,34,36,37,41,42,44,[66][67][68][69][70][71][72][73].…”
Section: Selection and Spatialization Of Geochronological Datamentioning
confidence: 99%
“…Regarding the southern coast of Brazil, we used data from the surficial covers of low terraces located on coastal plains associated with the mouth of the Araranguá (see box G) [36,76] and Itapocu (see box G) [73] rivers. Within the scope of the continental morphological compartments of Northeast Brazil, absolute ages correspond to surficial covers associated with low terraces located at the middle course of the Itapicuru (see box C of Figure 1) [42,69,72] and Grande (see box B) rivers, both in the Southern Sertaneja Depression. Meanwhile, the areas analyzed in Southeast Brazil are associated with the Paulista Peripheral Depression [27,34,37], the Paulista Western Plateau [34,68], and the Uberlândia-Uberaba plateau on the edge of the Brazilian Central Plateau [70].…”
Section: Selection and Spatialization Of Geochronological Datamentioning
confidence: 99%
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“…e frias entre 21.400 e 7.300 anos AP em Águas Emendadas (DF); e Ferraz-Vincentini &Salgado-Laboriau (1996) inferiram condições áridas e relativamente mais quentes no período entre 10.500 e 7.700 anos AP em Cromínea (GO). de 6.100 anos AP é indicado como um período mais seco(Góes, 2019).…”
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