The endorheic – Exorheic transition and later stage of fluvial incision in a wet tropical margin setting: The Atlantic draining Paraíba do Sul River basin (Brazil)

Morphostructural influence and neotectonic activity in the geomorphological configuration of southeast Paraíba and northeast Pernambuco, Brazil

“…Recent studies propose that these domes might represent a push-up structure [ 48 ], potentially linked to late activations of the splays of the Congo-Coxixola Lineament. However, their causes and interrelationships necessitate further subsurface research [ 49 ]. Despite the need for additional detail on their genesis, the significant effect of these domes on the local drainage network's configuration and, consequently, on the geomorphological development of the area is unquestionable.…”

Application of the authigenic 10Be/9Be dating to constrain the age of a long-lived lake and its regression in an isolated intermontane basin: The case of Late Miocene Lake Turiec, Western Carpathians

“…Low precipitation and high uplift rates enhance the formation of an internal drainage and thus reduce the connectivity of an intermontane basin with a drainage network of the orogenic belt and foreland (Sobel et al, 2003;Garcia-Castellanos, 2006). On the other hand, an outflowing lake connected with the regional drainage and underfilled with sediment could form, but its persistency is limited by potential breakage of topographic barriers, especially in humid conditions, limited water depth and low uplift rates of its margins (Sobel et al, 2003;Bridgland et al, 2020;Freitas et al, 2022). Another major factor related to the role of an intermontane basin in the drainage network of an orogenic belt is the redistribution of sediment and its transient storage.…”