Stepped surfaces and palaeolandforms in the northern Brazilian «Nordeste»: constraints on models of morphotectonic evolution

• Published in: Geomorphology (Amsterdam, Netherlands) Vol. 62; no. 1; pp. 89 - 122
• Main Authors: Peulvast, Jean-Pierre, de Claudino Sales, Vanda
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 06.09.2004; Elsevier
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; Geomorphology, landform evolution; Marine and continental quaternary; Morphostratigraphy; Palaeolandform; Pediplain; Planation surface; Structural geomorphology; Surficial geology; Tectonics. Structural geology. Plate tectonics; Borborema; Brazil; Parnaiba Basin; Jaguaribe; Ceara Brazil; AS, Equatorial Atlantic; ASW, Brazil; Structural geomorphology; Pediplain; Palaeolandform; Morphostratigraphy; Planation surface; South America; Mesozoic; planation; fault scarps; plateaus; plains; Upper Cretaceous; tectonic controls; models; Cenomanian; topography; Cretaceous; landforms; Lower Cretaceous; uplifts; Aptian; drainage; rifting; Phanerozoic; landform evolution
• ISSN: 0169-555X; 1872-695X
• DOI: 10.1016/j.geomorph.2004.02.006

From the Parnaiba Basin to the Borborema Plateau (northeastern Brazil), the crystalline and sedimentary highlands and plains of the huge Jaguaribe–Piranhas amphitheatre are intersected seawards by offset elements of a marginal scarp which overlooks coastal lowlands along the Equatorial Atlantic transform margin. Its stepped surfaces are classically related to regional uplift induced by the break-up of the Gondwana supercontinent, supposed to have triggered the formation, until the Plio-Pleistocene, of successively younger planation surfaces below a culminating Cretaceous surface. A reinterpretation of this topography, combined with analyses of palaeolandforms, surface deposits, drainage anomalies, and structural controls on landforms, is used to obtain ages for significant features of the stepped patterns and to propose a morphostratigraphic scheme for the whole area. It is shown that the regional morphology is widely controlled by structures formed during Early Cretaceous continental rifting and later Aptian oceanic opening. Exhumed pre-Cenomanian palaeolandforms—planation surfaces, residual Cretaceous fault scarps—are identified. This study points out the value of the morphostructural approach for revisiting classical problems of geomorphology such as the meaning of stepped landforms (identification of palaeosurfaces of Cretaceous age at various levels), and the age and origin of planation surfaces. Its results are considered as constraining elements for a further tentative reconstruction of the morphotectonic evolution of this margin.