Denudation history and landscape evolution of the northern East-Brazilian continental margin from apatite fission-track thermochronology

• Published in: Journal of South American earth sciences Vol. 54; pp. 158 - 181
• Main Authors: Jelinek, A.R., Chemale, F., van der Beek, P.A., Guadagnin, F., Cupertino, J.A., Viana, A.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-10-2014
• Subjects: Apatite fission-track thermochronology; Denudation; NE-Brazil; Passive continental margin; Apatite fission-track thermochronology; NE-Brazil; Passive continental margin; Denudation
• ISSN: 0895-9811; 1873-0647
• DOI: 10.1016/j.jsames.2014.06.001

We reconstruct the history of denudation and landscape evolution of the northern East- Brazilian continental margin using apatite fission-track thermochronology and thermal history modeling. This part of the Brazilian Atlantic margin is morphologically characterized by inland and coastal plateaus surrounding a wide low-lying inland region, the Sertaneja Depression. The apatite fission track ages and mean track lengths vary from 39 ± 4 to 350 ± 57 Ma and from 10.0 ± 0.3 to 14.2 ± 0.2 μm, respectively, implying a protracted history of spatially variable denudation since the Permian at relatively low rates (<50 m My−1). The Sertaneja Depression and inland plateaus record Permian-Early Jurassic (300–180 Ma) denudation that precedes rifting of the margin by > 60 Myrs. In contrast, the coastal regions record up to 2.5 km of Late Jurassic-Early Cretaceous (150–120 Ma) denudation, coeval with rifting of the margin. The samples from elevated coastal regions, the Borborema Plateau and the Mantiqueira Range, record cooling from temperatures above 120 °C since the Late Cretaceous extending to the Cenozoic. We interpret this denudation as related to post-rift uplift of these parts of the margin, possibly resulting from compressional stresses transmitted from the Andes and/or magmatism at that time. Several samples from these areas also record accelerated Neogene (<30 Ma) cooling, which may record landscape response to a change from a tropical to a more erosive semi-arid climate during this time. The inferred denudation history is consistent with the offshore sedimentary record, but not with evolutionary scenarios inferred from the recognition of “planation surfaces” on the margin. The denudation history of the northeastern Brazilian margin implies a control of pre-, syn- and post-rift tectonic and climatic events on landscape evolution.
•The continental margin of NE-Brazil underwent a protracted denudation.•The AFT data allow determining the timing of four cooling/denudation episodes.•The denudation history is consistent with the offshore sedimentary record.