Post-rift landscape development of north-east Brazil

Authors

  • Johan M. Bonow Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K. Denmark
  • Peter Japsen Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K. Denmark
  • Paul F. Green Geotrack International, 37 Melville Road, Brunswick West, Victoria 3055, Australia
  • Peter R. Cobbold Géosciences-Rennes (UMR6118 du CNRS), Université de Rennes, 35042 Rennes Cedex, France
  • Augusto J. Pedreira Geological Survey of Brazil (CPRM), Avenida Ulysses Guimaraes, 2862, 41213-000 Salvador, Brazil
  • Ragnhild Lilletveit StatoilHydro, Angola team, Stavanger, Norway
  • Dario Chiossi StatoilHydro do Brazil, Rio de Janeiro, Brazil

DOI:

https://doi.org/10.34194/geusb.v17.5020

Abstract

The evolution of the landscape of north-east Brazil in relation to the burial and exhumation history of both onshore and offshore areas is the focus of a research project carried out for StatoilHydrodo Brasil and Petrobras from 2007 to 2009 by the Geological Survey of Denmark and Greenland in collaboration with Geotrack International. In hydrocarbon exploration it is important to understand the regional tectonic framework and thus also to consider the volumes of rocks that may have been present and then removed during the geological past. For example, the timing of hydrocarbon generation and changes in migration routes can be assessed when the timing and magnitude of uplift and erosion is known. Studies in West Greenland have demonstrated the usefulness of large-scale, low-relief, high-level landscapes as markers of uplift events, and in particular the strength of combining the denudation history from landscape analysis with the cooling history from apatite fission-track analysis (AFTA) data and the stratigraphic record (Bonow et al. 2006, 2007; Japsen et al. 2006, 2009). In the study area, there are two plateaux with elevations up to c. 1300 m above sea level (a.s.l.). The plateaux are currently being dissected by deeply incised fluvial valleys, and escarpments separate the two plateaux. The lowlands cut across Early Cretaceous rift systems along the Atlantic margin, including the intracontinental Recôncavo–Tucano–Jatobá (RTJ) Rift and also the Camamu Basin, of which the western margin is exposed onshore (Fig. 1). The RTJ Rift is a mature hydrocarbon province, whereas the deep-water parts of the Camamu Basin are the target of frontier exploration (e.g. Magnavita et al. 1994; Davison 1999; Cobbold et al. 2008). The post-rift sequence in the RTJ Rift and the inshore Camamu Basin is thin or absent. However, it has been estimated that up to 2000 m of sedimentary cover once was present, but has now been removed (Magnavita et al. 1994).

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Published

2009-07-08

How to Cite

Bonow, J. M., Japsen, P., Green, P. F., Cobbold, P. R., Pedreira, A. J., Lilletveit, R., & Chiossi, D. (2009). Post-rift landscape development of north-east Brazil. GEUS Bulletin, 17, 81–84. https://doi.org/10.34194/geusb.v17.5020

Issue

Section

RESEARCH ARTICLE | SHORT

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