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Journal of the Geological Society; 2006; v. 163; issue.5; p. 761-774;
DOI: 10.1144/0016-76492005-146
© 2006 Geological Society of London

Original Article

Severity and timing of Cenozoic exhumation in the southwestern Barents Sea

Andrew J. Cavanagh1,2, R. Di Primio1, M. Scheck-Wenderoth1 & B. Horsfield1

1 1GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473, Germany
2 2Present address: School of GeoSciences, University of Edinburgh, Grant Institute, West Mains Road, Edinburgh EH9 3JW, UK (e-mail: acavanagh@staffmail.ed.ac.uk)

The juxtaposition of the North Atlantic rift system with the borderlands of the Eurasian Arctic shelf has resulted in an unusual basin evolution in the southwestern Barents Sea. Exploration has concentrated on the Mesozoic sandstone plays of the Hammerfest Basin. These have yielded abundant gas and very little oil. Such findings are typical of peripheral North Atlantic margin basins that have undergone Cenozoic exhumation. This is generally thought to have occurred during the Palaeocene, Oligocene–Miocene or Pleistocene. Hammerfest Basin erosion is widely estimated to be in the range of 500–1500 m. However, the relative severity of individual episodes and impact on fluid dynamics within the basin are poorly constrained. We apply basin modelling tools to establish the sensitivity of the petroleum system to three cited scenarios for Cenozoic exhumation. Vitrinite reflectance and temperature data constrain burial and thermal histories. Calibration is not possible using heat flow variations alone; erosion timing and magnitude are required to match available data. The calibrated model indicates a significant thermal disequilibrium in the Hammerfest Basin at the present day resulting from Late Cenozoic exhumation. Forward modelling of Pleistocene ice sheets allows for an estimation of pressure and temperature fluctuations in response to glacial–interglacial cycles.




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