Lyell Collection

Geological Society, London, Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF) FREE
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Viana, A. R.
Right arrow Articles by Bulhões, E. M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 2007; v. 276; p. 1-23;
DOI: 10.1144/GSL.SP.2007.276.01.01
© 2007 Geological Society of London

The economic importance of contourites

A. R. Viana, W. Almeida, Jr, M. C. V. Nunes & E. M. Bulhões

Petrobras, E&P-Exploration, Rio de Janeiro, RJ 20031-912, Brazil (e-mail: aviana{at}petrobras.com)

The importance of contour currents in shaping and building continental margins has long been accepted. Their economic implications and the stratigraphic framework in which they are developed remain largely unknown. Data retrieved from sidescan sonar images, seismic profiles and their attribute maps, as well as sea-floor coring, boreholes and the few known outcrops around the world, suggest that bottom currents can locally develop large deposits of relatively coarse-grained sediments. Accumulation of coarse-grained deposits under the influence of bottom currents requires sediment availability, a geologically persistent strong circulation regime and a favourable physiographic setting both for enhancing the currents and for hosting the sediments. The hydrocarbon exploration of oceanic depositional systems demands a better understanding of the role of bottom currents and their implications for petroleum systems such as reservoir and sealing rocks. Such understanding implies additional alternatives for the definition of exploration targets and prospect risk reduction. Correlating seismic anomalies from 3D mapping with core and well logging data reveals the depositional geometry and sedimentological characteristics of coarse-grained contourites. Fine-grained drifts can locally and regionally develop large and thick accumulations, which have an important seal potential for trapping hydrocarbon.





This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
M. Rebesco, A. Camerlenghi, V. Volpi, C. Neagu, D. Accettella, B. Lindberg, A. Cova, F. Zgur, and Magico Party
Interaction of processes and importance of contourites: insights from the detailed morphology of sediment Drift 7, Antarctica
Geological Society, London, Special Publications, 2007; 276: 95 - 110.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
C. S. L. Duarte and A. R. Viana
Santos Drift System: stratigraphic organization and implications for late Cenozoic palaeocirculation in the Santos Basin, SW Atlantic Ocean
Geological Society, London, Special Publications, 2007; 276: 171 - 198.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
G. Georgiev and N. Botoucharov
Are there Middle Jurassic contourites in the Tarnovo depression (Southern Moesian platform margin)?
Geological Society, London, Special Publications, 2007; 276: 283 - 298.
[Abstract] [PDF]