High-resolution heat flow density in the lower Congo basin

Author:

Lucazeau Francis1,Brigaud Frédéric2,Bouroullec Jean Luc3

Affiliation:

1. Laboratoire de Géosciences Marines, UMR 7097; Institut de Physique du Globe; 4 Place Jussieu, 75252 Paris Cedex 05 France

2. Total E&P Norge AS; FinnestadVeien 44, Dusavik, P.O. Box 168 N-4001 Stavanger Norway

3. Total E&P Congo; CSTJF; 64018 Pau France

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. Morphology and architecture of the present canyon and channel system of the Zaire deep-sea fan;Babonneau;Mar. Pet. Geol.,2002

2. Diversion of heat by Archean cratons: A model for southern Africa;Ballard;Earth Planet. Sci. Lett.,1987

3. Heat flow from the West African Shield;Brigaud;Geophys. Res. Lett.,1985

4. Estimating thermal conductivity in sedimentary basins using lithologic data and geophysical well logs;Brigaud;AAPG Bull.,1990

5. Thermal state in the north Viking Graben (North Sea) determined from oil exploration well data;Brigaud;Geophysics,1992

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