Heat flow from the West African Shield
- 1 September 1985
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 12 (9) , 549-552
- https://doi.org/10.1029/gl012i009p00549
Abstract
The heat flow over Precambrian shields is generally lower than over other continental provinces. Previous observations at 9 sites of the West African shield have shown that heat flow ranges from 20 mW m −2 in Niger to 38‐42 mW m −2 in Liberia, Ghana and Nigeria. Since some of these values are lower than expected for Precambrian shields, it is important to find out whether or not they are representative of the entire shield before trying to derive its thermal structure. In this paper, we present new heat flow determinations from seven sites of the West African shield. These indicate that the surface heat flow is comparable with that of other Precambrian shields in the world.This publication has 6 references indexed in Scilit:
- Oceans and continents: Similarities and differences in the mechanisms of heat lossJournal of Geophysical Research, 1981
- Heat flow from the Liberian Precambrian ShieldJournal of Geophysical Research, 1980
- On the variation of continental heat flow with age and the thermal evolution of continentsJournal of Geophysical Research, 1980
- Heat-flow measurements in the ririwai ring complex, NigeriaTectonophysics, 1979
- A Comparison of the Thermal Characters of ShieldsCanadian Journal of Earth Sciences, 1975
- ‘Cold spot’ in West Africa: anchoring the African plateNature, 1974