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Continental Heat-Flow Density

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Handbook of Terrestrial Heat-Flow Density Determination

Part of the book series: Solid Earth Sciences Library ((SESL,volume 4))

Abstract

Although on the geological time and space scales the geothermal regime of the Earth is, strictly speaking, both a transient and three dimensional phenomenon, on the global scale by far the most important component of heat transfer is radial. Furthermore, over times of the order of the thermal time constant for the crust, that is a few hundred thousand to a few million years, we consider the thermal regime to be quasi-steady state.

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Author information

Authors and Affiliations

  1. Department of Geology and Geophysics, University of Utah, Salt Lake City, USA

    W. G. Powell & D. S. Chapman

  2. Laboratoriet for Geofysik, Geologisk Institut, Aarhus Universitet, Denmark

    N. Balling

  3. Department of Geophysics, The University of Western Ontario, London, Canada

    A. E. Beck

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  1. W. G. Powell
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  2. D. S. Chapman
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  3. N. Balling
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  4. A. E. Beck
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Editor information

Editors and Affiliations

  1. Department of Geophysics, Geological Survey of Lower Saxony, Hannover, Germany

    R. Haenel

  2. Institute of Geophysics, ETH Zürich, Switzerland

    L. Rybach

  3. Department of Environmental Physics, Roland Eötvös University, Budapest, Hungary

    L. Stegena

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© 1988 Kluwer Academic Publishers

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Powell, W.G., Chapman, D.S., Balling, N., Beck, A.E. (1988). Continental Heat-Flow Density. In: Haenel, R., Rybach, L., Stegena, L. (eds) Handbook of Terrestrial Heat-Flow Density Determination. Solid Earth Sciences Library, vol 4. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-2847-3_5

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  • DOI: https://doi.org/10.1007/978-94-009-2847-3_5

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