Skip to main content
Log in

Temperature and distribution of radioactive matter in the upper mantle

  • Ière Partie Communications Présentées Au Symposium De Volcanologie Physique Zurich, Sept. 1967
  • Published:
Bulletin Volcanologique Aims and scope Submit manuscript

Abstract

Temperatures of the Earth’s upper mantle, derived from Gutenberg’s seismic velocities, have been revised, using some recent determinations of the clastic constants of dunites. For depths greater than about 50 km the temperature obtained is sufficient to melt the basaltic fraction of a periodotitic mantle (if this low-melting fraction still exists at those depths). The distribution of the radioactive heat sources appears to be fairly uniform down to about 110 km; below this level the radioactive matter is probably absent. This is what would be expected for the upper mantle below the oceans; therefore, Gutenberg’s velocities seem to correspond to oceanic areas, rather than to the mantle below a continental shield.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Birch, F., 1943,Elasticity of igneous rocks at high temperatures and pressures. Geol. Soc. Amer. Bull., v. 54, pp. 263–285.

    Google Scholar 

  • —————, 1960,The velocity of compressional waves in rocks to 10 kilobars, Part I, J. Geoph. Res., v. 65, pp. 1083–1102.

    Google Scholar 

  • —————, 1965,Speculations on the Earth’s thermal history. Geol. Soc. Amer. Bull., v. 76, pp. 133–153.

    Article  Google Scholar 

  • Bullen, K. E., 1963,An Introduction to the Theory of Seismology, 3rd ed. Univ. Press, Cambridge, 381 pp.

    Google Scholar 

  • Clark, Jr., S. P., 1966,Thermal conductivity. Hb. Physical Constants (Clark, ed.), pp. 459–482, Geol. Soc. Amer. mem. 97.

  • Gutenberg, B., 1959,Wave velocity below the Mohorovicic discontinuity. Geoph. J., v. 2, pp. 348–352.

    Google Scholar 

  • Hughes, D. S., andCross, J. H., 1951,Elastic wave velocities in rocks at high pressures and temperatures, Geophysics, v. 16, pp. 577–593.

    Article  Google Scholar 

  • Jeffreys, H., 1959,The Earth, 4th ed., Univ. Press, Cambridge, 420 pp.

    Google Scholar 

  • Macdonald, G. J. F., 1959,Calculations on the thermal history of the Earth. J. Geoph. Res., v. 64, pp. 1967–2000.

    Google Scholar 

  • Machado, F., 1964,Sobre a constituição do interior da Terra. Rev. Fac. Cien. Lisboa, 2a. ser. C, v. 12, pp. 83–101.

    Google Scholar 

  • —————, 1966,Temperature and fractional melting in the upper mantle. Nature (London), v. 211, pp. 285–287.

    Article  Google Scholar 

  • Simmons, G., 1964,Velocity of shear waves in rocks to 10 kilobars. J. Geoph. Res., v. 69, pp. 1123–1130.

    Article  Google Scholar 

  • Wager, L. R., 1958,Beneath the Earth’s crust. Adv. Sci., v. 15, pp. 31–45.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Machado, F. Temperature and distribution of radioactive matter in the upper mantle. Bull Volcanol 32, 403–413 (1968). https://doi.org/10.1007/BF02599780

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02599780

Keywords

Navigation