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The Spread of the Continents

Published online by Cambridge University Press:  01 May 2009

G. F. S. Hills
Affiliation:
63 West End Avenue, Pinner, Middx.

Abstract

It is generally accepted that the continents contain more radio-activity than the Pacific floor. The two continents, Laurasia and Gondwanaland, would therefore expand the rocks below, relative to that floor. The plastic substratum under the continents would be forced higher in their centres than at their centres than at their Pacific margins. It would creep towards those margins and would carry part of the overlying granite to them, piling it high at their margins and thinning it at their centres. The plastic substratum would continually carry its heat to the cold Pacific substratum and render it plastic into which the continents would be impelled.

Type
Articles
Copyright
Copyright © Cambridge University Press 1953

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References

REFERENCES

Bullen, K. E., 1936. M.N.R.A.S., Geophysical Supp. (April), p. 400.Google Scholar
Field, R. M., 1936. Amer. Geophys. Union Trans., 2023.Google Scholar
Gregory, J. W., 1930. Quart. Journ. Geol. Soc., lxxii–cxxxvi.Google Scholar
Gutenberg, B., 1936. Bull. Geol. Soc. Amer., xlvii, 15871610.CrossRefGoogle Scholar
Gutenberg, B., 1939. Internal Constitution of the Earth, p. 210.Google Scholar
Hills, G. F. S., 1947. The Formation of the Continents by Convection. (London.)Google Scholar
Jeffreys, H., 1932. M.N.R.A.S., Geophysical Supp. (May), p. 59.Google Scholar
Jeffreys, H., 1939. Deep Focus Earthquakes. Ergebnisse der Kosmischen Physik, iv, 103.Google Scholar