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Some remarks on continental drift

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Summary

The continental drift may be explained by an expanding Earth only. In fact, there is a differences in the rate of heat flow between continents and oceans. Principially, there is a possibility of deriving the value of ancient radii by palaeomagnetic and age measurements.

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References

  1. Jacobs J. A.: Nature, 185, p. 231 (1960).

    Google Scholar 

  2. Egyed L.: Acta Geol. Sc. Hung., IV, pp. 43–83 (1956).

    Google Scholar 

  3. Egyed L.: Geofisica pura e appl., 33, pp. 42–48 (1956).

    Google Scholar 

  4. Egyed L.: Geol. Rundschau, 46, pp. 101–121 (1957).

    Google Scholar 

  5. Egyed L. &Stegena L.: Zeitschrift für Geophysik, 24, pp. 260–267 (1958).

    Google Scholar 

  6. von Herzen R.: Nature, 183, pp. 882 (1953).

    Google Scholar 

  7. Heezen B.: Am. Geoph. Un. Trans., 38, p. 394 (1957).

    Google Scholar 

  8. Contini C.: Annali di Geofisica, IX, pp. 561–575 (1956).

    Google Scholar 

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Egyed, L. Some remarks on continental drift. Geofisica Pura e Applicata 45, 115–116 (1960). https://doi.org/10.1007/BF01996578

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  • DOI: https://doi.org/10.1007/BF01996578

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