Riassunto
Si esamina il regime termico negli strati superiori della crosta terrestre in alcuni casi elementari di discontinuità del materiale, nonchè nell'ipotesi di una superficie esterna sagomata a gradino, traendone deduzioni atte a facilitare l'interpretazione ed a valorizzare i dati geotermici.
Summary
In the present paper the thermal conditions in the heigher layer of the earth's crust are examined, in some elementary cases with discontinuity of the material as well as when the external surface presents a step. The results may facilitate the interpretation and application of the geothermic data.
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Note Bibliografiche
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H. Jeffreys,The Disturbance of the Temperature Gradient in the Earth's Crust by inequalities of Height, Monthly Notices R. Astr. Soc. Geophys. Suppl. p. 309, January 1938.
A. Nadai Theory of Flow and Fracture of Solids, vol. I, McGraw-Hill, New York (1950).
H. Reich &R. v. Zwerger,Taschenbuch der angewandten Geophysik, p. 392, Akadem. Verlagsgesell., Leipzig 1943.
E. C. Bullard inLandolt-Börstein Zahlenwerte und Funktionen, Vol. III, p. 385, Springer-Verlag, Berlin 1952.
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Sbrana, F., Bossolasco, M. Sul regime termico degli strati superiori della crosta terrestre. Geofisica Pura e Applicata 23, 21–26 (1952). https://doi.org/10.1007/BF01992453
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DOI: https://doi.org/10.1007/BF01992453