TEMPI DI TRAGITTO DELLE ONDE P* E SPESSORE DELLO STRATO DEL GRANITO NELL'ITALIA CENTRALE
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Abstract
Proseguendo lo studio del terremoto del Gran Sasso d'Italia del5 settembre 1950 si rilevano alcune caratteristiche sismiche dell'Italiacentrale.Si determina la profondità ipocentrale con il metodo dell'angolodi emergenza. Indi si costruisce la dromocrona delle P* e si calcolalo spessore dello strato del granito relativamente alla zona.
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DI FILIPPO D, Marcelli L. TEMPI DI TRAGITTO DELLE ONDE P* E SPESSORE DELLO STRATO DEL GRANITO NELL’ITALIA CENTRALE. Ann. Geophys. [Internet]. 1951Nov.25 [cited 2022Sep.28];4(4):579-8. Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/5931
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