Contributo alla conoscenza delle caratteristiche sismiche dell'Iran settentrionale
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Abstract
Proseguendo nello studio delle caratteristiche sismiche del massiccioiraniano, si determinano i dati ipocentrali e l'ora origine del terremoto del2 luglio 1957 avvenuto a N di Teheran. Si è quindi indagato sulla naturadel movimento sismico giungendo alla conclusione che trattasi di una frattura-,di essa sono stati calcolati gli elementi caratteristici. Analogo studiocondotto per il terremoto di Farsinaj del 13 Dicembre 1957, ha mostratoche anche per esso trattasi di una frattura.
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How to Cite
Peronacci, f. (1959) “Contributo alla conoscenza delle caratteristiche sismiche dell’Iran settentrionale”, Annals of Geophysics, 12(4), pp. 523–534. doi: 10.4401/ag-5735.
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