La sismicita del « Campo fagliato » dell'Aterno
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Abstract
After determining the epicentral coordinates, the originhour,
the depth, and the dromochrones of the earthquaqe of June 24, 1958,
at L'Aquila, the physical nature of the quake at its hypocentre is esamined,
thus completing a lifting scheme. The comparison between the seismic, geological,
and tectonic nature of the Aterno valley supplies, together with the
results of the above-mentioned micro-seismic study, a probable explanation
of the faulted field.
the depth, and the dromochrones of the earthquaqe of June 24, 1958,
at L'Aquila, the physical nature of the quake at its hypocentre is esamined,
thus completing a lifting scheme. The comparison between the seismic, geological,
and tectonic nature of the Aterno valley supplies, together with the
results of the above-mentioned micro-seismic study, a probable explanation
of the faulted field.
Article Details
How to Cite
1.
DI FILIPPO D, PERONACI F. La sismicita del « Campo fagliato » dell’Aterno. Ann. Geophys. [Internet]. 1964Nov.25 [cited 2021Sep.28];17(1):195-210. Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/5206
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