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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.
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