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Shaking
We analyzed the capability of the Anghiari fault (Upper Tiber Valley, Northern Apennines of Italy) to reach and break the topographic surface during a strong earthquake. The paleoseismological data revealed the seismic history of the Anghiari fault, assessing its capability to recurrently break the surface during strong earthquakes.
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The first Italian study on the probability of surface faulting of a dam with strategic importance is presented at the Ministry of Infrastructure and Transport
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