The Maiella Massif is the outermostcarbonate anticline of the central Apennines, and it is considered as the epicentral areas of two major historical earthquakes: the 1706 (Maw=6.60) and 1933 (Maw=5.57) events.
Active faulting in the Maiella massif (Central Apennines, Italy)
Messina P;Giaccio B;Sposato A
2010
Abstract
The Maiella Massif is the outermostcarbonate anticline of the central Apennines, and it is considered as the epicentral areas of two major historical earthquakes: the 1706 (Maw=6.60) and 1933 (Maw=5.57) events.File in questo prodotto:
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