Active faulting in the Maiella massif (Central Apennines, Italy)

Academic Article
Publication Date:
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.
Iris type:
01.01 Articolo in rivista
List of contributors:
Authors of the University:
Handle:
https://iris.cnr.it/handle/20.500.14243/83461
Published in:
GEOACTA
Journal