Insights into the geometry and faulting style of the causative faults of the M6.7 1805 and M6.7 1930 earthquakes in the Southern Apennines (Italy) from coseismic hydrological changes

Author:

Cucci L.ORCID

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference81 articles.

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4. Normal faulting along the western side of the Matese Mountains: implications for active tectonics in the Central Apennines (Italy);Boncio;J. Struct. Geol.,2016

5. A mechanism for sustained groundwater pressure changes induced by distant earthquakes;Brodsky;J. Geophys. Res.,2003

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