In the Salerno district large scale extensional tectonics on low angle detachment faults has produced a significant thinning and the dismemberment of the Mesozoic carbonate platform successions that compose the thrust belt in this region. The geometrical characteristics and kinematics of this extensional detachment array have been reconstructed through detailed structural mapping on land and the integration of offshore seismic lines and stratigraphic analyses.
Stratigraphic and structural setting of the Salerno area
2006
Abstract
In the Salerno district large scale extensional tectonics on low angle detachment faults has produced a significant thinning and the dismemberment of the Mesozoic carbonate platform successions that compose the thrust belt in this region. The geometrical characteristics and kinematics of this extensional detachment array have been reconstructed through detailed structural mapping on land and the integration of offshore seismic lines and stratigraphic analyses.File in questo prodotto:
Non ci sono file associati a questo prodotto.
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
