The stratigraphic and structural analysis carried out along the Corfù Line indicates the space orientation of the stress ellipsoid and the age of the different tectonic phases. The data show evidence for a Burdigalian ENE-trending compressional phase and one or more neotectonic events (Pliocene-Quaternary).
Geologia della zona trascorrente di Corf� (Grecia)
CAPUTO, Riccardo
1984
Abstract
The stratigraphic and structural analysis carried out along the Corfù Line indicates the space orientation of the stress ellipsoid and the age of the different tectonic phases. The data show evidence for a Burdigalian ENE-trending compressional phase and one or more neotectonic events (Pliocene-Quaternary).File in questo prodotto:
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