Abstract
Structural deformation of the island of Hvar allows three tangential tectonic phases to be determined: the Laramian (F I), the Pyrenean, ( F II) and the Neotectonic phase (F III ). Preserved relics of Laramian and Pyrenean folds with intact structural elements, indicates that the Neotectonic orientation of structures (E-W) is a consequence of refolding of the older structural fabric, rather than horizontal rotation.
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