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Viozene shear zone

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Journal Article
Published: 01 October 2014
Italian Journal of Geosciences (2014) 133 (3): 445–454.
... the Colle di Tenda region to the West and Triora to the South-East ( figs. 1 and 2 ). The geometric arrangement of the tectonic units occurring in this area is due to a major transpressive shear zone (Limone-Viozene Zone-LiVZ, P iana et alii , 2009 ) that is connected to NW (Gardetta Pass-Demonte region...
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Journal Article
Published: 01 June 2009
Italian Journal of Geosciences (2009) 128 (2): 353–366.
... of its stratigraphic and structural feature are still in progress. The Verzera shear zone and the Viozene deformation zone are the most important tectonic boundaries of CELB, because they are the most laterally persistent structures marking the largest differences in strain and metamorphism...
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Image
a)  Geological sketch of Ligurian Alps;  b)  Schematic NE-SW section (AA’) ...
Published: 01 June 2009
: Argentera Massif; CM: Calizzano Massif; PPU: Pre-Piedmont Units; HF: Helminthoides Flysch; DD: Dauphinois Domain; VIDZ: Viozene deformation zone; CHFZ: Chiusetta fault zone; UPFZ: Upega fault zone; VZSZ: Verzera shear zone (modified from S eno et alii , 2005a ). a) Schema geologico delle Alpi Liguri
Journal Article
Published: 01 August 2017
Environmental and Engineering Geoscience (2017) 23 (3): 179–190.
... are unconformably overlain by Triassic to Early Cretaceous carbonates, which are mostly detached above Late Triassic evaporites, with the basement-cover contact mainly striking NW-SE ( Guglielmetti et al., 2013 ). The AM is characterized by Alpine-stage ductile shear zones and strike-slip and reverse faults...
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