LOCATELLI M.

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Eclogite-facies breccias from the Monviso metaophiolite complex (N-Italy and W-Alps) represent a unique opportunity to study the triggering mechanisms for transient brittle deformation at eclogite-facies conditions in ductilely deforming subducted oceanic lithosphere. Here the intact foliation of Fe-Ti-rich and Mg-Al-rich metagabbro clasts,...

The northern termination of the Transantarctic Mts in North Victoria Land is characterized by a complex architecture deriving from long-lived tectonic activity along major crustal shear zones that have been reactivated several times until Recent. These are both first-order faults, which separate the Wilson, Bowers and Robertson Bay crustal...

North Victoria Land (NVL), located at the Pacific-Southern Ocean termination of the Transantarctic Mountains (TAM), presents a complex architecture deriving from a long-lasting tectonic evolution. After the Paleozoic juxtaposition to the East Antarctic craton, NVL was affected by i) the Gondwana breakup which led to the Meso-Cenozoic...