ARCHITECTURE AND EVOLUTION OF THE ALPINE-MEDITERRANEAN COLLISION ZONE
The transition from subduction driven by overall Africa-Europe plate convergence (“hard collision”) to subduction induced by the negative buoyancy of the subducting slab (“soft collision”) led to a more dramatic reorganization within the Western Mediterranean realm starting in latest Eocene times. This reorganization led to the opening of large new oceanic domains in the Western Mediterranean while old branches of Alpine Tethys totally disappeared by subduction or obduction, and additionally, to a reversal of subduction polarity affecting the SW intra-oceanic prolongation of the former Alps (Handy et al 2010). Rollback subduction of the Ligurian part of Alpine Tethys attached to the Adria microplate involved the formation of the eastward retreating Calabrian arc since about 35 Ma ago, linked to orogeny in the Apennines and Northern Africa. The westward retreating Gibraltar arc represents a second arc-trench system. These reorganizations were driven primarily by the pull of the gravitationally unstable, retreating oceanic parts of the Adriatic and African slabs during slow convergence of Africa and Europe.
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