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Mapping upper mantle anisotropy beneath SE France by SKS splitting indicates Neogene asthenospheric flow induced by Apenninic slab roll-back and deflected by the deep Alpine roots.
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Mapping upper mantle anisotropy beneath SE France by SKS splitting indicates Neogene asthenospheric flow induced by Apenninic slab roll-back and deflected by the deep Alpine roots.

Guilhem Barruol, Anne Deschamps et Olivier Coutant
Tectonophysics, Vol.394(1-2), pp.125-138
2004

Résumé

Massif Central hotspot Alpine collision Western Mediterranean Asthenosphere Anisotropy Shear wave splitting

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