The asymmetries between W-directed (e.g. Apennines) and E- or NE- directed (e.g. Alps) subduction zones are robust features of a polarized geodynamics and they can be ascribed to the generalized westward drift of the lithosphere relative to the underlying mantle.
The Alps and the deep revolution against standard plate tectonics: polarized plate tectonics.
PANZA, GIULIANO;BRANDMAYR, ENRICO;ROMANELLI, Fabio
2015
Abstract
The asymmetries between W-directed (e.g. Apennines) and E- or NE- directed (e.g. Alps) subduction zones are robust features of a polarized geodynamics and they can be ascribed to the generalized westward drift of the lithosphere relative to the underlying mantle.File in questo prodotto:
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