Metadata
Author: ParaCrawl Corpus
Data
English[en]
The unroofing took place locally under an inverted temperature gradient, caused by a detachment which carried a part of the hot mantle wedge, above the subduction zone, over the Subduction and syn-collisional exhumation of a Paleozoic continental margin: an integrated study based on structures and P-T paths of the Basal Units Resumen
Spanish[es]
La denudación tectónica se produjo localmente bajo un gradiente inverso de temperatura, causado por un despegue que puso en contacto una parte de la cuña mantélica caliente, situada por encima de la zona de subducción, con las unidades subducidas URI