Rubio Pascual, F. J.Arenas, R.Díaz García, F.2017-11-062017-11-061992http://hdl.handle.net/10272/14123The syn-D2 uplift of the Santiago Unit, inmediately after of the high-pressure eo-Hercynian metamorphic event, cause a markedly decompressive-slightly prograde P,T,t path. This path very likely suggests that the majority of the rising history of the unit took place in a context of ductile extension, related to the continued underplating of the continental margin of Condwana and compensating extension above. The actual disposition of the syn-D2 metamorphic zones is inverse, w ith the staurolite zone (which represents the thermal peak) occupying the top o f the unitspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/High-pressure eo-Hercynian metamorphismPTT evolutionInverted metamorphic gradientAllochthonous ComplexesGaliciajournal articleopen access