Fig. 4
a Distribution of different types of granitoids in the Iberian Peninsula, after Bard et al. (1971). GA autochthonous anatectic granodiorites, LP parautochthonous leucogranites, LA allochthonous leucogranites, GP early granodiorites, GT late granodiorites. Coordinates and scale have been added. b Distribution of Variscan gneiss domes and granitoids in the Iberian Massif. The dashed line enveloping the gneiss domes and abundant synkinematic granitoids probably marks the original limit of the northwest Iberian allochthon