The presence of clorithic nodules inside Iow grade metamorphic rocks (Purbecl<-Weald facies), to the NE ofAgreda (Soria), has allowëd to characterize, by means of the Rf/Ø technique, an oblate strain ellipsoid with The moderate rate of shortening that this type of ellipsoid imp/ies has a close relationship with the macroestructura/ features
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