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- W1601103634 abstract "In the northern portion of the Sierra de Valle Fertil, there are migmatite rocks which have been classify as metatexite and diatexite according to their fabric, and as pelitic and semipelitic-greywacke in function of their protoliths. Field relationships and a detail structural analysis of the migmatites and the resisters associated to them, allow constraining the presence of pre-migmatitic structures (S 0 -S R ) interpreted as sedimentary stratification and a relictic metamorphic foliation with static recrystallization. Also, the develop of migmatic fabrics (S 1a,b,c ) and (P 1a,b ), and the generation of anatectic granites, are associated to a deformational phase (D1) develop at high temperature conditions (granulite facies) and contemporary with the magmatismo. At least, postmigmatic fabrics (S 2a and S 2b ) related to a deformational event (D 2 ), shows an evolution under ductile-fragile conditions related to the close and exhumation stage of the Famatinian arc. This fabric is superimposed by a planar structure of fragile character. Thus, we establish that the Famatinian magmatic arc is developed in a thick sedimentary sequence, deposited and to consolidate since the medium Cambric. This sequence does not record a previous deformational history to the emplacement of Ordovician plutonism. In contrast, all the preserved structural features are related to metamorphism (migmatization) and exhumation during the arc stage." @default.
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- W1601103634 date "2012-06-15" @default.
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- W1601103634 title "ESTRUCTURA INTERNA DE LAS MIGMATITAS DE LA PORCIÓN NORTE DE LA SIERRA DE VALLE FÉRTIL, SAN JUAN" @default.
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