Abstract (EN):
Mindelo Migmatitic Complex outcrops in the coastal-zone, north of Porto. This complex consists on a set of diverse lithologies including metasedimentary, migmatitic and granitic rocks, and pegmatite veins. Field relationships, petrography, geochemistry and isotopic signature of these lithologies allow inferring the sequence of anatectic processes that are responsible for the lithological heterogeneity. The melting occurred at different structural levels, and thus at different pressure and temperature conditions, generating rocks with specific characteristics: i) in shallow levels (<3.5 Kbar) metatexites are produced essentially by water-saturated melting followed by water-undersaturated biotite melting. Leucogranites resulted from migration of leucosomes; (ii) in slightly deeper levels the melting rate is higher which leads to the formation of diatexites that intruded metatexites; (iii) in even deeper levels (~ 5 Kbar) higher pressure and temperature permit the melting of muscovite producing a large amount of typical two-mica granite melts. This material rises in the crust and incorporates abundant xenoliths forming a very heterogeneous granitic body. In subsolidus conditions, structurally controlled metasomatic processes lead to feldspatization of migmatites and granitoids. Later, installation of aplite-pegmatites and local tourmalinization previously formed granitoids took place. © 2014 LNEG ¿ Laboratório Nacional de Geologia e Energia IP.
Language:
Portuguese
Type (Professor's evaluation):
Scientific