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THE F GRANITIC GNEISS, IN THE CENTRAL PART OF THE PALEOPROTEROZOICMINEIRO BELT, SW SO FRANCISCO CRATON: U-PB GEOCHRONOLOGY, SM-ND ISOTOPIC GEOCHEMISTRY AND TECTONIC IMPLICATIONS
The present work deals with the magmatic evolution of the F granitic gneiss, one of the plutons that crop out in the central part of the Mineiro belt.
Reference:
Organization:
Geochronological Research Center of the University of So Paulo, SP, Brazil.
Brazil
Geochronological Research Center of the University of So Paulo, SP, Brazil.
Brazil
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