Diversity of Rhyacian granitoids in the basement of the Neoproterozoic-Early Cambrian Gurupi Belt, northern Brazil: Geochemistry, U-Pb zircon geochronology, and Nd isotope constraints on the Paleoproterozoic magmatic and crustal evolution

Precambrian Research

Volumn 220-221, Issue , 2012, Pages 192-216

  Klein, Evandro L ^a   Rodrigues, Joseneusa B ^b   Lopes, Elem C S ^a   Soledade, Gilvana L ^a,c,d  

^a CPRM/Geological Survey of Brazil   (Brazil)

^b CPRM Geological Survey of Brazil   (Brazil)

^c FEDERAL UNIVERSITY OF PARÁ   (Brazil)

^d VALE S A   (Brazil)

Author keywords

Collision; Granitoid magmatism; Gurupi Belt; Neoproterozoic; Paleoproterozoic; U Pb

Indexed keywords

ARCHEAN; BIOTITE; CAMBRIAN; CRUSTAL EVOLUTION; DEFORMATION; EMPLACEMENT; GEOCHRONOLOGY; GRANITOID; MAGMATISM; METAMORPHISM; MONZONITE; MUSCOVITE; NEODYMIUM ISOTOPE; PLUTONIC ROCK; POTASSIC ROCK; PROTEROZOIC; URANIUM-LEAD DATING;

BRAZIL;

CANTAO; RHYACIA;

EID: 84865985163     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.precamres.2012.08.007     Document Type: Article

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