Sources of granite magmatism in the Embu Terrane (Ribeira Belt, Brazil): Neoproterozoic crust recycling constrained by elemental and isotope (Sr-Nd-Pb) geochemistry

Author:

Alves Adriana,Janasi Valdecir de Assis,Campos Neto Mario da Costa

Funder

FAPESP

CAPES

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference44 articles.

1. Kinematic evolution of the Araçuaí-West Congo orogen in Brazil and Africa: Nutcracker tectonics during the Neoproterozoic assembly of Gondwana;Alkmim;Precambrian Res.,2006

2. Microgranitic enclaves as products of self-mixing events: a study of open-system processes in the Mauá Granite, São Paulo, Brazil, based on in situ isotopic and trace elements in plagioclase;Alves;J. Petrol.,2009

3. U-Pb geochronology of the granite magmatism in the Embu Terrane: implications for the evolution of the Central Ribeira Belt, SE Brazil;Alves;Precambrian Res.,2013

4. Metodologia Isotópica Pb/Pb. Aplicação aos migmatitos e rochas associadas da região de São José dos Campos;Babinski,1988

5. U-Pb SHRIMP zircon ages of migmatites from the basement of the Embu Complex, Ribeira Fold Belt, Brazil: indications for ∼1.4–1.3 Ga Pb-Pb and Rb-Sr “isochron” ages of no geological meaning;Babinski,2001

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