Imaging the roots of a post-collisional pluton: Implications for the voluminous Cambrian magmatism in the Araçuaí orogen (Brazil)

Author:

Souza Junior G.F.,Trindade R.I.F.,Temporim F.A.,Bellon U.D.,Gouvêa L.P.,Soares C.C.,Amaral C.A.D.,Louro V.

Funder

ASCRS Research Foundation

FAPESP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference78 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. Sobre a Evolução Tectônica do Orógeno Araçuaí-Congo Ocidental;Alkmim;Geonomos,2007

3. Geophysical imaging of the shape of granitic intrusions at depth: a review;Améglio;Geol. Soc. Spec. Publ.,1999

4. Granite pluton geometry and emplacement mode inferred from combined fabric and gravity data;Améglio,1997

5. Midcrust deformation regime variations across the Neoproterozoic Araçuaí hot orogen (SE Brazil): insights from structural and magnetic fabric analyses;Angelo;J. Struct. Geol.,2020

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