Transition from subduction to Post-Collisional Paleoproterozoic magmatism in the Correntina erosive window of the north São Francisco craton: Evidence for mantle source and slab breakoff from alkaline magmatism by U-Pb, Nd-Sr radiometric and geochemistry data-Reference-Cited by-同舟云学术

Transition from subduction to Post-Collisional Paleoproterozoic magmatism in the Correntina erosive window of the north São Francisco craton: Evidence for mantle source and slab breakoff from alkaline magmatism by U-Pb, Nd-Sr radiometric and geochemistry data

Published:2021-08 Issue: Volume:362 Page:106314
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Barbosa N.,Debruyne D.,Barbosa N.S.,Luciano R.L.,Guedes T.R.S.,Reis C.,Barbosa J.S.F.,Pinho I.C.A.,Santos R.L.,Brito R.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference111 articles.

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5. Chemical variations and regional diversity observed in MORB;Arevalo;Chem. Geol.,2010

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