Neoarchean and Rhyacian TTG-Sanukitoid suites in the southern São Francisco Paleocontinent, Brazil: Evidence for diachronous change towards modern tectonics
Author:
Funder
FAPERJ
CNPQ
CAPES
FINEP
Publisher
Elsevier BV
Subject
General Earth and Planetary Sciences
Reference110 articles.
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2. Kinematic evolution of the Araçuaí-West Congo orogeny in Brazil and Africa: nutcracker tectonics during the Neoproterozoic assembly of Gondwana;Alkmim;Precambrian Res.,2006
3. Outline of the geology of Quadrilátero Ferrífero;Alkmim,2006
4. The Paleoproterozoic Mineiro belt and the Quadrilátero Ferrífero;Alkmim,2017
5. Proterozoic first-order sedimentary sequences of the São Francisco craton, eastern Brazil;Alkmim;Mar. Petrol. Geol.,2012
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1. An oblique transpressive soft-collision records the amalgamation of the Siderian-Orosirian Mineiro belt (Brazil) and the São Francisco paleo-craton (Kenorland Supercontinent): Insights from the Bom Sucesso metasedimentary sequence;Journal of South American Earth Sciences;2024-10
2. Reply to comment on “The passive margin of the southern São Francisco paleocontinent, metamorphic record and implications for the assembly of West Gondwana: Evidence from the Lima Duarte Nappe, Ribeira orogen (SE Brazil)” by Trouw and Ribeiro;Precambrian Research;2024-09
3. The Congonhas-Itaverava Shear Zone in the Southern São Francisco craton: Implications for the Rhyacian amalgamation in the Minas-Bahia orogen;Journal of South American Earth Sciences;2024-07
4. Rhyacian-Orosirian transitional arc-collisional magmatism in the Archean Piedade Microcontinent, southern São Francisco Paleocontinent, Brazil;Precambrian Research;2024-05
5. Evidence of Siderian juvenile-like contribution to the continental arc magmatism in the Western Guanambi-Correntina block, São Francisco Craton (Brazil);Journal of South American Earth Sciences;2024-05
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