The diversity of sources of late Archean granites reflects a transition from plume-dominated to plate tectonics in the Superior Province, Canada

Author:

Ackerman Lukáš,Žák Jiří,Kachlík Václav,Svojtka Martin,Tomek Filip,Santolík Václav,Sláma Jiří,Trubač Jakub,Strnad Ladislav,Vacek František

Funder

Univerzita Karlova v Praze

Center for Geosphere Dynamics, Charles University

Czech Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference125 articles.

1. Origin of the Archean leucogranodiorite–granite suites: Evidence from the Rio Maria terrane and implications for granite magmatism in the Archean;Almeida;Lithos,2010

2. Formation and evolution of the continental crust;Arndt;Geochem. Perspect.,2013

3. Bandyayera, D., Daoudene, Y., 2018. Géologie de la région du lac Champion, sous-provinces de La Grande et de Nemiscau, à l’est de Waskaganish, Municipalité Eeyou Istchee Baie-James, Québec, Canada. Ministère de l’Énergie et des Ressources naturelles, Québec. Bulletin géologique (https://gq.mines.gouv.qc.ca/bulletins-geologiques/lac-champion/).

4. Evolution and tectonic significance of intermediate to felsic plutonism associated with the Hemlo greenstone belt, Superior Province;Beakhouse;Canada. Precambr. Res.,2005

5. Archaean cratonization and deformation in the northern Superior Province, Canada: An evaluation of plate tectonic versus vertical tectonic models;Bédard;Precambr. Res.,2003

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