Linked evolution and in situ growth of the Wabigoon superterrane, Superior Craton: evidence from zircon U-Pb isotopes and whole-rock geochemistry-Reference-Cited by-同舟云学术

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Linked evolution and in situ growth of the Wabigoon superterrane, Superior Craton: evidence from zircon U-Pb isotopes and whole-rock geochemistry

Published:2024-05 Issue: Volume:404 Page:107341
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Bjorkman Katarina E.,Lu Yongjun,Campbell McCuaig T.,Kemp Anthony I.S.,Hollings Pete

Funder

Society of Economic Geologists Foundation

Australian Research Council Centre of Excellence for Core to Crust Fluid Systems

Publisher

Elsevier BV

Reference169 articles.

1. The intensity, occurrence, and duration of superplume events and eras over geological time;Abbott;J. Geodyn.,2002

2. Archaean greenstone belts and associated granitic rocks – a review;Anhaeusser;J. Afr. Earth Sc.,2014

3. Neoarchean evolution of differing convergent margin assemblages in the Wabigoon Subprovince: geochemical and geochronological evidence from the Lake of the Woods greenstone belt, Superior Province, Northwestern Ontario;Ayer;Precambr. Res.,1997

4. Metallogeny of granitoid rocks in the Canadian Shield;Ayres;Can. Mineral.,1982

5. Neoarchean supra-subduction gold in Mesoarchean tonalite-granodiorite: Two separate mineralization events at Hammond Reef defined by disseminated and channelized fluid flow;Backeberg;Precambr. Res.,2018

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1. Is plate tectonics a post-Archean phenomenon? A petrological perspective;Journal of the Geological Society;2024-08-27

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