Comment on: ‘Growth and recycling of early Archaean continental crust: geochemical evidence from the Coonterunah and Warrawoona groups, Pilbara Craton, Australia’ by Green, M.G. et al. (Tectonophysics 322, 69-88)

2002 ◽  
Vol 344 (3-4) ◽  
pp. 289-292 ◽  
Author(s):  
Robert Bolhar ◽  
Jon D Woodhead ◽  
Janet M Hergt
Keyword(s):  
Continental Crust ◽  
Geochemical Evidence ◽  
Pilbara Craton

scholarly journals Non-subduction petrological mechanisms for the growth of the neoarcheam continental crust of the Kola–Norwegian terrane, Fennoscandian shield: geological and isotope-geochemical evidence

2019 ◽  
Vol 27 (2) ◽  
pp. 161-186
Author(s):  
A. B. Vrevskii
Keyword(s):  
Continental Crust ◽  
Greenstone Belt ◽  
Geochemical Modeling ◽  
Volcanic Rocks ◽  
Fennoscandian Shield ◽  
Crustal Growth ◽  
Calc Alkaline ◽  
Geochemical Evidence

The paper reports new data on the composition and age of the Neoarchean calc-alkaline volcanic rocks of the Uraguba–Kolmozero–Voron’ya greenstone belt (UKV GB). Petrological-geochemical modeling indicates a polygenetic origin of primary melts of the basalt–andesite–dacite association and non-subduction geodynamic mechanisms for the crustal growth in the largest greenstone belt of the Kola–Norwegian Block of the Fennoscandian shield.

Geochronological and geochemical evidence of continental crust ‘relamination’ in the origin of intermediate arc magmas

Lithos ◽  
2018 ◽  
Vol 322 ◽  
pp. 52-66 ◽  
Author(s):  
Arturo Gómez-Tuena ◽  
José G. Cavazos-Tovar ◽  
Mattia Parolari ◽  
Susanne M. Straub ◽  
Ramón Espinasa-Pereña
Keyword(s):  
Continental Crust ◽  
Geochemical Evidence ◽  
Arc Magmas
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