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The emergence of the Eoarchaean proto-arc: evolution of a c. 3700 Ma convergent plate boundary at Isua, southern West Greenland

Nutman, Allen P; Bennett, Victoria; Friend, Clark


Eoarchaean juvenile crust formed as 'proto-arcs'. The northern side of the Isua supracrustal belt is an archetypal proto-arc, with ≥3720 Ma boninites, c. 3720 Ma basalts and gabbros, 3720-3710 Ma andesites, diorites and mafic tonalites, 3710-3700 Ma int

CollectionsANU Research Publications
Date published: 2013
Type: Journal article
Source: Geological Society of London Special Publication
DOI: 10.1144/SP389.5


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