The emergence of the Eoarchaean proto-arc: evolution of a c. 3700 Ma convergent plate boundary at Isua, southern West Greenland
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Nutman, Allen P
Bennett, Victoria
Friend, Clark
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Geological Society of London
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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
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Geological Society of London Special Publication
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2037-12-31
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