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

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Publication date

December 2015

DOI

10.1144/SP389.5

Publisher

Geological Society of London

Journal

Geological Society London Special Publications

Abstract

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 in

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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

Abstract

Extracted data

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

Abstract

Extracted data

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