Boninite-like volcanic rocks in the 3.7–3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth

Polat, A.; Hofmann, A.W.; Rosing, M.T.

doi:10.1016/S0009-2541(01)00363-1

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Boninite-like volcanic rocks in the 3.7–3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth

Author(s): A Polat , A.W Hofmann , M.T Rosing

Publication date Created: April 2002

Publication date (Print): April 2002

Journal: Chemical Geology

Publisher: Elsevier BV

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Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes

W. F. McDonough, S.-s. Sun (1989)

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Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

Albrecht Hofmann (1988)

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Tectonic setting of basic volcanic rocks determined using trace element analyses

J.R. Cann, J.A. Pearce (1973)

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Title: Chemical Geology

Abbreviated Title: Chemical Geology

Publisher: Elsevier BV

ISSN (Print): 00092541

Publication date Created: April 2002

Publication date (Print): April 2002

Volume: 184

Issue: 3-4

Pages: 231-254

Article

DOI: 10.1016/S0009-2541(01)00363-1

SO-VID: 5b61c8f2-0fd0-4260-91b7-6e5658697539

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Boninite-like volcanic rocks in the 3.7–3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth

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IODP Expedition 400: NW Greenland Glaciated Margin

Most cited references 56

Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes

Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

Tectonic setting of basic volcanic rocks determined using trace element analyses

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