Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present

Earth and Planetary Science Letters

Volumn 288, Issue 1-2, 2009, Pages 255-267

  Dauphas, Nicolas ^a,b   Craddock, Paul R ^a   Asimow, Paul D ^b   Bennett, Vickie C ^c   Nutman, Allen P ^d   Ohnenstetter, Daniel ^e  

^a UNIVERSITY OF CHICAGO   (United States)

^b CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

^c AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^d INSTITUTE OF GEOLOGY   (China)

^e UNIVERSITÉ DE LORRAINE   (France)

Author keywords

Archean; iron; island arc; isotope; mantle; melting; redox

Indexed keywords

ARCHEAN; BASALTIC MAGMA; BONINITES; BUFFERING CAPACITIES; BULK SILICATE EARTH; EARLY EARTH; HIGH-PRECISION; IRON ISOTOPES; IRON ISOTOPIC COMPOSITIONS; ISLAND ARC; ISOTOPE FRACTIONATION; ISOTOPIC DATA; ISOTOPIC FRACTIONATIONS; MAGMA GENESIS; MANTLE; MANTLE MELTING; MANTLE SOURCE; MID-OCEAN RIDGES; NEW APPROACHES; OCEANIC CRUST; OCEANIC ISLAND BASALTS; PARTIAL MELTING; QUANTITATIVE MODELS; REDOX; REDOX CONDITION;

ABUTMENTS (BRIDGE); BASALT; CAVITY RESONATORS; GALLIUM; MELTING; OCEANOGRAPHY; SILICATES;

ISOTOPES;

ARCHEAN; IRON; ISLAND ARC; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; MAGMA; MANTLE CHEMISTRY; MID-OCEAN RIDGE BASALT; OCEAN ISLAND BASALT; PARTIAL MELTING; REDOX CONDITIONS;

EID: 70350786277     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2009.09.029     Document Type: Article

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