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Iron isotopes may reveal the redox conditions of mantle melting from Archean Nicolas Dauphas a,b,
 

Summary: Iron isotopes may reveal the redox conditions of mantle melting from Archean
to Present
Nicolas Dauphas a,b,
, Paul R. Craddock a
, Paul D. Asimow b
, Vickie C. Bennett c
,
Allen P. Nutman d
, Daniel Ohnenstetter e
a
Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, USA
b
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA
c
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
d
Institute of Geology and Chinese International Centre for Precambrian Research, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing, 100037, China
e
Centre de Recherches Pétrographiques et Géochimiques, CNRS-Université de Nancy, 15 rue Notre-Dame-des-Pauvres, 54501 Vandoeuvre-lès-Nancy, France
a b s t r a c ta r t i c l e i n f o

  

Source: Asimow, Paul D. - Division of Geological and Planetary Sciences, California Institute of Technology,

 

Collections: Geosciences