Fe-isotope fractionation during partial melting on Earth and the current view on the Fe-isotope budgets of the planets (reply to the comment of F. Poitrasson and to the comment of B.L. Beard and C.M. Johnson on "Iron isotope fractionation during planetary differentiation" by S. Weyer, A.D. Anbar, G.P. Brey, C. Münker, K. Mezger and A.B. Woodland)

Earth and Planetary Science Letters

Volumn 256, Issue 3-4, 2007, Pages 638-646

  Weyer, S ^a   Anbar, A D ^b   Brey, G P ^a   Munker C ^c   Mezger, K ^d   Woodland, A B ^a  

^a GOETHE UNIVERSITY   (Germany)

^b ARIZONA STATE UNIVERSITY   (United States)

^c UNIVERSITY OF BONN   (Germany)

^d UNIVERSITY OF MÜNSTER   (Germany)

Author keywords

core formation; iron isotopes; mantle; partial melting; planets; solar system

Indexed keywords

GEOCHEMISTRY; GEOMORPHOLOGY; IRON; SILICATES; STRUCTURAL GEOLOGY;

ISOTOPE FRACTIONATION; PARTIAL MELTING; PLANETARY DIFFERENTIATION; SILICATE DIFFERENTIATION;

EARTH (PLANET);

BASALT; CRUSTAL STRUCTURE; EARTH; IRON; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; MARS; MOON; PARTIAL MELTING; SOLAR SYSTEM; UPPER MANTLE;

EID: 34047178399     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2007.01.038     Document Type: Note

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