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Rare earth element partitioning between sulphides and melt: Evidence for Yb2+ and Sm2+ in EH chondrites

  • Published:2019-11 Issue: Volume:265 Page:182-197
  • ISSN:0016-7037
  • Container-title:Geochimica et Cosmochimica Acta
  • language:en
  • Short-container-title:Geochimica et Cosmochimica Acta

Author:

Ingrao N.J.,Hammouda T.,Boyet M.,Gaborieau M.,Moine B.N.,Vlastelic I.,Bouhifd M.A.,Devidal J.-L.,Mathon O.,Testemale D.,Hazemann J.-L.,Proux O.ORCID

Funder

European Research Council

European Synchrotron Radiation Facility

Centre National de la Recherche Scientifique

Agence Nationale de la Recherche

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference72 articles.

1. Trace element geochemistry of enstatite chondrites: the so-called “Refractory Lithophile” elements;Barrat;Meteorit. Planet. Sci. Suppl.,2011

2. Prediction of crystal-melt partition coefficients from elastic moduli;Blundy;Nature,1994

3. Enstatite chondrites EL3 as building blocks for the Earth: The debate over the 146Sm-142Nd systematics;Boyet;Earth Planet. Sci. Lett.,2018

4. Intrinsic oxygen fugacity measurements on seven chondrites, a pallasite, and a tektite and the redox state of meteorite parent bodies;Brett;Geochim. Cosmochim. Acta,1983

5. Evidence for Nb2+ and Ta3+ in silicate melts under highly reducing conditions: a XANES study;Cartier;Am. Mineral.,2015
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