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Experimental chlorine partitioning between forsterite, enstatite and aqueous fluid at upper mantle conditions()
Cl partition coefficients between forsterite, enstatite and coexisting Cl-bearing aqueous fluids were determined in a series of high pressure and temperature piston cylinder experiments at 2 GPa between 900 and 1300 °C in the system MgO–SiO(2)–H(2)O–NaCl–BaO–C±CaCl(2)±TiO(2)±Al(2)O(3)±F. Diamond agg...
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| Gepubliceerd in: | Geochim Cosmochim Acta |
|---|---|
| Hoofdauteurs: | , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Pergamon Press
2013
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4375631/ https://ncbi.nlm.nih.gov/pubmed/25843971 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1016/j.gca.2013.05.026 |
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