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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...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Pergamon Press
2013
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4375631/ https://www.ncbi.nlm.nih.gov/pubmed/25843971 http://dx.doi.org/10.1016/j.gca.2013.05.026 |