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Erratum to: Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite

Author(s)
Till, Christy B.; Krawczynski, Michael J.; Holbig, Eva S.; Grove, Timothy L.; Barr, Jay A.
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Abstract
An unfortunate coding error led to erroneous predicted abundances of Na[subscript 2]O in the melting models presented in Table 5 of Grove et al. (2013). The source of this error has been discovered and corrected; the cause of the discrepancy was an error in assignment of the partition coefficient expressions used for orthopyroxene and clinopyroxene. The values presented in a corrected Table 5 are the ones obtained using the appropriate partition coefficients for Na[subscript 2]O. Our models of garnet lherzolite melts now have Na[subscript 2]O abundances that are similar to the melts predicted by Longhi (2002) and the experimentally produced melt of Walter (1998).
Date issued
2014-11
URI
http://hdl.handle.net/1721.1/107263
Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Journal
Contributions to Mineralogy and Petrology
Publisher
Springer Berlin Heidelberg
Citation
Grove, Timothy L. et al. “Erratum to: Melts of Garnet Lherzolite: Experiments, Models and Comparison to Melts of Pyroxenite and Carbonated Lherzolite.” Contributions to Mineralogy and Petrology 168.6 (2014): n. pag.
Version: Author's final manuscript
ISSN
0010-7999
1432-0967

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