Erratum to: Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite
Name
410_2014_1086_ReferencePDF.pdf
Size
329.36 KB
Format
Adobe PDF
Checksum (MD5)
8d8400895869a6ab1626e9f82d5db847
Author(s)
Till, Christy B.
Krawczynski, Michael J.
Holbig, Eva S.
Grove, Timothy L.
Barr, Jay A.
Date Issued
November 2014
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
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).
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Terms of Use
Creative Commons Attribution-Noncommercial-Share Alike
Persistent DSpace Link
DOI of Published Version
https://doi.org/10.1007/s00410-014-1086-3
