TY - JOUR
T1 - Correction to
T2 - Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle (Contributions to Mineralogy and Petrology, (2021), 176, 9, (67), 10.1007/s00410-021-01823-3)
AU - Davis, Fred A.
AU - Cottrell, Elizabeth
N1 - Publisher Copyright:
© Springer-Verlag GmbH Germany, part of Springer Nature 2022.
PY - 2022/7
Y1 - 2022/7
N2 - 1. Published Eq. (2) contains a typo. The correct version of Eq. (2) should be: (Formula presented.) (2) where T is temperature in Kelvin and CFe2O3spl is wt.% of Fe2O3 in spinel. Fits are a = 0.87 ± 0.07, b = −4.6 ± 0.4, and c = 0.24 ± 0.02. We used the correct version of the equation in all our calculations, models, and figures; our results, discussion, and conclusions remain unchanged. 2. We did not provide the duration of the piston cylinder experiments. Each experiment had a run duration of 24 h after reaching the run temperature. 3. In the abstract, the line beginning, “If we allow DFe2O3opx/melt and DFe2O3opx/melt to also vary with temperature...” should instead be, “If we allow DFe2O3opx/melt and DFe2O3cpx/melt to also vary with temperature...” 4. The green and orange lines in Fig. 9 are mineral/melt partition coefficients estimated by Mallmann and O’Neill (2009) for DFe2O3cpx/melt and DFe2O3opx/melt, respectively.
AB - 1. Published Eq. (2) contains a typo. The correct version of Eq. (2) should be: (Formula presented.) (2) where T is temperature in Kelvin and CFe2O3spl is wt.% of Fe2O3 in spinel. Fits are a = 0.87 ± 0.07, b = −4.6 ± 0.4, and c = 0.24 ± 0.02. We used the correct version of the equation in all our calculations, models, and figures; our results, discussion, and conclusions remain unchanged. 2. We did not provide the duration of the piston cylinder experiments. Each experiment had a run duration of 24 h after reaching the run temperature. 3. In the abstract, the line beginning, “If we allow DFe2O3opx/melt and DFe2O3opx/melt to also vary with temperature...” should instead be, “If we allow DFe2O3opx/melt and DFe2O3cpx/melt to also vary with temperature...” 4. The green and orange lines in Fig. 9 are mineral/melt partition coefficients estimated by Mallmann and O’Neill (2009) for DFe2O3cpx/melt and DFe2O3opx/melt, respectively.
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U2 - 10.1007/s00410-022-01933-6
DO - 10.1007/s00410-022-01933-6
M3 - Comment/debate
AN - SCOPUS:85132972226
SN - 0010-7999
VL - 177
JO - Contributions to Mineralogy and Petrology
JF - Contributions to Mineralogy and Petrology
IS - 7
M1 - 68
ER -