Corrigendum to “Experimental evidence for fluid-induced melting in subduction zones” by Rustioni et al., 2019
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Corrigendum
Correction to: Geochemical Perspectives Letters 11, 49-54, doi: 10.7185/geochemlet.1925, published on 22 October 2019.
In the original version of Supplementary Table S-3, the sequence of numbers given does not correspond to the legend in the left column. The real sequence from top to bottom is: SiO2 - FeO - MgO - TiO2 - CaO - Al2O3 - Na2O - Total.
The authors apologise for the mistake.
A corrected version of Table S-3 is shown below, and the table has now been corrected in the Supplementary Information PDF that accompanies the original article.
Table S-3 Microprobe analyses of garnet and omphacite (in wt. %).
| Garnet | |||||||||
| SiO2 | 39.17 | 39.32 | 39.86 | 39.43 | 39.25 | 38.77 | 39.02 | 39.19 | 39.26 |
| TiO2 | 0.69 | 0.69 | 0.71 | 0.64 | 0.63 | 0.89 | 0.79 | 0.63 | 0.74 |
| Al2O3 | 22 | 21.53 | 21.91 | 21.93 | 21.67 | 20.83 | 21.33 | 21.47 | 20.8 |
| MgO | 7.35 | 7.46 | 7.36 | 7.15 | 7.17 | 7.29 | 6.66 | 8.18 | 6.69 |
| CaO | 11.37 | 10.82 | 10.74 | 10.76 | 10.18 | 9.85 | 11.32 | 8.5 | 10.89 |
| FeO | 20.04 | 20.83 | 21.08 | 20.57 | 21.6 | 22.27 | 21.21 | 22.14 | 21.8 |
| Na2O | 0.06 | 0.06 | 0.05 | 0.09 | 0.06 | 0.07 | 0.09 | 0.06 | 0.21 |
| Total | 100.7 | 100.7 | 101.7 | 100.6 | 100.6 | 100 | 100.4 | 100.2 | 100.4 |
| Omphacite | |||||
| SiO2 | 54.57 | 54.69 | 55.81 | 53.81 | 53.53 |
| TiO2 | 0.28 | 0.21 | 0.13 | 0.49 | 0.84 |
| Al2O3 | 12.23 | 12.61 | 10.2 | 10.5 | 10.62 |
| MgO | 7.8 | 8.3 | 9.77 | 8.9 | 8.23 |
| CaO | 12.91 | 12.78 | 14.76 | 13.55 | 13.83 |
| FeO | 4.13 | 3.05 | 5.18 | 7.64 | 6.9 |
| Na2O | 6.01 | 6.52 | 5.81 | 5.46 | 5.9 |
| Total | 97.9 | 98.1 | 101.6 | 100.3 | 99.8 |
Garnet and omphacite compositions were measured on grains across the capsule in one single experiment (PC09). The average garnet composition is (Ca0.29Mg0.27Fe0.44)3(Al0.97Fe0.03)2(SiO4)3, the average pyroxene composition is Ca0.52Na0.41Mg0.46Fe0.16Al0.44Si1.96O6.