Comment on “Compositional and temperature effects on sulfur speciation and solubility in silicate melts” by Nash et al. [Earth Planet. Sci. Lett. 507 (2019) 187–198
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Cooling a silicate melt isochemically may change Fe3+/Fe2+ if interaction with other redox couples is sufficiently rapid relative to the cooling rate. For typical element concentrations in common magmas, re-speciation with sulfide and sulfate anions may be significant (Métrich et al., 2009):
| Collections | ANU Research Publications |
|---|---|
| Date published: | 2021 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/272732 |
| Source: | Earth and Planetary Science Letters |
| DOI: | 10.1016/j.epsl.2021.116843 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| Compositional and temperature.pdf | 233.12 kB | Adobe PDF | Request a copy |
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