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Primary phosphates usually crystallize from aqueous fluids derived from the late stages of crystallization.
We interpreted that abundant aqueous fluids supplied from the lower crust are responsible for this anomaly.
Such aqueous fluids are likely to contain Cl, although the amount remains to be quantified.
These calculations predicted considerable ion pairing and clustering of Na Cl in supercritical aqueous fluids.
The observed resistivity has suggested that aqueous fluids exist pervasively within the crust.
Hydrous Na-garnet probably forms in such metasomatized pyroxenites under Na-rich aqueous fluids environments.
Significant amounts of Na are likely dissolved to aqueous fluids released from hydrous subducted oceanic plates.
Critical to these latter observations is the high silicate concentration in aqueous fluids.
During ascent, aqueous fluids are also partly used for forming hydrated minerals (Peacock 1993).
To understand arc basalt formation, it is important to assess the mixing ratios of slab-derived aqueous fluids and melts, and in order to do so, the partitioning of trace elements between melts and aqueous fluids must be determined.
The composition control of how Zr4+ can form complexes with other solutes in an aqueous solution in aqueous fluids shows some similarities with the behavior of Ti4+ in aqueous fluids at similar temperatures and pressures.
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