Ca-Sr distribution among amphibole, clinopyroxene, and chloride-bearing solutions

The distribution of Sr between a 1 M (Ca,Sr)Cl 2 solution, (Ca,Sr)-tremolite and (Ca,Sr)-diopside was determined at 750 C and 200 MPa. The synthesized crystals of (Ca,Sr)-tremolite (2000 30 m) and (Ca,Sr)-diopside (1500 20 m) were large enough for accurate electron microprobe analysis. The experimental results indicate that Ca 2+ can be replaced completely by Sr 2+ on the M4-site in tremolite and on the M2-site in diopside. The compositions of the product fluid were analyzed by atomic absorption spectroscopy. In both the (Ca,Sr)-tremolite-fluid and (Ca,Sr)-diopside-fluid systems, Sr strongly fractionated into the fluid. For bulk compositions having low Sr concentrations, mineral/fluid partition coefficients, D Sr mineral/fluid , of 0.045 for (Ca,Sr)-tremolite/fluid and 0.082 for (Ca,Sr)diopside/fluid were derived. The experimental results were evaluated thermodynamically assuming Henry's law and simple mixing properties for SrCl 2 and CaCl 2 in the fluid. The mixing energies of the solids were calculated using a regular solution model. In the (Ca,Sr)-tremolite-(Ca,Sr)Cl 2 system, is 59.0 kJ and W CaSr amph = 9.8 kJ. In the system (Ca,Sr)-diopside-(Ca,Sr)Cl 2 is 30.8 kJ and W CaSr px is 11.7 kJ. The high values and, to a much lesser extent, the W CaSr values cause the strong fractionation of Sr into the fluid. The moderate values for W CaSr amph and W CaSr px strongly suggest that complete solid solution exists for (Ca,Sr)-tremolite and (Ca,Sr)-diopside at experimental run conditions. However, for the (Ca,Sr)-tremolite and (Ca,Sr)-diopside joins, limited miscibilities were calculated below 316 and 430 C, respectively.

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