Abstract
Quartz and rutile were synthesized from silica-saturated aqueous fluids between 5 and 20 kbar and from 700 to 940°C in a piston-cylinder apparatus to explore the potential pressure effect on Ti solubility in quartz. A systematic decrease in Ti-in-quartz solubility occurs between 5 and 20 kbar. Titanium K-edge X-ray absorption near-edge structure (XANES) measurements demonstrate that Ti4+ substitutes for Si4+ on fourfold tetrahedral sites in quartz at all conditions studied. Molecular dynamic simulations support XANES measurements and demonstrate that Ti incorporation onto fourfold sites is favored over interstitial solubility mechanisms. To account for the P–T dependence of Ti-in-quartz solubility, a least-squares method was used to fit Ti concentrations in quartz from all experiments to the simple expression
where R is the gas constant 8.3145 J/K, T is temperature in Kelvin, \( X_{{{\text{TiO}}_{ 2} }}^{\text{quartz}} \) is the mole fraction of TiO2 in quartz and \( a_{{{\text{TiO}}_{ 2} }} \) is the activity of TiO2 in the system. The P–T dependencies of Ti-in-quartz solubility can be used as a thermobarometer when used in combination with another thermobarometer in a coexisting mineral, an independent P or T estimate of quartz crystallization, or well-constrained phase equilibria. If temperature can be constrained within ±25°C, pressure can be constrained to approximately ±1.2 kbar. Alternatively, if pressure can be constrained to within ±1 kbar, then temperature can be constrained to approximately ±20°C.
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Acknowledgments
This work was supported by the Earth Sciences Division of the National Science Foundation through grant number EAR-0440228 to EBW. PTS thanks Dr. Alessandro Curioni for helpful discussions, the Interconnect Focus Center for funding, and the Computational Center for Nanotechnology Innovations (CCNI) at RPI for supercomputer access. Beamline X-26A at the NSLS is supported by the Department of Energy (DOE)—Geosciences through grant number DE-FG02-92ER14244 to The University of Chicago—CARS. The XANES measurements at NSLS would not have been possible without the dedicated assistance of William Rao. Reviews by John Ferry, John Mavrogenes and Roger Powell helped improve the final version of the manuscript.
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Communicated by T. L. Grove.
Appendix
Appendix
The equation to convert Ti (ppm) to mole fraction TiO2 in quartz (\( X_{{{\text{TiO}}_{ 2} }}^{\text{quartz}} \)) is
The equation to convert Zr (ppm) to mole fraction ZrO2 in rutile (\( X_{{{\text{ZrO}}_{ 2} }}^{\text{rutile}} \)) is
The equation to convert Zr (ppm) to mole fraction ZrO2 in sphene (\( X_{{{\text{ZrO}}_{ 2} }}^{\text{sphene}} \)) is
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Thomas, J.B., Bruce Watson, E., Spear, F.S. et al. TitaniQ under pressure: the effect of pressure and temperature on the solubility of Ti in quartz. Contrib Mineral Petrol 160, 743–759 (2010). https://doi.org/10.1007/s00410-010-0505-3
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DOI: https://doi.org/10.1007/s00410-010-0505-3