An experimental study of OH solubility in rutile at 500-900 C, 0.5-2 GPa, and a range of oxygen fugacities-Reference-Cited by-同舟云学术

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An experimental study of OH solubility in rutile at 500-900 C, 0.5-2 GPa, and a range of oxygen fugacities

Published:2011-08-01 Issue:8-9 Volume:96 Page:1291-1299
ISSN:0003-004X
Container-title:American Mineralogist
language:en
Short-container-title:American Mineralogist

Author:

Colasanti C. V.,Johnson E. A.,Manning C. E.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

Cited by 19 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Al and H incorporation and Al-diffusion in natural rutile and its high-pressure polymorph TiO ₂ (II);Geological Society, London, Special Publications;2023-10-18

2. A framework for quantitative in situ evaluation of coupled substitutions between H⁺ and trace elements in natural rutile;European Journal of Mineralogy;2023-04-05

3. Redox‐Independent Low Water Solubility in Quartz and Implications for Water Storage in the Crust;Journal of Geophysical Research: Solid Earth;2023-04

4. Effects of Oxygen Fugacity on Hydroxyl Incorporation in Garnet at 1–3 GPa and 800–1000°C and Implications for Water Storage in the Mantle;Journal of Geophysical Research: Solid Earth;2022-04

5. Experimental quantification of vanadium partitioning between eclogitic minerals (garnet, clinopyroxene, rutile) and silicate melt as a function of temperature and oxygen fugacity;Contributions to Mineralogy and Petrology;2022-01-22

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