Experimental constraints on trace element partitioning between coesite and hydrous silicate melt at 5 GPa and 1500–1750°C
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s11430-020-9745-2.pdf
Reference57 articles.
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2. Blundy J D, Falloon T J, Wood B J, Dalton J A. 1995. Sodium partitioning between clinopyroxene and silicate melts. J Geophys Res, 100: 15501–15515
3. Blundy J, Wood B. 1994. Prediction of crystal-melt partition coefficients from elastic moduli. Nature, 372: 452–454
4. Brey G P, Girnis A V, Bulatov V K, Höfer H E, Gerdes A, Woodland A B. 2015. Reduced sediment melting at 7.5–12 GPa: Phase relations, geochemical signals and diamond nucleation. Contrib Mineral Petrol, 170: 18
5. Brice J C. 1975. Some thermodynamic aspects of the growth of strained crystals. J Cryst Growth, 28: 249–253
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2. Effect of second Si–O vibrational overtones/combinations on quantifying water in silicate and silica minerals using infrared spectroscopy, and an experimental method for its removal;Physics and Chemistry of Minerals;2022-02-11
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