Ti–in–garnet thermometer for ultrahigh–temperature granulites
Author:
Affiliation:
1. Department of Earth Sciences, Faculty of Science, Ehime University
2. National Institute of Polar Research
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/111/3/111_150709/_pdf
Reference78 articles.
1. Ague, J.J. and Eckert, J.O.Jr. (2012) Precipitation of rutile and ilmenite needles in garnet: Implications for extreme metamorphic conditions in the Acadian Orogen, U.S.A. American Mineralogist, 97, 840–855.
2. Akaogi, M. and Akimoto, S. (1977) Pyroxene–garnet solid solution equilibria in the systems Mg4Si4O12–Mg3Al2Si3O12 and Fe4Si4O12–Fe3Al2Si3O12 at high pressures and temperatures. Physics of the Earth and Planetary Interiors, 15, 90–106.
3. Aranovich, L.Y. and Berman, R.G. (1997) A new garnet–orthopyroxene thermometer based on reversed Al2O3 solubility in FeO–Al2O3–SiO2 orthopyroxene. American Mineralogist, 82, 345–353.
4. Armbruster, T., Birrer, J., Libowitzky, E. and Beran, A. (1998) Crystal chemistry of Ti–bearing andradites. European Journal of Mineralogy, 10, 907–921.
5. Bohlen, S.R. and Boettcher, A.L. (1982) The quartz ⇌ coesite transformation: A precise determination and the effects of other components. Journal of Geophysical Research, 87, 7073–7078.
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