Low-pressure–temperature stability of pyrope + quartz relative to orthopyroxene + kyanite: a new model for aluminous orthopyroxene with vacancies
Author:
Funder
Division of Earth Sciences
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-019-1567-5.pdf
Reference58 articles.
1. Aranovich LY, Berman RG (1997) A new garnet–orthopyroxene thermometer based on reversed Al2O3 solubility in FeO–Al2O3–SiO2 orthopyroxene. Am Mineral 82:345–353. https://doi.org/10.2138/am-1997-3-413
2. Aranovich LY, Podlesskii KK (1989) Geothermobarometry of high-grade metapelites: simultaneously operating reactions. Geol Soc Lond Spec Publ 43:45–61. https://doi.org/10.1144/GSL.SP.1989.043.01.03
3. Arima M, Onuma K (1977) The solubility of alumina in enstatite and the phase equilibria in the join MgSiO3–MgAl2SiO6 at 10–25 kbar. Contrib Mineral Petrol 61:251–265. https://doi.org/10.1007/BF00376700
4. Baba S (1999) Sapphirine-bearing orthopyroxene–kyanite/sillimanite granulites from South Harris, NW Scotland: evidence for Proterozoic UHT metamorphism in the Lewisian. Contrib Mineral Petrol 136:33–47. https://doi.org/10.1007/s004100050522
5. Bohlen SR, Essene EJ, Boettcher AL (1980) Reinvestigation and application of olivine–quartz–orthopyroxene barometry. Earth Planet Sci Lett 47:1–10. https://doi.org/10.1016/0012-821X(80)90098-9
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