The K2CO3 fusion curve revisited: New experiments at pressures up to 12 GPa
Author:
Affiliation:
1. Key Laboratory of Orogenic Belts and Crustal Evolution, MOE, Peking University
2. School of Earth and Space Sciences, Peking University
3. Geodynamics Research Center, Ehime University
4. Mineral Physics Institute, State University of New York
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/111/4/111_150417/_pdf
Reference75 articles.
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2. Akaogi, M. (2007) Phase transitions of minerals in the transition zone and upper part of the lower mantle. Advances in High–Pressure Mineralogy: Geological Society of America Special Paper, 421, 1–13.
3. Akaogi, M., Ito, E. and Navrotsky, A. (1989) Olivine–modified spinel–spinel transitions in the system MgSiO4–FeSiO4 calorimetric measurements, thermochemical calculation, and geophysical application. Journal of Geophysical Research: Solid Earth, 94, 15671–15685.
4. Birch, F. (1978) Finite strain isotherm and velocities for single–crystal and polycrystalline NaCl at high–pressures and 300–degree–K. Journal of Geophysical Research: Solid Earth, 83, 1257–1268.
5. Brey, G.P., Bulatov, V.K. and Girnis, A.V. (2011) Melting of K–rich carbonated peridotite at 6–10 GPa and the stability of K–phases in the upper mantle. Chemical Geology, 281, 333–342.
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