Do carbonate liquids become denser than silicate liquids at pressure? Constraints from the fusion curve of K2CO3 to 3.2 GPa

Author:

Liu Qiong,Tenner Travis J.,Lange Rebecca A.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference35 articles.

1. Agee CB, Walker D (1993) Olivine flotation in mantle melt. Earth Planet Sci Lett 114:315–324

2. Ai Y, Lange RA (2005) Sound velocity measurements of CaO–MgO–Al2O3–SiO2 liquids: reevaluation of the equation of state for CaMgSi2O6–CaAl2Si2O8 liquids. American Geophysical Union, EOS Transactions, Fall meeting supplement, Abstract MR13A-0063

3. Anderson OL (1995) Equation of state of solids for geophysics and ceramic science. Oxford University Press, New York, 405 pp

4. Berman RG, Brown TH (1985) The heat capacity of minerals in the system K2O–Na2O–CaO–MgO–FeO–Fe2O3–Al2O3–SiO2–TiO2–H2O–CO2: representation, estimation, and high temperature extrapolation. Contrib Mineral Petrol 89:168–183

5. Birch F (1978) Finite strain isotherm and velocities for single-crystal and polycrystalline NaCl at high-pressures and 300-degree-K. J Geophys Res 83:1257–1268

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