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In-situ measurement of viscosity and density of carbonate melts at high pressure
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Carbonatite melts in the upper mantle have a low viscosity because of the ionic nature of these melts and the impossibility of having polymers based on trigonal carbonate units.
“It is a known fact that carbonatite melts in the upper mantle have a sensible low viscosity (e.g.Dobson et al., 1996;Jones et al., 2013) because of the ionic nature of these melts and the impossibility of having polymers based on trigonal carbonate units.”
From Structures and Crystal Chemistry of Carbonate at Earth's Mantle Conditions (2020) · cites this paper as Dobson et al., 1996
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Research works printed but not linked: 27
- Wallace, 1988, An experimental determination of primary carbonatite magma composition, Nature, 335, 343, 10.1038/335343a0 · DOI
- Thibault, 1992, Experimental investigation of melts from a carbonated phlogopite Iherzolite: implications for metasomatism in the continental lithospheric mantle, Am. Mineral., 77, 784
- Dalton, 1993, The compositions of primary carbonate melts and their evolution through wallrock reaction in the mantle, Earth Planet. Sci. Lett., 119, 511, 10.1016/0012-821X(93)90059-I · DOI
- Kjarsgaard, 1993, The immiscibility of silicate and carbonate liquids, S. Afr. J. Geol., 96, 139
- Bailey, 1993, Carbonate magmas, J. Geol. Soc. London, 150, 637, 10.1144/gsjgs.150.4.0637 · DOI
- Nelson, 1988, Geochemical and isotope systematics in carbonatites and implications for the evolution of ocean-island sources, Geochim. Cosmochim. Acta, 52, 1, 10.1016/0016-7037(88)90051-8 · DOI
- Sweeney, 1992, Trace and minor element partitioning between garnet and amphibole and carbonatitic melt, Earth Planet. Sci. Lett., 113, 1, 10.1016/0012-821X(92)90207-C · DOI
- Ionov, 1993, Carbonated peridotite xenoliths from Spitsbergen: implications for trace element signature of mantle arbonate metasomatism, Earth Planet. Sci. Lett., 119, 283, 10.1016/0012-821X(93)90139-Z · DOI
- Rudnick, 1993, Carbonatite metasomatism in the northern Tanzanian mantle: petrographic and geochemical characteristics, Earth Planet. Sci. Lett., 114, 463, 10.1016/0012-821X(93)90076-L · DOI
- Hunter, 1989, The equilibrium geometry of carbonate melts in rocks of mantle composition, Earth Planet. Sci. Lett., 92, 347, 10.1016/0012-821X(89)90059-9 · DOI
- Minarik, 1995, Interconnectivity of carbonate melt at low melt fraction, Earth Planet. Sci. Lett., 133, 423, 10.1016/0012-821X(95)00085-Q · DOI
- Wolff, 1995, Physical properties of carbonatite magmas inferred from molten salt data, and application to extraction patterns from carbonate-silicate magma chambers, Geol. Mag., 131, 145, 10.1017/S0016756800010682 · DOI
- Trieman, 1983, Properties of carbonatite magma and processes in carbonatite magma chambers, J. Geol., 91, 437, 10.1086/628789 · DOI
- Janz, 1988, Thermodynamic and transport properties for molten salts: correlation equations for critically evaluated density, surface tension, electrical conductance and viscosity data, J. Phys. Chem. Ref. Data, 17, 309
- Sykes, 1992, Viscous properties of carbonate melts at high pressure, EOS Trans. AGU, 73, 372
- Jones, 1995, Comment on physical properties of carbonatite magmas inferred from molten salt data, and application to extraction patterns from carbonatite-silicate magma chambers, Geol. Mag., 132, 121, 10.1017/S0016756800011481 · DOI
- Genge, 1995, Molecular dynamics simulations of CaCO3 melts to mantle pressures and temperatures: implications for carbonatite magmas, Earth Planet. Sci. Lett., 131, 225, 10.1016/0012-821X(95)00020-D · DOI
- Genge, 1995, An infrared and raman study of carbonate glasses: implications for the structure of carbonate magmas, Geochim. Cosmochim. Acta, 59, 927, 10.1016/0016-7037(95)00010-0 · DOI
- Faxen, 1925, Gegenseitige Einwirkung zweier Kugeln, die in einer zähen Flüssigkeit fallen, Ark. Mat. Astron. Fys., 19, 1
- Decker, 1971, High pressure equation of state for NaCl, KCl and CsCl, J. Appl. Phys., 42, 3239, 10.1063/1.1660714 · DOI
- Baumgartl, 1989, Studies of buoyancy driven convection in a vertical cylinder with a parabolic temperature profile, J. Cryst. Growth, 97, 9, 10.1016/0022-0248(89)90241-8 · DOI
- Rigden, 1984, Densities of liquid silicates at high pressures, Science, 226, 1071, 10.1126/science.226.4678.1071 · DOI
- Bottinga, 1972, The viscosity of magmatic silicate liquids: a model for calculation, Am. J. Sci., 272, 438, 10.2475/ajs.272.5.438 · DOI
- Shaw, 1972, Viscosities of magmatic silicate liquids: an empirical method of prediction, Am. J. Sci., 272, 870, 10.2475/ajs.272.9.870 · DOI
- LeBlanc, 1996, Viscosity of an FeS liquid up to 1300°C and 5 GPa, Geophys. Res. Lett., 23, 213, 10.1029/96GL00216 · DOI
- Poirier, 1988, Transport properties of liquid metals and viscosity of the Earth's core, Geophys. J., 92, 99, 10.1111/j.1365-246X.1988.tb01124.x · DOI
- Jones, 1983, Low temperature glass quenched from a synthetic rare earth carbonate: implications for the origin of Mountain Pass deposit, California, Econ. Geol., 78, 1721, 10.2113/gsecongeo.78.8.1721 · DOI
Cited by
Sorted by citations
Structures and Crystal Chemistry of Carbonate at Earth's Mantle Conditions
Merlini, M., Milani, S., & Maurice, J. (2020) · Geophysical Monograph Series · doi:10.1002/9781119508229.ch9 · Cited by 7
“It is a known fact that carbonatite melts in the upper mantle have a sensible low viscosity (e.g. Dobson et al., 1996; Jones et al., 2013) because of the ionic nature of these melts and the impossibility of having polymers based on trigonal carbonate units.”
Background
Metadata
- Authors
- Dobson, D. P., Jones, A. P., Rabe, R., Sekine, T., Kurita, K., Taniguchi, T., Kondo, T., Kato, T., Shimomura, O., & Urakawa, S.
- Affiliations
- University College London (GB)
- National Institute for Materials Science (JP)
- University of Tsukuba (JP)
- The University of Tokyo (JP)
- Nagoya University (JP)
- Institute of High Energy Physics (CN)
- Corresponding author
- Dobson, David P.
- ORCID
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1996-09
- Volume
- 143
- Issue
- 1-4
- Pages
- 207-215
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2026862001
- Cited by
- 233
- References
- 0
- Citations by year
- 2026: 5 · 2025: 6 · 2024: 6 · 2023: 5 · 2022: 8 · 2021: 20 · 2020: 16 · 2019: 14 · 2018: 13 · 2017: 5 · 2016: 6 · 2015: 9 · 2014: 14 · 2013: 10 · 2012: 16
- FWCI
- 2.22
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- UCL Discovery (University College London) (submittedVersion)
- Funders
- Natural Environment Research Council
- Japan Society for the Promotion of Science
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Keywords
- carbonate melts, melt viscosity, melt density, high pressure, mantle, carbonatites, falling sphere method, synchrotron radiation, terminal velocity, molecular dynamics
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