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Veksler, Ilya V., Fedorchuk, Yana M., Nielsen, Troels F. D. (1998) Phase equilibria in the silica-undersaturated part of the KAlSiO 4 - Mg 2 SiO 4 - Ca 2 SiO 4 - SiO 2 - F system at 1 atm and the larnite-normative trend of melt evolution. Contributions to Mineralogy and Petrology, 131 (4) 347-363 doi:10.1007/s004100050397

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Reference TypeJournal (article/letter/editorial)
TitlePhase equilibria in the silica-undersaturated part of the KAlSiO 4 - Mg 2 SiO 4 - Ca 2 SiO 4 - SiO 2 - F system at 1 atm and the larnite-normative trend of melt evolution
JournalContributions to Mineralogy and Petrology
AuthorsVeksler, Ilya V.Author
Fedorchuk, Yana M.Author
Nielsen, Troels F. D.Author
Year1998 (May 28)Volume131
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050397Search in ResearchGate
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Mindat Ref. ID77641Long-form Identifiermindat:1:5:77641:7
GUID0
Full ReferenceVeksler, Ilya V., Fedorchuk, Yana M., Nielsen, Troels F. D. (1998) Phase equilibria in the silica-undersaturated part of the KAlSiO 4 - Mg 2 SiO 4 - Ca 2 SiO 4 - SiO 2 - F system at 1 atm and the larnite-normative trend of melt evolution. Contributions to Mineralogy and Petrology, 131 (4) 347-363 doi:10.1007/s004100050397
Plain TextVeksler, Ilya V., Fedorchuk, Yana M., Nielsen, Troels F. D. (1998) Phase equilibria in the silica-undersaturated part of the KAlSiO 4 - Mg 2 SiO 4 - Ca 2 SiO 4 - SiO 2 - F system at 1 atm and the larnite-normative trend of melt evolution. Contributions to Mineralogy and Petrology, 131 (4) 347-363 doi:10.1007/s004100050397
In(1998, May) Contributions to Mineralogy and Petrology Vol. 131 (4) Springer Science and Business Media LLC

See Also

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Melzer, Stefan, Foley, Stephen F. (2000) Phase relations and fractionation sequences in potassic magma series modelled in the system CaMgSi 2 O 6 -KAlSiO 4 -Mg 2 SiO 4 -SiO 2 -F 2 O −1 at 1 bar to 18 kbar. Contributions to Mineralogy and Petrology, 138 (2) 186-197 doi:10.1007/s004100050017
Wendlandt, R. F., Eggler, D. H. (1980) The origins of potassic magmas; 1, Melting relations in the systems KAlSiO 4 -Mg 2 SiO 4 -SiO 2 and KAlSiO 4 MgO-SiO 2 -CO 2 to 30 kilobars. American Journal of Science, 280 (5) 385-420 doi:10.2475/ajs.280.5.385
Pan, V., Longhi, J. (1989) Low pressure liquidus relations in the system Mg 2 SiO 4 -Ca 2 SiO 4 -NaAlSiO 4 -SiO 2. American Journal of Science, 289 (1) 1-16 doi:10.2475/ajs.289.1.1
Nielsen, Troels F., Veksler, Ilya V. (2002) Is natrocarbonatite a cognate fluid condensate?. Contributions to Mineralogy and Petrology, 142 (4) 425-435 doi:10.1007/s004100100306
Glasser, F. P. (1961) The system Ca 2 SiO 4 -Mn 2 SiO 4. American Journal of Science, 259 (1) 46-59 doi:10.2475/ajs.259.1.46
Kohlstedt, D. L., Keppler, H., Rubie, D. C. (1996) Solubility of water in the α, β and γ phases of (Mg,Fe) 2 SiO 4. Contributions to Mineralogy and Petrology, 123 (4) 345-357 doi:10.1007/s004100050161
Longhi, J. (1987) Liquidus equilibria and solid solution in the system CaAl 2 Si 2 O 8 -Mg 2 SiO 4 -CaSiO 3 -SiO 2 at low pressure. American Journal of Science, 287 (4) 265-331 doi:10.2475/ajs.287.4.265
Churakov, S. V., Khisina, N. R., Urusov, V. S., Wirth, R. (2003) First-principles study of (MgH 2 SiO 4 )? n (Mg 2 SiO 4 ) hydrous olivine structures. I. Crystal structure modelling of hydrous olivine Hy-2 a (MgH 2 SiO 4 ) ? 3(Mg 2 SiO 4 ) Physics and Chemistry of Minerals, 30 (1) 1-11 doi:10.1007/s00269-002-0288-9
Matsuzaka, K., Suzuki, T., Suda, T., Akaogi, M. (2000) Mg-Fe partitioning between silicate spinel and magnesiow�stite at high pressure: experimental determination and calculation of phase relations in the system Mg 2 SiO 4 -Fe 2 SiO 4. Physics and Chemistry of Minerals, 27 (5) 310-319 doi:10.1007/s002690050260
Fockenberg, Thomas (1998) An experimental investigation on the P - T stability of Mg-staurolite in the system MgO-Al 2 O 3 -SiO 2 -H 2 O. Contributions to Mineralogy and Petrology, 130 (2) 187-198 doi:10.1007/s004100050359
Ringwood, A.F., Major, A. (1970) The system Mg2SiO4-Fe2SiO4 at high pressures and temperatures. Physics of the Earth and Planetary Interiors: 3: 89-108.
 
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