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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 βˆ’1 at 1 bar to 18 kbar. Contributions to Mineralogy and Petrology, 138 (2) 186-197 doi:10.1007/s004100050017

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Reference TypeJournal (article/letter/editorial)
TitlePhase 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 βˆ’1 at 1 bar to 18 kbar
JournalContributions to Mineralogy and Petrology
AuthorsMelzer, StefanAuthor
Foley, Stephen F.Author
Year2000 (February 9)Volume138
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050017Search in ResearchGate
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Mindat Ref. ID77859Long-form Identifiermindat:1:5:77859:4
GUID0
Full ReferenceMelzer, 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 βˆ’1 at 1 bar to 18 kbar. Contributions to Mineralogy and Petrology, 138 (2) 186-197 doi:10.1007/s004100050017
Plain TextMelzer, 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 βˆ’1 at 1 bar to 18 kbar. Contributions to Mineralogy and Petrology, 138 (2) 186-197 doi:10.1007/s004100050017
In(2000, February) Contributions to Mineralogy and Petrology Vol. 138 (2) Springer Science and Business Media LLC

See Also

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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
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
Fischer, H., Schreyer, W., Maresch, W. V. (1999) Synthetic gedrite: a stable phase in the system MgO-Al 2 O 3 -SiO 2 -H 2 O (MASH) at 800 Β°C and 10 kbar water pressure, and the influence of FeNaCa impurities. Contributions to Mineralogy and Petrology, 136 (1) 184-191 doi:10.1007/s004100050531
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
Klemme, Stephan, O'Neill, Hugh S. C. (1997) The reaction MgCr 2 O 4 + SiO 2 = Cr 2 O 3 + MgSiO 3 and the free energy of formation of magnesiochromite (MgCr 2 O 4 ) Contributions to Mineralogy and Petrology, 130 (1) 59-65 doi:10.1007/s004100050349
Wendlandt, R. F., Eggler, D. H. (1980) The origins of potassic magmas; 2, Stability of phlogopite in natural spinel lherzolite and in the system KAlSiO 4 -MgO-SiO 2 -H 2 O-CO 2 at high pressures and high temperatures. American Journal of Science, 280 (5) 421-458 doi:10.2475/ajs.280.5.421
Sharma, Anurag (1996) Experimentally derived thermochemical data for pargasite and reinvestigation of its stability with quartz in the system Na 2 O-CaO->MgO-Al 2 O 3 -SiO 2 -H 2 O. Contributions to Mineralogy and Petrology, 125 (2) 263-275 doi:10.1007/s004100050221
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
Lange, Rebecca A. (1997) A revised model for the density and thermal expansivity of K 2 O-Na 2 O-CaO-MgO-Al 2 O 3 -SiO 2 liquids from 700 to 1900 K: extension to crustal magmatic temperatures. Contributions to Mineralogy and Petrology, 130 (1) 1-11 doi:10.1007/s004100050345
Schairer, J. F., Bowen, N. L. (1947) Melting relations in the systems Na 2 O-Al 2 O 3 -SiO 2 and K 2 O-Al 2 O 3 -SiO 2. American Journal of Science, 245 (4) 193-204 doi:10.2475/ajs.245.4.193
Watson, E. B., Wark, D. A. (1997) Diffusion of dissolved SiO 2 in H 2 O at 1 GPa, with implications for mass transport in the crust and upper mantle. Contributions to Mineralogy and Petrology, 130 (1) 66-80 doi:10.1007/s004100050350
 
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