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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

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Reference TypeJournal (article/letter/editorial)
TitleA 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
JournalContributions to Mineralogy and Petrology
AuthorsLange, Rebecca A.Author
Year1997 (December 16)Volume130
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050345Search in ResearchGate
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Mindat Ref. ID77581Long-form Identifiermindat:1:5:77581:6
GUID0
Full ReferenceLange, 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
Plain TextLange, 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
In(1997, December) Contributions to Mineralogy and Petrology Vol. 130 (1) Springer Science and Business Media LLC

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Ochs III., Frederick A., Lange, Rebecca A. (1997) The partial molar volume, thermal expansivity, and compressibility of H 2 O in NaAlSi 3 O 8 liquid: new measurements and an internally consistent model. Contributions to Mineralogy and Petrology, 129 (2) 155-165 doi:10.1007/s004100050329
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
Dalton, John A., Presnall, Dean C. (1998) Carbonatitic melts along the solidus of model lherzolite in the system CaO-MgO-Al 2 O 3 -SiO 2 -CO 2 from 3 to 7 GPa. Contributions to Mineralogy and Petrology, 131 (2) 123-135 doi:10.1007/s004100050383
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
Quirion, Diane M., Jenkins, David M. (1998) Dehydration and partial melting of tremolitic amphibole coexisting with zoisite, quartz, anorthite, diopside, and water in the system H 2 O-CaO-MgO-Al 2 O 3 -SiO 2. Contributions to Mineralogy and Petrology, 130 (3) 379-389 doi:10.1007/s004100050372
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
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
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 °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
von Goerne, G., Franz, G. (2000) Synthesis of Ca-tourmaline in the system CaO-MgO-Al 2 O 3 -SiO 2 -B 2 O 3 -H 2 O-HCl. Mineralogy and Petrology, 69 (3) 161-182 doi:10.1007/s007100070019
Papale, Paolo (1997) Modeling of the solubility of a one-component H 2 O or CO 2 fluid in silicate liquids. Contributions to Mineralogy and Petrology, 126 (3) 237-251 doi:10.1007/s004100050247
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
 
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