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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

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Reference TypeJournal (article/letter/editorial)
TitleSynthetic 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
JournalContributions to Mineralogy and Petrology
AuthorsFischer, H.Author
Schreyer, W.Author
Maresch, W. V.Author
Year1999 (July 15)Volume136
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050531Search in ResearchGate
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Mindat Ref. ID77794Long-form Identifiermindat:1:5:77794:8
GUID0
Full ReferenceFischer, 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
Plain TextFischer, 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
In(1999, July) Contributions to Mineralogy and Petrology Vol. 136 (1) Springer Science and Business Media LLC

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Shmulovich, Kirill I., Graham, Colin M. (1999) An experimental study of phase equilibria in the system H 2 O-CO 2 -NaCl at 800 °C and 9 kbar. Contributions to Mineralogy and Petrology, 136 (3) 247-257 doi:10.1007/s004100050536
Schreyer, W., Seifert, F. (1969) Compatibility relations of the aluminum silicates in the systems MgO-Al 2 O 3 -SiO 2 -H 2 O and K 2 O-MgO-Al 2 O 3 -SiO 2 -H 2 O at high pressures. American Journal of Science, 267 (3) 371-388 doi:10.2475/ajs.267.3.371
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
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
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
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
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
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
Johannes, W. (1989) Melting of plagioclase-quartz assemblages at 2 kbar water pressure. Contributions to Mineralogy and Petrology, 103 (3) 270-276 doi:10.1007/bf00402914
Schreyer, W., Maresch, W. V., Daniels, P., Wolfsdorff, P. (1990) Potassic cordierites: characteristic minerals for high-temperature, very low-pressure environments. Contributions to Mineralogy and Petrology, 105 (2) 162-172 doi:10.1007/bf00678983
Rebay, Gisella, Powell, Roger, Holland, Tim J. B. (2022) Calculated phase equilibria for high‐pressure serpentinites and compositionally related rocks close to the MgO–Al 2 O 3 –SiO 2 –H 2 O (MASH) system. Journal of Metamorphic Geology, 40 (7) 1219-1234 doi:10.1111/jmg.12663
 
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