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Chu, Linglin, Enggist, Andreas, Luth, Robert W. (2011) Effect of KCl on melting in the Mg2SiO4–MgSiO3–H2O system at 5 GPa. Contributions to Mineralogy and Petrology, 162 (3) 565-571 doi:10.1007/s00410-011-0612-9

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Reference TypeJournal (article/letter/editorial)
TitleEffect of KCl on melting in the Mg2SiO4–MgSiO3–H2O system at 5 GPa
JournalContributions to Mineralogy and Petrology
AuthorsChu, LinglinAuthor
Enggist, AndreasAuthor
Luth, Robert W.Author
Year2011 (September)Volume162
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-011-0612-9Search in ResearchGate
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Mindat Ref. ID79216Long-form Identifiermindat:1:5:79216:9
GUID0
Full ReferenceChu, Linglin, Enggist, Andreas, Luth, Robert W. (2011) Effect of KCl on melting in the Mg2SiO4–MgSiO3–H2O system at 5 GPa. Contributions to Mineralogy and Petrology, 162 (3) 565-571 doi:10.1007/s00410-011-0612-9
Plain TextChu, Linglin, Enggist, Andreas, Luth, Robert W. (2011) Effect of KCl on melting in the Mg2SiO4–MgSiO3–H2O system at 5 GPa. Contributions to Mineralogy and Petrology, 162 (3) 565-571 doi:10.1007/s00410-011-0612-9
In(2011, September) Contributions to Mineralogy and Petrology Vol. 162 (3) Springer Science and Business Media LLC

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Enggist, Andreas, Chu, Linglin, Luth, Robert W. (2012) Phase relations of phlogopite with magnesite from 4 to 8 GPa. Contributions to Mineralogy and Petrology, 163 (3) 467-481 doi:10.1007/s00410-011-0681-9
Enggist, Andreas, Luth, Robert W. (2016) Phase relations of phlogopite and pyroxene with magnesite from 4 to 8 GPa: KCMAS–H2O and KCMAS–H2O–CO2. Contributions to Mineralogy and Petrology, 171 (11) doi:10.1007/s00410-016-1304-2
Luth, Robert W. (2006) Experimental study of the CaMgSi2O6–CO2 system at 3–8 GPa. Contributions to Mineralogy and Petrology, 151 (2) 141-157 doi:10.1007/s00410-005-0051-6
Luth, Robert W. (1993) Melting in the Mg2SiO4-H2O system at 3 to 12 GPa. Geophysical Research Letters, 20 (3) 233-235 doi:10.1029/92gl03008
Luth, Robert W. (2001) Experimental determination of the reaction aragonite + magnesite = dolomite at 5 to 9 GPa. Contributions to Mineralogy and Petrology, 141 (2) 222-232 doi:10.1007/s004100100238
Grassi, Daniele, Schmidt, Max W. (2011) Melting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism. Contributions to Mineralogy and Petrology, 162 (1) 169-191 doi:10.1007/s00410-010-0589-9
Fagan, Andrew J., Luth, Robert W. (2011) Growth of diamond in hydrous silicate melts. Contributions to Mineralogy and Petrology, 161 (2) 229-236 doi:10.1007/s00410-010-0528-9
Withers, A. C., Hirschmann, M. M. (2007) H2O storage capacity of MgSiO3 clinoenstatite at 8–13 GPa, 1,100–1,400°C. Contributions to Mineralogy and Petrology, 154 (6) 663-674 doi:10.1007/s00410-007-0215-7
Luth, Robert W. (2009) The activity of silica in kimberlites, revisited. Contributions to Mineralogy and Petrology, 158 (2) 283-294 doi:10.1007/s00410-009-0383-8
Luth, Robert W., Stachel, Thomas (2014) The buffering capacity of lithospheric mantle: implications for diamond formation. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1083-6
Ni, Huaiwei, Keppler, Hans, Behrens, Harald (2011) Electrical conductivity of hydrous basaltic melts: implications for partial melting in the upper mantle. Contributions to Mineralogy and Petrology, 162 (3) 637-650 doi:10.1007/s00410-011-0617-4
 
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