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Johnson, Kevin T. M. (1998) Experimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures. Contributions to Mineralogy and Petrology, 133 (1) 60-68 doi:10.1007/s004100050437

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Reference TypeJournal (article/letter/editorial)
TitleExperimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures
JournalContributions to Mineralogy and Petrology
AuthorsJohnson, Kevin T. M.Author
Year1998 (October)Volume133
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050437Search in ResearchGate
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Mindat Ref. ID77688Long-form Identifiermindat:1:5:77688:8
GUID0
Full ReferenceJohnson, Kevin T. M. (1998) Experimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures. Contributions to Mineralogy and Petrology, 133 (1) 60-68 doi:10.1007/s004100050437
Plain TextJohnson, Kevin T. M. (1998) Experimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures. Contributions to Mineralogy and Petrology, 133 (1) 60-68 doi:10.1007/s004100050437
In(1998, October) Contributions to Mineralogy and Petrology Vol. 133 (1) Springer Science and Business Media LLC

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Masuda, Akimasa, Kushiro, Ikuo (1970) Experimental determination of partition coefficients of ten rare earth elements and barium between clinopyroxene and liquid in the synthetic silicate system at 20 kilobar pressure. Contributions to Mineralogy and Petrology, 26 (1) 42-49 doi:10.1007/bf00373339
Dalpé, Claude, Baker, Don R. (2000) Experimental investigation of large-ion-lithophile-element-, high-field-strength-element- and rare-earth-element-partitioning between calcic amphibole and basaltic melt: the effects of pressure and oxygen fugacity. Contributions to Mineralogy and Petrology, 140 (2) 233-250 doi:10.1007/s004100000181
Green, T. H., Pearson, N. J. (1985) Rare earth element partitioning between clinopyroxene and silicate liquid at moderate to high pressure. Contributions to Mineralogy and Petrology, 91 (1) 24-36 doi:10.1007/bf00429424
R�heim, Arne, Green, David H. (1974) Experimental determination of the temperature and pressure dependence of the Fe-Mg partition coefficient for coexisting garnet and clinopyroxene. Contributions to Mineralogy and Petrology, 48 (3) 179-203 doi:10.1007/bf00383355
Klein, M., Stosch, H.-G., Seck, H.A., Shimizu, N. (2000) Experimental partitioning of high field strength and rare earth elements between clinopyroxene and garnet in andesitic to tonalitic systems. Geochimica et Cosmochimica Acta, 64 (1) 99-115 doi:10.1016/s0016-7037(99)00178-7
Wood, Bernard J., Blundy, Jonathan D. (1997) A predictive model for rare earth element partitioning between clinopyroxene and anhydrous silicate melt. Contributions to Mineralogy and Petrology, 129 (2) 166-181 doi:10.1007/s004100050330
Johnson, K. T. M. (1994) Experimental cpx/ and Garnet/Melt Partitioning of REE and Other Trace Elements at High Pressures: Petrogenetic Implications. Mineralogical Magazine, 58 (1) 454-455 doi:10.1180/minmag.1994.58a.1.236
Beattie, Paul, Ford, Clifford, Russel, Douglas (1993) Partition coefficients for olivine-melt and orthopyroxene-melt systems. Contributions to Mineralogy and Petrology, 114 (2) 288 doi:10.1007/bf00307763
Whitehouse, Martin J., Platt, John P. (2003) Dating high-grade metamorphism—constraints from rare-earth elements in zircon and garnet. Contributions to Mineralogy and Petrology, 145 (1) 61-74 doi:10.1007/s00410-002-0432-z
Schosnig, Michael, Hoffer, Edgar (1998) Compositional dependence of REE partitioning between diopside and melt at 1 atmosphere. Contributions to Mineralogy and Petrology, 133 (3) 205-216 doi:10.1007/s004100050448
Reed, Marshall J., Candela, Philip A., Piccoli, Philip M. (2000) The distribution of rare earth elements between monzogranitic melt and the aqueous volatile phase in experimental investigations at 800 °C and 200 MPa. Contributions to Mineralogy and Petrology, 140 (2) 251-262 doi:10.1007/s004100000182
 
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