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Konzett, Jürgen (1997) Phase relations and chemistry of Ti-rich K-richterite-bearing mantle assemblages: an experimental study to 8.0 GPa in a Ti-KNCMASH system. Contributions to Mineralogy and Petrology, 128 (4) 385-404 doi:10.1007/s004100050316

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Reference TypeJournal (article/letter/editorial)
TitlePhase relations and chemistry of Ti-rich K-richterite-bearing mantle assemblages: an experimental study to 8.0 GPa in a Ti-KNCMASH system
JournalContributions to Mineralogy and Petrology
AuthorsKonzett, JürgenAuthor
Year1997 (August 14)Volume128
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050316Search in ResearchGate
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Mindat Ref. ID77548Long-form Identifiermindat:1:5:77548:1
GUID0
Full ReferenceKonzett, Jürgen (1997) Phase relations and chemistry of Ti-rich K-richterite-bearing mantle assemblages: an experimental study to 8.0 GPa in a Ti-KNCMASH system. Contributions to Mineralogy and Petrology, 128 (4) 385-404 doi:10.1007/s004100050316
Plain TextKonzett, Jürgen (1997) Phase relations and chemistry of Ti-rich K-richterite-bearing mantle assemblages: an experimental study to 8.0 GPa in a Ti-KNCMASH system. Contributions to Mineralogy and Petrology, 128 (4) 385-404 doi:10.1007/s004100050316
In(1997, August) Contributions to Mineralogy and Petrology Vol. 128 (4) Springer Science and Business Media LLC

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Konzett, J., Sweeney, R.J., Thompson, A.B., Ulmer, P. (1997) Potassium Amphibole Stability in the Upper Mantle: an Experimental Study in a Peralkaline KNCMASH System to 8.5 GPa. Journal of Petrology, 38 (5) 537-568 doi:10.1093/petroj/38.5.537
KONZETT, J. (2004) Phase Relations and Stability of Magnetoplumbite- and Crichtonite-Series Phases under Upper-Mantle P-T Conditions: an Experimental Study to 15 GPa with Implications for LILE Metasomatism in the Lithospheric Mantle. Journal of Petrology, 46 (4) 749-781 doi:10.1093/petrology/egh096
Bertka, Constance M., Holloway, John R. (1994) Anhydrous partial melting of an iron-rich mantle I: subsolidus phase assemblages and partial melting phase relations at 10 to 30 kbar. Contributions to Mineralogy and Petrology, 115 (3) 313-322 doi:10.1007/bf00310770
Yaxley, Gregory M., Brey, Gerhard P. (2004) Phase relations of carbonate-bearing eclogite assemblages from 2.5 to 5.5�GPa: implications for petrogenesis of carbonatites. Contributions to Mineralogy and Petrology, 146 (5) 606-619 doi:10.1007/s00410-003-0517-3
Pedersen, A. K. (1981) Armalcolite-bearing Fe-Ti oxide assemblages in graphite-equilibrated salic volcanic rocks with native iron from Disko, central West Greenland. Contributions to Mineralogy and Petrology, 77 (4) 307-324 doi:10.1007/bf00371560
Lattard, Dominique (1987) Subsolidus phase relations in the system Zr-Fe-Ti-O in equilibrium with metallic iron. Implications for lunar petrology. Contributions to Mineralogy and Petrology, 97 (2) 264-278 doi:10.1007/bf00371245
Konzett, Jürgen, Rhede, Dieter, Frost, Daniel J. (2012) The high PT stability of apatite and Cl partitioning between apatite and hydrous potassic phases in peridotite: an experimental study to 19 GPa with implications for the transport of P, Cl and K in the upper mantle. Contributions to Mineralogy and Petrology, 163 (2) 277-296 doi:10.1007/s00410-011-0672-x
Ghosh, Sujoy, Litasov, Konstantin, Ohtani, Eiji (2014) Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle. Contributions to Mineralogy and Petrology, 167 (2) doi:10.1007/s00410-014-0964-z
Pearce, Mark, Escolme, Angela (2021) Phase heritage during replacement reactions in Ti-bearing minerals. Contributions to Mineralogy and Petrology, 176 (3) doi:10.1007/s00410-021-01775-8
Konzett, J., Ulmer, P. (1999) The Stability of Hydrous Potassic Phases in Lherzolitic Mantle--an Experimental Study to 9.5 GPa in Simplified and Natural Bulk Compositions. Journal of Petrology, 40 (4) 629-652 doi:10.1093/petroj/40.4.629
KONZETT, JÜRGEN, FEI, YINGWEI (2000) Transport and Storage of Potassium in the Earth’s Upper Mantle and Transition Zone: an Experimental Study to 23 GPa in Simplified and Natural Bulk Compositions. Journal of Petrology, 41 (4) 583-603 doi:10.1093/petrology/41.4.583
 
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