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Stalder, Roland, Ulmer, Peter (2001) Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone. Contributions to Mineralogy and Petrology, 140 (6) 670-679 doi:10.1007/s004100000208

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Reference TypeJournal (article/letter/editorial)
TitlePhase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone
JournalContributions to Mineralogy and Petrology
AuthorsStalder, RolandAuthor
Ulmer, PeterAuthor
Year2001 (March)Volume140
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100000208Search in ResearchGate
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Mindat Ref. ID77986Long-form Identifiermindat:1:5:77986:7
GUID0
Full ReferenceStalder, Roland, Ulmer, Peter (2001) Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone. Contributions to Mineralogy and Petrology, 140 (6) 670-679 doi:10.1007/s004100000208
Plain TextStalder, Roland, Ulmer, Peter (2001) Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone. Contributions to Mineralogy and Petrology, 140 (6) 670-679 doi:10.1007/s004100000208
In(2001, March) Contributions to Mineralogy and Petrology Vol. 140 (6) Springer Science and Business Media LLC

See Also

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Stalder, Roland, Ulmer, Peter (2001) Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone. Contributions to Mineralogy and Petrology, 140 (6) 754 doi:10.1007/s004100100246
Franz, G., Ackermand, D. (1980) Phase relations and metamorphic history of a clinohumite-chlorite-serpentine-marble from the Western Tauern Area (Austria) Contributions to Mineralogy and Petrology, 75 (2) 97-110 doi:10.1007/bf00389771
Stalder, R., Ulmer, P., Thompson, A., Günther, D. (2001) High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions. Contributions to Mineralogy and Petrology, 140 (5) 607-618 doi:10.1007/s004100000212
Sweeney, R. J., Thompson, A. B., Ulmer, P. (1993) Phase relations of a natural MARID composition and implications for MARID genesis, lithospheric melting and mantle metasomatism. Contributions to Mineralogy and Petrology, 115 (2) 225-241 doi:10.1007/bf00321222
Okay, A. I. (1980) Mineralogy, petrology, and phase relations of glaucophane-lawsonite zone blueschists from the Tav?anli Region, Northwest Turkey. Contributions to Mineralogy and Petrology, 72 (3) 243-255 doi:10.1007/bf00376143
Nandedkar, Rohit H., Ulmer, Peter, Müntener, Othmar (2014) Fractional crystallization of primitive, hydrous arc magmas: an experimental study at 0.7 GPa. Contributions to Mineralogy and Petrology, 167 (6) doi:10.1007/s00410-014-1015-5
Stalder, Roland, Karimova, Asiya, Konzett, Jürgen (2015) OH-defects in multiple-doped orthoenstatite at 4–8 GPa: filling the gap between pure and natural systems. Contributions to Mineralogy and Petrology, 169 (4) doi:10.1007/s00410-015-1133-8
Ulmer, Peter (1989) The dependence of the Fe2+-Mg cation-partitioning between olivine and basaltic liquid on pressure, temperature and composition. Contributions to Mineralogy and Petrology, 101 (3) 261-273 doi:10.1007/bf00375311
Prechtel, Felix, Stalder, Roland (2011) The potential use of OH-defects in enstatite as geobarometer. Contributions to Mineralogy and Petrology, 162 (3) 615-623 doi:10.1007/s00410-011-0615-6
Stalder, Roland (2012) Comment on “The beginnings of hydrous mantle wedge melting”, CB Till, TL Grove, AC Withers, Contributions to Mineralogy and Petrology, DOI 10.1007/s00410-011-0692-6. Contributions to Mineralogy and Petrology, 164 (6) 1069-1071 doi:10.1007/s00410-012-0795-8
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
 
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