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Hagen, Bettina, Hoernes, Stephan Rötzler (2008) Geothermometry of the ultrahigh-temperature Saxon granulites revisited. Part II: Thermal peak conditions and cooling rates inferred from oxygen-isotope fractionations. European Journal of Mineralogy, 20 (6) 1117-1133 doi:10.1127/0935-1221/2008/0020-1858

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Reference TypeJournal (article/letter/editorial)
TitleGeothermometry of the ultrahigh-temperature Saxon granulites revisited. Part II: Thermal peak conditions and cooling rates inferred from oxygen-isotope fractionations
JournalEuropean Journal of Mineralogy
AuthorsHagen, BettinaAuthor
Hoernes, Stephan RötzlerAuthor
Year2008 (December 15)Volume20
Page(s)1117-1133Issue6
PublisherSchweizerbart
DOIdoi:10.1127/0935-1221/2008/0020-1858Search in ResearchGate
Mindat Ref. ID128783Long-form Identifiermindat:1:5:128783:1
GUID7be1ad1e-1823-49da-837a-e91239ad81a0
Full ReferenceHagen, Bettina, Hoernes, Stephan Rötzler (2008) Geothermometry of the ultrahigh-temperature Saxon granulites revisited. Part II: Thermal peak conditions and cooling rates inferred from oxygen-isotope fractionations. European Journal of Mineralogy, 20 (6) 1117-1133 doi:10.1127/0935-1221/2008/0020-1858
Plain TextHagen, Bettina, Hoernes, Stephan Rötzler (2008) Geothermometry of the ultrahigh-temperature Saxon granulites revisited. Part II: Thermal peak conditions and cooling rates inferred from oxygen-isotope fractionations. European Journal of Mineralogy, 20 (6) 1117-1133 doi:10.1127/0935-1221/2008/0020-1858
In(2008, December) European Journal of Mineralogy Vol. 20 (6) Schweizerbart


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