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Schorn, Simon, Diener, Johann F.A. (2019) Seemingly disparate temperatures recorded in coexisting granulite facies lithologies. Journal of Metamorphic Geology, 37 (8) 1049-1078 doi:10.1111/jmg.12500

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Reference TypeJournal (article/letter/editorial)
TitleSeemingly disparate temperatures recorded in coexisting granulite facies lithologies
JournalJournal of Metamorphic Geology
AuthorsSchorn, SimonAuthor
Diener, Johann F.A.Author
Year2019 (October)Volume37
Issue8
PublisherWiley
DOIdoi:10.1111/jmg.12500Search in ResearchGate
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Mindat Ref. ID159076Long-form Identifiermindat:1:5:159076:4
GUID0
Full ReferenceSchorn, Simon, Diener, Johann F.A. (2019) Seemingly disparate temperatures recorded in coexisting granulite facies lithologies. Journal of Metamorphic Geology, 37 (8) 1049-1078 doi:10.1111/jmg.12500
Plain TextSchorn, Simon, Diener, Johann F.A. (2019) Seemingly disparate temperatures recorded in coexisting granulite facies lithologies. Journal of Metamorphic Geology, 37 (8) 1049-1078 doi:10.1111/jmg.12500
In(2019, October) Journal of Metamorphic Geology Vol. 37 (8) Wiley

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Diener, Johann F. A., Macey, Paul H. (2024) Orogen‐scale uniformity of recorded granulite facies conditions due to thermal buffering and melt retention. Journal of Metamorphic Geology, 42 (7) 909-931 doi:10.1111/jmg.12778
Schorn, Simon, Diener, Johann F.A., Sorger, Dominik, Clark, Chris (2020) The contribution of charnockite magmatism to achieve near-ultrahigh temperatures in the Namaqua–Natal Metamorphic Province, South Africa. Lithos, 368. 105585pp. doi:10.1016/j.lithos.2020.105585
Schorn, Simon, Diener, Johann F.A., Powell, Roger, StĂźwe, Kurt (2018) Thermal buffering in the orogenic crust. Geology, 46 (7) 643-646 doi:10.1130/g40246.1
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(2019) Issue Information. Journal of Metamorphic Geology, 37 (8) doi:10.1111/jmg.12438
Schorn, Simon (2022) Self‐induced incipient ‘eclogitization’ of metagranitoids at closed‐system conditions. Journal of Metamorphic Geology, 40 (7) 1271-1290 doi:10.1111/jmg.12665
Schorn, S., Diener, J. F. A. (2017) Details of the gabbro-to-eclogite transition determined from microtextures and calculated chemical potential relationships. Journal of Metamorphic Geology, 35 (1) 55-75 doi:10.1111/jmg.12220
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