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Jung, S., Mezger, K., Hoernes, S., Hoffbauer, R. (2007) Altered mafic lower continental crust as a source for low δ18O-granodiorites (Damara orogen, Namibia)?. Mineralogy and Petrology, 91 (1) 1-10 doi:10.1007/s00710-007-0181-9

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Reference TypeJournal (article/letter/editorial)
TitleAltered mafic lower continental crust as a source for low δ18O-granodiorites (Damara orogen, Namibia)?
JournalMineralogy and Petrology
AuthorsJung, S.Author
Mezger, K.Author
Hoernes, S.Author
Hoffbauer, R.Author
Year2007 (September)Volume91
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00710-007-0181-9Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID16806Long-form Identifiermindat:1:5:16806:1
GUID0
Full ReferenceJung, S., Mezger, K., Hoernes, S., Hoffbauer, R. (2007) Altered mafic lower continental crust as a source for low δ18O-granodiorites (Damara orogen, Namibia)?. Mineralogy and Petrology, 91 (1) 1-10 doi:10.1007/s00710-007-0181-9
Plain TextJung, S., Mezger, K., Hoernes, S., Hoffbauer, R. (2007) Altered mafic lower continental crust as a source for low δ18O-granodiorites (Damara orogen, Namibia)?. Mineralogy and Petrology, 91 (1) 1-10 doi:10.1007/s00710-007-0181-9
In(2007, September) Mineralogy and Petrology Vol. 91 (1) Springer Science and Business Media LLC

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Jung, S., Hoernes, S., Mezger, K. (2002) Synorogenic melting of mafic lower crust: constraints from geochronology, petrology and Sr, Nd, Pb and O isotope geochemistry of quartz diorites (Damara orogen, Namibia) Contributions to Mineralogy and Petrology, 143 (5) 551-566 doi:10.1007/s00410-002-0366-5
Jung, S., Mezger, K., Hoernes, S. (2004) Shear zone-related syenites in the Damara belt (Namibia): the role of crustal contamination and source composition. Contributions to Mineralogy and Petrology, 148 (1) 104-121 doi:10.1007/s00410-004-0589-8
Bergemann, C., Jung, S., Berndt, J., Stracke, A., Hauff, F. (2014) Generation of magnesian, high-K alkali-calcic granites and granodiorites from amphibolitic continental crust in the Damara orogen, Namibia. Lithos, 198. 217-233 doi:10.1016/j.lithos.2014.03.033
Jung, S, Mezger, K, Hoernes, S (1998) Petrology and geochemistry of syn- to post-collisional metaluminous A-type granites—a major and trace element and Nd–Sr–Pb–O-isotope study from the Proterozoic Damara Belt, Namibia. Lithos, 45 (1) 147-175 doi:10.1016/s0024-4937(98)00030-9
Hoernes, S., Hoffer, E. (1985) Stable isotope evidence for fluid-present and fluid-absent metamorphism in metapelites from the Damara Orogen, Namibia. Contributions to Mineralogy and Petrology, 90 (4) 322-330 doi:10.1007/bf00384711
Simon, I., Jung, S., Romer, R.L., Garbe-Schönberg, D., Berndt, J. (2017) Geochemical and Nd-Sr-Pb isotope characteristics of synorogenic lower crust-derived granodiorites (Central Damara orogen, Namibia) Lithos, 274. 397-411 doi:10.1016/j.lithos.2016.12.033
Jung, S., Hoernes, S., Masberg, P., Hoffer, E. (1999) The Petrogenesis of Some Migmatites and Granites (Central Damara Orogen, Namibia): Evidence for Disequilibrium Melting, Wall-Rock Contamination and Crystal Fractionation. Journal of Petrology, 40 (8) 1241-1269 doi:10.1093/petroj/40.8.1241
Jung, S, Hoernes, S, Mezger, K (2000) Geochronology and petrology of migmatites from the Proterozoic Damara Belt — importance of episodic fluid-present disequilibrium melting and consequences for granite petrology. Lithos, 51 (3) 153-179 doi:10.1016/s0024-4937(99)00062-6
Masberg, H.P., Hoffer, E., Hoernes, S. (1992) Microfabrics indicating granulite-facies metamorphism in the low-pressure central Damara Orogen, Namibia. Precambrian Research, 55 (1) 243-257 doi:10.1016/0301-9268(92)90026-k
Jung, S., Mezger, K. (2003) U-Pb garnet chronometry in high-grade rocks?case studies from the central Damara orogen (Namibia) and implications for the interpretation of Sm-Nd garnet ages and the role of high U-Th inclusions. Contributions to Mineralogy and Petrology, 146 (3) 382-396 doi:10.1007/s00410-003-0506-6
Stammeier, J., Jung, S., Romer, R.L., Berndt, J., Garbe-Schönberg, D. (2015) Petrology of ferroan alkali-calcic granites: Synorogenic high-temperature melting of undepleted felsic lower crust (Damara orogen, Namibia) Lithos, 224. 114-125 doi:10.1016/j.lithos.2015.03.004
 
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