Professur für Mineralogie

Address:
Schlossgarten 5
91054 Erlangen


Publications (Download BibTeX)

Go to first page Go to previous page 1 of 3 Go to next page Go to last page

Gose, J., & Schmädicke, E. (2018). Water incorporation in garnet: Coesite versus quartz eclogite from Erzgebirge and Fichtelgebirge. Journal of Petrology, 59(2), 207-232. https://dx.doi.org/10.1093/petrology/egy022
Schmädicke, E., Gose, J., & Stalder, R. (2018). Water in Abyssal Peridotite: Why Are Melt-Depleted Rocks so Water Rich? Geochemistry Geophysics Geosystems, 19(6), 1824-1843. https://dx.doi.org/10.1029/2017GC007390
Will, T.M., Schmädicke, E., Ling, X.-X., Li, X.-H., & Li, Q.-L. (2018). New evidence for an old idea: Geochronological constraints for a paired metamorphic belt in the central European Variscides. Lithos, 278-297. https://dx.doi.org/10.1016/j.lithos.2018.01.008
Schmädicke, E., Will, T.M., Ling, X., Li, X.-H., & Li, Q.-L. (2018). Rare peak and ubiquitous post-peak zircon in eclogite: Constraints for the timing of UHP and HP metamorphism in Erzgebirge, Germany. Lithos, 322, 250-267. https://dx.doi.org/10.1016/j.lithos.2018.10.017
Will, T.M., Schulz, B., & Schmädicke, E. (2017). The timing of metamorphism in the Odenwald–Spessart basement, Mid-German Crystalline Zone. International Journal of Earth Sciences, 106(5), 1631-1649. https://dx.doi.org/10.1007/s00531-016-1375-3
Gose, J., & Schmädicke, E. (2017). Water transport by subduction: Clues from garnet of Erzgebirge UHP eclogite. American Mineralogist, 102(5), 975-986. https://dx.doi.org/10.2138/am-2017-5920
Schmädicke, E., Gose, J., Reinhardt, J., Will, T.M., & Stalder, R. (2015). Garnet in cratonic and non-cratonic mantle and lower crustal xenoliths from southern Africa: Composition, water incorporation and geodynamic constraints. Precambrian Research, 270, 285-299. https://dx.doi.org/10.1016/j.precamres.2015.09.019
Will, T.M., Lee, S.-H., Schmädicke, E., Frimmel, H.E., & Okrusch, M. (2015). Variscan terrane boundaries in the Odenwald-Spessart basement, Mid-German Crystalline Zone: New evidence from ocean ridge, intraplate and arc-derived metabasaltic rocks. Lithos, 23-42. https://dx.doi.org/10.1016/j.lithos.2015.01.018
Schmädicke, E., Will, T.M., & Mezger, K. (2015). Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? Lithos, 238, 185-206. https://dx.doi.org/10.1016/j.lithos.2015.09.016
Ling, X.-X., Schmädicke, E., Li, Q.-L., Gose, J., Wu, R.-H., Wang, S.-Q.,... Li, X.-H. (2015). Age determination of nephrite by in-situ SIMS U-Pb dating syngenetic titanite: A case study of the nephrite deposit from Luanchuan, Henan, China. Lithos, 289-299. https://dx.doi.org/10.1016/j.lithos.2015.02.019
Hesse, K., Gose, J., Stalder, R., & Schmädicke, E. (2015). Water in orthopyroxene from abyssal spinel peridotites of the East Pacific Rise (ODP Leg 147: Hess Deep). Lithos, 232, 23-34. https://dx.doi.org/10.1016/j.lithos.2015.06.011
Schmädicke, E. (2013). Composition and distinction of white nephrite from Asian deposits. Neues Jahrbuch für Mineralogie-Abhandlungen, 190(1), 49-65. https://dx.doi.org/10.1127/0077-7757/2013/0229
Schmädicke, E. (2012). Olivine from spinel peridotite xenoliths: Hydroxyl incorporation and mineral composition. American Mineralogist, 98(10), 1870-1880. https://dx.doi.org/10.2138/am.2013.4440
Schmädicke, E. (2011). Heterogeneous mantle underneath the North Atlantic: Evidence from water in orthopyroxene, mineral composition and equilibrium conditions of spinel peridotite from different locations at the Mid-Atlantic Ridge. Lithos, 125, 308-320. https://dx.doi.org/10.1016/j.lithos.2011.02.014
Schmädicke, E., Okrusch, M., Rupprecht-Gutowski, P., & Will, T.M. (2011). Garnet pyroxenite, eclogite and alkremite xenoliths from the off-craton Gibeon Kimberlite Field, Namibia: A window into the upper mantle of the Rehoboth Terrane. Precambrian Research, 191, 1-17. https://dx.doi.org/10.1016/j.precamres.2011.07.010
Schmädicke, E. (2011). Water in mantle orthopyroxene-no visible change in defect water during serpentinization. European Journal of Mineralogy, 23(4), 529-536. https://dx.doi.org/10.1127/0935-1221/2011/0023-2122
Schmädicke, E., Gose, J., & Will, T.M. (2010). The P-T evolution of ultra high temperature garnet-bearing ultramafic rocks from the Saxonian Granulitgebirge Core Complex, Bohemian Massif. Journal of Metamorphic Geology, 28(5), 489-508. https://dx.doi.org/10.1111/j.1525-1314.2010.00876.x
Will, T.M., Frimmel, H.E., Zeh, A., Le Roux, P., & Schmädicke, E. (2010). Tectonic and crustal evolution of the Shackleton Range, East Antarctica: Geochemical and isotope contraints. Precambrian Research, 180, 85-112. https://dx.doi.org/10.1016/j.precamres.2010.03.005
Will, T.M., Frimmel, H.E., Zeh, A., Le Roux, P., & Schmädicke, E. (2010). Geochemical and isotopic constraints on the tectonic and crustal evolution of the Shackleton Range, East Antarctica, and correlation with other Gondwana crustal segments. Precambrian Research, 180, 85-112. https://dx.doi.org/10.1016/j.precamres.2010.03.005
Will, T.M., Schmädicke, E., & Frimmel, H.E. (2010). Deep solid-state equilibration and deep melting of plagioclase-free spinel peridotite from the slow-spreading Mid-Atlantic Ridge, ODP Leg 153. Mineralogy and Petrology, 100(3), 185-200. https://dx.doi.org/10.1007/s00710-010-0125-7

Last updated on 2019-24-04 at 10:27