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2018
Oeser, M., Ruprecht, P., & Weyer, S. (2018). Combined Fe-Mg chemical and isotopic zoning in olivine constraining magma mixing-to-eruption timescales for the continental arc volcano Irazú (Costa Rica) and Cr diffusion in olivine. American Mineralogist, 103(4), 582-599. https://doi.org/10.2138/am-2018-6258
Roebbert, Y., Rabe, K., Lazarov, M., Schuth, S., Schippers, A., Dold, B., & Weyer, S. (2018). Fractionation of Fe and Cu isotopes in acid mine tailings: Modification and application of a sequential extraction method. Chemical geology, 493, 67-79. https://doi.org/10.1016/j.chemgeo.2018.05.026
Shishkina, T. A., Portnyagin, M. V., Botcharnikov, R. E., Almeev, R. R., Simonyan, A. V., Garbe-Schönberg, DI., Schuth, S., Oeser, M., & Holtz, F. (2018). Experimental calibration and implications of olivine-melt vanadium oxybarometry for hydrous basaltic arc magmas. American Mineralogist, 103(3), 369-383. https://doi.org/10.2138/am-2018-6210
Wang, Z., Lazarov, M., Steinmann, L. K., Becker, H., Zou, Z., & Geng, X. (2018). The distribution of lead and thallium in mantle rocks: Insights from the Balmuccia peridotite massif (Italian Alps). American mineralogist, 103(8 ), 1185-1199. https://doi.org/10.2138/am-2018-6423
Wegwerth, A., Eckert, S., Dellwig, O., Schnetger, B., Severmann, S., Weyer, S., Brüske, A., Kaiser, J., Köster, J., Arz, H. W., & Brumsack, H. J. (2018). Redox evolution during Eemian and Holocene sapropel formation in the Black Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 489, 249-260. https://doi.org/10.1016/j.palaeo.2017.10.014
2017
Andersen, M. B., Stirling, C. H., & Weyer, S. (2017). Uranium isotope fractionation. In Non-Traditional Stable Isotopes (Band 82, S. 799-850). (Reviews in Mineralogy and Geochemistry). Walter de Gruyter GmbH. https://doi.org/10.2138/rmg.2017.82.19
Andersen, M. B., Stirling, C. H., & Weyer, S. (2017). Uranium isotope fractionation. In N. Dauphas, J. Watkins, & F.-Z. Teng (Hrsg.), Non-Traditional Stable Isotopes (S. 799-850). (Reviews in Mineralogy and Geochemistry; Band 82). Mineralogical Society of America. https://doi.org/10.2138/rmg.2017.82.19
Bhattacharyya, A., Campbell, K. M., Kelly, S. D., Roebbert, Y., Weyer, S., Bernier-Latmani, R., & Borch, T. (2017). Biogenic non-crystalline U (IV) revealed as major component in uranium ore deposits. Nature Communications, 8, Artikel 15538. https://doi.org/10.1038/ncomms15538
Chernonozhkin, S. M., Weyrauch, M., Goderis, S., Oeser, M., McKibbin, S. J., Horn, I., Hecht, L., Weyer, S., Claeys, P., & Vanhaecke, F. (2017). Thermal equilibration of iron meteorite and pallasite parent bodies recorded at the mineral scale by Fe and Ni isotope systematics. Geochimica et cosmochimica acta, 217, 95-111. https://doi.org/10.1016/j.gca.2017.08.022
Collinet, M., Charlier, B., Namur, O., Oeser, M., Médard, E., & Weyer, S. (2017). Crystallization history of enriched shergottites from Fe and Mg isotope fractionation in olivine megacrysts. Geochimica et cosmochimica acta, 207, 277-297. https://doi.org/10.1016/j.gca.2017.03.029