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Nägler, Thomas; Vögelin, Andrea; Neubert, Nadja; Greber, Nicolas; Villa, Igor Maria (2013). Mo isotope fractionation in surface processes: an unwanted complication (invited) (Unpublished). In: Environmetal Isotopes EMI13. Ascona. 18-23 August 2013.
Nägler, Thomas; Pierret, Marie-Claire; Vögelin, Andrea; Pettke, Thomas; Aschwanden, Lukas; Villa, Igor Maria (2020). Small catchment scale Mo isotope balance and its implications for global Mo isotope cycling. In: Dontsova, Katerina; Balogh-Brunstad, Zsuzsanna; Le Roux, Gaël (eds.) Biogeochemical Cycles: Ecological Drivers and Environmental Impact. Geophysical Monograph Series: Vol. 251 (pp. 163-189). American Geophysical Union 10.1002/9781119413332.ch8
Vögelin, Andrea; Pettke, Thomas; Greber, Nicolas; von Niederhäusern, Brigitte; Nägler, Thomas (2014). Magma differentiation fractionates Mo isotope ratios: Evidence from the Kos Plateau Tuff (Aegean Arc). Lithos, 190-191, pp. 440-448. Elsevier 10.1016/j.lithos.2013.12.016
Cabral, Alexandre R.; Creaser, Robert A.; Nägler, Thomas; Lehmann, Bernd; Vögelin, Andrea R.; Belyatsky, Boris; Pašava, Jan; Seabra Gomes, Antônio A.; Galbiatti, Henry; Böttcher, Michael E.; Escher, Peter (2013). Trace-element and multi-isotope geochemistry of Late-Archean black shales in the Carajás iron-ore district, Brazil. Chemical geology, 362, pp. 91-104. Elsevier 10.1016/j.chemgeo.2013.08.041
Greber, Nicolas; Hofmann, B.A.; Voegelin, A.; Villa, I.M.; Nägler, T.F. (2011). Mo isotope composition in Mo-rich high- and low-T hydrothermal systems from the Swiss Alps. Geochimica et cosmochimica acta, 75(21), pp. 6600-6609. New York, N.Y.: Elsevier Science 10.1016/j.gca.2011.08.034
Voegelin, Andrea R.; Nägler, Thomas; Samankassou, Elias; Villa, Igor (2009). Molybdenum isotopic composition of modern and Carboniferous carbonates. Chemical geology, 265(3-4), pp. 488-498. Amsterdam: Elsevier 10.1016/j.chemgeo.2009.05.015
Wille, M.; Kramers, J. D.; Nägler, T. F.; Beukes, N. J.; Schröder, S.; Meisel, Th.; Lacassie, J. P.; Voegelin, A. R. (2007). Evidence for a gradual rise of oxygen between 2.6 and 2.5 Ga from Mo isotopes and Re-PGE signatures in shales. Geochimica et cosmochimica acta, 71(10), pp. 2417-2434. New York, N.Y.: Elsevier Science 10.1016/j.gca.2007.02.019
