Koninklijk Museum voor Midden Afrika; Afdeling Mineralogie, more
Function: PhD
Direct contact at institute:
Tel.: +32-(0)2-769 54 60
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| A1 Publications (4) [show] |
- Dehant, V.; Asael, D.; Baland, R.-M.; Baludikay, B.K.; Beghin, J.; Belza, J.; Beuthe, M.; Breuer, D.; Chernonozhkin, S.; Claeys, P.; Cornet, Y.; Cornet, L.; Coyette, A.; Debaille, V.; Delvigne, C.; Deproost, M.H.; De Winter, N.; Duchemin, C.; El Atrassi, F.; François, C.; De Keyser, J.; Gillmann, C.; Gloesener, E.; Goderis, S.; Hidaka, Y.; Höning, D.; Huber, M.; Hublet, G.; Javaux, E.J.; Karatekin, O.; Kodolanyi, J.; Lobo Revilla, L.; Maes, L.; Maggiolo, R.; Mattielli, N.; Maurice, M.; McKibbin, S.; Morschhauser, A.; Neumann, W.; Noack, L.; Pham, L.B.S.; Pittarello, L.; Plesa, A.C.; Rivoldini, A.; Robert, S.; Rosenblatt, P.; Spohn, T.; Storme, J.-Y.; Tosi, N.; Trinh, A.; Valdes, M.; Vandaele, A.C.; Vanhaecke, F.; Van Hoolst, T.; Van Roosbroek, N.; Wilquet, V.; Yseboodt, M. (2016). PLANET TOPERS: Planets, Tracing the Transfer, Origin, Preservation, and Evolution of their ReservoirS. Orig. Life Evol. Biosph. 46(4): 369-384. https://dx.doi.org/10.1007/s11084-016-9488-z, more
- Delvigne, C.; Opfergelt, S.; Cardinal, D.; Hofmann, A.; André, L. (2016). Desilication in Archean weathering processes traced by silicon isotopes and Ge/Si ratios. Chem. Geol. 420: 139-147. https://dx.doi.org/10.1016/j.chemgeo.2015.11.007, more
- Bolhar, R.; Hofmann, A.; Siahi, M.; Feng, Y.; Delvigne, C. (2015). A trace element and Pb isotopic investigation into the provenance and deposition of stromatolitic carbonates, ironstones and associated shales of the similar to 3.0 Ga Pongola Supergroup, Kaapvaal Craton. Geochim. Cosmochim. Acta 158: 57-78. https://dx.doi.org/10.1016/j.gca.2015.02.026, more
- Delvigne, C.; Cardinal, D.; Hofmann, A.; André, L. (2012). Stratigraphic changes of Ge/Si, REE+Y and silicon isotopes as insights into the deposition of a Mesoarchaean banded iron formation. Earth Planet. Sci. Lett. 355-356: 109-118. https://dx.doi.org/10.1016/j.epsl.2012.07.035, more
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