| Elsen, Jan |
ORCID
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Informatie laatst gewijzigd: 2016-07-08 |
Katholieke Universiteit Leuven; Departement Aard- en Omgevingswetenschappen; Afdeling Geologie, meer
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| A1 publicaties (5) [show] |
 Goolaerts, S.; De Ceuster, J.; Mollen, F.H.; Gijsen, B.; Bosselaers, M.; Lambert, O.; Uchman, A.; Van Herck, M.; Adriaens, R.; Houthuys, R.; Louwye, S.; Bruneel, Y.; Elsen, J.; Hoedemakers, K. (2020). The upper Miocene Deurne Member of the Diest Formation revisited: unexpected results from the study of a large temporary outcrop near Antwerp International Airport, Belgium. Geol. Belg. 23(3-4): 219-252. https://dx.doi.org/10.20341/gb.2020.011, meer- Adriaens, R.; Zeelmaekers, E.; Fettweis, M.; Vanlierde, E.; Vanlede, J.; Stassen, P.; Elsen, J.; Srodon, J.; Vandenberghe, N. (2018). Quantitative clay mineralogy as provenance indicator for recent muds in the southern North Sea. Mar. Geol. 398: 48-58. https://dx.doi.org/10.1016/j.margeo.2017.12.011, meer
- Blomme, A.; Elsen, J.; Brems, D.; Shortland, A.; Dotsika, E.; Degryse, P. (2016). Tracing the primary production location of core-formed glass vessels, Mediterranean Group I. Journal of Archaeological Science: Reports 5: 1-9. https://dx.doi.org/10.1016/j.jasrep.2015.10.031, meer
- Machiels, L.; Garces, D.; Snellings, R.; Vilema, W.; Morante, F.; Paredes, C.; Elsen, J. (2014). Zeolite occurrence and genesis in the Late-Cretaceous Cayo arc of Coastal Ecuador: Evidence for zeolite formation in cooling marine pyroclastic flow deposits. Applied Clay Science 87: 108-119. dx.doi.org/10.1016/j.clay.2013.10.018, meer
- Machiels, L.; Morante, F.; Snellings, R.; Calvo, B.; Canoira, L.; Paredes, C.; Elsen, J. (2008). Zeolite mineralogy of the Cayo formation in Guayaquil, Ecuador. Applied Clay Science 42(1-2): 180-188. https://dx.doi.org/10.1016/j.clay.2008.01.012, meer
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| Boekhoofdstuk [show] |
- Adriaens, R.; Zeelmakers, E.; Fettweis, M.; Vanlierde, E.; Vanlede, J.; Stassen, P.; Elsen, J.; Srodon, J.; Vandenberghe, N. (2017). Quantitative clay mineralogy as provenance indicator for the recent muds located at the marine limit of influence of the Scheldt estuary, in: Schelde-Ems workshop 2017. pp. 12-16, meer
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