Aarhus University Seal

Publications from Department of Geoscience

Sort by: Date | Author | Title

Rasmussen, E. S., Heilmann-Clausen, C., Waagstein, R. & Eidvin, T. (2008). The Tertiary of Norden. Episodes, 31(1), 66-72.
Rasmussen, K. R., Looms, M. C., Haarder, E. B., Nielsen, L. & Jensen, K. H. (2008). Detailed hydrogeophysical investigation of the unsaturated flow patterns. Abstract from EGU2008, Vienna, Austria.
Rasmussen, C. & Mootz, K. (2011). Dynamic Image Analysis (DIA). Geologisk Nyt, (6).
Rasmussen, K. R., Merrison, J. P. & Nørnberg, P. (2011). Wind Tunnels for the Study of Particle Transport. In J. Colman Lerner & U. Boldes (Eds.), Wind Tunnels and Experimental Fluid Dynamics Research (pp. 51-74). InTech - Open Access Publisher. http://www.intechopen.com/books/wind-tunnels-and-experimental-fluid-dynamics-research
Rasmussen, K. R. & Kristiansen, S. M. (2013). Hvor udspringer kilden under Aarhus Universitet? Morgensavisen Jyllands-Posten, Sektion: Newton(Artikel-id: e39ad2eb ), 2.
Rasmussen, T., Thomsen, E., Skirbekk, K., Slubowska-Woldengen, M., Klitgaard-Kristensen, D. & Koc, N. (2014). Spatial and temporal distribution of Holocene temperature maxima in the northern Nordic seas: interplay of Atlantic-, Arctic- and polar water masses. Quaternary Science Reviews, 92(SI), 280-291. https://doi.org/10.1016/j.quascirev.2013.10.034
Rasmussen, C. F., Christiansen, H. H., Buylaert, J. P., Cunningham, A., Schneider, R., Knudsen, M. F. & Stevens, T. (2023). High-resolution OSL dating of loess in Adventdalen, Svalbard: Late Holocene dust activity and permafrost development. Quaternary Science Reviews, 310, Article 108137. https://doi.org/10.1016/j.quascirev.2023.108137
Rasmussen, T. L., Thomsen, E., Van Weering, T. C. E. & Labeyrie, L. (1996). Rapid changes in surface and deep water conditions at the Faeroe Margin during the last 58,000 years. Paleoceanography and Paleoclimatology, 11(6), 757-771. https://doi.org/10.1029/96PA02618
Rasmusen, T. L., Thomsen, E., Kuijpers, A. & Vastegård, S. (2003). Late warming and early cooling of the sea surface in the Nordic seas during MIS 5e (Eemian Interglacial). Quaternary Science Review, 22, 809-821.