- Hellingsinstabiliteiten en massatransport langsheen glaciale continentale randen, meer
- Slope instability and mass wasting events along glacial continental margins, meer
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A1 publicaties (2) [show] |
- Canals, M.; Lastras, G.; Urgeles, R.; Casamor, J.L.; Mienert, J.; Cattaneo, A.; De Batist, M.; Haflidason, H.; Imbo, Y.; Laberg, J.S.; Locat, J.; Long, D.; Longva, O.; Masson, D.G.; Sultan, N.; Trincardi, F.; Bryn, P. (2004). Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project. Mar. Geol. 213(1-4): 9-72. dx.doi.org/10.1016/j.margeo.2004.10.001, meer
- Imbo, Y.; De Batist, M.; Canals, M.; Prieto, M.J.; Baraza, J. (2003). The Gebra slide: a submarine slide on the Trinity Peninsula Margin, Antarctica. Mar. Geol. 193(3-4): 235-252. dx.doi.org/10.1016/S0025-3227(02)00664-3, meer
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Boekhoofdstuk [show] |
- De Batist, M. ; Imbo, Y.; Vermeesch, P.; Klerkx, J.; Giralt, S.; Delvaux, D.; Lignier, V.; Beck, C.; Kalugin, I.; Abdrakhmatov, K. (2002). Bathymetry and sedimentary environments of Lake Issyk-Kul, Kyrgyz Republic (Central Asia): a large, high-altitude, tectonic lake, in: Klerkx, J. et al. Lake Issyk-Kul: its natural environment. Nato Science Series: 4. Earth and Environmental Sciences, 13: pp. 101-123, meer
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Thesis [show] |
Imbo, Y. (2003). Hellingsinstabiliteiten en massatransport langsheen een glaciale continentale rand. PhD Thesis. Universiteit Gent, Faculteit Wetenschappen, Vakgroep Geologie en Bodemkunde: Gent. 186 pp., meer
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Abstract [show] |
Imbo, Y.; De Batist, M. (2001). Modern large submarine slides on continental margins: a case study on the Antarctic Peninsula margin, the Gebra Slide, in: VLIZ Young Scientists' Day, Brugge, Belgium 23 February 2001: book of abstracts. VLIZ Special Publication, 1: pp. 47, meer
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Overige publicatie [show] |
- Imbo, Y.; De Batist, M.; Baraza, J.; Canals, M. (2001). The Gebra Slide: A Late Quaternary large-scale sliding event along the Trinity Peninsula Margin, Antarctic Peninsula. J. Conf. Abstr. 6: 740, meer
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