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Combating flooding togetherKRASOVSKAIA, Irina; GOTTSCHALK, Lars; BERG, Hallvard et al.IAHS-AISH publication. 2007, pp 377-383, issn 0144-7815, isbn 1-901502-29-5, 1Vol, 7 p.Conference Paper

Pliocene paleoenvironment evolution as interpreted from 3D-seismic data in the southern North Sea, Dutch offshore sectorKUHLMANN, Gesa; WONG, Theo E.Marine and petroleum geology. 2008, Vol 25, Num 2, pp 173-189, issn 0264-8172, 17 p.Article

Source inversion of regional intensity patterns of five earthquakes from south-western NorwayPETTENATI, F; SIROVICH, L; BUNGUM, H et al.Bollettino di Geofisica Teorica ed Applicata. 2005, Vol 46, Num 2-3, pp 111-134, issn 0006-6729, 24 p.Conference Paper

Adaptation of water management to regional climate change in a coastal region: Hydrological change vs. community perception and strategiesBORMANN, Helge; AHLHORN, Frank; KLENKE, Thomas et al.Journal of hydrology (Amsterdam). 2012, Vol 454-55, pp 64-75, issn 0022-1694, 12 p.Article

Implications of continuous structural inversion in the West Netherlands Basin for understanding controls on Palaeogene deformation in NW EuropeWORUM, Geza; MICHON, Laurent.Journal of the Geological Society (London). 2005, Vol 162, pp 73-85, issn 0016-7649, 13 p., 1Article

Impact of deglaciation on present-day intraplate seismicity in eastern North America and western Europe = Impact de la déglaciation sur la sismicité intra-plaque actuelle dans l'Est de l'Amérique du Nord et en Europe occidentaleZOBACK, Mark D; GROLLIMUND, Balz.Comptes rendus de l'Académie des sciences. Série 2. Sciences de la terre et des planètes. 2001, Vol 333, Num 1, pp 23-33, issn 1251-8050Conference Paper

1,2,4-Trichlorobenzene marine risk assessment with special emphasis on the Osparcom region North SeaVAN WIJK, D; COHET, E; GARD, A et al.Chemosphere (Oxford). 2006, Vol 62, Num 8, pp 1294-1310, issn 0045-6535, 17 p.Article

In situ stress from breakouts in the Danish Sector of the North SeaASK, M. V. S.Marine and petroleum geology. 1997, Vol 14, Num 3, pp 231-243, issn 0264-8172Article

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