Humez, Pauline; Négrel, Philippe; Lagneau, Vincent; Lions, Julie; Kloppmann, Wolfram; Gal, Frédérick; Millot, Romain; Guerrot, Catherine; Flehoc, Christine (12. mars 2014). «CO2–water–mineral reactions during CO2 leakage: Geochemical and isotopic monitoring of a CO2 injection field test». Chemical Geology(engelsk). 368: 11–30. ISSN0009-2541. doi:10.1016/j.chemgeo.2014.01.001. Besøkt 13. november 2021. «The “Svelvik moraine”, mainly consisting of fluvioglacial gravel from the last Holocene deglaciation, nearly bars a branch of Oslofjord, called Drammensfjord, on its western side, forming a narrow peninsula. The depth of underlying Permian sedimentary bedrock and granite (Holtedahl et al., 1934) is between 300 and 400 m. The central part of the ridge rises to 70 m above sea level, constituting a sandy phreatic aquifer with a depositional dip of about 10° south. The sediments present are mostly well sorted coarse-grained sand with gravel lenses.»
dt.no
Kristiansen, Håkon Aase (19. februar 2023). «(+) Svelvikferjas historie». Drammens Tidende(norsk). Besøkt 20. februar 2023.
Humez, Pauline; Négrel, Philippe; Lagneau, Vincent; Lions, Julie; Kloppmann, Wolfram; Gal, Frédérick; Millot, Romain; Guerrot, Catherine; Flehoc, Christine (12. mars 2014). «CO2–water–mineral reactions during CO2 leakage: Geochemical and isotopic monitoring of a CO2 injection field test». Chemical Geology(engelsk). 368: 11–30. ISSN0009-2541. doi:10.1016/j.chemgeo.2014.01.001. Besøkt 13. november 2021. «The “Svelvik moraine”, mainly consisting of fluvioglacial gravel from the last Holocene deglaciation, nearly bars a branch of Oslofjord, called Drammensfjord, on its western side, forming a narrow peninsula. The depth of underlying Permian sedimentary bedrock and granite (Holtedahl et al., 1934) is between 300 and 400 m. The central part of the ridge rises to 70 m above sea level, constituting a sandy phreatic aquifer with a depositional dip of about 10° south. The sediments present are mostly well sorted coarse-grained sand with gravel lenses.»
Humez, Pauline; Négrel, Philippe; Lagneau, Vincent; Lions, Julie; Kloppmann, Wolfram; Gal, Frédérick; Millot, Romain; Guerrot, Catherine; Flehoc, Christine (12. mars 2014). «CO2–water–mineral reactions during CO2 leakage: Geochemical and isotopic monitoring of a CO2 injection field test». Chemical Geology(engelsk). 368: 11–30. ISSN0009-2541. doi:10.1016/j.chemgeo.2014.01.001. Besøkt 13. november 2021. «The “Svelvik moraine”, mainly consisting of fluvioglacial gravel from the last Holocene deglaciation, nearly bars a branch of Oslofjord, called Drammensfjord, on its western side, forming a narrow peninsula. The depth of underlying Permian sedimentary bedrock and granite (Holtedahl et al., 1934) is between 300 and 400 m. The central part of the ridge rises to 70 m above sea level, constituting a sandy phreatic aquifer with a depositional dip of about 10° south. The sediments present are mostly well sorted coarse-grained sand with gravel lenses.»
