georefid:2002-039919SEDIS Publication Catalogue
ana.macario@awi.de
http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2002-039919<gco:CharacterString>Flow in the lower continental crust as a mechanism for the Quaternary uplift of the Rhenish Massif, North-west Europe</gco:CharacterString>2001-01-01publicationgeorefid:2002-039919Westaway, RobertConsultant, 16 Neville Square, GBR, United KingdomauthorA.A. Balkema Publishers, NetherlandspublisherdocumentHardcopyIn: Maddy, Darrel (editor), Macklin, Mark G. (editor), Woodward, Jamie C. (editor), River basin sediment systems; archives of environmental change87-167completedSolid-earth geophysicsGeomorphologyBelgiumcausesCenozoicCentral Europeclimate changecontinental crustcrustcrustal thickeningdrainage basinsEifelElbe RiverEquatorial Pacificerosion featureserosion rateserosion surfacesEuropefluvial featuresfluvial sedimentationgeochronologygeomorphologyGermanyHoloceneincision ratesintraplate processesisostasyisotope ratiosisotopesLeg 138lower crustLuxembourgmagmatismmagnetostratigraphymechanismMeuse RiverMeuse ValleymodelsNeogeneneotectonicsNetherlandsnorthwestern EuropeO-18/O-16Ocean Drilling ProgramODP Site 846oxygenPacific OceanpaleohydrologyPleistocenePlioceneQuaternaryrelative agereliefRhenish SchiefergebirgeRhine RiverRhine ValleyRhineland-Palatinate GermanyriversScheldt Riversea-level changessedimentationstable isotopesstructural controlsSwitzerlandtectonicsterracesTertiarytheoretical studiesupliftsupper PliocenevolcanismWeser RiverWestern Europeurn:org.iodp:exp:138urnlargerWorkCitationcampaignurn:org.iodp:exp:138:site:846urnlargerWorkCitationstudyurn:org.iodp:exp:138urnlargerWorkCitationcampaignEnglishgeoscientificInformation-90.490616.3000-3.054953.5500BelgiumEifelElbe RiverLuxembourgMeuse RiverNetherlandsRhine RiverSwitzerlandWeser RiverIncludes appendix