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dc.creatorMorner, Nils-Axel
dc.date.accessioned2011-09-07T16:54:26Z
dc.date.available2011-09-07T16:54:26Z
dc.date.issued1984-06
dc.identifier.issn0742-6054
dc.identifier.urihttp://hdl.handle.net/1969.3/28270
dc.descriptionMorner, Nils-Axel. Differential Holocene sea level changes over the globe; evidence for glacial eustasy, geoidal eustasy, and crustal movements. Litoralia, vol. 1, no. 1, summer 1984. Pages 83-86.en
dc.description.abstractThe old theory of eustasy implied that the eustatic ocean level was displaced up and down simultaneously and equally over the globe. Due to the geoid deformation, however, two eustatic levels are never quite parallel. The present paper deals with the complexity of variables and the Holocene global observational records.en
dc.language.isoen_USen
dc.relation.ispartofseriesLitoralia;Vol 1, no. 1
dc.subjecttectonicsen
dc.subjectsea level changeen
dc.subjectisotasyen
dc.subjectgeoid deformationen
dc.subjecteustasyen
dc.subjectestuaryen
dc.titleDifferential Holocene sea level changes over the globe; evidence for glacial eustasy, geoidal eustasy, and crustal movementsen
dc.title.alternativeLitoralia: Technical Communicationsen
dc.typeArticleen


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