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(Article of periodic en Anglais - 1984)

Document title

Differential Holocene sea level changes over the Globe. Evidence for glacial eustasy, geoidal eustasy, and crustal movements

Authors(s) and Affiliation(s)

MORNER N. A. ;

Abstract

The 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.

Keyword(s)

En français : Déformation du géoïde ; Géoïde ; Isostasi`; >a href="/advancedsearch/results?raz=true&mc=%22Variation%20du%20niveau%20marin%22" title="Relancer la recherche sur ce mot-clé">Variation du niveau marin ; Tectonique ; Holocène ; Eustatisme ; Glacio-eustatisme ; Géoïdo-eustatisme ; Quaternaire marin ; PICG 200 ; Niveau marin ; Théorie ; Gphy ; Géographie physique

En anglais : Physical geography

Source

Article of periodic

published at : Litoralia. An international journal for the coastal sciences Ft. Landerdale, Fla

Editor :

Millesime : 1984, vol. 1, no1 [pp. 83-86]

Language

Anglais

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