Global sea‐level changes have been occurring since the last Pleistocene deglaciation. Recently the contribution of current postglacial rebound to local sea‐level variations has been removed by means of a radially stratified earth model in order to assess the amount of sea‐level rise due to recent climatic changes. We have studied the effects of lateral variations in the viscosity structure on the postglacial uplift rates along the continental margins. Finite‐element calculations in cylindrical geometry show that the spread in the cumulative vertical displacement may be affected by 20% in the presence of lateral rheological contrasts. But the vertical rates of deformation can attain differences of up to 50% for the different models. Horizontal deformation rates along continental margins are much more affected by the lateral variations in viscosity and can be used in the future as constraints on mantle rheology. Copyright 1990 by the American Geophysical Union.
Effects of lateral viscosity variations on postglacial rebound: Implications for recent sea‐level trends / Gasperini P.; Yuen D.A.; Sabadini R.. - In: GEOPHYSICAL RESEARCH LETTERS. - ISSN 0094-8276. - STAMPA. - 17:1(1990), pp. 5-8. [10.1029/GL017i001p00005]
Effects of lateral viscosity variations on postglacial rebound: Implications for recent sea‐level trends
Gasperini P.
Primo
Membro del Collaboration Group
;Sabadini R.Ultimo
Membro del Collaboration Group
1990
Abstract
Global sea‐level changes have been occurring since the last Pleistocene deglaciation. Recently the contribution of current postglacial rebound to local sea‐level variations has been removed by means of a radially stratified earth model in order to assess the amount of sea‐level rise due to recent climatic changes. We have studied the effects of lateral variations in the viscosity structure on the postglacial uplift rates along the continental margins. Finite‐element calculations in cylindrical geometry show that the spread in the cumulative vertical displacement may be affected by 20% in the presence of lateral rheological contrasts. But the vertical rates of deformation can attain differences of up to 50% for the different models. Horizontal deformation rates along continental margins are much more affected by the lateral variations in viscosity and can be used in the future as constraints on mantle rheology. Copyright 1990 by the American Geophysical Union.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.