Mantle phase transitions and the free air gravity anomalies over Fennoscandia and Laurentia

The interpretation of free air gravity anomalies over present day centers of postglacial rebound has always been controversial. We show that the observed gravity anomalies over both Fennoscandia and Laurentia and the associated relative sea level variations since deglaciation are explicable with a s...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Peltier, WR, Wu, P
Format: Article in Journal/Newspaper
Language:English
Published: 1982
Subjects:
Online Access:https://doi.org/10.1029/GL009i007p00731
http://hdl.handle.net/10722/192110
Description
Summary:The interpretation of free air gravity anomalies over present day centers of postglacial rebound has always been controversial. We show that the observed gravity anomalies over both Fennoscandia and Laurentia and the associated relative sea level variations since deglaciation are explicable with a simple Newtonian viscoelastic model of the earth if the earth model includes the density jumps in the mantle associated with the phase transitions at 420 and 670 km depth. The result has important implications for mantle convection since the observed free air anomalies are very sensitive to the viscosity of the mantle beneath the deepest phase transition.