The Hudson Bay free-air gravity anomaly and glacial rebound

Details The Hudson Bay free-air gravity anomaly and glacial rebound The Hudson Bay free-air gravity anomaly and glacial rebound

May 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19..861j&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 19, no. 9, May 4, 1992, p. 861-864.

Physics

11

Glaciology, Gravity Anomalies, Hudson Bay (Canada), Isostasy, Earth Mantle, Geoids, Models

Scientific paper

Current models of the Laurentide deglaciation predict only 15 percent to
30 percent of the observed Hudson Bay free-air gravity anomaly low.
Unless these models are able to be modified, the source of the remainder
of this free-air gravity anomaly must be sought elsewhere, such as in
mantle convection.

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