Published August 6, 1993 | Version Published
Journal Article Open

Comment on "Dynamic surface topography: A new interpretation based upon mantle flow models derived from seismic tomography" by A. M. Forte, W. R. Peltier, A. M. Dziewonski and R. L. Woodward

  • 1. ROR icon University of Michigan–Ann Arbor

Abstract

In a recent paper in this journal, Forte et al. [1993] have proposed a model of global dynamic topography with an amplitude of three kilometers (six kilometers peak to peak). If North America, Australia, and other continents were dynamically depressed by the one to two kilometers predicted, then these continents would today be below sea level and nearly covered by epeiric seas. Since the continents are nearly entirely exposed and have become progressively exposed since the Late Mesozoic the amplitude of the Forte et al., model is clearly much too large.

Additional Information

© 1993 American Geophysical Union. Received: March 9, 1993; Accepted: June 3, 1993. Funded by a NSF Presidential Young Investigator Award and a Fellowship from the David and Lucile Packard Foundation.

Attached Files

Published - 1993_Gurnis_GRL.pdf

Files

1993_Gurnis_GRL.pdf

Files (173.2 kB)

Name Size
md5:7e0c39f6a814e6232ae9128f98850de5
173.2 kB Preview Download

Additional details

Identifiers

Eprint ID
38271
Resolver ID
CaltechAUTHORS:20130503-153019049

Funding

NSF Presidential Young Investigator Award
David and Lucile Packard Foundation

Dates

Created
2013-05-03
Created from EPrint's datestamp field
Updated
2021-11-09
Created from EPrint's last_modified field

Caltech Custom Metadata