Intermediate-wavelength (400–600 km), South Pacific geoidal undulations: their relationship to linear volcanic chains-Reference-Cited by-同舟云学术

Intermediate-wavelength (400–600 km), South Pacific geoidal undulations: their relationship to linear volcanic chains

Published:1991-03 Issue:3-4 Volume:102 Page:430-443
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Baudry Nicolas,Kroenke Loren

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference23 articles.

1. Evidence for small-scale mantle convection from Seasat altimeter data;Haxby;J. Geophys. Res.,1986

2. Platform of mantle convection beneath the Pacific ocean;McKenzie;Nature,1980

3. Compensation of swells and plateaus in the North Pacific: No direct evidence for mantle convection;Sandwell;J. Geophys. Res.,1988

4. Properties of wide-spread, intermediate wavelength (400–600 km), South Pacific geoidal undulations: their relationship to linear volcanic seamount chains;Baudry;EOS Trans. Am. Geophys. Union,1989

5. Grim gravity model improvement using LAGEOS (GRIM3-L1);Reigber;J. Geophys. Res.,1985

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