Geoid heights over the Louisville Ridge (South Pacific)
- 10 December 1984
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 89 (B13) , 11171-11179
- https://doi.org/10.1029/jb089ib13p11171
Abstract
Geoid heights over the Louisville Ridge seamount chain, deduced from the Seasat satellite altimeter data, have been analyzed and interpreted. Two uncharted seamounts belonging to the chain have been detected. The elastic thickness of the oceanic lithosphere has been determined along the chain. This was done rigorously using the three‐dimensional geoid and bathymetry maps and was also computed approximately using spectral methods on geoid and bathymetry profiles. A slightly increasing elastic thickness from the southeast to the northwest, in the range 15.5–22.5 km has been estimated.Keywords
This publication has 31 references indexed in Scilit:
- Bathymetry estimates in the southern oceans from Seasat altimetryNature, 1983
- Thermal parameters of the oceanic lithosphere estimated from geoid height dataJournal of Geophysical Research, 1983
- Regional compensation of subducted lithosphere: effects on geoid, gravity and topography from a preliminary modelEarth and Planetary Science Letters, 1981
- On the response of the ocean lithosphere to sea-mount loads from Geos 3 satellite radar altimeter observationsGeophysical Journal International, 1980
- An analysis of isostasy in the world's oceans: 2. Midocean ridge crestsJournal of Geophysical Research, 1979
- An analysis of isostasy in the world's oceans: 3. Aseismic ridgesJournal of Geophysical Research, 1979
- Geoid of the Kerguelen Islands area determined from Geos 3 altimeter dataJournal of Geophysical Research, 1979
- Tertiary Pacific Plate Motion Deduced from the Hawaiian-Emperor ChainGSA Bulletin, 1973
- The Louisville Ridge—A possible extention of the Eltanin Fracture ZonePublished by Wiley ,1971
- Experimental isostasy: 1. Theory of the determination of the Earth's isostatic response to a concentrated loadJournal of Geophysical Research, 1970