Global relationship between oceanic geoid and seafloor depth: New results
- 1 January 1987
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 14 (1), 1-4
- https://doi.org/10.1029/gl014i001p00001
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- Crustal structure in the Society and Tuamotu Islands, French PolynesiaGeophysical Journal International, 1987
- Global relationship between oceanic geoid and topographyJournal of Geophysical Research, 1986
- Gravity and convection in a two-layer mantleEarth and Planetary Science Letters, 1985
- GRIM gravity model improvement using LAGEOS (GRIM3‐L1)Journal of Geophysical Research, 1985
- Lower mantle heterogeneity, dynamic topography and the geoidNature, 1985
- Steady state, secondary convection beneath lithospheric plates with temperature‐ and pressure‐dependent viscosityJournal of Geophysical Research, 1984
- Planform of mantle convection beneath the Pacific OceanNature, 1980
- Anomalous crustal structures in ocean basins: Continental fragments and oceanic plateausEarth and Planetary Science Letters, 1980
- An analysis of the variation of ocean floor bathymetry and heat flow with ageJournal of Geophysical Research, 1977
- Surface deformation, gravity anomalies and convectionGeophysical Journal International, 1977