Glacial isostasy and the interplay between upper and lower mantle lateral viscosity heterogeneities
- 1 May 1989
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 16 (5) , 429-432
- https://doi.org/10.1029/gl016i005p00429
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Deep Slabs, Geochemical Heterogeneity, and the Large-Scale Structure of Mantle Convection: Investigation of an Enduring ParadoxAnnual Review of Earth and Planetary Sciences, 1988
- Tomographic Inversion for Shear Velocity Beneath the North American PlateJournal of Geophysical Research, 1987
- Glacial rebound and relative sea-level variations: a new appraisalGeophysical Journal International, 1987
- The effects of transient rheology on the interpretation of lower mantle viscosityGeophysical Research Letters, 1985
- Steady state, secondary convection beneath lithospheric plates with temperature‐ and pressure‐dependent viscosityJournal of Geophysical Research, 1984
- Mapping the upper mantle: Three‐dimensional modeling of earth structure by inversion of seismic waveformsJournal of Geophysical Research, 1984
- Convection with pressure- and temperature-dependent non-Newtonian rheologyGeophysical Journal International, 1984
- Anelastic response of the Earth to a dip slip earthquakeJournal of Geophysical Research, 1983
- Studies of finite amplitude non-Newtonian thermal convection with application to convection in the Earth's mantleJournal of Geophysical Research, 1976