Constraints on the lateral strength of slabs from three-dimensional dynamic flow models
- 1 February 1996
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 138 (1-4) , 15-28
- https://doi.org/10.1016/0012-821x(95)00221-w
Abstract
No abstract availableThis publication has 29 references indexed in Scilit:
- Interpreting gravity, geoid, and topography for convection with temperature dependent viscosity: Application to surface features on VenusJournal of Geophysical Research, 1995
- Marine geodynamics: Depth‐age revisitedReviews of Geophysics, 1995
- Slab weakening: Mechanical and thermal‐mechanical consequences for slab detachmentIsland Arc, 1995
- Effects of multiple phase transitions in a three‐dimensional spherical model of convection in Earth's mantleJournal of Geophysical Research, 1994
- Iterative solution techniques for the stokes and Navier‐Stokes equationsInternational Journal for Numerical Methods in Fluids, 1994
- Dynamic topography compared with residual depth anomalies in oceans and implications for age‐depth curvesGeophysical Research Letters, 1994
- Geoid effects in a convecting system with lateral viscosity variationsGeophysical Research Letters, 1992
- Detachment of part of the downgoing slab and uplift of the New Hebrides (Vanuatu) IslandsGeophysical Research Letters, 1992
- Long-wavelength variations in Earth’s geoid: physical models and dynamical implicationsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1989
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980