The influence of rheological weakening and yield stress on the interaction of slabs with the 670 km discontinuity
- 11 April 2002
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 199 (3-4) , 447-457
- https://doi.org/10.1016/s0012-821x(02)00586-1
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Latent heat effects of the major mantle phase transitions on low-angle subductionEarth and Planetary Science Letters, 2001
- Thermal-mechanical effects of low-temperature plasticity (the Peierls mechanism) on the deformation of a viscoelastic shear zoneEarth and Planetary Science Letters, 1999
- Closing the gap between regional and global travel time tomographyJournal of Geophysical Research, 1998
- Formation of a metastable olivine wedge in a descending slabJournal of Geophysical Research, 1997
- Trench migration and subduction zone geometryGeophysical Research Letters, 1997
- Rheological control of oceanic crust separation in the transition zoneGeophysical Research Letters, 1996
- Sensitivity of convection with an endothermic phase change to the form of governing equations, initial conditions, boundary conditions, and equation of stateJournal of Geophysical Research, 1994
- Controls on trench topography from dynamic models of subducted slabsJournal of Geophysical Research, 1994
- Mantle shear structure beneath the Americas and surrounding oceansJournal of Geophysical Research, 1994
- The upper mantle transition region: Eclogite?Geophysical Research Letters, 1979