Is subducted lithosphere trapped at the 670-km discontinuity?
- 1 December 1988
- journal article
- Published by Springer Nature in Nature
- Vol. 336 (6198) , 462-463
- https://doi.org/10.1038/336462a0
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Time-dependent thermal convection - a possible explanation for a multiscale flow in the Earth's mantleGeophysical Journal International, 1988
- Nature of the 650–km seismic discontinuity: implications for mantle dynamics and differentiationNature, 1988
- Phase transformations in a harzburgite composition to 26 GPa: implications for dynamical behaviour of the subducting slabEarth and Planetary Science Letters, 1987
- Time-dependent convection in elongated Rayleigh-Benard cellsGeophysical Research Letters, 1987
- The effects of chemical density differences on convective mixing in the Earth's mantleJournal of Geophysical Research, 1986
- Layered convection induced by phase transitionsJournal of Geophysical Research, 1985
- Stability Relations of Silicate Spinels, Ilmenites, and PerovskitesPublished by Springer Nature ,1982