Chemical stratification in the silicate Earth
- 29 February 1984
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 67 (2), 249-260
- https://doi.org/10.1016/0012-821x(84)90120-1
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Destabilization of a 650 km chemical boundary layer and its bearing on the evolution of the continental crustPhysics of the Earth and Planetary Interiors, 1983
- Mantle reservoirs and ocean island basaltsNature, 1983
- Modes of mantle convection and the removal of heat from the Earth's interiorJournal of Geophysical Research, 1982
- Thermochemical plumes and mantle phase transitionsJournal of Geophysical Research, 1982
- On some consequences and possible causes of layered mantle convectionJournal of Geophysical Research, 1981
- Partial molar volumes of oxide components in silicate liquidsContributions to Mineralogy and Petrology, 1979
- Focal mechanisms and seismic energy release of deep and intermediate earthquakes in the Tonga‐Kermadec Region and their bearing on the depth extent of mantle flowJournal of Geophysical Research, 1979
- Whole-mantle convection and plate tectonicsGeophysical Journal International, 1977
- Stability of a chemically layered mantleJournal of Geophysical Research, 1974
- Densities of liquid silicate systems calculated from partial molar volumes of oxide componentsAmerican Journal of Science, 1970