Destabilization of a 650 km chemical boundary layer and its bearing on the evolution of the continental crust
- 31 July 1983
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 32 (4), 352-360
- https://doi.org/10.1016/0031-9201(83)90035-3
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Solidus and liquidus temperatures and mineralogies for anhydrous garnet-lherzolite to 15 GPaPhysics of the Earth and Planetary Interiors, 1983
- Are anharmonicity corrections needed for temperature-profile calculations of interiors of terrestrial planets?Physics of the Earth and Planetary Interiors, 1982
- Metamorphism of the ca. 3800 Ma supracrustal rocks at Isua, West Greenland: implications for early Archaean crustal evolutionEarth and Planetary Science Letters, 1982
- Thermodynamic parameters in the Earth as determined from seismic profilesGeophysical Journal International, 1981
- Nd Isotopic Studies: Some new perspectives on Earth structure and evolutionEos, 1981
- The mean age of mantle and crustal reservoirsJournal of Geophysical Research, 1979
- The Mesozoic development of aseismic continental marginsJournal of the Geological Society, 1977
- Lateral heterogeneity and mantle dynamicsNature, 1975
- Elastic moduli, pressure derivatives, and temperature derivatives of single-crystal olivine and single-crystal forsteriteJournal of Geophysical Research, 1969
- The distribution of mineral dates in time and spaceAmerican Journal of Science, 1960