The 650 km mantle discontinuity
- 1 June 1976
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 3 (6), 347-349
- https://doi.org/10.1029/gl003i006p00347
Abstract
No abstract availableThis publication has 21 references indexed in Scilit:
- Post-oxide phases of olivine and pyroxene and mineralogy of the mantleNature, 1975
- Elasticity of Olivine (α), Beta(β), and Spinel (γ) Polymorphs of Germanates and SilicatesGeophysical Journal of the Royal Astronomical Society, 1975
- High-pressure X-ray diffraction studies on β- and γ-Mg2SiO4Physics of the Earth and Planetary Interiors, 1975
- Elasticity, crystal structure and phase transitionsEarth and Planetary Science Letters, 1974
- Elasticity of pyroxene-garnet and pyroxene-ilmenite phase transformations in germanatesPhysics of the Earth and Planetary Interiors, 1974
- Petrologic properties of the upper 670 km of the earth's mantle; geophysical implicationsPhysics of the Earth and Planetary Interiors, 1973
- The mineralogic distribution of iron in the upper mantlePhysics of the Earth and Planetary Interiors, 1972
- Seismic Waves Reflected from Discontinuities within Earth's Upper MantleScience, 1969
- Phase Changes in the Upper MantleScience, 1967
- The pyroxene-garnet transformation in the earth's mantleEarth and Planetary Science Letters, 1967