Mineralogic Distribution of Iron in the Upper Half of the Transition Zone in the Earth'S Mantle
- 17 March 2013
- book chapter
- Published by Wiley in Geophysical Monograph Series
- Vol. 19, 399-405
- https://doi.org/10.1029/gm019p0399
Abstract
No abstract availableKeywords
This publication has 102 references indexed in Scilit:
- A review of experimental evidence on the origin of basaltic and nephelinitic magmasPublished by Elsevier ,2002
- Petrologic properties of the upper 670 km of the earth's mantle; geophysical implicationsPhysics of the Earth and Planetary Interiors, 1973
- Source process of a large deep-focus earthquake and its tectonic implications — the Western Brazil earthquake of 1963Physics of the Earth and Planetary Interiors, 1972
- Olivine-Spinel transformation in a natural forsteritePhysics of the Earth and Planetary Interiors, 1971
- High-pressure decomposition of the system FeSiO3MgSiO3Physics of the Earth and Planetary Interiors, 1970
- Phase transformations and the constitution of the mantlePhysics of the Earth and Planetary Interiors, 1970
- Earth models consistent with geophysical dataPhysics of the Earth and Planetary Interiors, 1970
- Partial melting and the low-velocity zonePhysics of the Earth and Planetary Interiors, 1970
- Split sphere high pressure vessel and phase equilibrium relation in the system Mg2SiO4Fe2SiO4Physics of the Earth and Planetary Interiors, 1970
- A fluid theory for the deep structure of dip-slip fault zonesPhysics of the Earth and Planetary Interiors, 1968