The effect of alumina on phase transformations at the 660-kilometer discontinuity from Fe-Mg partitioning experiments
Experimental data on the partitioning of Fe and Mg between coexisting silicate perovskite, magnesiowustite, and γ-(Mg,Fe)2SiO4 demonstrate that Fe substitution in perovskite is strongly coupled to Al2O3 concentration. In Al2O3-free compositions, perovskite has a low Fe/(Fe+Mg) ratio: for a bulk Fe/(...
Main Authors: | Wood, B, Rubie, D |
---|---|
Format: | Journal article |
Language: | English |
Published: |
1996
|
Similar Items
-
The nature of the 660-kilometer discontinuity in Earth's mantle from global seismic observations of PP precursors.
by: Deuss, A, et al.
Published: (2006) -
The Effect of H2O on the 410-Kilometer Seismic Discontinuity.
by: Wood, B
Published: (1995) -
Compositional effects on element partitioning between Mg-silicate perovskite and silicate melts
by: Liebske, C, et al.
Published: (2005) -
Effects of Al on Mg-silicate perovskite composition and trace element partitioning
by: Liebske, C, et al.
Published: (2004) -
Sharpness of the paired 660-km discontinuity beneath the Izu-Bonin area
by: LiMing Wang, et al.
Published: (2020-11-01)