Role of iron-spin transition in ferropericlase on seismic interpretation: A broad thermochemical transition in the mid mantle?
Author:
Affiliation:
1. Geophysical Fluid Dynamics; ETH Zürich; Zurich; Switzerland
2. GFZ German Research Centre for Geosciences; Potsdam; Germany
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1003/2009GL041583/2009GL041583.pdf
Reference33 articles.
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2. Iron partitioning in Earth's mantle: Toward a deep lower mantle discontinuity;Badro;Science,2003
3. Elasticity and constitution of the Earth's interior;Birch;J. Geophys. Res,1952
4. Mantle plumes: Dynamic models and seismic images;Boschi;Geochem. Geophys. Geosyst.,2007
5. Thermodynamic parameters in the Earth as determined from seismic profiles 66;Brown;Geophys. J. R. Astron. Soc.,1981
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2. Compressibility of ferropericlase at high-temperature: Evidence for the iron spin crossover in seismic tomography;Earth and Planetary Science Letters;2023-09
3. Broad Elastic Softening of (Mg,Fe)O Ferropericlase Across the Iron Spin Crossover and a Mixed‐Spin Lower Mantle;Journal of Geophysical Research: Solid Earth;2022-08
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