EFFECTS OF THE ELECTRONIC SPIN TRANSITIONS OF IRON IN LOWER MANTLE MINERALS: IMPLICATIONS FOR DEEP MANTLE GEOPHYSICS AND GEOCHEMISTRY
Author:
Affiliation:
1. Department of Geological Sciences, Jackson School of Geosciences; University of Texas at Austin; Austin Texas USA
2. Helmholtz Center Potsdam; German Research Center for Geosciences GFZ; Potsdam Germany
Funder
US National Science Foundation
NSF Instrumentation and Facility
Publisher
American Geophysical Union (AGU)
Subject
Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/rog.20010/fullpdf
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3. Evaluation of (Mg,Fe) partitioning between silicate perovskite and magnesiowüstite up to 120 GPa and 2300 K;Andrault;J. Geophys. Res.,2001
4. Experimental evidence for perovskite and post-perovskite coexistence throughout the whole D″ region;Andrault;Earth Planet. Sci. Lett.,2010
5. Solid-liquid iron partitioning in Earth's deep mantle;Andrault;Nature,2012
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