Spin Crossover in Ferropericlase at High Pressure: A Seismologically Transparent Transition?-Reference-Cited by-同舟云学术

Spin Crossover in Ferropericlase at High Pressure: A Seismologically Transparent Transition?

Published:2011-01-07 Issue:6013 Volume:331 Page:64-67
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Antonangeli Daniele¹²,Siebert Julien¹²,Aracne Chantel M.²,Farber Daniel L.²³,Bosak A.⁴,Hoesch M.⁴,Krisch M.⁴,Ryerson Frederick J.²,Fiquet Guillaume¹,Badro James¹²

Affiliation:

1. Institut de Minéralogie et de Physique des Milieux Condensés, UMR CNRS 7590, Institut de Physique du Globe de Paris, Université Pierre et Marie Curie, Université Paris Diderot, 75005 Paris, France.

2. Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.

3. Department of Earth and Planetary Sciences, University of California, Santa Cruz, Santa Cruz, CA, 95064, USA.

4. European Synchrotron Radiation Facility, BP 220, 38043 Grenoble Cedex, France.

Abstract

An iron spin transition has no effect on the seismologic properties of lower-mantle minerals.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference32 articles.

1. J.-P. Poirier Introduction to the Physics of the Earth's Interior (Cambridge Univ. Press Cambridge 2000).

2. Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity

3. Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle

4. Spin transition of iron in magnesiowüstite in the Earth's lower mantle

5. Sound velocities of ferropericlase in the Earth's lower mantle

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