Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition
Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition
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Berlin/Heidelberg: Springer-Verlag
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Language
English
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Berlin/Heidelberg: Springer-Verlag
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Recent high-pressure studies have shown that an electronic spin transition of iron in ferropericlase, an expected major phase of Earth’s lower mantle, results in changes in its properties, including density, incompressibility, radiative thermal conductivity, electrical conductivity, and sound velocities. To understand the rheology of ferropericlase...
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Full title
Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition
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TN_cdi_proquest_journals_2262079792
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2262079792
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ISSN
0342-1791
E-ISSN
1432-2021
DOI
10.1007/s00269-009-0303-5